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Reproducing sediment transport conditions on Mars, P. Claudin and co-workers show that at very low pressure, a new grain movement regime appears, compatible with the observations made on the Red Planet.
Reproducing sediment transport conditions on Mars, P. Claudin and co-workers show that at very low pressure, a new grain movement regime appears, compatible with the observations made on the Red Planet.
Researchers from CNRS, ESPCI Paris, and Saint-Gobain used a 3D imaging technique of X-ray micro-tomography to follow the evolution of a mixture (...)
Dew condensing on an inclined, grooved surface rapidly forms large drops that roll quickly to the bottom for collection. Collecting dew could (...)
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