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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.
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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