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Estimation of residence time and catchment area for spring water using radioactive isotope and groundwater flow model

Hiroshiro, Yoshinari ; Jinno, Kenji ; Tsutsumi, Atsushi ; Matsumoto, Masataka and Berndtsson, Ronny LU orcid (2007) In Memoirs of the Faculty of Engineering, Kyushu University 67(1). p.1-9
Abstract

Spring water, however, is often formed in complex geological formations and therefore it is difficult to determine the catchment area contributing to the flow. The Sayanokami spring, located in western part of Fukuoka City, Japan, is such a spring and an important water resource for the local agriculture. In order to better understand the hydrological properties of infiltration and groundwater processes for the spring water, 222Rn and tritium were used as tracers. Results showed that the residence time for the spring water is 10 - 20 years. A groundwater model confirmed these results and the travel time from the catchment border estimated to be about 25 years. Using this information the catchment border and uptake area were... (More)

Spring water, however, is often formed in complex geological formations and therefore it is difficult to determine the catchment area contributing to the flow. The Sayanokami spring, located in western part of Fukuoka City, Japan, is such a spring and an important water resource for the local agriculture. In order to better understand the hydrological properties of infiltration and groundwater processes for the spring water, 222Rn and tritium were used as tracers. Results showed that the residence time for the spring water is 10 - 20 years. A groundwater model confirmed these results and the travel time from the catchment border estimated to be about 25 years. Using this information the catchment border and uptake area were estimated. The method can be used to more efficiently determine catchment area and travel time for groundwater and thus to better manage the spring water.

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publication status
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keywords
Rn, Estimation of residence time and catchment area of spring water, Groundwater flow model, Tritium
in
Memoirs of the Faculty of Engineering, Kyushu University
volume
67
issue
1
pages
9 pages
publisher
Kyushu University, Faculty of Science
external identifiers
  • scopus:34147100553
language
English
LU publication?
yes
id
ab778f79-29ad-4486-b07b-6b3a85ade234
date added to LUP
2023-08-17 15:02:56
date last changed
2024-01-05 04:40:51
@article{ab778f79-29ad-4486-b07b-6b3a85ade234,
  abstract     = {{<p>Spring water, however, is often formed in complex geological formations and therefore it is difficult to determine the catchment area contributing to the flow. The Sayanokami spring, located in western part of Fukuoka City, Japan, is such a spring and an important water resource for the local agriculture. In order to better understand the hydrological properties of infiltration and groundwater processes for the spring water, <sup>222</sup>Rn and tritium were used as tracers. Results showed that the residence time for the spring water is 10 - 20 years. A groundwater model confirmed these results and the travel time from the catchment border estimated to be about 25 years. Using this information the catchment border and uptake area were estimated. The method can be used to more efficiently determine catchment area and travel time for groundwater and thus to better manage the spring water.</p>}},
  author       = {{Hiroshiro, Yoshinari and Jinno, Kenji and Tsutsumi, Atsushi and Matsumoto, Masataka and Berndtsson, Ronny}},
  keywords     = {{Rn; Estimation of residence time and catchment area of spring water; Groundwater flow model; Tritium}},
  language     = {{eng}},
  month        = {{03}},
  number       = {{1}},
  pages        = {{1--9}},
  publisher    = {{Kyushu University, Faculty of Science}},
  series       = {{Memoirs of the Faculty of Engineering, Kyushu University}},
  title        = {{Estimation of residence time and catchment area for spring water using radioactive isotope and groundwater flow model}},
  volume       = {{67}},
  year         = {{2007}},
}