| Literature DB >> 17781576 |
R A Robie, B S Hemingway, W H Wilson.
Abstract
The specific heats of lunar samples 10057 and 10084 returned by the Apollo 11 mission have been measured between 90 and 350 degrees Kelvin by use of an adiabatic calorimeter. The samples are representative of type A vesicular basalt-like rocks and of finely divided lunar soil. The specific heat of these materials changes smoothly from about 0.06 calorie per gram per degree at 90 degrees Kelvin to about 0.2 calorie per gram per degree at 350 degrees Kelvin. The thermal parameter gamma=(kpC-(1/2) for the lunar surface will accordingly vary by a factor of about 2 between lunar noon and midnight.Year: 1970 PMID: 17781576 DOI: 10.1126/science.167.3918.749
Source DB: PubMed Journal: Science ISSN: 0036-8075 Impact factor: 47.728