Related Experiment Video
Updated: Jul 12, 2026

09:38
Single-throughput Complementary High-resolution Analytical Techniques for Characterizing Complex Natural Organic Matter Mixtures
Published on: January 7, 2019
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.
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