Page 5: Research news on regolith

Regolith is the unconsolidated, heterogeneous layer of fragmented mineral and rock material that overlies coherent bedrock on planetary surfaces, including Earth, the Moon, Mars, asteroids, and other solid bodies. As a substance, it comprises varying proportions of rock fragments, mineral grains, dust, ice, and, on some planets, secondary alteration products such as clays or salts. Regolith forms primarily through mechanical and chemical weathering, impact comminution, and volcanic or sedimentary processes, and its physical properties—such as grain size distribution, porosity, cohesion, and volatile content—critically influence surface-atmosphere interactions, geotechnical behavior, resource potential, and the performance of in situ exploration and construction activities.

Adsorptive regolith on Mars soaks up water, updated model shows

Mars, the next frontier in space exploration, still poses many questions for scientists. The planet was once more hospitable, characterized by a warm and wet climate with liquid oceans. But today Mars is cold and dry, with ...

Burrowing mole-bot could characterize other planets' soil

Burrowing under soil opens up a whole new world, especially when that soil is on other planets. Getting under the top layer of regolith on a world such as Mars could give access to a world still extant with life, whereas, ...

Building concrete on Mars from local materials

Imagine you've just gotten to Mars as part of the first contingent of settlers. Your first challenge: build a long-term habitat using local materials. Those might include water from the polar caps mixed with specific surface ...

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