Mystery over ‘strange giant spiders’ found on Mars finally solved after scientists ‘recreate red planet in a barrel’ --[Reported by Umva mag]

SCARS on the red planet’s surface have baffled scientists for decades – but an explanation may lie in their recreation of Mars in a barrel. The spider-like geologic formations have been known to scientists since Mars orbiters returned images in 2003. NASA / JPL-Caltech / University of ArizonaSpider-like features called araneiform terrain are pictured in the southern hemisphere of Mars[/caption] However, the spindly structures appear only on the planet’s southern hemisphere. Dubbed araneiform terrain, they can stretch more than a half mile from end to end, with hundreds of branched “legs.” The leading theory says the structures were created by carbon dioxide ice, a substance that couldn’t be found on Earth – until now. A team of Nasa scientists recreated Mars-like conditions on Earth to simulate the process. Their findings were published yesterday in The Planetary Science Journal. The study supports processes detailed by the Kieffer model, a widely accepted explanation for seasonal changes on the Mars surface. According to the theory, sunlight heats the Martian soil when it shines through slabs of carbon dioxide ice that build up on the Martian surface each winter. The soil absorbs the heat and causes nearby ice to turn directly into carbon dioxide gas without becoming liquid first – a process known as sublimation. As pressure builds, the Martian ice splinters, allowing the gas to escape. It travels upwards, carrying a stream of dark dust and sand that lands on the surface of the ice. When seasons change and the remaining ice turns to gas, the spiderlike formations remain. This is, of course, according to theory – leaving Nasa scientists with the momentous task of proving it was possible. The researchers knew they had to recreate the red planet’s low air pressure and temperatures around negative 301 degrees Fahrenheit (negative 185 degrees Celsius). Luckily, a test chamber at Nasa‘s Jet Propulsion Laboratory was perfectly suited for the task. The barrel-sized device is called the Dirty Under-vacuum Simulation Testbed for Icy Environments, but scientists know it by its nickname, DUSTIE. The researchers chilled Martian soil simulant in a container submerged within a liquid nitrogen bath. They placed it in the DUSTIE chamber, where the air pressure was reduced to mirror the red planet’s southern hemisphere. NASA / JPL-CaltechThe Dirty Under-vacuum Simulation Testbed for Icy Environments (DUSTIE) is a barrel-size chamber that can recreate conditions on the red planet[/caption] Carbon dioxide filled the chamber and turned from gas to ice over the next three to five hours. After several attempts, the team achieved the necessary conditions for thick, translucent ice. A heater was set inside the chamber to warm the simulant from below, melting the ice. Lead author Lauren Mc Keown recalled her shock when a dark plume of carbon dioxide gas emerged. “It was late on a Friday evening and the lab manager burst in after hearing me shrieking,” Mc Keown said. “She thought there had been an accident.” NASA / JPL-CaltechResearchers were able to recreate spindly structures in their simulation[/caption] The pressurized gas tore holes in the simulant as it was expelled, scattering debris. The team noticed how ice formed between the simulant grains before cracking it open – a possibility excluded from the Kieffer model. Future experiments will simulate sunlight from above, rather than below, to narrow down the conditions under which “spiders” form. Bigger questions – including whether the scars are vestiges of a different time and climate – must go unanswered for now. NASA / JPL-Caltech / University of ArizonaDark spots seen in araneiform terrain were captured by NASA’s Mars Reconnaissance Orbiter[/caption] Although the Curiosity and Perseverance rovers are trekking across Mars, they are far from the southern hemisphere. Conditions on the red planet’s hemispheres are notoriously harsh. The Phoenix lander, which touched down in the north, only lasted a few months before succumbing to the limited sunlight and punishing chill. Mars facts Here's what you need to know about the red planet... Mars is the fourth planet from the Sun It is named after the Roman god of war The landmass of Mars is very similar to Earth but due to the difference in gravity you could jump three times higher there than you can here Mars is mountainous and hosts the tallest mountain known in the Solar System called Olympus Mons, which is three times higher than Everest Mars is considered to be the second most habitable planet after Earth It takes the planet 687 Earth days to orbit the Sun The planet has a diameter of 4,212 miles, and has an average distance from Earth of 140 million miles M

Sep 19, 2024 - 18:34

Mystery over ‘strange giant spiders’ found on Mars finally solved after scientists ‘recreate red planet in a barrel’ --[Reported by Umva mag]

SCARS on the red planet’s surface have baffled scientists for decades – but an explanation may lie in their recreation of Mars in a barrel.

The spider-like geologic formations have been known to scientists since Mars orbiters returned images in 2003.

a close up of a brown surface with holes in it

Spider-like features called araneiform terrain are pictured in the southern hemisphere of Mars[/caption]

However, the spindly structures appear only on the planet’s southern hemisphere.

Dubbed araneiform terrain, they can stretch more than a half mile from end to end, with hundreds of branched “legs.”

The leading theory says the structures were created by carbon dioxide ice, a substance that couldn’t be found on Earth – until now.

A team of Nasa scientists recreated Mars-like conditions on Earth to simulate the process. Their findings were published yesterday in The Planetary Science Journal.

The study supports processes detailed by the Kieffer model, a widely accepted explanation for seasonal changes on the Mars surface.

According to the theory, sunlight heats the Martian soil when it shines through slabs of carbon dioxide ice that build up on the Martian surface each winter.

The soil absorbs the heat and causes nearby ice to turn directly into carbon dioxide gas without becoming liquid first – a process known as sublimation.

As pressure builds, the Martian ice splinters, allowing the gas to escape. It travels upwards, carrying a stream of dark dust and sand that lands on the surface of the ice.

When seasons change and the remaining ice turns to gas, the spiderlike formations remain.

This is, of course, according to theory – leaving Nasa scientists with the momentous task of proving it was possible.

The researchers knew they had to recreate the red planet’s low air pressure and temperatures around negative 301 degrees Fahrenheit (negative 185 degrees Celsius).

Luckily, a test chamber at Nasa‘s Jet Propulsion Laboratory was perfectly suited for the task.

The barrel-sized device is called the Dirty Under-vacuum Simulation Testbed for Icy Environments, but scientists know it by its nickname, DUSTIE.

The researchers chilled Martian soil simulant in a container submerged within a liquid nitrogen bath.

They placed it in the DUSTIE chamber, where the air pressure was reduced to mirror the red planet’s southern hemisphere.

the inside of a vacuum chamber with a box on a table

The Dirty Under-vacuum Simulation Testbed for Icy Environments (DUSTIE) is a barrel-size chamber that can recreate conditions on the red planet[/caption]

Carbon dioxide filled the chamber and turned from gas to ice over the next three to five hours.

After several attempts, the team achieved the necessary conditions for thick, translucent ice. A heater was set inside the chamber to warm the simulant from below, melting the ice.

Lead author Lauren Mc Keown recalled her shock when a dark plume of carbon dioxide gas emerged.

“It was late on a Friday evening and the lab manager burst in after hearing me shrieking,” Mc Keown said. “She thought there had been an accident.”

Researchers were able to recreate spindly structures in their simulation[/caption]

The pressurized gas tore holes in the simulant as it was expelled, scattering debris.

The team noticed how ice formed between the simulant grains before cracking it open – a possibility excluded from the Kieffer model.

Future experiments will simulate sunlight from above, rather than below, to narrow down the conditions under which “spiders” form.

Bigger questions – including whether the scars are vestiges of a different time and climate – must go unanswered for now.

Dark spots seen in araneiform terrain were captured by NASA’s Mars Reconnaissance Orbiter[/caption]

Although the Curiosity and Perseverance rovers are trekking across Mars, they are far from the southern hemisphere.

Conditions on the red planet’s hemispheres are notoriously harsh.

The Phoenix lander, which touched down in the north, only lasted a few months before succumbing to the limited sunlight and punishing chill.

Mars facts

Here's what you need to know about the red planet...

Mars is the fourth planet from the Sun
It is named after the Roman god of war
The landmass of Mars is very similar to Earth but due to the difference in gravity you could jump three times higher there than you can here
Mars is mountainous and hosts the tallest mountain known in the Solar System called Olympus Mons, which is three times higher than Everest
Mars is considered to be the second most habitable planet after Earth
It takes the planet 687 Earth days to orbit the Sun
The planet has a diameter of 4,212 miles, and has an average distance from Earth of 140 million miles
Martian temperatures can vary wildly, reaching as high as 70F/20C or as low as -225F/-153C

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