| Literature DB >> 17748119 |
Abstract
Two measurements of the temperature gradient in salt-marsh peat made at an interval of (1/2) year permit the upward flow of heat to be estimated as 1.37 x 10(-6) cal cm(-2) sec(-1). This value corresponds closely to the average terrestrial heat flow, obtained in mines and wells.Entities:
Year: 1965 PMID： 17748119 DOI： 10.1126/science.148.3674.1219
Source DB: PubMed Journal: Science ISSN： 0036-8075 Impact factor: 47.728