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Long-term changes associated with exploitation of the Beppu hydrothermal system, Japan

โœ Scribed by Yuki Yusa; Shinji Ohsawa; Koichi Kitaoka


Book ID
104333238
Publisher
Elsevier Science
Year
2000
Tongue
English
Weight
811 KB
Volume
29
Category
Article
ISSN
0375-6505

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โœฆ Synopsis


Exploitation of the Beppu hydrothermal system started mainly in the lowland areas as early as the 1880s, and by the 1920s the number of wells had increased to about 1000. This caused the piezometric head of the thermal groundwater to draw down, and seawater to intrude into the thermal groundwater aquifer near the coast. A second ยฏurry of exploitation occurred during the 1960sยฑ70s, by which time there were over 2300 wells, and the mass and heat ยฏows had increased due mainly to the discharge of high-temperature chloride waters in the highland areas. This caused a decline in piezometric head of the deep chloride water, a decline in the subsurface ยฏow of chloride water towards the lowlands, and intrusion of steam-heated shallow water into the chloride water layer.


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