Kan een afbeelding zijn van hond

Dit is ons nieuw hondje Kira, een kruising van een waterhond en een Podenko. Ze is sinds 7 februari 2024 bij ons en druk bezig ons hart te veroveren. Het is een lief, aanhankelijk hondje, dat zich op een week snel aan ons heeft aangepast. Ze is heel vinnig en nieuwsgierig, een heel ander hondje dan Noleke.

This is our new dog Kira, a cross between a water dog and a Podenko. She has been with us since February 7, 2024 and is busy winning our hearts. She is a sweet, affectionate dog who quickly adapted to us within a week. She is very quick and curious, a very different dog than Noleke.

Carl Sagan Space GIF by Feliks Tomasz Konczakowski

X Files Ufo GIF by SeeRoswell.com

1990: Petit-Rechain, Belgium triangle UFO photograph - Think AboutIts

Ufo Pentagon GIF

ufo abduction GIF by Ski Mask The Slump God

Flying Sci-Fi GIF by Feliks Tomasz Konczakowski

Season 3 Ufo GIF by Paramount+

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Inhoud blog
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    The purpose of  this blog is the creation of an open, international, independent and  free forum, where every UFO-researcher can publish the results of his/her research. The languagues, used for this blog, are Dutch, English and French.You can find the articles of a collegue by selecting his category.
    Each author stays resposable for the continue of his articles. As blogmaster I have the right to refuse an addition or an article, when it attacks other collegues or UFO-groupes.
     

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    Deze blog is opgedragen aan mijn overleden echtgenote Lucienne.

    In 2012 verloor ze haar moedige strijd tegen kanker!

    In 2011 startte ik deze blog, omdat ik niet mocht stoppen met mijn UFO-onderzoek.

    BEDANKT!!!

    Een interessant adres?
    UFO'S of UAP'S, ASTRONOMIE, RUIMTEVAART, ARCHEOLOGIE, OUDHEIDKUNDE, SF-SNUFJES EN ANDERE ESOTERISCHE WETENSCHAPPEN - DE ALLERLAATSTE NIEUWTJES
    UFO's of UAP'S in België en de rest van de wereld
    In België had je vooral BUFON of het Belgisch UFO-Netwerk, dat zich met UFO's bezighoudt. BEZOEK DUS ZEKER VOOR ALLE OBJECTIEVE INFORMATIE , enkel nog beschikbaar via Facebook en deze blog. Verder heb je ook het Belgisch-Ufo-meldpunt en Caelestia, die prachtig, doch ZEER kritisch werk leveren, ja soms zelfs héél sceptisch... Voor Nederland kan je de mooie site www.ufowijzer.nl bezoeken van Paul Harmans. Een mooie site met veel informatie en artikels. MUFON of het Mutual UFO Network Inc is een Amerikaanse UFO-vereniging met afdelingen in alle USA-staten en diverse landen. MUFON's mission is the analytical and scientific investigation of the UFO- Phenomenon for the benefit of humanity... Je kan ook hun site bekijken onder www.mufon.com. Ze geven een maandelijks tijdschrift uit, namelijk The MUFON UFO-Journal. Since 02/01/2020 is Pieter ex-president (=voorzitter) of BUFON, but also ex-National Director MUFON / Flanders and the Netherlands. We work together with the French MUFON Reseau MUFON/EUROP. ER IS EEN NIEUWE GROEPERING DIE ZICH BUFON NOEMT, MAAR DIE HEBBEN NIETS MET ONZE GROEP TE MAKEN. DEZE COLLEGA'S GEBRUIKEN DE NAAM BUFON VOOR HUN SITE... Ik wens hen veel succes met de verdere uitbouw van hun groep. Zij kunnen de naam BUFON wel geregistreerd hebben, maar het rijke verleden van BUFON kunnen ze niet wegnemen...
    06-05-2024
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.China Just Launched its Chang'e-6 Mission To Grab Samples From the Elusive Far Side of the Moon

    China Just Launched its Chang'e-6 Mission To Grab Samples From the Elusive Far Side of the Moon

    Liftoff for the Moon’s newest robotic visitor.

    TOPSHOT - A Long March 5 rocket, carrying the Chang'e-6 mission lunar probe, lifts off as it rains a...
    Hector Retamal / AFP / Getty Images

    China has launched the Chang’e-6 rover to the Moon.

    Chang’e-6 is the latest of the Chang’e fleet, named after the Chinese goddess of the Moon. On Friday, the rover launched atop a Chinese Long March-5 rocket from Wenchang Space Launch Site in south China's Hainan Province. Chang’e-6 has successfully deployed into space, and it’s now heading for the enigmatic far side of the Moon.

    Its predecessor, Chang’e-5, collected about 2 kilograms of lunar material from the near side of the Moon in late 2020. This was the first time since the 1970s that humanity had brought samples from the Moon to Earth. In early 2019, Chang’e-4 was the first mission ever to land on the far side of the Moon. Chang’e-6 builds upon all that work.

    WHY GO TO THE FAR SIDE OF THE MOON?

    The battered, cratered surface of the Moon. This is the far side, which humans cannot see from Earth...

    This monochrome mosaic is centered in the middle of the South Pole-Aitken basin. It comes from NASA’s Lunar Reconnaissance Orbiter. 

    NASA/GSFC/ARIZONA STATE UNIVERSITY

    Chang’e-6 will be a blend of both those earlier missions: It will retrieve samples from the far side of the Moon. Chang’e-6 will land in the largest and oldest known impact basin on the Moon. Known as the South Pole-Aitken (SPA) basin, it “stretches across nearly a quarter of the Moon,” according to the team that operates NASA’s Lunar Reconnaissance Orbiter.

    It’s a fascinating place. The terrain is quite dramatic. The craters are also thought to have formed 3.9 billion years ago when life was just beginning to form on Earth. If the craters owe their existence to a chaotic episode of rocky bombardment, that same rocky rainfall likely struck Earth and the other terrestrial planets.

    According to Chinese state media Xinhua, Chang’e-6 will deploy its robotic arm about 48 hours after landing. It will scoop up rocks and lunar dirt, called regolith. It will also excavate samples with a drill. The 53-day mission will culminate in samples, sealed away and ferried into an orbiter, flying to Earth. They’re expected to land in Inner Mongolia at the end of June.

    Chang’e-6 is also carrying scientific instruments from other countries. “The Chang'e-6 mission is carrying four payloads developed through international cooperation. Scientific instruments from France, Italy, and the European Space Agency/Sweden are aboard the Chang'e-6 lander, and a small satellite from Pakistan is aboard the orbiter,” according to Xinhua.

    In a year packed with lunar visits from other robots, like Odysseus of Houston-based Intuitive Machines, and Japan’s SLIM lander, Chang’e-6 is set to keep the momentum of 2024 Moon exploration building.

    https://www.inverse.com/ }

    06-05-2024 om 00:37 geschreven door peter  

    0 1 2 3 4 5 - Gemiddelde waardering: 0/5 - (0 Stemmen)
    Categorie:ASTRONOMIE / RUIMTEVAART
    05-05-2024
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.'Tic Tac' UFO exposed by US whistle blowers 'hovered above USO emerging from ocean'

    'Tic Tac' UFO exposed by US whistleblowers 'hovered above USO emerging from ocean'

    Researcher Mark Christopher Lee claims the 'Tic Tac' UFO exposed by US whistle blowers 'hovered above a USO emerging from the ocean'

    The infamous 'Tic-Tac' UFO exposed by US whistle blowers was "hovering above an unidentified submerged object (USO) emerging from the ocean".

    This is the claim by UFO researcher and filmmaker Mark Christopher Lee who said the US Military and Navy have been inundated with UFO and USO confrontations since the 1950s, with the navy dubbing USOs their "biggest threat" yet.

    The infamous interaction with the Tic-Tac UFO captured by crew members from the USS Nimitz in 2004 marked a significant turning point in human history – with two former Navy pilots having come forward to share their discomforting encounters with the alien craft.

    READ MORE: 

    But now expert Lee has thrown more questions into the mix as he boldly claimed the Tic-Tac UFO was seen hovering above a USO, something not previously addressed.

    Researcher Mark Christopher Lee claims the 'Tic Tac' UFO exposed by US whistle blowers 'hovered above a USO emerging from the ocean'

    The infamous interaction with the Tic-Tac UFO captured by crew members from the USS Nimitz in 2004 

    "USOs have been seen coming from the oceans for hundreds of years," Lee told the Daily Star. "Even Christopher Columbus saw a USO on his voyage to the new world and the US Navy has had plenty of confrontations with USOs since the 50s and have identified them as the biggest threat.

    "Note that the Tic-Tac UFO reported by the recent US whistle blowers was seen hovering above a USO emerging from the ocean. [This makes me think UFOs and USOs] are linked and the tic tac and other UFOs are all able to enter the oceans at will.

    https://www.dailystar.co.uk/news/ }

    05-05-2024 om 21:19 geschreven door peter  

    0 1 2 3 4 5 - Gemiddelde waardering: 0/5 - (0 Stemmen)
    Categorie:ASTRONOMIE / RUIMTEVAART
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Manganese-Rich Sandstones Point to Earth-Like Environment on Ancient Mars

    Manganese-Rich Sandstones Point to Earth-Like Environment on Ancient Mars

    In May 2017, NASA’s Curiosity rover observed higher than usual amounts of manganese in the lakebed rocks within Gale crater, Mars. These sedimentary rocks have larger grain sizes than what is typical for the lakebed rocks in the crater. This may indicate that the original sediments were formed in a river, delta, or near the shoreline in the ancient lake. In a new paper, Dr. Patrick Gasda from Los Alamos National Laboratory and his colleagues discuss how manganese could have been enriched in these rocks — for example, by percolation of groundwater through the original sediments or through the rock afterward — and what oxidant could be responsible for the precipitation of manganese in the rocks. On Earth, manganese becomes enriched because of oxygen in the atmosphere and this process is often sped up by the presence of microbes. Microbes on Earth can use the many oxidation states of manganese as energy for metabolism; if life was present on ancient Mars, the increased amounts of manganese in these rocks along the lake shore would be a helpful energy source for life.

    Mastcam mosaic from the Sol 1686 rover location looking behind the rover (downslope) at the transition point between the Sutton Island and Blunts Point Murray members. Images from Sols 1685-1689 display sedimentary textures of dark-toned manganese-rich sandstones and nearby rocks. Dashed line boxes in the large mosaic are shown as insets along the bottom of figure. Small red outlines show the approximate locations and extent of ChemCam observations. Throughout this transition area, dark-toned sandstones (presumably manganese-rich based on ChemCam observations at three locations) overlie light-toned materials. Insets from left to right: (a) Denning Brook, a manganese-rich fine-grained dark-toned sandstone ChemCam observation; (b) and (c) two light-toned blocks with cross-stratified textures, highlighted with yellow lines, 6 m away from Denning Brook and to the upper left in the large mosaic; (d) dark-toned materials (center of mosaic); and (E1) Newport Ledge, (E2) AEGIS post 1685a, (E3) Sugarloaf Mountain, three thin planar laminated dark-toned sandstones. Image credit: NASA / Caltech-JPL / MSSS.

    Mastcam mosaic from the Sol 1686 rover location looking behind the rover (downslope) at the transition point between the Sutton Island and Blunts Point Murray members. Images from Sols 1685-1689 display sedimentary textures of dark-toned manganese-rich sandstones and nearby rocks. Dashed line boxes in the large mosaic are shown as insets along the bottom of figure. Small red outlines show the approximate locations and extent of ChemCam observations. Throughout this transition area, dark-toned sandstones (presumably manganese-rich based on ChemCam observations at three locations) overlie light-toned materials. Insets from left to right: (a) Denning Brook, a manganese-rich fine-grained dark-toned sandstone ChemCam observation; (b) and (c) two light-toned blocks with cross-stratified textures, highlighted with yellow lines, 6 m away from Denning Brook and to the upper left in the large mosaic; (d) dark-toned materials (center of mosaic); and (E1) Newport Ledge, (E2) AEGIS post 1685a, (E3) Sugarloaf Mountain, three thin planar laminated dark-toned sandstones.

    Image credit: NASA / Caltech-JPL / MSSS.

    “It is difficult for manganese oxide to form on the surface of Mars, so we didn’t expect to find it in such high concentrations in a shoreline deposit,” Dr. Gasda said.

    “On Earth, these types of deposits happen all the time because of the high oxygen in our atmosphere produced by photosynthetic life, and from microbes that help catalyze those manganese oxidation reactions.”

    “On Mars, we don’t have evidence for life, and the mechanism to produce oxygen in Mars’ ancient atmosphere is unclear, so how the manganese oxide was formed and concentrated here is really puzzling.”

    “These findings point to larger processes occurring in the Martian atmosphere or surface water and shows that more work needs to be done to understand oxidation on Mars.”

    To measure manganese abundances in lakebed rocks within Gale crater, Dr. Gasda and co-authors used the ChemCam instrument onboard NASA’s Curiosity rover.

    “ChemCam is an atomic emission spectroscopy instrument that uses laser-induced breakdown spectroscopy (LIBS) to quantify elemental abundances present in a target,” they explained.

    “The ChemCam LIBS uses a pulsed laser emitting a 1,067 nm beam that is focused onto a target up to 7 m from the rover, which produces an analytical footprint of 350-550 μm.”

    2024-05-01

    NASA’s Curiosity rover continues to search for signs that Mars’ Gale Crater conditions could support microbial life. 

    Photo credit: NASA/JPL-Caltech/MSSS.

    “Each laser pulse ablates and ionizes a small (nanograms to micrograms) amount of material.”

    “Light emitted from the plasma formed by each laser pulse is collected by the ChemCam telescope, and spectra are recorded by the ultraviolet, violet, and visible to near infrared spectrometers.”

    The sedimentary rocks explored by the Curiosity rover are a mix of sands, silts, and muds.

    The sandy rocks are more porous, and groundwater can more easily pass through sands compared to the muds that make up most of the lakebed rocks in Gale crater.

    The researchers looked at how manganese could have been enriched in these sands — for example, by percolation of groundwater through the sands on the shore of a lake or mouth of a delta — and what oxidant could be responsible for the precipitation of manganese in the rocks.

    On Earth, manganese becomes enriched because of oxygen in the atmosphere, and this process is often sped up by the presence of microbes.

    This scene shows NASA's Curiosity Mars rover at a location called "Windjana," where the rover found rocks containing manganese-oxide minerals, which require abundant water and strongly oxidizing conditions to form.› Full image and caption
     Credit: NASA/JPL-Caltech/MSSS

    Microbes on Earth can use the many oxidation states of manganese as energy for metabolism; if life was present on ancient Mars, the increased amounts of manganese in these rocks along the lake shore would have been a helpful energy source for life.

    “The Gale lake environment, as revealed by these ancient rocks, gives us a window into a habitable environment that looks surprisingly similar to places on Earth today,” said ChemCam principal investigator Dr. Nina Lanza, a researcher at Los Alamos National Laboratory.

    “Manganese minerals are common in the shallow, oxic waters found on lake shores on Earth, and it’s remarkable to find such recognizable features on ancient Mars.”

    • The team’s paper was published in the Journal of Geophysical Research: Planets.
      • P.J. Gasda et al. 2024. Manganese-Rich Sandstones as an Indicator of Ancient Oxic Lake Water Conditions in Gale Crater, Mars. JGR: Planets 129 (5): e2023JE007923; doi: 10.1029/2023JE007923

    https://www.sci.news/ }

    05-05-2024 om 20:54 geschreven door peter  

    0 1 2 3 4 5 - Gemiddelde waardering: 0/5 - (0 Stemmen)
    Categorie:ASTRONOMIE / RUIMTEVAART
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Webb Probably Didn’t Detect Biosignature Gas on K2-18b

    Webb Probably Didn’t Detect Biosignature Gas on K2-18b

    James Webb Space Telescope

    This illustration depicts NASA’s James Webb Space Telescope – the largest, most powerful, and most complex space science telescope ever built – fully unfolded in space.

    (Credits: NASA/Adriana Manrique Gutierrez)

    In 2023, astronomers reported a tentative detection of dimethyl sulfide — which is predominately produced by marine microbes on Earth and regarded as a biosignature gas — in the atmosphere of the super-Earth exoplanet K2-18b. In a paper published in the Astrophysical Journal Letters, University of California, Riverside astronomer Shang-Min Tsai and colleagues challenge this finding, but also outline how the NASA/ESA/CSA James Webb Space Telescope might verify the presence of dimethyl sulfide.

    Rendering of the likely view on a Hycean world. Image credit: Shang-Min Tsai / UCR.

    Rendering of the likely view on a Hycean world.

    Image credit: Shang-Min Tsai / UCR.

    K2-18 is a red dwarf located approximately 111 light-years away in the constellation of Leo.

    Also known as EPIC 201912552, the star hosts two massive exoplanets: K2-18b and K2-18c.

    First discovered in 2015, K2-18b has a radius of 2.2 times that of Earth and is about 8 times as massive.

    The planet orbits its star every 33 days at a distance of approximately 0.15 AU and has an Earth Similarity Index of 0.73.

    It receives 1.28 times the light intensity of Earth, and its equilibrium temperature is 28 degrees Fahrenheit (minus 2 degrees Celsius).

    K2-18c, discovered in 2017, has a mass about 7.5 times that of Earth, orbits the host star one every 9 days, and is probably too hot to be in the habitable zone.

    In 2023, astronomers reported a tentative detection of dimethyl sulfide (DMS) in the atmosphere of K2-18b.

    “K2-18b gets almost the same amount of solar radiation as Earth,” Dr. Tsai said.

    “And if atmosphere is removed as a factor, K2-18b has a temperature close to Earth’s, which is also an ideal situation in which to find life.”

    “K2-18b’s atmosphere is mainly hydrogen, unlike our nitrogen-based atmosphere.”

    “But there was speculation that K2-18b has water oceans, like Earth. That makes K2-18b a potentially Hycean world, which means a combination of a hydrogen atmosphere and water oceans.”

    “What was icing on the cake, in terms of the search for life, is that last year researchers reported a tentative detection of DMS in the atmosphere of that planet, which is produced by ocean phytoplankton on Earth.”

    “DMS is the main source of airborne sulfur on our planet and may play a role in cloud formation.”

    Because the telescope data were inconclusive, Dr. Tsai and co-authors wanted to understand whether enough DMS could accumulate to detectable levels on K2-18b.

    “The DMS signal from Webb was not very strong and only showed up in certain ways when analyzing the data,” Dr. Tsai said.

    “We wanted to know if we could be sure of what seemed like a hint about DMS.”

    This artist’s impression shows planets K2-18b and c and their host star. Image credit: NASA / ESA / Hubble / M. Kornmesser.

    This art’s tisimpression shows planets K2-18b and c and their host star.

    Image credit: NASA / ESA / Hubble / M. Kornmesser.

    Based on computer models that account for the physics and chemistry of DMS, as well as the hydrogen-based atmosphere, the researchers found that it is unlikely the data show the presence of DMS.

    “The signal strongly overlaps with methane, and we think that picking out DMS from methane is beyond this instrument’s capability,” Dr. Tsai said.

    However, the scientists believe it is possible for DMS to accumulate to detectable levels.

    For that to happen, plankton or some other life form would have to produce 20 times more DMS than is present on Earth.

    Detecting life on exoplanets is a daunting task, given their distance from Earth.

    To find DMS, Webb would need to use an instrument better able to detect infrared wavelengths in the atmosphere than the one used last year.

    Fortunately, the telescope will use such an instrument later this year, revealing definitively whether DMS exists on K2-18b.

    “The best biosignatures on an exoplanet may differ significantly from those we find most abundant on Earth today,” said Dr. Eddie Schwieterman, an astrobiologist at the University of California, Riverside.

    “On a planet with a hydrogen-rich atmosphere, we may be more likely to find DMS made by life instead of oxygen made by plants and bacteria as on Earth.”

    • Shang-Min Tsai et al. 2024. Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds. ApJL 966, L24; doi: 10.3847/2041-8213/ad3801

    LINKS VIDEOS

    https://www.sci.news/ }

    05-05-2024 om 20:38 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Vera Rubin’s Primary Mirror Gets its First Reflective Coating
    A drone's view of the Rubin Observatory under construction in 2023. The 8.4-meter is getting closer to completion and first light in 2025. The primary/tertiary mirror has its first reflective coating.
    Image Credit: Rubin Observatory/NSF/AURA/A. Pizarro D

    Vera Rubin’s Primary Mirror Gets its First Reflective Coating

    First light for the Vera Rubin Observatory (VRO) is quickly approaching and the telescope is reaching milestone after milestone. A few weeks ago, the observatory announced that its digital camera, the largest one ever made, is complete.

    Now the observatory has announced that its unique primary/tertiary mirror has its first reflective coating.

    The Rubin’s massive digital camera has an important job and garners a lot of attention. But it’s powerless without the telescope’s innovative primary/tertiary mirror. Primary mirrors are always the most critical and time-consuming part of modern observatories. The VRO’s primary/tertiary mirror took seven years to make.

    The mirror is called a primary/tertiary mirror because it comprises two optical surfaces with different curvatures. The primary mirror is 8.4 meters, while the tertiary mirror is 5 meters in diameter. The pair of surfaces are combined into one large structure. The unique design reduces the telescope’s engineering complexity without reducing its impressive light-gathering capability. It can be rotated quickly and also settles quickly.

    The VRO's unique primary/tertiary mirror is two mirrors in one. It's mounted on lightweight honeycomb material for strength. Image Credit: VRO
    The VRO’s unique primary/tertiary mirror is two mirrors in one. It’s mounted on lightweight honeycomb material for strength.
    Image Credit: VRO

    The outer surface forms the primary mirror. It captures light from space first, then that light reflects upwards to the 3.4-meter secondary mirror. After that, it’s reflected back down to the inner 5.0-meter surface that forms the tertiary mirror. Then, the light is sent to the camera.

    The primary mirror’s size is critical because it determines how much light the telescope can collect. More light means astronomers can study very faint or distant objects. The VRO’s design allows the camera to capture a large area of sky the size of 7 full moons across in a single image.

    via GIPHY

    Only meticulous engineering and construction can build a telescope like this. One of the stages is putting the reflective and protective coatings on the mirrors. The VRO announced that the primary/tertiary mirror has its first coating.

    This was a very well-conducted project from every angle, thanks to a combination of careful planning and the technical skills of our excellent team.

    Tomislav Vucina, Senior Coating Engineer, VRO

    The VRO has a special onsite coating chamber built just for this purpose. It’s a 128-ton chamber on the observatory’s maintenance floor. It uses a process called magnetron sputtering to apply coatings. The chamber will be reused during the telescope’s lifetime whenever the mirror needs re-coating.

    The chamber can apply coatings of different reflective materials alone or in combinations. It took a lot of work to determine the perfect coating for reflectivity and durability. Researchers tested different coatings on a steel stand-in mirror.

    The first layer was an adhesive layer of nickel-chromium. Next came an incredibly thin layer of silver weighing only 64 grams spread over the 8.4-meter mirror. On top of that, another nickel-chromium adhesive layer, then a protective layer of silicon nitride to shield the reflective layer.

    The person in charge of these precision coatings is Tomislav Vucina, the Senior Coating Engineer. Vucina describes the coatings as a balancing act. “This outer layer needs to be thick enough that it’s not worn off by cleaning,” said Vucina, “but not so thick that it absorbs too many photons and prevents the mirror from meeting Rubin’s scientific requirements.”

    This image shows the Rubin Observatory's 8.4-meter combined primary/tertiary mirror after being coated with protected silver in April 2024. The reflective coating was applied using the observatory's onsite coating chamber, which will also be used to re-coat the mirror as necessary during Rubin's 10-year Legacy Survey of Space and Time. Image Credit: RubinObs/NOIRLab/NSF/AURA
    This image shows the Rubin Observatory’s 8.4-meter combined primary/tertiary mirror after being coated with protected silver in April 2024. The reflective coating was applied using the observatory’s onsite coating chamber, which will also be used to re-coat the mirror as necessary during Rubin’s 10-year Legacy Survey of Space and Time.
    Image Credit: RubinObs/NOIRLab/NSF/AURA

    Until these coatings were applied, the glass was just glass. Highly specialized glass, but glass nonetheless. Now that the glass has received its reflective silver coating, it’s truly a mirror.

    The application process took only 4.5 hours, nothing compared to the 7 years required to build the primary/tertiary mirror. Vucina and his team subjected the mirror to a battery of tests: reflectivity, adhesion, pinhole, and cosmetic. According to Vucina, the application process was successful.

    “This was a very well-conducted project from every angle,” said Vucina, “thanks to a combination of careful planning and the technical skills of our excellent team.”

    It’s been a long road to completion for the VRO. But after a long wait, first light is rapidly approaching. Excitement and anticipation for the observatory’s unique and powerful scientific contribution is growing. Its main output is the decade-long Legacy Survey of Space and Time.

    “We’re extremely excited that both mirrors are now coated and will be installed on the telescope very soon,” said Sandrine Thomas, Deputy Director for Rubin Construction. “The combined reflectivity of these mirrors will enable Rubin to detect very faint and far-away objects, leading to great science!”

    https://www.universetoday.com/ }

    05-05-2024 om 18:29 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Did You Hear Webb Found Life on an Exoplanet? Not so Fast…
    Artist rendering of the view on a Hycean world. The recent detection of a biosignature on the Hycean world K2-18b attracted a lot of attention.
    Image Credit: Shang-Min Tsai/UCR

    Did You Hear Webb Found Life on an Exoplanet? Not so Fast…

    The JWST is astronomers’ best tool for probing exoplanet atmospheres. Its capable instruments can dissect the light passing through a distant world’s atmosphere and determine its chemical components. Scientists are interested in everything the JWST finds, but when it finds something indicating the possibility of life it seizes everyone’s attention.

    That’s what happened in September 2023, when the JWST found dimethyl sulphide (DMS) in the atmosphere of the exoplanet K2-18b.

    K2-18b orbits a red dwarf star about 124 light-years away. It’s a sub-Neptune with about 2.5 times Earth’s radius and 8.6 Earth masses. The exoplanet may be a Hycean world, a temperate ocean-covered world with a large hydrogen atmosphere.

    In October 2023, researchers announced the tentative detection of dimethyl sulphide in K2-18b’s atmosphere. They found it in JWST observations of the planet’s atmospheric spectrum. “The spectrum also suggests potential signs of dimethyl sulphide (DMS), which has been predicted to be an observable biomarker in Hycean worlds, motivating considerations of possible biological activity on the planet,” the researchers wrote.

    The DMS caught people’s attention because it’s produced by living organisms here on Earth, mostly by marine microbes. So, finding it on an ocean world is cause for a deeper look. A team of researchers from the USA, Germany, and the UK examined the detection to see how it fits with atmospheric models.

    The best biosignatures on an exoplanet may differ significantly from those we find most abundant on Earth today.”

    Eddie Schwieterman, astrobiologist, University of California, Riverside

    They published their results in a paper in the Astrophysical Journal Letters. It’s titled “Biogenic Sulfur Gases as Biosignatures on Temperate Sub-Neptune Waterworlds.” The lead author is Shang-Min Tsai, a University of California Riverside project scientist.

    Most of the thousands of exoplanets we’ve discovered are nothing like Earth. Habitability is impossible according to every known metric. But some are more intriguing. Some, like K2-18b, are more difficult to understand regarding habitability.

    There’s some disagreement over what type of planet K2-18b is. It was the first exoplanet scientists ever detected water vapour on. It may be the first example of a Hycean world if they exist.

    Artist depiction of the mini-Neptune K2-18 b. Credit: NASA, CSA, ESA, J. Olmstead (STScI), N. Madhusudhan
    (Cambridge University)

    There are some clear differences between K2-18b and Earth. Our atmosphere is dominated by nitrogen, which makes up about 78%. K2-18b’s atmosphere is dominated by hydrogen. But it’s enough like Earth in some ways that scientists are keen to understand it better.

    “This planet gets almost the same amount of solar radiation as Earth. And if atmosphere is removed as a factor, K2-18b has a temperature close to Earth’s, which is also an ideal situation in which to find life,” said lead author Shang-Min Tsai.

    The researchers who found DMS in K2-18b’s atmosphere also found carbon dioxide and methane. Finding CO2 and CH4 is noteworthy, but finding DMS with them is even more intriguing.

    “What was icing on the cake, in terms of the search for life, is that last year these researchers reported a tentative detection of dimethyl sulfide, or DMS, in the atmosphere of that planet, which is produced by ocean phytoplankton on Earth,” Tsai said. DMS is oxidized in Earth’s oceans and is the planet’s main source of atmospheric sulphur.

    K2-18b's atmospheric composition as measured by the JWST's near-infrared instruments. The detection of Dimethyl Sulphide is not holding up under increased scrutiny. Image Credit: NASA/CSA/ESA/STScI
    K2-18b’s atmospheric composition as measured by the JWST’s near-infrared instruments. The detection of Dimethyl Sulphide is not holding up under increased scrutiny.
    Image Credit: NASA/CSA/ESA/STScI

    However, the 2023 findings were not conclusive. There were hints of DMS but nothing strong enough to convince scientists and overcome their professional skepticism. “The potential inference of DMS is of high importance, as it is known to be a robust biomarker on Earth and has been extensively advocated to be a promising biomarker for exoplanets,” the authors of the 2023 paper explained.

    “The DMS signal from the Webb telescope was not very strong and only showed up in certain ways when analyzing the data,” Tsai said. “We wanted to know if we could be sure of what seemed like a hint about DMS.”

    The JWST has no alarm bell and flashing indicator that lights up and says, ‘Biomarker Detected!’ It produces data that must be processed to tease out its secrets. Scientists also rely on battle-tested climate and atmospheric chemistry models to understand what the JWST sees.

    “In this study, we explore biogenic sulphur across a wide range of biological fluxes and stellar UV environments,” the researchers write. They performed experiments with a 2D photochemical model and a 3D general circulation model (GCM.) According to Tsai and his co-researchers, the data is unlikely to show the presence of DMS in K2-18b’s atmosphere.

    “The signal strongly overlaps with methane, and we think that picking out DMS from methane is beyond this instrument’s capability,” Tsai said.

    That doesn’t mean that DMS is ruled out. It’s possible that the chemical could build up to detectable levels if plankton or some other life form were producing it. But, they’d have to produce about 20 times more DMS than there is on Earth.

    Professor Madhusudhan from Cambridge University is the lead author of the 2023 paper on K2-18b’s atmosphere. He’s being touted in the media as the man who discovered alien life on another planet. He’s clearly uncomfortable with some of the hyperbole, but the message is becoming bigger than the messenger.

    This study will probably put a damper on the media’s enthusiasm. But for people who follow science, this is just another instance of science correcting itself.

    The fact is, we’re only groping our way toward understanding exoplanet atmospheres. Scientists have a powerful tool in the JWST, but it has limitations. It measures light in extreme detail and leaves the rest up to us. “We find that it is challenging to identify DMS at 3.4 ?m where it strongly overlaps with CH4,” the authors explain. But, they continue, “it is more plausible to detect DMS … in the mid-infrared between 9 and 13 ?m,” the authors explain.

    This figure from the research compares how detectable DMS is in NIR (left) vs MIR (right.) We're mostly interested in the 20xSorg (20 x organic sulphur.) Its presence at that concentration is muddy in NIR but stands out more clearly in simulated MIR data. Image Credit: Left: Madhusudhan et al. 2023. Right: Batalha et al. 2017.
    This figure from the research compares how detectable DMS is in NIR (left) vs MIR (right.) We’re mostly interested in the 20xSorg (20 x organic sulphur.) Its presence at that concentration is muddy in NIR but stands out more clearly in simulated MIR data.
    Image Credit: Left: Madhusudhan et al. 2023. Right: Batalha et al. 2017.

    That means there’s hope for K2-18b. These observations were taken with the JWST’s near-infrared instruments, the NIRISS and the NIRSpec. Sometime next year, the JWST will examine the exoplanet’s atmosphere again, this time with its mid-infrared instrument MIRI. This instrument should tell us definitively whether DMS is present.

    This figure shows the wavelength ranges of its instruments and the modes available to them. Image Credit: NASA/STScI
    This figure shows the wavelength ranges of its instruments and the modes available to them.
    Image Credit: NASA/STScI

    Scientists’ understanding of biosignatures has grown more detailed. Instead of searching for biosignatures like the ones on Earth, scientists are taking a larger, more holistic view of biosignatures and the nature of the atmospheres they might be present in.

    “The best biosignatures on an exoplanet may differ significantly from those we find most abundant on Earth today. On a planet with a hydrogen-rich atmosphere, we may be more likely to find DMS made by life instead of oxygen made by plants and bacteria as on Earth,” said UCR astrobiologist Eddie Schwieterman, a senior author of the study.

    The team’s work does show that sulphur could be a detectable biomarker for Hycean worlds. “The moderate threshold for biological production suggests that the search for biogenic sulphur gases as one class of potential biosignature is plausible for Hycean worlds,” they conclude.

    https://www.universetoday.com/ }

    05-05-2024 om 18:16 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.What Can AI Learn About the Universe?
    Will AI become indispensable in an age of "big data" astronomy?
    Credit: DALL-E

    What Can AI Learn About the Universe?

    Artificial intelligence and machine learning have become ubiquitous, with applications ranging from data analysis, cybersecurity, pharmaceutical development, music composition, and artistic renderings. In recent years, large language models (LLMs) have also emerged, adding human interaction and writing to the long list of applications. This includes ChatGPT, an LLM that has had a profound impact since it was introduced less than two years ago. This application has sparked considerable debate (and controversy) about AI’s potential uses and implications.

    Astronomy has also benefitted immensely, where machine learning is used to sort through massive volumes of data to look for signs of planetary transits, correct for atmospheric interference, and find patterns in the noise. According to an international team of astrophysicists, this may just be the beginning of what AI could do for astronomy. In a recent study, the team fine-tuned a Generative Pre-trained Transformer (GPT) model using observations of astronomical objects. In the process, they successfully demonstrated that GPT models can effectively assist with scientific research.

    The study was conducted by the International Center for Relativistic Astrophysics Network (ICRANet), an international consortium made up of researchers from the International Center for Relativistic Astrophysics (ICRA), the National Institute for Astrophysics (INAF), the University of Science and Technology of China, the Chinese Academy of Sciences Institute of High Energy Physics (CAS-IHEP), the University of Padova, the Isfahan University of Technology, and the University of Ferrera. The preprint of their paper, “Test of Fine-Tuning GPT by Astrophysical Data,” recently appeared online.

    Illustration of an active quasar. New research shows AI can identify and classify them.
    Credit: ESO/M. Kornmesser

    As mentioned, astronomers rely extensively on machine learning algorithms to sort through the volumes of data obtained by modern telescopes and instruments. This practice began about a decade ago and has since grown by leaps and bounds to the point where AI has been integrated into the entire research process. As ICRA President and the study’s lead author Yu Wang told Universe Today via email:

    Astronomy has always been driven by data and astronomers are some of the first scientists to adopt and employ machine learning. Now, machine learning has been integrated into the entire astronomical research process, from the manufacturing and control of ground-based and space-based telescopes (e.g., optimizing the performance of adaptive optics systems, improving the initiation of specific actions (triggers) of satellites under certain conditions, etc.), to data analysis (e.g., noise reduction, data imputation, classification, simulation, etc.), and the establishment and validation of theoretical models (e.g., testing modified gravity, constraining the equation of state of neutron stars, etc.).

    Data analysis remains the most common among these applications since it is the easiest area where machine learning can be integrated. Traditionally, dozens of researchers and hundreds of citizen scientists would analyze the volumes of data produced by an observation campaign. However, this is not practical in an age where modern telescopes are collecting terabytes of data daily. This includes all-sky surveys like the Very Large Array Sky Survey (VLASS) and the many phases conducted by the Sloan Digital Sky Survey (SDSS).

    To date, LLMs have only been applied sporadically to astronomical research, given that they are a relatively recent creation. But according to proponents like Wang, it has had a tremendous societal impact and has a lower-limit potential equivalent to an “Industrial Revolution.” As for the upper limit, Wang predicts that that could range considerably and could perhaps result in humanity’s “enlightenment or destruction.” However, unlike the Industrial Revolution, the pace of change and integration is far more rapid for AI, raising questions about how far its adoption will go.

    The Sloan Digital Sky Survey telescope stands out against the breaktaking backdrop of the Sacramento Mountains. 234 stars out of the Sloan's catalogue of over 2.5 million stars are producing an unexplained pulsed signal. Image: SDSS, Fermilab Visual Media Services
    The Sloan Digital Sky Survey telescope stands out against the breathtaking backdrop of the Sacramento Mountains.
    Credit: SDSS/Fermilab Visual Media Services

    To determine its potential for the field of astronomy, said Wang, he and his colleagues adopted a pre-trained GPT model and fine-tuned it to identify astronomical phenomena:

    “OpenAI provides pre-trained models, and what we did is fine-tuning, which involves altering some parameters based on the original model, allowing it to recognize astronomical data and calculate results from this data. This is somewhat like OpenAI providing us with an undergraduate student, whom we then trained to become a graduate student in astronomy. 

    “We provided limited data with modest resolution and trained the GPT fewer times compared to normal models. Nevertheless, the outcomes are impressive, achieving an accuracy of about 90%. This high level of accuracy is attributable to the robust foundation of the GPT, which already understands data processing and possesses logical inference capabilities, as well as communication skills.”

    To fine-tune their model, the team introduced observations of various astronomical phenomena derived from various catalogs. This included 2000 samples of quasars, galaxies, stars, and broad absorption line (BAL) quasars from the SDSS (500 each). They also integrated observations of short and long gamma-ray bursts (GRBs), galaxies, stars, and black hole simulations. When tested, their model successfully classified different phenomena, distinguished between types of quasars, inferred their distance based on redshift, and measured the spin and inclination of black holes.

    “This work at least demonstrates that LLMs are capable of processing astronomical data,” said Wang. “Moreover, the ability of a model to handle various types of astronomical data is a capability not possessed by other specialized models. We hope that LLMs can integrate various kinds of data and then identify common underlying principles to help us understand the world. Of course, this is a challenging task and not one that astronomers can accomplish alone.”

    The Vera Rubin Observatory at twilight on April 2021. It’s been a long wait, but the observatory should see first light later this year.
    Credit: Rubin Obs/NSF/AURA

    Of course, the team acknowledges that the dataset they experimented with was very small compared to the data output of modern observatories. This is particularly true of next-generation facilities like the Vera C. Rubin Observatory, which recently received its LSST camera, the largest digital camera in the world! Once Rubin is operational, it will conduct the ten-year Legacy Survey of Space and Time (LSST), which is expected to yield 15 terabytes of data per night! Satisfying the demands of future campaigns, says Wang, will require improvements and collaboration between observatories and professional AI companies.

    Nevertheless, it’s a foregone conclusion that there will be more LLM applications for astronomy in the near future. Not only is this a likely development, but a necessary one considering the sheer volumes of data astronomical studies are generating today. And since this is likely to increase exponentially in the near future, AI will likely become indispensable to the field of study.

    Further Reading: 

    https://www.universetoday.com/ }

    05-05-2024 om 17:59 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Solar Orbiter Takes a Mind-Boggling Video of the Sun
    The 'fuzzy' Sun.
    Credit: ESA & NASA/Solar Orbiter/EUI Team

    Solar Orbiter Takes a Mind-Boggling Video of the Sun

    You’ve seen the Sun, but you’ve never seen the Sun like this. This single frame from a video captured by ESA’s Solar Orbiter mission shows the Sun looking very …. fluffy!  You can see feathery, hair-like structures made of plasma following magnetic field lines in the Sun’s lower atmosphere as it transitions into the much hotter outer corona. The video was taken from about a third of the distance between the Earth and the Sun.

    See the full video below, which shows unusual features on the Sun, including coronal moss, spicules, and coronal rain.  

    Solar Orbiter recorded this video on September 27, 2023 using its Extreme Ultraviolet Imager (EUI) instrument.

    ESA said the brightest regions are around one million degrees Celsius, while cooler material looks darker, as it absorbs radiation.

    So, just what is coronal moss? It’s what gives the Sun its fluffy appearance here. These peculiar structures on the Sun resemble the moss we find on Earth, in that it appears like fine, lacy features. But on the Sun, they usually can be found around the center of sunspot groups, where magnetic conditions are strong and large coronal loops are forming. The moss is so hot, most instruments can’t detect them. The moss spans two atmospheric layers, the chromosphere and corona.

    Features on the Sun’s surface, as seen by Solar Orbiter.
    Credit: ESA & NASA/Solar Orbiter/EUI Team

    Spicules, as their name implies, are tall spires of gas seen on the solar horizon that reach up from the Sun’s chromosphere. These can reach up to a height of 10,000 km (6,000 miles).

    At about 0:30 in the video, you’ll see coronal rain. This material is cooler than the rest of the solar surface (probably less than 10,000 °C) versus the one million degrees C of the coronal loops. The rain is made of higher-density clumps of plasma that fall back towards the Sun under the influence of gravity.

    Did you see the small eruption in the center of the field of view at about 0:20 seconds in the video? , with cooler material being lifted upwards before mostly falling back down. It’s not small at all — this eruption is bigger than Earth!

    Missions like Solar Orbiter, the Parker Solar Probe and the Solar Dynamics Observatory are giving us unprecedented views of the Sun, helping astronomers to learn more about the dynamic ball of gas that powers our entire Solar System.

    Further reading: 

    https://www.universetoday.com/ }

    05-05-2024 om 17:45 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Maar liefst een derde van veelvoorkomende planeten in ons Melkwegstelsel zit mogelijk in bewoonbare zone

    Maar liefst een derde van veelvoorkomende planeten in ons Melkwegstelsel zit mogelijk in bewoonbare zone

    Hoe is het weer? Dat is niet alleen een belangrijke vraag in de vakantie, het is ook een van de eerste dingen die astronomen zich afvragen als ze op een nieuwe planeet stuiten. Of een planeet zich in de zogenoemde leefbare zone bevindt, is namelijk cruciaal voor de mogelijke aanwezigheid van water en dus leven. Nu blijkt dat meer planeten dan gedacht voldoen aan die voorwaarde.

    Onze grote hete zon is een relatieve zeldzaamheid in de Melkweg. Verreweg de meeste sterren zijn kleiner en kouder, met een massa van hooguit de helft van de zon. Miljarden planeten draaien rond deze dwergsterren. Maar willen ze leefbaar zijn dan moeten ze erg dicht rond hun kleine sterren draaien, omdat het anders te koud is. Dat maakt ze echter weer erg vatbaar voor extreme getijdenkrachten.

    Bewoonbare zone
    De bewoonbare of leefbare zone is het gebied dat zich op een dusdanige afstand bevindt van een ster dat er eventueel leven mogelijk is. Belangrijkste voorwaarde daarbij is de temperatuur. Het moet er niet te warm of te koud zijn, zodat water niet bevriest of verdampt, maar vloeibaar blijft. Leuk weetje: dit gebied wordt ook wel de Goldilocks-zone genoemd, naar het sprookje van Goudlokje en de drie beren. Volgens het verhaal moet een meisje van drie borden pap proeven, waarbij het eerste te warm is, het tweede te koud en het derde precies goed.

    Volgende fase onderzoek 
    Volgens een nieuwe analyse van telescoopdata bevindt twee derde van de planeten zich te dicht bij hun ster om bestand te zijn tegen deze extreme getijdenkrachten waardoor ze te veel worden opgewarmd. Maar dat betekent dus dat een derde van de planeten – nog altijd honderden miljoenen exemplaren, alleen al in ons sterrenstelsel – zich op de juiste afstand van zijn ster bevindt om vloeibaar water te kunnen herbergen en daarmee mogelijk leven.

    Onderzoeker van de University of Florida Sarah Ballard reageert: “Ik denk dat dit resultaat erg belangrijk is voor het volgende decennium aan exoplaneetonderzoek, omdat onze ogen nu meer gericht zijn op deze groep sterren. Deze sterren zijn perfect om op zoek te gaan naar kleine planeten in een baan die vloeibaar water mogelijk maakt, waardoor er leven kan zijn”, aldus de onderzoeker die al heel lang exoplaneten bestudeert.

    Geen perfecte cirkel
    Samen met onderzoeker Sheila Sagear keek ze naar de excentriciteit van meer dan 150 planeten rond rode dwergsterren (M-sterren), die ongeveer zo groot zijn als Jupiter. Hoe ovaler of elliptischer een baan – dus hoe meer hij afwijkt van een perfecte cirkel – hoe excentrischer hij is. Als een planeet erg dicht bij zijn ster staat, ongeveer zo ver als Mercurius van de zon, dan kan een excentrische baan ervoor zorgen dat de planeet te maken krijgt met zogenoemde getijdenopwarming. Onder invloed van de steeds veranderende zwaartekracht tijdens zijn onregelmatige baan wordt de planeet uitgerekt en vervormd. In het extreemste geval wordt de planeet veel te heet, waardoor al het eventueel vloeibare water verdampt. “Alleen voor deze kleine sterren geldt dat de leefbare zone zo dichtbij is dat deze getijdenkrachten relevant worden”, verklaart Ballard.

    Kepler en Gaia
    De data zijn afkomstig van de Kepler-telescoop van NASA die informatie opvangt van exoplaneten als ze voor hun gastster langs bewegen. Om de banen van de planeten te meten, focusten de onderzoekers vooral op hoe lang het duurde voor een planeet voor een ster langs was getrokken. Daarbij gebruikten ze ook nieuwe data van de Gaia-telescoop, die de afstand meet tot miljarden sterren in ons sterrenstelsel. “De afstand was echt het stukje informatie dat we tot nu toe misten en waardoor we nu wel een goede analyse konden doen”, reageert Sagear.

    Meerdere planeten rond één ster
    De twee onderzoekers ontdekten dat sterren met meerdere planeten de grootste kans hadden op de soort cirkelvormige baan die nodig is om vloeibaar water vast te houden. Sterren met slechts één planeet hadden het vaakst getijdenextremen waardoor het oppervlak onleefbaar werd.

    Een derde van de planeten in deze kleine steekproef had een dusdanig ‘vriendelijke’ baan rond een ster dat vloeibaar water tot de mogelijkheden behoort. Dat betekent dat de Melkweg waarschijnlijk honderden miljoenen planeten herbergt buiten ons zonnestelsel waar astronomen kunnen zoeken naar tekenen van leven.

    Bronmateriaal

    https://scientias.nl/ }

    05-05-2024 om 00:21 geschreven door peter  

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    Categorie:ASTRONOMIE / RUIMTEVAART
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Maar liefst een derde van veelvoorkomende planeten in ons Melkwegstelsel zit mogelijk in bewoonbare zone

    Maar liefst een derde van veelvoorkomende planeten in ons Melkwegstelsel zit mogelijk in bewoonbare zone

    Hoe is het weer? Dat is niet alleen een belangrijke vraag in de vakantie, het is ook een van de eerste dingen die astronomen zich afvragen als ze op een nieuwe planeet stuiten. Of een planeet zich in de zogenoemde leefbare zone bevindt, is namelijk cruciaal voor de mogelijke aanwezigheid van water en dus leven. Nu blijkt dat meer planeten dan gedacht voldoen aan die voorwaarde.

    Onze grote hete zon is een relatieve zeldzaamheid in de Melkweg. Verreweg de meeste sterren zijn kleiner en kouder, met een massa van hooguit de helft van de zon. Miljarden planeten draaien rond deze dwergsterren. Maar willen ze leefbaar zijn dan moeten ze erg dicht rond hun kleine sterren draaien, omdat het anders te koud is. Dat maakt ze echter weer erg vatbaar voor extreme getijdenkrachten.

    Bewoonbare zone
    De bewoonbare of leefbare zone is het gebied dat zich op een dusdanige afstand bevindt van een ster dat er eventueel leven mogelijk is. Belangrijkste voorwaarde daarbij is de temperatuur. Het moet er niet te warm of te koud zijn, zodat water niet bevriest of verdampt, maar vloeibaar blijft. Leuk weetje: dit gebied wordt ook wel de Goldilocks-zone genoemd, naar het sprookje van Goudlokje en de drie beren. Volgens het verhaal moet een meisje van drie borden pap proeven, waarbij het eerste te warm is, het tweede te koud en het derde precies goed.

    Volgende fase onderzoek 
    Volgens een nieuwe analyse van telescoopdata bevindt twee derde van de planeten zich te dicht bij hun ster om bestand te zijn tegen deze extreme getijdenkrachten waardoor ze te veel worden opgewarmd. Maar dat betekent dus dat een derde van de planeten – nog altijd honderden miljoenen exemplaren, alleen al in ons sterrenstelsel – zich op de juiste afstand van zijn ster bevindt om vloeibaar water te kunnen herbergen en daarmee mogelijk leven.

    Onderzoeker van de University of Florida Sarah Ballard reageert: “Ik denk dat dit resultaat erg belangrijk is voor het volgende decennium aan exoplaneetonderzoek, omdat onze ogen nu meer gericht zijn op deze groep sterren. Deze sterren zijn perfect om op zoek te gaan naar kleine planeten in een baan die vloeibaar water mogelijk maakt, waardoor er leven kan zijn”, aldus de onderzoeker die al heel lang exoplaneten bestudeert.

    Geen perfecte cirkel
    Samen met onderzoeker Sheila Sagear keek ze naar de excentriciteit van meer dan 150 planeten rond rode dwergsterren (M-sterren), die ongeveer zo groot zijn als Jupiter. Hoe ovaler of elliptischer een baan – dus hoe meer hij afwijkt van een perfecte cirkel – hoe excentrischer hij is. Als een planeet erg dicht bij zijn ster staat, ongeveer zo ver als Mercurius van de zon, dan kan een excentrische baan ervoor zorgen dat de planeet te maken krijgt met zogenoemde getijdenopwarming. Onder invloed van de steeds veranderende zwaartekracht tijdens zijn onregelmatige baan wordt de planeet uitgerekt en vervormd. In het extreemste geval wordt de planeet veel te heet, waardoor al het eventueel vloeibare water verdampt. “Alleen voor deze kleine sterren geldt dat de leefbare zone zo dichtbij is dat deze getijdenkrachten relevant worden”, verklaart Ballard.

    Kepler en Gaia
    De data zijn afkomstig van de Kepler-telescoop van NASA die informatie opvangt van exoplaneten als ze voor hun gastster langs bewegen. Om de banen van de planeten te meten, focusten de onderzoekers vooral op hoe lang het duurde voor een planeet voor een ster langs was getrokken. Daarbij gebruikten ze ook nieuwe data van de Gaia-telescoop, die de afstand meet tot miljarden sterren in ons sterrenstelsel. “De afstand was echt het stukje informatie dat we tot nu toe misten en waardoor we nu wel een goede analyse konden doen”, reageert Sagear.

    Meerdere planeten rond één ster
    De twee onderzoekers ontdekten dat sterren met meerdere planeten de grootste kans hadden op de soort cirkelvormige baan die nodig is om vloeibaar water vast te houden. Sterren met slechts één planeet hadden het vaakst getijdenextremen waardoor het oppervlak onleefbaar werd.

    Een derde van de planeten in deze kleine steekproef had een dusdanig ‘vriendelijke’ baan rond een ster dat vloeibaar water tot de mogelijkheden behoort. Dat betekent dat de Melkweg waarschijnlijk honderden miljoenen planeten herbergt buiten ons zonnestelsel waar astronomen kunnen zoeken naar tekenen van leven.

    Bronmateriaal

    https://scientias.nl/ }

    05-05-2024 om 00:21 geschreven door peter  

    0 1 2 3 4 5 - Gemiddelde waardering: 0/5 - (0 Stemmen)
    Categorie:ASTRONOMIE / RUIMTEVAART
    04-05-2024
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Wanneer vindt de volgende massa-extinctie plaats? De wetenschap weet het

    Wanneer vindt de volgende massa-extinctie plaats? De wetenschap weet het

    Slechts een klein deel van de aarde zal bewoonbaar blijven tijdens wat volgens wetenschappers de grootste massa-extinctie sinds de ondergang van de dinosauriërs kan worden.

    DOOR 

    Extreme temperaturen, intense straling en een totale instorting van de voedselvoorziening.

    Dat klinkt niet bijster aantrekkelijk, maar het kan de harde werkelijkheid worden wanneer in de verre toekomst de landmassa’s van de aarde fuseren om het volgende supercontinent te vormen.

    Dit is een deel van de conclusie van een onderzoek van de Universiteit van Bristol, waarin wetenschappers computersimulaties maakten van de invloed van het samenkomen van de landmassa’s op landzoogdieren.

    En volgens hun resultaten ziet het er op zijn zachtst gezegd niet best uit.

    Het toekomstige supercontinent zal naar verwachting over 250 miljoen jaar rond de evenaar ontstaan en wordt Pangea Ultima genoemd: een verwijzing naar het supercontinent Pangea, dat bestond in het tijdperk van de dinosauriërs.

    De afgelopen 2 miljard jaar zijn de continenten verschillende keren verenigd, met zo’n 600 miljoen jaar ertussen. Geologen spreken van de supercontinentcyclus.

    Supercomputer voorspelt de toekomst

    De oorzaak van de herschikking van het landoppervlak is te vinden in het middelste deel van de aardmantel, waar een hete oceaan van magma de buitenste, vaste platen tegen elkaar duwt.

    De onderzoekers gebruikten supercomputers en geavanceerde klimaatmodellen om te simuleren wat de geologische herschikking betekent voor temperaturen, windomstandigheden, regenval en vochtigheid op het nieuwe supercontinent.

    En we kunnen verklappen dat het nogal warm wordt voor alle levende wezens die er op dat moment rondlopen.

    Enorme botsing creëerde Pangea

    Door botsingen tussen de continentale platen waarop de landmassa’s van de aarde rusten, ontstond zo’n 325 miljoen jaar geleden het supercontinent Pangea.

    Pangea continentale platen botsen
    © Claus Lunau

    325 miljoen jaar geleden: Continenten botsen

    Bijna al het land op aarde is gegroepeerd in twee continenten, Euramerika en Gondwana. De continentale platen waarop de twee landmassa’s rusten, botsen op elkaar, waardoor de Paleo-Tethysoceaan zich sluit.

    Pangea een groot continent
    © Claus Lunau

    235 miljoen jaar geleden: Al het land komt samen in Pangea

    Alle landmassa’s zijn nu verzameld in Pangea – naar de twee Griekse woorden voor alles (pan) en land/aarde (gaia), terwijl de rest van de aarde wordt bedekt door de oceaan Panthalassa. Thalassa betekent zee.

    Pangea de werelddelen ontstaan
    © Claus Lunau

    140 miljoen jaar geleden: Werelddelen ontstaan

    De continentale platen bewegen uit elkaar, en Pangea verbrokkelt. De Noord-Atlantische Oceaan is een smalle zeestraat, terwijl Afrika en Zuid-Amerika zich nog aan elkaar vastklampen.

    Het extreem grote landoppervlak zal het verkoelende effect van de omringende oceanen ontberen. Daarnaast verwachten de onderzoekers dat de zon, die dan de jongste niet meer is, zo’n 2,5 procent meer straling zal uitzenden dan nu.

    En alsof dat nog niet genoeg is, wordt de planeet ook nog eens getroffen door veel meer vulkaanuitbarstingen, waardoor grote hoeveelheden kooldioxide in de atmosfeer terechtkomen. Dit warmt onze planeet verder op en leidt tot een vijandig milieu zonder drinkwater en voedsel.

    Pangea Ultima

    Op de illustratie zijn de huidige landmassa’s afgebeeld en de verwachte situatie over 250 miljoen jaar, als alle continenten samen het supercontinent Pangea Ultima vormen.

    © University of Bristol

    De wetenschappers verwachten dat slechts tussen de 8 en 16 procent van het land bewoonbaar zal blijven voor zoogdieren en dat een groot deel van de planeet te maken kan krijgen met constante temperaturen tussen de 40 en 70 °C.

    Volgens de onderzoekers kan dit de doodsteek betekenen voor de overgrote meerderheid van de zoogdieren, die zich tot nu toe hebben aangepast aan hitte met bijvoorbeeld zweetklieren.

    Het vermogen om overtollige warmte kwijt te raken kan echter zijn grenzen bereiken als de temperatuur gedurende langere tijd boven de 40 °C blijft bij een lage luchtvochtigheid, of 35 °C bij een hoge luchtvochtigheid, leggen de onderzoekers uit.

    ‘Mensen zullen – net als vele andere diersoorten – omkomen doordat ze niet genoeg hitte kunnen afgeven door middel van zweten en hun lichaam onvoldoende kunnen koelen,’ zegt hoofdauteur Alexander Farnsworth in een persbericht.

    ‘Terwijl we een onbewoonbare planeet voorspellen over 250 miljoen jaar, hebben we nu al te maken met extreme hitte, die de gezondheid schaadt. Daarom is het cruciaal om zo snel mogelijk de uitstoot tot netto nul terug te brengen,’ zegt Eunice Lo, coauteur van het onderzoek, dat is gepubliceerd in het gerenommeerde wetenschappelijke tijdschrift Nature Geoscience.

    https://wibnet.nl/heelal }

    04-05-2024 om 23:57 geschreven door peter  

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    Categorie:ASTRONOMIE / RUIMTEVAART
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.China wil de donkere kant van de maan veroveren: de missie vindt dit jaar al plaats

    China wil de donkere kant van de maan veroveren: de missie vindt dit jaar al plaats

    Janine image Door Janine
    China wil de donkere kant van de maan veroveren: de Chang'e 6-missie vindt dit jaar al plaats

    De donkere kant van de maan fascineert de mens al heel lang: we zien immers maar één vlak van onze satelliet. De mens heeft echter al enkele jaren grote vooruitgang geboekt bij het verkennen van de verborgen kant van de maan. In het bijzonder zou de Chinese Chang'e 6-ruimtemissie eindelijk monsters naar de aarde kunnen brengen van de kant die we nooit zien. Zo zullen ze dit gaan doen.

    Wat bevindt zich aan de donkere kant van de maan?

    De verborgen kant van de maan

    NASA

    Ten eerste moet duidelijk worden gemaakt dat het technisch onjuist is om van een donkere kant van de Maan te spreken. Zoals bij alle hemellichamen die rond de zon draaien, zijn er niet per se donkere kanten: we zien de andere kant van onze satelliet gewoon nooit. Daarom is het beter om te spreken van de verborgen kant van de Maan of de verre kant van de Maan. Verborgen en ver van ons op Aarde, uiteraard.

    Al bij de eerste waarnemingen door astronauten in een baan om de Maan was te zien dat dit verborgen gebied heel anders is dan wij kennen. Er zijn minder maanzeeën en meer kraters, wat duidt op een dikkere korst, evenals meer radioactieve elementen zoals thorium. Afgezien van wetenschappelijke analyses kunnen aardsondes de verborgen kant van de maan al tientallen jaren van veraf bekijken, maar dat betekent niet dat ze niet al hebben geprobeerd om er dichtbij te komen.

    Aan de andere kant van de maan landen

    Vertegenwoordiging van de lander van de Chinese Chang'e 6-missie aan de andere kant van de maan

    China News Service/Wikimedia Commons 

    CC BY 3.0 LEGAL CODE / NASA

    Wat betreft het verkennen van de verborgen kant van de Maan heeft China andere ruimtevaartorganisaties ingehaald. In slechts een paar decennia is het Aziatische land een van de belangrijkste landen geworden die proberen op de maan te landen. Met name de twee missies van de Chinese ruimtevaartorganisatie Chang'e 3 en Chang'e 4 waren gericht op de verborgen kant van onze satelliet. De eerste, in 2013, maakte een eerste zachte landing niet ver van het doel. De tweede, gelanceerd in 2018, is in plaats daarvan de sonde die verantwoordelijk is voor de eerste landing op de verre kant van de maan, meer bepaald in de Von Kármán-krater in het Zuidpool-Aitken-bekken.

    Chang'e 4 werd gevolgd door Chang'e 5, gelanceerd in 2020 en werd de eerste ruimtemissie die maanmonsters terug naar de aarde bracht sinds de Luna 24-missie van de Sovjet-Unie. Hoewel Chang'e 5 niet op de verborgen kant van de maan landde, is China van plan om daar terug te keren met de Chang'e 6-missie, die in mei 2024 vertrekt.

    Er wordt begonnen met verkenning van de andere kant van de maan

    De lander van de Chang'e 4-missie, de eerste die op de andere kant van de maan landde

    CSNA/Siyu Zhang/Kevin M. Gill/Wikimedia Commons

    CC BY 2.0 DEED

    Hoewel er al een eerste landing op de verborgen kant van de maan heeft plaatsgevonden, is de Chang'e 6-missie anders. In zekere zin wil deze missie de resultaten van de twee missies die eraan voorafgingen combineren: landen aan de andere kant van onze satelliet en, na het verzamelen van monsters van de maanbodem, deze terugbrengen naar de aarde voor verder onderzoek. De missie bestaat uit een orbiter, een lander, een opstijgmodule en een terugkeermodule: de verkenning zelf zal slechts 53 dagen duren, maar zelfs een paar uur zal gegevens opleveren die nog nooit eerder zijn verzameld.

    Concluderend kunnen we zeggen dat er niet langer een donkere kant van de Maan is: die was er nooit vanuit fysiek oogpunt en zal er ook niet meer zijn vanuit metaforisch oogpunt. Aan de andere kant is de Chinese missie Chang'e 6 slechts de eerste die ons de komende jaren meer over onze satelliet zal leren. Misschien met de bedoeling er ooit te leven, hetzij aan de bekende kant, hetzij aan de andere kant, de verborgen kant.

    https://www.curioctopus.nl/ }

    04-05-2024 om 18:34 geschreven door peter  

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    Categorie:ASTRONOMIE / RUIMTEVAART
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Vreemde witte stenen gevonden op Mars: Perseverance heeft er duizenden gevonden

    Vreemde witte stenen gevonden op Mars: Perseverance heeft er duizenden gevonden

    Janine image Door Janine
    Vreemde witte stenen gevonden op Mars: er zijn er duizenden
    Mars is de planeet van het zonnestelsel die we het beste kennen, afgezien van de aarde. De afgelopen jaren is er een continue stroom informatie ontstaan ​​dankzij rovers als Curiosity, de quadcopter Ingenuity en de Perseverance rover. In het bijzonder leverde Perseverance ongelooflijke foto's op van het oppervlak van Mars en van enkele details, zoals stenen die wel erg lichtgekleurd waren. Wat kunnen ze zijn en vooral: zal het ooit mogelijk zijn om ze in het echt te bestuderen?

    Vreemde stenen op het oppervlak van Mars: Perseverance heeft ze geïdentificeerd

    Simulatie van Perseverance in actie op Mars

    NASA/JPL

    We weten allemaal dat Mars de rode planeet is, dankzij de ijzeroxiden die hem zijn karakteristieke kleur geven. Toch bevinden zich op het oppervlak duizenden lichtgekleurde stenen, verspreid over de krater Jezero, het gebied dat door Perseverance is bestudeerd. De kleur neigt bijna naar wit en de stenen lijken bijna op kiezelstenen, willekeurig verspreid over het oppervlak. Maar wat zijn ze precies?

    Op dit moment is er niet veel bekend over de vreemde witte stenen op Mars, en er zijn verschillende wetenschappers die ze graag zouden willen analyseren om te begrijpen waar het om gaat. Vanuit dit oogpunt kan zelfs een beetje informatie helpen enkele geheimen van de rode planeet te onthullen. Op dit moment is uit de eerste analyses van Perseverance gebleken dat de stenen geen water of andere mineralen zoals ijzer, magnesium, calcium en natrium bevatten. Dit is een indicatie die ons al in staat stelt te veronderstellen dat deze stenen werden verwarmd door lavastromen of werden aangetast door de inslag van asteroïden. Maar voor een vollediger antwoord moeten we misschien wachten.

    De missie van Perseverance naar de rode planeet

    NASA/JPL-Caltech

    Zoals we al zeiden, was het mogelijk om veel gegevens te verzamelen, vooral dankzij de inspanningen van de Perseverance rover en de Ingenuity quadcopter. Nu is de missie Ingenuity helaas beëindigd vanwege een probleem met de vleugels van de quadcopter, na meer dan 70 vluchten. Perseverance heeft daarentegen ruim 20 kilometer afgelegd sinds zijn aankomst op Mars en heeft al meer dan de helft van de beschikbare buisjes voltooid om gesteentemonsters van Mars te verzamelen. Bovendien is de rover onlangs begonnen zich te verplaatsen naar de rand van de Jezero-krater, waar hij tot nu toe zijn verkenningen heeft uitgevoerd, waarbij hij daar ook de lichtgekleurde stenen heeft gevonden die van groot belang zijn voor astronomen.

    Eenmaal vrijgegeven zal Perseverance oudere gesteenten kunnen bestuderen dan die aanwezig in de Jezero-krater, die ook biosignaturen kunnen bevatten, oftewel sporen van complexe moleculen of ingrediënten voor leven. Als het echter nodig is om enige tijd te wachten om deze informatie te verkrijgen, zal het onderzoek van de witte stenen op korte termijn niet mogelijk zijn. Alleen op aarde zullen wetenschappers de door Perseverance verzamelde monsters kunnen bestuderen en misschien een antwoord kunnen vinden.

    De toekomst van de verkenning van Mars, beginnend bij de terugkeer naar de aarde

    Landschap van Mars

    NASA/JPL-Caltech/ASU/MSSS

    Bij de terugkeer naar de aarde via het programma Mars Sample Return van NASA, zal Perseverance de verzamelde monsters terug naar onze planeet brengen. Als naar Mars gaan helemaal niet gemakkelijk is, is terugkeren naar de blauwe planeet zelfs nog moeilijker. Tot op heden, en ondanks de begrotingsproblemen waar NASA helaas altijd last van heeft gehad, bevindt de MSR zich nog in de voorbereidingsfase, maar zou binnenkort klaar kunnen zijn.

    Als alles volgens plan verloopt, zal dit niet alleen de eerste “terugreis” zijn van de rode planeet naar de aarde. We zullen voor het eerst in de geschiedenis ook monsters van Mars-gesteente kunnen aanraken. En misschien begrijpen wat die witte stenen zijn, waarom ze op Mars waren en wat ze ons kunnen vertellen over een planeet die veel op de onze lijkt, maar ook heel verschillend.

     { https://www.curioctopus.nl/ }

    04-05-2024 om 00:13 geschreven door peter  

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    Categorie:ASTRONOMIE / RUIMTEVAART
    02-05-2024
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.New Starfield Update Will Finally Add These Widely Requested Features

    New Starfield Update Will Finally Add These Widely Requested Features

    Getting lost in Neon will be a thing of the past.

    Bethesda Game Studios

    On the heels of the somewhat contentious release of Fallout 4’s Next-Gen update, Bethesda Game Studios announced that some long-awaited quality-of-life features are finally being added to their space-faring role-playing game.

    Starfield’s fourth major update will add a wave of new features according to a video update from Bethesda, including new planet surface maps that will communicate a more detailed view of explorable celestial bodies like terrain, vegetation, and the locations of man-made structures. The update will improve how players get around the game’s major cities by adding UI markers for shops, fast travel points, and other points of interest.

    Bethesda will also give players more control over how they want to experience Starfield. New difficulty modes and setting sliders will let them adjust everything from combat encounters, how XP is distributed, carrying capacity, and the damage players dole out and receive. More customization options are being added for players who opt into the game’s interesting twist on new game plus, allowing them a chance to roll a character with different traits and new appearance.

    For the sickos who spent hours in New Atlantis’ ship ports getting their rigs just right, the developer is adding not just new ship pieces, but an entirely new element to the creation suite: customizable interiors. They’ll now be able to furnish their ships with chairs, carpets, posters, and visual decor to make space travel a little cozier.

    Lastly, Starfield is getting a handful of presentation and performance options. Console players will now have a 60 frames per second mode for smoother, more responsive action. Conversations with NPCs can now be had without Bethesda’s signature zoom-in thanks to a toggle for the dialogue camera.

    Bethesda also teased what additions are on the game’s event horizon: new quests, and the oft-request land vehicles. The latter in particular is something players have wanted since launch, as the on-foot-only approach to planet exploration slowed a crucial, frequent pillar of the game’s loop to a crawl.

    Bethesda is adding land vehicles to Starfield, which could make late-game planet exploration less of a slog.

    BESTHESDA GAME STUDIOS

    Wednesday’s announcement was a welcome surprise for Starfield players. It was proof that the Maryland-based developer is listening to the community, and is working hard to improve their first original game in more than 30 years.

    But as exciting as these additions are, one can’t help but wonder why the features weren’t added to the game closer to launch. Starfield received a mixed reception when it finally hit digital storefronts last September, and much of that was because of many missing quality-of-life features. The aforementioned absence of land vehicles, clunky UI and inventory system, and a lack of performance options all held back an otherwise wonderfully ambitious role-playing game.

    It goes without saying that a substantial amount of work obviously went into Starfield’s promising new update. But when Bethesda releases a patch for an older game (one that did more harm than good on certain platforms) after promising big changes and fixes every six weeks for their newest one, you can’t help but wonder why Starfield wasn’t more of a priority these last seven months.

    Thankfully players won’t have to wait much longer for these long-overdue additions. Bethesda says Update 4 will drop on May 15. Other features, like the planetary land vehicles, and the game’s first expansion, Shattered Space, are expected later this year.

    https://www.inverse.com/ }

    02-05-2024 om 22:24 geschreven door peter  

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    Categorie:ASTRONOMIE / RUIMTEVAART
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.This New Telescope Could Create the Greatest Space Movie of All Time

    This New Telescope Could Create the Greatest Space Movie of All Time

    The world’s largest digital camera is epic, from its size to its ambitious movie.

    The completed LSST camera.

    Like the family camcorder, the largest digital camera in the world will capture the next 10 years of cosmic life in memorable detail.

    In mid-May, the Legacy Survey of Space and Time (LSST) Digital Camera, now officially called the Vera C. Rubin Observatory, will travel from its current home in California to Cerro Pachón, a mountain in northern Chile.

    The camera, the team behind it purports, will take the greatest movie of all time. Observations will begin around January 2025.

    Trilogy enthusiasts be warned: to watch all the video clips back to back, each packed with a decade’s worth of observations of just one slice of the southern sky, would take a year. That’s without sleeping, too, Rubin Observatory construction director ´eljko Ivezić tells Inverse.

    Aerial view of Vera C. Rubin Observatory located in the Pachon hill, approximately 80 km from the ci...

    Aerial view of Vera C. Rubin Observatory.

    JAVIER TORRES/AFP/GETTY IMAGES

    The camera will record our celestial family. That includes close cousin asteroids, infrequent visitors like comets, the Sun’s community of stars whizzing around the center of the Milky Way and outside the galaxy, to the far reaches of our celestial family tree. Ivezić is optimistic the LSST Camera will discover five million asteroids, and see about 20 billion stars in our galaxy, plus about 20 billion galaxies.

    Imaging the cosmos and how it changes at varying distances will help reveal many dynamics at play. The camera’s work will complement other missions surveying the night sky such as Gaia and Euclid. The science produced can help answer questions about whether or not Albert Einstein had it entirely right with his theory of general relativity, reveal new transient phenomena like supernovas and variable stars, and quintuple the number of known asteroids zipping through the Solar System.

    The idea of a massive digital camera isn’t revolutionary. But the technology is. The University of Arizona produced the camera’s most critical component, the three mirrors, for the low price of $30 million. Ivezić says before modern advancements in manufacturing, the mirrors would have cost hundreds of millions of dollars. The camera’s field of view required computers to be capable of storing 3,200 megapixels and processing them. This wasn’t possible until recently.

    A massive camera lens towers above. Its lens cap is off.

    The LSST Camera, the world's largest digital camera, has its lens cap off in this September 2022 photo. 

    JACQUELINE RAMSEYER ORRELL/SLAC NATIONAL ACCELERATOR LABORATORY

    LSST Camera will hone in on a section of the southern night sky, about 45 times larger than the size of the Full Moon, for 30 seconds. It rapidly repoints to the next 9.6 square degrees slice of space, and repeats. This way, the camera shoots the entire night sky in three nights. To observe the southern sky in its totality in all six color filters of its carousel takes about three weeks. When the round is complete, the camera starts all over again. This will go on and on for ten years.

    The repetition increases the exposure time of each segment. This makes the images more sensitive to dimmer objects. The numerous exposures reveal an average appearance. That’s how the team hopes to discover interlopers, like asteroids and comets.

    Over more repetitions, the subtle motions of stars relative to the Sun will also become apparent. Star motions are much gnarlier than they seem. “Those motions are actually faster than the motion of Earth around the Sun,” Ivezić says. “The relative speed is actually higher between the stars, but when you look at images, it’s much smaller because they are thousands of times farther away.”

    A technician wears a protective, thin fabric outfit. This person's eyes are all that are visible on ...

    LSST Camera Deputy Project Manager Travis Lange (left) and science and engineering associate Mike Silva (right) inspect the L3 lens in preparation of its installation onto the focal plane of the camera.

    JACQUELINE RAMSEYER ORRELL/SLAC NATIONAL ACCELERATOR LABORATORY

    Astronomers will use the LSST Camera to measure galaxy traits. Their colors reveal their distances. Distortion to their shapes would hint at gravitational lensing, as extraordinarily massive structures bend light. Their placements would fine-tune ideas about how galaxies distribute over time. The expansion of the universe may also get less mysterious.

    The SUV-sized camera will soon begin a daunting journey. The Boeing 747 that will fly it across the Americas can land in La Serena, Chile. But it cannot take off from this small airport. So the big plane will have to land farther from the observatory site, in Santiago. A truck carrying the camera will sojourn out of the capital into the Andean highlands. Once it reaches the road that leads up to the 8,900-foot-high summit of Cerro Pachón, it won’t go more than a few miles an hour.

    To say the cargo is precious is putting it mildly. It’s covered by insurance, but the team never wants to have to cash in. “They would get money back, but there is no place to go to buy a new camera,” Ivezić says.

    https://www.inverse.com/ }

    02-05-2024 om 22:14 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Boeing Starliner Is Just Days Away From Its First Human Test Flight

    Boeing Starliner Is Just Days Away From Its First Human Test Flight

    All eyes are on Starliner.

    CAPE CANAVERAL, FLORIDA, UNITED STATES - APRIL 16: Boeing's CST-100 Starliner spacecraft rolls out o...
    Anadolu/Anadolu/Getty Images

    The Boeing Starliner is less than a week away from its critical Crew Flight Test.

    NASA astronauts Sunita “Suni” Williams and Barry “Butch” Wilmore will be the first humans to fly aboard the low-Earth orbit spacecraft. Their flight will take off as early as Monday, May 6 at 10:34 p.m. Eastern from Cape Canaveral Space Force Station in Florida, atop a United Launch Alliance Atlas V rocket. NASA will be streaming the event live, which you can watch here.

    Williams and Wilmore will run tests onboard the spacecraft. Starliner will then dock with the International Space Station (ISS). After a week inside the orbiting laboratory, they’ll reboard Starliner. The reusable spacecraft will land back to Earth in the southwestern United States.

    WHY IS THIS LAUNCH SO IMPORTANT?

    CAPE CANAVERAL, FLORIDA, UNITED STATES - APRIL 25: NASA astronauts Suni Williams and Butch Wilmore (...

    NASA astronaut Suni Williams arrives at the Kennedy Space Center ahead of the May 6 Starliner launch. She is the Crew Flight Test pilot.

    ANADOLU/ANADOLU/GETTY IMAGES

    Starliner flew crewless in late 2019 for Orbital Flight Test 1. But it failed to dock with the ISS. This important maneuver finally happened on the following test, Orbital Flight Test 2, in mid-2022. On Friday, NASA announced Williams and Wilmore had completed a start-to-finish mission dress rehearsal for the upcoming launch.

    If Starliner aces Crew Flight Test, NASA will have a second company to take its astronauts into Earth’s atmosphere. NASA has already ordered six Starliner crew rotation missions to the space station. It can carry up to four astronauts, or a mix of passengers and cargo.

    A MUCH NEEDED BACK UP PLAN

    Currently only one spacecraft, the SpaceX Crew Dragon, launches astronauts from the United States. After the Space Shuttle Program ended in July 2011, spacefarers could only launch from Russia or China.

    CAPE CANAVERAL, FLORIDA - APRIL 16: (L-R) Suni Williams, NASA astronaut and Starliner mission pilot,...

    Suni Williams, NASA astronaut and Starliner mission pilot, and Butch Wilmore, NASA astronaut and Starliner mission commander, speak to the media as the Boeing Starliner spacecraft rolls out of the Commercial Crew and Cargo Processing Facility on its way to Space Launch Complex 41 at Kennedy Space Center on April 16, 2024 in Cape Canaveral, Florida.

    JOE RAEDLE/GETTY IMAGES NEWS/GETTY IMAGES

    NASA awarded contracts to SpaceX and Boeing to develop spacecraft that could carry astronauts into low-Earth orbit as part of its Commercial Crew Program. SpaceX debuted Crew Dragon on May 30, 2020. Monday will be Boeing’s first crewed flight.

    Boeing would provide a backup plan. The ISS must be continuously occupied and if something unexpected happens in orbit, station maintenance and upkeep must continue.

    If a spacecraft cannot continue its work, having two low-Earth orbit providers rather than one would provide greater flexibility. In a press conference on March 22, Dana Weigel, deputy manager of the ISS Program at NASA, cited a recent example. A micrometeoroid strike in December 2022 left a Russian Soyuz capsule defunct in space. But since Crew Dragon was in operation, other crews could fly up and back. NASA also had to depend on another country to return NASA astronaut Frank Rubio to Earth. Stranded until a rescue Russian Soyuz replaced it, Rubio wound up breaking the record for longest single spaceflight in U.S. history, at 371 days.

    It’s a situation NASA hopes never to repeat. Starliner may soon be ready to answer the call.

    https://www.inverse.com/ }

    02-05-2024 om 22:04 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.FROM 186,000 MILES PER SECOND TO ZERO: SCIENTISTS USE PHOTONIC CRYSTAL TO STOP LIGHT IN ITS TRACKS

    FROM 186,000 MILES PER SECOND TO ZERO: SCIENTISTS USE PHOTONIC CRYSTAL TO STOP LIGHT IN ITS TRACKS

    Researchers from the Institute for Atomic and Molecular Physics (AMOLF) in The Netherlands say they have shown that manipulating a two-dimensional material known as a photonic crystal can stop light in its tracks.

    Scientists have previously demonstrated the ability to trap light using powerful magnets. At the same time, other research showed the ability to halt individual electrons in two-dimensional materials like graphene by simulating the effects of magnetic fields. However, the AMOLF team is the first to use the unique properties of two-dimensional materials to stop light in its tracks without employing any magnetic fields.

    The researchers behind the novel accomplishment believe their work may open up several practical applications, ranging from sensing and on-chip routing to lasing and quantum light-matter interfaces.

    “This principle offers a new approach to slow down light fields and thereby enhance their strength,” explained AMOLF group leader Ewold Verhagen. “Realizing this on a chip is particularly important for many applications.”

    EXPLORING TWISTRONICS AND MAGIC ANGLES TO STOP LIGHT IN ITS TRACKS

    In their research, published in the journal Nature Photonics, the AMOLF team explains how the unique properties of two-dimensional materials allowed them such precise control over light waves. Sometimes referred to as “Twistronics,” researchers have found that simply deforming or “twisting” two-dimensional materials can create a number of unexpected and sometimes useful consequences.

    For example, researchers have been able to induce certain types of superconductivity by twisting a two-layered stack of graphene, which consists of two sheets of individual carbon atoms, to exactly 1.08 degrees. This so-called “magic angle” has offered hope that these types of materials may one day lead to functional, room-temperature superconductors.

    Of course, manipulating electrons, which have a charge, is completely different from manipulating individual light waves since they are essentially massless and do not possess an electromagnetic charge. As the researchers explain, “In electronic crystals, magnetic fields can be used to induce a multitude of unique phenomena; [however] the uncharged nature of photons necessitates alternative approaches to bring about similar control over photons at the nanoscale.”

    PHOTONIC CRYSTALS AND LANDAU LINES

    To successfully stop light in its tracks, the team tapped into a type of two-dimensional material known as a photonic crystal. Like graphene, this material is made up of individual atoms attached at their sides to create a two-dimensional sheet. However, the carbon used to make graphene is replaced with silicon, and the resulting two-dimensional sheet also contains a regular pattern of holes.

    “A photonic crystal normally consists of a regular—two–dimensional—pattern of holes in a silicon layer,” explained first author René Barczyk, who successfully defended his PhD thesis on this topic last year. Barczyk also noted that light can move freely in this material, “just like electrons in graphene.”

    “In general, graphene is a good electronic conductor, but this changes when the crystal array is deformed, for instance, by stretching it like elastics,” Verhagen explained. “Such mechanical deformation stops conduction; the material turns into an insulator, and consequently, the electrons are bound to Landau levels.”

    In effect, stretching the graphene had the same effect as applying a magnetic field, only without a magnet. Verhagen says that given how this artificial creation of these “Landau levels” controls the motion of electrons, his team wondered “if a similar approach would also work for photons.”

    Sure enough, after multiple experiments, the team found success. The twisting and stretching of the photonic crystals created the desired Landau levels, offering the ability to manipulate the flow of light through the material.

    “By playing with the deformation pattern, we even managed to establish various types of effective magnetic fields in one material,” Verhagen explained. “As a result, photons can move through certain parts of the material but not in others. Hence, these insights also provide new ways to steer light on a chip.”

    Perhaps more significantly, the process allowed the researchers to stop light in its tracks, offering a unique level of control over individual photons.

    “Breaking this regularity in exactly the right manner will deform the array and consequently lock the photons,” said Barczyk. “This is how we create Landau levels for photons.”

    PARTNERING WITH OTHER RESEARCHERS

    During their research, the team discovered that researchers from Pennsylvania State University and Columbia University were working on the same idea. While some aspects were different, the press release explains that “both teams were able to stop light waves from moving and observe Landau levels by deforming a two-dimensional photonic crystal.”

    “When we were doing our first measurements, I happened to speak to one of the authors of this other study,” said Verhagen. “When it turned out that they were also looking for experimental evidence of the effect, we decided not to compete in being first to publish but instead to submit the work simultaneously to the publisher.”

    The researchers believe that their new method for stopping light is a significant breakthrough. If harnessed correctly, it could also prove critical in several potential applications.

    “If we can confine light at the nanoscale and bring it to a halt like this, its strength will be enhanced tremendously,” said Verhagen. “And not only at one location but over the entire crystal surface. Such light concentration is very important in nanophotonic devices, for example, for the development of efficient lasers or quantum light sources.”

    • Christopher Plain is a Science Fiction and Fantasy novelist and Head Science Writer at The Debrief. Follow and connect with him on X, learn about his books at plainfiction.com, or email him directly at christopher@thedebrief.org.

    02-05-2024 om 21:53 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Insanely Detailed Webb Image of the Horsehead Nebula
    The NASA/ESA/CSA James Webb Space Telescope has captured the sharpest infrared images to date of one of the most distinctive objects in our skies, the Horsehead Nebula. The observations show a part of the iconic nebula in a whole new light, capturing its complexity with unprecedented spatial resolution.
    Image Credits: ESA/Euclid/Euclid Consortium/NASA, image processing by J.-C. Cuillandre (CEA Paris-Saclay), G. Anselmi, NASA, ESA, and the Hubble Heritage Team (AURA/STScI), ESA/Webb, CSA, K. Misselt, M. Zamani (ESA/Webb) LICENCE CC BY 4.0 INT or ESA Standard Licence

    Insanely Detailed Webb Image of the Horsehead Nebula

    Few space images are as iconic as those of the Horsehead Nebula. Its shape makes it instantly recognizable. Over the decades, a number of telescopes have captured its image, turning it into a sort of test case for a telescope’s power.

    The JWST has them all beat.

    The Horsehead Nebula is about 1300 light-years away in Orion. It’s part of the much larger Orion Molecular Cloud Complex. Horsehead is visible near the three stars in Orion’s Belt in a zoomed-in image

    The Horsehead Nebula is visible in this image of Orion's Belt. It's in the lower left, extending horizontally, to the lower left of the belt star Alnitak. Image Credit: By Davide De Martin (http://www.skyfactory.org); Credit: Digitized Sky Survey, ESA/ESO/NASA FITS Liberator - https://www.spacetelescope.org/projects/fits_liberator/fitsimages/davidedemartin_12/ (direct link), Public Domain, https://commons.wikimedia.org/w/index.php?curid=1329999

    The Horsehead Nebula is visible in this image of Orion’s Belt. It’s in the lower left, extending horizontally, to the lower left of the belt star Alnitak.
    Image Credit: By Davide De Martin (http://www.skyfactory.org);
    Credit: Digitized Sky Survey, ESA/ESO/NASA FITS Liberator – https://www.spacetelescope.org/projects/fits_liberator/fitsimages/davidedemartin_12/ (direct link),
    Public Domain, https://commons.wikimedia.org/w/index.php?curid=1329999

    The leading image shows JWST’s view of the Horsehead Nebula alongside two other views. The Euclid image was captured in November 2023. Euclid features a wide-angle, 600-megapixel camera, and its primary job is to measure the redshift of galaxies and the Universe’s expansion due to dark energy. It took Euclid about one hour to capture the image, showcasing the telescope’s ability to gather highly detailed images quickly.

    The Hubble captured its image in 2013 and was released as the telescope’s 23rd-anniversary featured image. The venerable Hubble does a good job of revealing structures hidden by dust. There’s nothing left to say about the Hubble that hasn’t been said already. It’s the revered elder among telescopes, and if you feel no reverence towards it, its contribution to science, and the people responsible for it, you may have a bad case of ennui.

    The third image is a new one from the JWST’s NIRCam instrument. It’s described as the sharpest image of the Horsehead ever taken. It shows a small part of the iconic nebula in detail we don’t usually see. The JWST is so powerful it even shows background galaxies.

    A zoom-in of the JWST image. Image Credit: ESA/Webb, CSA, K. Misselt, M. Zamani (ESA/Webb)
    A zoom-in of the JWST image. The detail is incredible.
    Image Credit: ESA/Webb, CSA, K. Misselt, M. Zamani (ESA/Webb)

    The Horsehead Nebula is the result of stellar erosion. The nebula itself was formed by a collapsing cloud of material, and a nearby hot star called Sigma Orionis illuminates the structure. The nebula is denser than its surrounding gas and has resisted the dissipative energy of the star, while the gas that used to surround it is long gone.

    This definitely isn’t the last we’ll see of Horsehead. New, powerful telescopes coming online soon, like the Giant Magellan Telescope and the European Extremely Large Telescope will likely take a crack at the nebula. Prepare to be wowed.

    There’s no rush. According to astronomers, the Horsehead Nebula will eventually be eroded away, too, but not for another five million years or so.

    The “mane” of the Horsehead Nebula

    The “mane” of the Horsehead Nebula is shown here imaged by Webb’s MIRI instrument. The mid-infrared light captured by MIRI reveals substances like dusty silicates and soot-like molecules called polycyclic aromatic hydrocarbons. 

    Credit: NASA, ESA, CSA, K. Misselt (University of Arizona) and A. Abergel (IAS/University Paris-Saclay, CNRS)

    Horsehead Nebula

    The Horsehead Nebula, imaged by the NIRCam instrument on NASA’s Webb Telescope, features a portion of the horse’s “mane” about 0.8 light-years wide. The blue clouds at the bottom of the image are dominated by cold, molecular hydrogen. Red wisps above the nebula represent mainly atomic hydrogen gas.

     Credit: NASA, ESA, CSA, K. Misselt (University of Arizona) and A. Abergel (IAS/University Paris-Saclay, CNRS)
    Horsehead Nebula

    The “mane” of the Horsehead Nebula is shown here imaged by Webb’s MIRI instrument. The mid-infrared light captured by MIRI reveals substances like dusty silicates and soot-like molecules called polycyclic aromatic hydrocarbons.

     Credit: ESA/Euclid/Euclid Consortium/NASA, image processing by J.-C. Cuillandre (CEA Paris-Saclay), G. Anselmi, NASA, ESA, and the Hubble Heritage Team (AURA/STScI), ESA/Webb, CSA, K. Misselt (University of Arizona), M. Zamani (ESA/Webb)

    https://www.universetoday.com/ }

    02-05-2024 om 17:45 geschreven door peter  

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    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.Earth Had a Magnetosphere 3.7 Billion Years Ago
    The magnetic field and electric currents in and around Earth generate complex forces that have immeasurable impact on every day life. The field can be thought of as a huge bubble -- called the magnetosphere -- protecting us from cosmic radiation and charged particles that bombard Earth in solar winds.
    Credit: ESA/ATG medialab

    Earth Had a Magnetosphere 3.7 Billion Years Ago

    We go about our daily lives sheltered under an invisible magnetic field generated deep inside Earth. It forms the magnetosphere, a region dominated by the magnetic field. Without that planetary protection shield, we’d experience harmful cosmic radiation and charged particles from the Sun.

    Has Earth always had this deflector shield? Probably so, and the evidence is in old rocks. A team of researchers at University of Oxford and MIT found the earliest evidence for its existence in stones found along the coast of Greenland in a region called the Isua Supercrustal Belt.

    Geologists have long known that iron particles in rocks “entrain” a print of the magnetic field that was in place when they formed. So, the research team uncovered rocks that formed some 3.7 billion years ago. It’s not an easy task, according to team lead Claire Nichols of the Department of Earth Sciences at Oxford. “Extracting reliable records from rocks this old is extremely challenging,” Nichols pointed out. “It was really exciting to see primary magnetic signals begin to emerge when we analyzed these samples in the lab. This is a really important step forward as we try and determine the role of the ancient magnetic field when life on Earth was first emerging.”

    This 3.7-billion-year-old rock from Greenland. Entrained magnetic field fingerprints help scientists determine that our magnetosphere and magnetic field existed when this rock formed.
    Courtesy: Claire Nichols.

    The team’s samples recorded a magnetic field strength of 15 microteslas at the time they formed. Today, Earth’s field strength is closer to 30 microteslas, so it’s obvious that our magnetic field and magnetosphere have been there for billions of years. It’s also clear that the field changes over time. The science team also found that early Earth’s magnetosphere was amazingly similar to the one it has today.

    Tracking Earth’s Magnetosphere through Time

    Our planet has a main dynamo at its heart. There are two cores—an inner one and an outer one. Motions in the core regions generate the magnetic field that defines our magnetosphere. Molten iron mixes and moves in the fluid outer core and the inner core solidifies. The two actions together create that dynamo. That’s what’s happening inside our planet today.

    This cutaway of planet Earth shows the familiar exterior of air, water and land as well as the interior: from the mantle down to the outer and inner cores. Currents in hot, liquid iron-nickel in the outer core create our planet's protective but fluctuating magnetic field and magnetosphere. Credit: Kelvinsong / Wikipedia
    This cutaway of planet Earth shows the familiar exterior of air, water and land as well as the interior: from the mantle down to the outer and inner cores. Currents in hot, liquid iron-nickel in the outer core create our planet’s protective but fluctuating magnetic field and magnetosphere.
    Credit: Kelvinsong / Wikipedia

    However, when Earth was first forming some 4.5 billion years ago, that solid inner core didn’t exist. Without the interaction we see today between the two parts of the core, it’s hard to know how any early magnetic field existed. That’s an open question among geologists and planetary scientists: how did it form and how was it sustained?

    Another question relates to how much the planetary magnetic field has varied over time. Answering that one would help geologists understand just when the solid inner core formed. It would also show how much heat has escaped our planet from deep inside over time. Heat escape drives plate tectonics, which uses large “plates” of rock to shift things around on the surface over hundreds of millions of years.

    What Do the Rocks Tell Us?

    Rocks have a long and complex history. They form as a molten mixture that solidifies, or in the case of sandstones, are laid down in layers that then harden. In the case of molten rocks, they have magnetic field fingerprints entrained at the time of formation. In measuring those fingerprints, geologists account for any heating that could “reset” the magnetic signatures over time. The Greenland rocks are relatively pristine, meaning they haven’t been significantly heated since they formed. That means their magnetic fingerprints haven’t changed since formation.

    Lava cooling after an eruption. This rock has an entrained magnetic field fingerprint from the time it formed. Credit: kalapanaculturaltours.com
    Lava cooling after an eruption. This rock has an entrained magnetic field fingerprint from the time it formed.
    Credit: kalapanaculturaltours.com

    Rocks also get weathered by wind, temperature changes and erosion, but the Isuan samples seem to be relatively pristine, according to Benjamin Weiss of MIT. “Northern Isua has the oldest known well-preserved rocks on Earth,” Weiss said. “Not only have they not been significantly heated since 3.7 billion years ago but they have also been scraped clean by the Greenland ice sheet.”

    Rocks Through Time

    The rocks the team studied date back to the Archean Eon—the second-oldest geologic eon in Earth’s history. That period began about 4 billion years ago, and during that time Earth was largely an ocean world with a limited amount of continental surface. Since then, Earth’s surface has changed a great deal, destroying or burying rocks from earlier times. So, finding rocks that date back that far in time is a big deal.

    The Isuan rocks are relatively unchanged since they formed, and bear proof of a magnetic field existing less than a billion years after the planet formed. That same early magnetic field could have played a role in the development of our planet’s atmosphere, by assisting in removing xenon gas. Other old rocks may well tell scientists more about the birth of the magnetic field. There are rocks in Canada, Australia and South Africa that could give unique insight into the formation of the field and its role in making Earth habitable for life.

    For More Information

    https://www.universetoday.com }

    02-05-2024 om 16:44 geschreven door peter  

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    01-05-2024
    Klik hier om een link te hebben waarmee u dit artikel later terug kunt lezen.CHINA IS PREPARING TO SEND ITS CHANG’E-6 SPACECRAFT TO EXPLORE THE FAR SIDE OF THE MOON

    Image: Pixabay

    CHINA IS PREPARING TO SEND ITS CHANG’E-6 SPACECRAFT TO EXPLORE THE FAR SIDE OF THE MOON

    China is reportedly preparing to deliver a robotic spacecraft to the Moon’s far side as part of a series of upcoming missions in advance of the country’s aims to establish a presence on the lounar Suth Pole.

    The forthcoming launch of China’s Chang’e-6, the nation’s second attempted sample return mission, is expected to occur this week. The mission, if successful, plans to retrieve what will be recognized as the first samples of soil and rock from the far side of the Moon.

    The mission plans to use the backup spacecraft from China’s first sample return mission, which occurred in 2020, marking the first successful retrieval of materials from the lunar surface in decades and another significant advancement in China’s exploration of space.

    The mission presents several technological hurdles and will require the assistance of the Quequao-2 relay satellite the country recently sent into lunar orbit, which will help to facilitate communications with the Chang’e-6 spacecraft from its position on the far side of the Moon.

    Chang'e
    Chang’e-5 spacecraft model on display at Zhuhai Aerospace Land
    (Credit: Shujianyang/CC 4.0).

    China plans to use Quequao-2 on future missions at least through the end of 2028, in advance of its exploration of the lunar South Pole that are expected to include the establishment of a lunar base, followed by crewed missions by the beginning of the next decade.

    China’s lunar ambitions are the foreign counterpart to NASA’s Artemis program, which currently plans to send astronauts back to the Moon. Following an initial pair of test missions, Artemis III will send astronauts back to the lunar surface by 2026, marking the time humans have walked on the lunar surface in more than half a century.

    Artemis III astronauts will similarly explore areas near the lunar South Pole, where NASA hopes they will be able to locate water and other resources that could be hidden in its permanently shadowed regions.

    Previously, the presence of ice was confirmed within craters near the Moon’s poles by India’s Chandrayaan-1 mission.

    If successful, the Chang’e-6 mission will place its spacecraft near the South Pole-Aitkin Basin, home to the oldest known crater that is presently known, where it will use a mechanical drill and a scooping instrument to collect samples that may be capable of revealing insights into the Moon’s origins, as well as the formation of the solar system.

    Prior to China’s successful sample return in 2020, samples collected during past lunar missions had all been retrieved from the near side of Earth’s natural satellite, either by the U.S. or during lunar explorations conducted by the Soviet Union.

    https://thedebrief.org/category/space/ }

    01-05-2024 om 00:27 geschreven door peter  

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    WELCOME TO THIS BLOG! I HOPE THAT YOU ENJOY THE LECTURE OF ALL ISSUES. If you did see a UFO, you can always mail it to us. Best wishes.

    Beste bezoeker,
    Heb je zelf al ooit een vreemde waarneming gedaan, laat dit dan even weten via email aan Frederick Delaere op
     www.ufomeldpunt.be. Deze onderzoekers behandelen jouw melding in volledige anonimiteit en met alle respect voor jouw privacy. Ze zijn kritisch, objectief  maar open minded aangelegd en zullen jou steeds een verklaring geven voor jouw waarneming!
    DUS AARZEL NIET, ALS JE EEN ANTWOORD OP JOUW VRAGEN WENST, CONTACTEER FREDERICK.
    BIJ VOORBAAT DANK...


    Laatste commentaren
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        op UFO'S FORM CROP CIRCLE IN LESS THAN 5 SECONDS - SCOTLAND 1996
  • crop cirkels (herman)
        op UFO'S FORM CROP CIRCLE IN LESS THAN 5 SECONDS - SCOTLAND 1996
  • Een zonnige vrijdag middag en avond (Patricia)
        op MUFON UFO Symposium with Greg Meholic: Advanced Propulsion For Interstellar Travel
  • Dropbox

    Druk op onderstaande knop om je bestand , jouw artikel naar mij te verzenden. INDIEN HET DE MOEITE WAARD IS, PLAATS IK HET OP DE BLOG ONDER DIVERSEN MET JOUW NAAM...


    Gastenboek
  • Nog een fijne avond
  • Hallo Lieverd
  • kiekeboe
  • Een goeie middag bezoekje
  • Zomaar een blogbezoekje

    Druk op onderstaande knop om een berichtje achter te laten in mijn gastenboek Alvast bedankt voor al jouw bezoekjes en jouw reacties. Nog een prettige dag verder!!!


    Over mijzelf
    Ik ben Pieter, en gebruik soms ook wel de schuilnaam Peter2011.
    Ik ben een man en woon in Linter (België) en mijn beroep is Ik ben op rust..
    Ik ben geboren op 18/10/1950 en ben nu dus 73 jaar jong.
    Mijn hobby's zijn: Ufologie en andere esoterische onderwerpen.
    Op deze blog vind je onder artikels, werk van mezelf. Mijn dank gaat ook naar André, Ingrid, Oliver, Paul, Vincent, Georges Filer en MUFON voor de bijdragen voor de verschillende categorieën... Veel leesplezier en geef je mening over deze blog.
    Zoeken in blog


    LINKS NAAR BEKENDE UFO-VERENIGINGEN - DEEL 1
  • http://www.ufonieuws.nl/
  • http://www.grenswetenschap.nl/
  • http://www.beamsinvestigations.org.uk/
  • http://www.mufon.com/
  • http://www.ufomeldpunt.be/
  • http://www.ufowijzer.nl/
  • http://www.ufoplaza.nl/
  • http://www.ufowereld.nl/
  • http://www.stantonfriedman.com/
  • http://ufo.start.be/

    LINKS NAAR BEKENDE UFO-VERENIGINGEN - DEEL 2
  • www.ufo.be
  • www.caelestia.be
  • ufo.startpagina.nl.
  • www.wszechocean.blogspot.com.
  • AsocCivil Unifa
  • UFO DISCLOSURE PROJECT

  • Startpagina !


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