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Tracers determine movement of soil moisture and evapotranspiration

U Zimmermann, K O Münnich, W Roether

    Science (New York, N.Y.)
    |April 15, 1966
    PubMed

    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.

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