Hydrogeologic-structure and groundwater-movement imaging in tideland using electrical sounding resistivity: a case study on the Ariake Sea coast, southwest Japan
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- 作者：Toshiharu Misonou (1)
Hisafumi Asaue (2)
Tohru Yoshinaga (3)
Yuta Matsukuma (4)
Katsuaki Koike (5)
Jun Shimada (2) - 关键词：Chargeability ; Active fault ; Sea and freshwater boundary ; Groundwater flow ; Japan
- 刊名：Hydrogeology Journal
- 出版年：2013
- 出版时间：November 2013
- 年：2013
- 卷：21
- 期：7
- 页码：1593-1603
- 全文大小：1053KB
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Hisafumi Asaue (2)
Tohru Yoshinaga (3)
Yuta Matsukuma (4)
Katsuaki Koike (5)
Jun Shimada (2)
1. Priority Organization for Innovation and Excellence, Kumamoto University, Kumamoto, Japan
2. Graduate School of Science & Technology, Kumamoto University, Kumamoto, Japan
3. Technical Division, Faculty of Engineering, Kumamoto University, Kumamoto, Japan
4. Nittetsu Mining Co., Ltd, Tokyo, Japan
5. Graduate School of Engineering, Kyoto University, Kyoto, Japan - ISSN：1435-0157
文摘
Groundwater flow exerts a crucial control on the boundary between the sea and freshwater and is thus a key factor for preserving groundwater resources and preventing seawater intrusion in coastal areas. Although it is highly probable that geological faults in coastal areas affect groundwater flow patterns, the effect has not been described yet in detail. This study is aimed at detecting and imaging groundwater flow and its temporal change around a fault in a coastal area through resistivity and chargeability distributions using electrical sounding. The Okoshiki area in central Kyushu, southwest Japan, was selected as a case study area, because of the presence of Kamiouda Fault. The measurements were conducted along six lines of both parallel and perpendicular orientations to the coastline. A feature suggesting a fault zone was evident on two lines. Through the temporal change of resistivity, movement and mixing processes of the seawater and freshwater during the ebb, low and flood tides were interpreted. A conceptual model of the processes was constructed in which a fault zone and the configuration of bedrock are dominant elements by acting as a selective path and a barrier to the groundwater flow, respectively.