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Hydrogeology Journal

Erschienen in:

01.10.2004 | Report

The use of temperature, stable isotopes and water quality to determine the pattern and spatial extent of groundwater flow: Nagaoka area, Japan

verfasst von: Z. E. Salem, Y. Sakura, M. A. Mohammed Aslam

Erschienen in: Hydrogeology Journal | Ausgabe 5/2004

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Abstract

The purpose of this study was to trace the groundwater flow system in the Nagaoka area using subsurface temperature distribution, stable isotopes and water quality. Temperature-depth profiles were measured four times in observation wells during the period 2000–2002. Water was sampled from both observation and pumping wells during the same period. A combination of tracers was used to conceptualize the groundwater flow system. The flow system appears to be divided into shallow, intermediate and deep systems. It is clear that land use, pumping and the infiltration rate are affecting the shallow flow system.

Vorheriger Artikel Hydrogeological mapping as a basis for establishing site-specific groundwater protection zones in Denmark

Nächster Artikel A comparison of electrical and electromagnetic methods for the detection of hydraulic pathways in a fractured rock aquifer, Clare Valley, South Australia

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Titel: The use of temperature, stable isotopes and water quality to determine the pattern and spatial extent of groundwater flow: Nagaoka area, Japan
verfasst von: Z. E. Salem
Y. Sakura
M. A. Mohammed Aslam
Publikationsdatum: 01.10.2004
Verlag: Springer-Verlag
Erschienen in: Hydrogeology Journal / Ausgabe 5/2004
Print ISSN: 1431-2174
Elektronische ISSN: 1435-0157
DOI: https://doi.org/10.1007/s10040-004-0368-7

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