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A recent study indicates that water on the lunar surface may come from the solar wind. Water—of most importance as rocket fuel—is present in lunar surface dust, or regolith, produced by meteoroids and charged particles impacting lunar rock. The researchers discovered that several of this graph had evidence of dampness, with between 200 and 300 parts per million of water and the molecule hydroxyl. The water and hydroxyl in the lunar graph were both low in deuterium, suggesting their hydrogen came from the sun, likely delivered to the moon by solar winds.

When the hydrogen particles interact with oxygen present in lunar surface rocks, water molecules arise. The results suggest that other airless bodies in the solar system may also have water on their surfaces, therefore highlighting the possibility of finding such water on the surface of other such objects.

NASA Confirms Solar Wind May Create Water on the Moon’s Surface

As per the report, it is claimed that scientists have hypothesised—since the 1960s—that the Sun is the source of elements generating water on the Moon. The idea is that water molecules would be produced by a chemical reaction set off by a stream of charged particles—the solar wind— slamming onto the lunar surface. NASA-led researchers have confirmed this prediction in the most realistic lab simulation of this process yet.

Given much of the water on the Moon is believed to be frozen in continuously shadowed areas at the poles, the result affects NASA’s Artemis astronaut activities near the South Pole.

Solar Wind Can Create Water on the Moon, NASA Lab Test Confirms

Constantly flowing from the sun, solar wind is mostly composed of protons—nuclei of hydrogen atoms deprived of their electrons. Our planet’s magnetic shield and atmosphere help most of the solar particles to avoid reaching the surface of Earth. But the Moon has no such protection. As computer models and lab experiments have shown, when protons smash into the Moon’s surface, which is made of a dusty and rocky material called regolith, they collide with electrons and recombine to form hydrogen atoms.

Scientists have discovered proof of both hydroxyl and water molecules beneath the moon’s surface. These molecules leave a chemical imprint that interacts with light on the regolith. Generally speaking, “water” refers to either one or a mix of both molecules since hydroxyl and water cannot be differentiated right now.

NASA astronaut Yeo and colleagues examined Apollo lunar samples using a customised tool employing two samples worth of dust. Their little particle accelerator battered the dust to create a copy of solar wind spanning many days.

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NASA Hubble Space Telescope Helps Confirm the First Solitary Black Hole

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NASA Hubble Space Telescope Helps Confirm the First Solitary Black Hole

For the first time, the existence of a lone black hole has been confirmed by scientists. This black hole has no star orbiting it. According to the statement by Kailash Sahu, astronomer at the Space Telescope Science Institute in Baltimore, “it’s the only one so far”. The discovery made headlines in the year 2022, when Sahu and his Team claimed a dark object was moving through the constellation Sagittarius. However, another team of researchers disputed the claims by identifying the object as a neutron star.

About the Discovery

This discovery came into the light three years ago. All the stellar-mass black holes are accompanied by stars that betray their presence and race around an invisible star, along with three times the sun’s mass. Such a procedure indicates the presence of black holes rather than a neutron star.

On the contrary, the solitary black holes are expected to be common, but are very hard to find. Likewise, the one in Sagittarius was identified while passing through the dim background star and additionally shifting its position due to the black hole’s gravity. Recently, Sahu’s efforts were reported in the Astrophysical Journal, about the new observations from NASA’s Hubble Space Telescope, confirming the presence of a lone black hole in Sagittarious.

Black Hole Key Findings

Although the passage occurred first in the year 2011, the original discovery relied on the Hubble measurements from the year 2011 to 2017. However, the new data has been gained from the Hubble observations from the year 2021 to 2022, accompanied by the data received from the Gaia Spacecraft.

How Big is a Black Hole?

The ideal size of this lone black home is seven times as huge as the sun. In recent observations, a different team of scientists revisited the project and identified the size as massive as six times that of the sun. The theories of the scientists match with that of Sahu’s observation.

The research continues for detecting the black holes in Sagittarius. Located at a distance of 5,000 light years away from Earth, this solitary black hole is yet to be observed from different aspects. The astronomer, Sahu, hopes to find more lone black holes with the effective use of the Nancy Grace Roman Space Telescope, which is set to launch in the year 2027.

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Mars’ Carbonate Mystery and Ancient Atmosphere Deciphered

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Mars’ Carbonate Mystery and Ancient Atmosphere Deciphered

The evolution of Mars and its ancient atmosphere has been a prominent research topic for scientists. NASA’s Curiosity Mars rover could potentially be the ultimate solution for the temperature and other details about the planet. As per the assumptions made by the researchers, Mars’s atmosphere was crafted with a thick layer of carbon dioxide whereas the surface comprised liquid water. Likewise, the presence of carbonate minerals on the planet would be the result of a potential reaction between water, carbon dioxide, and Martian rocks, researchers say.

Presence of Siderite Detected

Recently reported in the April paper of Science, the presence of siderite has been discovered within the sulfate-rich rocky layers of Mount Sharp on Mars. The discovery was made at three of Curiosity’s drill sites.

According to the lead author and Associate Professor at the University of Calgary, Canada, Benjamin Tutolo, “The discovery of abundant siderite in Gale Crater represents both a surprising and important breakthrough in our understanding of the geologic and atmospheric evolution of Mars”.

About the Drilling Process

To achieve an understanding of the chemical and mineral makeup at the surface of Mars, Curiosity drills three to four centimeters down into the subsurface. Further, the powdered rock samples are then dropped into the CheMin instrument. This instrument analyses the rocks and soil via X-ray diffraction. The CheMin instrument is driven by NASA’s Ames Research Centre in California’s Silicon Valley.

The data analysis of the discovery was conducted by scientists at the Astromaterials Research and Exploration Science (ARES) Division at NASA Johnson Space Center in Houston.

Potential Findings and Atmosphere at Mars

The discovery of this carbonate mineral could potentially be hiding other minerals beneath the surface, in near-infrared satellite analysis. The possible presence of carbonates in sulfate-rich layers across Mars may result in the amount of carbon dioxide, which will be ideal to support the liquid water and create conditions warm enough to sustain water. Also, the scientists doubt the existence of other carbonates, or maybe they might have vanished from space.

To Conclude

The missions and analyses are still undergoing, and they will continue the research in the future. The findings can be confirmed post-research on the sulfate-rice area on the red planet. As the findings arrive, they will help us understand the transformation of the planet and will offer clarity on the ancient atmosphere.

Note: Curiosity is a part of NASA’s Mars Exploration Program (MEP) portfolio. It was built by NASA’s Jet Propulsion Laboratory, managed by Caltech in Pasadena, California. The mission is successfully led by JPL on behalf of NASA’s Science Mission Directorate in Washington.

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JWST Might Have Revealed New Signs of Alien Life on Nearby Exoplanet

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JWST Might Have Revealed New Signs of Alien Life on Nearby Exoplanet

Scientists discovered suitable biosignature gases for alien life on planet K2-18b. On K2-18b, NASA’s James Webb Space Telescope (JWST) noticed dimethyl sulfide (DMS), a chemical primarily produced by living creatures on Earth. Notably, the exoplanet is nine times the size of our planet and exists in the habitable zone of its planetary system. As exoplanets pass in front of their home stars, the team probes planetary atmospheres using JWST’s Mid-Infrared Instrument (MIRI). Based on its size and other properties, astronomers think K2-18b is a “Hycean” world—that is, one with a large liquid-water ocean and a hydrogen-rich atmosphere.

Although the researchers estimate concentrations of more than 10 parts per million by volume on Earth, they are less than one part per billion. However, further research is required to confirm and expand on their findings.

NASA’s Webb Telescope Finds Possible Life Signs on Exoplanet K2-18b

According to a new study, which was published in The Astrophysical Journal Letters, chemical proof of life on the far-off exoplanet K2-18b has come from NASA’s James Webb Space Telescope. Rare on other planets or moons, these signals, which point to the presence of dimethyl sulfide and dimethyl disulfide, are found in marine plants and bacteria on Earth.

Because K2-18b boasts a hydrogen-rich atmosphere and a planet-wide ocean, researchers classify it as a “hycean world.” Methane and carbon dioxide, found in the planet’s atmosphere in 2023, were the first carbon-based compounds found in the habitable zone of an exoplanet. Though the levels had minimal statistical significance, the researchers also found likely DMS signals, therefore confounding DMS diagnosis. The results underline the possibilities of life on exoplanets.

JWST Data Hints at High Sulfur Levels on Exoplanet, Life or Not

MIRI observations from the JWST expose features in planetary atmospheres that point to DMS or DMDS helping to explain them. Scientists estimate that atmospheric DMS and DMDS levels could be substantially greater than on Earth, that is, above 10 parts per million. Differentiating DMS from DMDS requires more data. Scientists want to investigate undiscovered chemical processes involving no living entities able to generate DMS and DMDS from nothing.

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