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Between now and the mid-2030s, multiple space agencies hope to send crewed missions to the Moon. of These plans all involve establishing bases around the Moon’s southern polar region, including the Artemis Base Camp and the International Lunar Research Station (ILRS). These facilities will enable a “sustained program of lunar exploration and development,” according to the NASA Artemis Program mission statement. In all cases, plans for building facilities on the surface call for a process known as In-Situ Resource Utilization (ISRU), where local resources are used as building materials.

This presents a bit of a problem since not all lunar soil (regolith) is well-suited for construction. Much like engineering and construction projects here on Earth, builders need to know what type of soil they are building on and if it can be used to make concrete. In a recent study, geologist Kevin M. Cannon proposed a lunar soil classification scheme for space resource utilization. This could have significant implications for future missions to the Moon, where it would help inform the construction of bases, habitats, and other facilities based on soil type and location.

Dr. Cannon is an assistant professor at the Department of Geology and Geological Engineering and Space Resources Program at the Colorado School of Mines, an engineering university in Golden, Colorado. His research is focused on the role geologic processes play in the formation and evolution of planetary materials on the surfaces of different bodies in the Solar System. The paper that describes his proposed scheme, “A lunar soil classification system for space resource utilization,” recently appeared in the journal Planetary and Space Science.

Multi dome base being constructed fullwidth 1
Multi-dome lunar base being constructed, based on the 3D printing concept. Credits: ESA/Foster + Partners

For space agencies, ISRU comes down to harvesting local resources to create building materials and provide for the crews’ basic needs (water, air, fuel, etc.). This reduces the amount of prefabricated components or materials that need to be launched into space, dramatically reducing costs in the process. For years, NASA, the ESA, and other space agencies have investigated how lunar regolith could be used as feedstock for 3D printers. Combined with a bonding agent or sintered to produce a molten ceramic, this regolith could then be “printed” onto inflatable modules to create various facilities.

Thanks to soil analysis and sample return missions conducted by robotic missions and the Apollo astronauts, scientists have learned a great deal about the composition of soil on the Moon. In particular, they learned that (like soils here on Earth) the composition varies from one location to another. “In any construction project on Earth, you’d want to know what kind of ground you’re building on,” explained Cannon via email. “The same will almost certainly be true on the Moon, and it helps to have a consistent scheme for one person to describe a soil to another.”

Here on Earth, soil classification schemes are used for everything from construction and civil engineering projects to environmental science. Soil types can also influence keep considerations, like how deep a foundation is needed depending on what is being built or what the slope should be on a highway embankment. However, these schemes do not apply to the lunar environment:

“Soil classifications on Earth are largely based on how ‘plastic’ the soil is due to clays and water, and often you get sorting that happens where for example a soil is mostly coarse gravel or mostly fine silt. On the Moon there are no clays, the soils are completely dry, and almost everywhere you have an even blend of different particle sizes. So the systems we use terrestrially really just don’t transfer.”

In addition, there are also the formation mechanisms, which are significantly different on the Moon. Whereas soil on Earth results from “weathering” (erosion) by water and wind, lunar regolith was created by a combination of volcanic activity and a long history of impacts by asteroids, meteoroids, and micrometeoroids.
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How Do Lava Worlds Become Earth-Like, Living Planets?

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September 27, 2023

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Earth was once entirely molten. Planetary scientists call this phase in a planet’s evolution a magma ocean, and Earth may have had more than one magma ocean phase. Earth cooled and, over 4.5 billion years, became the vibrant, life-supporting world it is today.

Can the same thing happen to exo-lava worlds? Can studying them shed light on Earth’s transition?

Planet-hunters like the Kepler Spacecraft and TESS have found thousands of worlds around other stars. Many of these worlds orbit their stars very closely, so close that they’re heated to extreme temperatures. A lot of these planets are gas giants, but a significant number are rocky, and the extreme heat keeps them molten, or at least partially molten. At least half of these super-heated rocky worlds are capable of maintaining magma on their surfaces.

There’s nothing like a lava world in our Solar System. The closest is Jupiter’s moon Io. But it’s volcanically active, which isn’t the same as a magma ocean. Studying lava worlds gives scientists a glimpse into Earth’s molten past, and luckily, they’re not hard to find.

A new study looked at hot rocky super-Earths, how their magma oceans affect our observations, and how they also influence their evolutionary paths.

The study is “Fizzy Super-Earths: Impacts of Magma Composition on the Bulk Density and Structure of Lava Worlds,” and it was published in The Astrophysical Journal. The lead author is Kiersten Boley, a graduate student in astronomy at The Ohio State University.

“When planets initially form, particularly for rocky terrestrial planets, they go through a magma ocean stage as they’re cooling down,” said Boley. “So lava worlds can give us some insight into what may have happened in the evolution of nearly any terrestrial planet.”

“Being able to trap a lot of volatile elements within their mantles could have greater implications for habitability.”

Kiersten Boley, lead author, Ohio State University.

The team used exoplanet modelling software to simulate Super-Earths that orbit their stars very closely. These planets are called ultra-short period (USP) planets. They simulated multiple evolutionary pathways for a planet similar to Earth but with surface temperatures between 2600 and 3860 F (1426 and 2126 C.) Within this range, a planet’s solid mantle would melt into magma depending largely on its composition.

Their work produced three classes of magma oceans, each with different mantle structures: a mantle magma ocean, a surface magma ocean, and one consisting of a surface magma ocean, a solid rock layer, and a basal magma ocean.

This figure from the study shows the three types of mantle structures in the simulations. The researchers found that the mantle may be a mantle magma ocean, a surface magma ocean and solid rock layer, or a MOSMO structure (i.e., Surface Magma Ocean (MO)–Solid Rock Layer (S)–Basal Magma Ocean (MO)). Image Credit: Boley et al. 2023.
This figure from the study shows the three types of mantle structures in the simulations. The researchers found that the mantle may be a mantle magma ocean, a surface magma ocean and solid rock layer, or a MOSMO structure (i.e., Surface Magma Ocean (MO)–Solid Rock Layer (S)–Basal Magma Ocean (MO)). Image Credit: Boley et al. 2023.

The research shows that mantle magma ocean planets are less common than the other two, but not by much. But when it comes to evolutionary pathways that might lead to habitable planets, it’s the planet’s composition that’s more important than its mantle structure. In lava worlds without atmospheres, the composition dictates how effective the magma is at trapping volatiles. That’s critical when it comes to life as we know it.

For a planet to one day express life, it needs an atmosphere with critical components like carbon and oxygen. Earth life is based on carbon, and oxygen is key to complex life here on Earth. So a magma planet with ample carbon and oxygen in its magma could eventually off-gas these critical materials into a planet’s burgeoning atmosphere if it held onto one.

Water, as we all know, is also critical to life, and some of the simulated planets had massive reserves of water. According to the study, a basal magma planet four times more massive than Earth—a
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Day Has Returned, but India’s Lander and Rover have Failed to Wake Up

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September 27, 2023

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India Moon Rover Traverse

It looks like India’s Chandrayaan-3 succumbed to the cold, and its mission is over. The frigid lunar night lasted about two weeks, and a new day has dawned. With that day came hopes of a sunlit revival for the lander and the rover, but the India Space Research Organization (ISRO) says the chances of the spacecraft awakening in the Sun are diminishing by the hour.

The lunar night that wrapped its cold arms around the lander and rover lasted 14 days, and so will the current lunar day. When the day dawned last Friday, ISRO began trying to communicate with the lander. There’s been no response so far, as both explorers may be forever entombed about 600km (373 mi) from the Moon’s south pole.

Even though things don’t look good for the mission, it’s still a success. It’s the first spacecraft to land in the Moon’s south pole region. The area is critical because it contains vast quantities of frozen water in its permanently shadowed crater. That water is a valuable resource for astronauts who’ll visit the Moon in the future and set up bases. It’s also the first time ISRO successfully landed a rover and lander on the Moon after its predecessor, Chandrayaan-2, crashed into the surface.

But it’s encouraging that Vikram and Pragyaan are still intact. ISRO hoped that the Sun would bring both back to life after the agency put them into sleep mode as night fell. There’s a chance that the sunlight would recharge the batteries.

“Once there is sufficient solar generation, they are expected to come back to life provided that they have survived the night.”

M Srikanth, Chandrayaan-3 Mission Operations Director.

ISRO released an update on Friday, the beginning of the new lunar day. Unfortunately, there was no response from either the lander or the rover.

Chandrayaan-3 Mission:
Efforts have been made to establish communication with the Vikram lander and Pragyan rover to ascertain their wake-up condition.

As of now, no signals have been received from them.

Efforts to establish contact will continue.

— ISRO (@isro) September 22, 2023

When night falls on the Moon’s south pole, temperatures plummet as low as -200C to -250C (-328F to -418F.) The lander and rover were never designed to handle these temperatures. The rover has only a small battery—10 amp-hours—that provides the necessary power to deploy its solar array. It was also included to help the rover survive a periodic eclipse. The small battery was fully charged when night came, and the solar panels were positioned to receive incoming starlight when morning came. The Vikram lander was also ready for the morning, and its 62.5 amp hour was fully charged.

Both vehicles are pre-programmed to come back to life as the Sun reappears. “When sunlight comes back, there’s an autonomous logic pre-loaded on both the lander and rover,” said M Srikanth, Chandrayaan-3 Mission Operations Director, in an interview with the Times of India. “Once there is sufficient solar generation, they are expected to come back to life provided that they have survived the night.”

If ISRO's Chandrayaan-3 mission is truly over, it was still a success. It was the first spacecraft to land at the Moon's south pole region. Image Credit: ISRO
If ISRO’s Chandrayaan-3 mission is truly over, it was still a success. It was the first spacecraft to land at the Moon’s south pole region. Image Credit: ISRO

But according to Isro chief AS Kiran Kumar, the “chances of reawakening are dimming with each passing hour.” In an interview with the BBC, Kumar added, “The lander and rover have so many components which may not have survived the frigid temperatures on the Moon.” In fairness, they were never designed to.

It’s all up to the lander’s transmitter now. It’s ISRO’s link with the mission, and if it won’t function, it won’t matter if some of the spacecraft’s other systems are somehow still working. “It has to tell us that it’s alive. Even if all other sub-systems work, we have no way of knowing that,” Kumar added.

Some of ISRO’s hopefulness is based on China’s successful Chang’e 4 mission. It landed on the lunar far side and was plunged into darkness and freezing temperatures, too. It woke up with the sunrise more than once.
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Review: Patagonia R1 Air Full-Zip Hoody

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1 day ago

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September 27, 2023

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Tet19 047 Me on Teton Crest Trail copy cropped 8

Hooded Fleece Jacket
Patagonia R1 Air Full-Zip Hoody
$179, 12.5 oz./354g (men’s medium)
Sizes: men’s XS-XXL, women’s XXS-XL, kids XS-XXL
backcountry.com

As I’ve repeatedly written at this blog, virtually no piece of outdoor apparel offers more versatility than a highly breathable, midweight insulation layer; arguably, the only “layer” you will wear more is your skin. Find a highly breathable midweight jacket that’s soft and fits like it was custom made for your torso and you have a winner. Patagonia’s R1 Air Full-Zip Hoody could play that role for almost any outdoor user, from hard-core backpackers, climbers, and backcountry skiers to the average dayhiker and fitness walker, as I found wearing it on backpacking trips in Glacier National Park and the Canadian Rockies, not to mention countless days around town and at home.

At 12.5 ounces/354 grams (men’s medium), this midweight fleece is designed for wearing as an outer or middle layer in a huge range of cool to cold temperatures, including activities and seasons as diverse as hiking or climbing in virtually any mountains in any month of the year, southern climes from fall through spring, or for any winter activity—skiing, hiking, running, walking, you pick.

Tet19 047 Me on Teton Crest Trail copy cropped 9
Hi, I’m Michael Lanza, creator of The Big Outside. Click here to sign up for my FREE email newsletter. Join The Big Outside to get full access to all of my blog’s stories. Click here for my e-guides to classic backpacking trips. Click here to learn how I can help you plan your next trip.

The Patagonia R1 Air Full-Zip Hoody.
” data-image-caption=”The Patagonia R1 Air Full-Zip Hoody.
” data-medium-file=”https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?fit=300%2C200&ssl=1″ data-large-file=”https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?fit=900%2C600&ssl=1″ src=”https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?resize=900%2C600&ssl=1″ alt=”The Patagonia R1 Air Full-Zip Hoody.” class=”wp-image-60252″ srcset=”https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?resize=1024%2C683&ssl=1 1024w, https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?resize=300%2C200&ssl=1 300w, https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?resize=768%2C512&ssl=1 768w, https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?resize=150%2C100&ssl=1 150w, https://i0.wp.com/thebigoutside.com/wp-content/uploads/2023/09/Patagonia-R1-Air-Full-Zip-Hoody.jpg?w=1200&ssl=1 1200w” sizes=”(max-width: 900px) 100vw, 900px” data-recalc-dims=”1″ />The Patagonia R1 Air Full-Zip Hoody.

It kept me warm without overheating—rarely even breaking a sweat—wearing it over one base layer while hiking with a full pack, uphill and downhill, on cool, generally calm mornings and some windy afternoons during a weeklong, nearly 70-mile September backpacking trip in Glacier National Park, and hiking in chilly, very strong wind on three-day hikes on both the Skyline Trail in Jasper National Park and the Nigel, Cataract, and Cline Passes Route in the White Goat Wilderness of the Canadian Rockies in the first week of August.

On those backpacking trips, I also wore it in camp both as an outer layer and, when temps dropped, under a down jacket—meaning the R1 Air Hoody doubled as an on-trail layer and a camp layer that allowed me to bring a lighter puffy and forego a midweight, long-sleeve shirt. To frame it another way: The R1 Air Hoody cut my layering system weight by replacing or reducing two other layers. Few pieces of apparel offer more versatility while reducing your pack weight.

I also wore it on breezy, cool evenings in the 50s between waves of thunderstorms
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