Articles | Volume 15, issue 5
https://doi.org/10.5194/hess-15-1629-2011
https://doi.org/10.5194/hess-15-1629-2011
Research article
 | 
27 May 2011
Research article |  | 27 May 2011

Capillary rise quantifications based on in-situ artificial deuterium peak displacement and laboratory soil characterization

O. Grünberger, J. L. Michelot, L. Bouchaou, P. Macaigne, Y. Hsissou, and C. Hammecker

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Subject: Vadose Zone Hydrology | Techniques and Approaches: Instruments and observation techniques
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Cited articles

Allison, G. B.: The relationship between 18O and Deuterium in water and sand columns undergoing evaporation, J. Hydrol., 55, 163–169, 1982.
Barnes, C. J. and Allison, G. B. : The distribution of deuterium and 18O in dry soils 1. Theory, J. Hydrol., 60, 141–156, 1983.
Barnes, C. J. and Allison, G. B.,: The distribution of deuterium and 18O in dry soils.3-Theory for non isothermal water movement, J. Hydrol., 74, 119–135, 1984.
Barnes, C. J. and Allison, G. B.: Tracing of water movement in the unsatured zone using stable isotopes of hydrogen and oxygen, J. Hydrol. 100, 143–176, 1988.
Barnes, C. J. and Hughes, M. W.: The use of natural tracers as indicators of soil water movement in a temperate semi arid region, J. Hydrol., 60, 157–173, 1983.
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