The quantitative evaluation of groundwater recharge rate using Displacement Flow Model with stable isotope ratio in the soil water of difference vegetation cover-Reference-Cited by-同舟云学术

The quantitative evaluation of groundwater recharge rate using Displacement Flow Model with stable isotope ratio in the soil water of difference vegetation cover

Published:2016 Issue:1 Volume:58 Page:31-45
ISSN:0913-4182
Container-title:Journal of Groundwater Hydrology
language:en
Short-container-title:Journal of Groundwater Hydrology

Author:

KUDO Keishi¹,SHIMADA Jun²,MARUYAMA Atsushi³,TANAKA Nobuhiro⁴

Affiliation:

1. Kokusai Kogyo Co., Ltd.

2. Graduate School of Science and Technology, Kumamoto University

3. National Agriculture and Food Research Organization

4. Kumamoto Prefectural Office

Publisher

Japanese Association of Groundwater Hydrology

Subject

General Medicine

Link

https://www.jstage.jst.go.jp/article/jagh/58/1/58_31/_pdf

Reference17 articles.

1. Andersen, J. and T. Sevel (1974): Six years environmental tritium profiles in the unsaturated zones. Grønhøj, Denmark. Isotope Techniques in Groundwater Hydrology 1, IAEA Vienna, 3-20.

2. Barnes, C.J. and J.V. Turner (1998): Isotopic exchange in soil water. Isotope Tracers in Catchment Hydrology, Kendall, C., McDonnell, J.J. (eds), Elsevier, 137-163.

3. Dansgaard, W. (1964): Stable isotopes in precipitation. Tellus, 16, 436-468.

4. Gehre, M., R. Hoefling, P. Kowski and G. Strauch (1996): Sample preparation device for quantitative hydrogen isotope analysis using chromium metal. Analytical Chemistry, 68, 4414-4417.

5. Gehrels, J.C., J.E.M. Peeters, J.J. Devries and M. Dekkers (1998): The mechanism of soil water movement as inferred from ¹⁸O stable isotope studies. Hydrological Sciences , 43(4), 579-594.

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