Tracers Determine Movement of Soil Moisture and Evapotranspiration
- 15 April 1966
- journal article
- research article
- Published by American Association for the Advancement of Science (AAAS) in Science
- Vol. 152 (3720), 346-347
- https://doi.org/10.1126/science.152.3720.346
Abstract
The downward movement of water in soil is a layered one. Marking a certain layer with hydrogen-isotope tracer, and watching its displacement, makes possible a water balance and gives information on evaporation and groundwater recharge.This publication has 1 reference indexed in Scilit:
- Über den Deuterium-Gehalt von Niederschlags- und GrundwasserThe Science of Nature, 1963