| Literature DB >> 17792056 |
D M Anderson, E S Gaffney, P F Low.
Abstract
The hypothesis that the Martian wave of darkening might be a frostheaving phenomenon has been examined. Consideration of the water-vapor sorption characteristics of a silicate mineral surface at temperatures below freezing leads to the conclusion that, without strongly deliquescent salts to attract and retain liquid water in the Martian soil, frost-heaving phenomena are not to be expected on Mars. On the other hand frost-heaving phenomena involving the freezing and thawing of ammonia may be common in the soils of Jupiter.Entities:
Year: 1967 PMID: 17792056 DOI: 10.1126/science.155.3760.319
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728