Literature DB >> 17775158

Tracers determine movement of soil moisture and evapotranspiration.

U Zimmermann, K O Münnich, W Roether, W Kreutz, K Schubach, O Siegel.   

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.

Entities:  

Year:  1966        PMID： 17775158     DOI： 10.1126/science.152.3720.346

Source DB:  PubMed          Journal:  Science        ISSN： 0036-8075            Impact factor:   47.728


  4 in total

1.  [Isotope dating of ground water].

Authors:  K O Münnich
Journal:  Naturwissenschaften       Date:  1968-04

2.  Spatially Resolved Root Water Uptake Determination Using a Precise Soil Water Sensor.

Authors:  Dagmar van Dusschoten; Johannes Kochs; Christian W Kuppe; Viktor A Sydoruk; Valentin Couvreur; Daniel Pflugfelder; Johannes A Postma
Journal:  Plant Physiol       Date:  2020-09-04       Impact factor: 8.340

3.  Spatial variation of deuterium enrichment in bulk water of snowgum leaves.

Authors:  Jirí Santrucek; Jirí Kveton; Jirí Setlík; Lenka Bulícková
Journal:  Plant Physiol       Date:  2006-12-08       Impact factor: 8.340

4.  Prevalence and magnitude of groundwater use by vegetation: a global stable isotope meta-analysis.

Authors:  Jaivime Evaristo; Jeffrey J McDonnell
Journal:  Sci Rep       Date:  2017-03-10       Impact factor: 4.379
  4 in total

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