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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.
P. Claudin, H. Jarry, G. Vignoles, M. Plapp, and B. Andreotti, Phys. Rev. E 92, 033015 (2015) - Snow penitentes form in sublimation conditions by (...)
Le 29 novembre 2016, l’École Supérieure de Physique et de Chimie Industrielles de la Ville de Paris – ESPCI Paris – a attribué le Titre de ESPCI Paris (...)
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