Groundwater-level Changes Due to Pressure Gradient Induced by Nearby Earthquakes off Izu Peninsula, 1997
Anomalous water level changes were observed at two wells associated with seismic swarm activity off Izu Peninsula on March, 1997. These are coseismic water level drops followed by gradual postseismic water level rise at the time of large earthquakes during the swarm activity. The post-seismic water...
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| Veröffentlicht in: | Pure and applied geophysics 2006-04, Vol.163 (4), p.647-655 |
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| container_title | Pure and applied geophysics |
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| creator | Ohno, Masao Sato, Tsutomu Notsu, Kenji Wakita, Hiroshi Ozawa, Kunio |
| description | Anomalous water level changes were observed at two wells associated with seismic swarm activity off Izu Peninsula on March, 1997. These are coseismic water level drops followed by gradual postseismic water level rise at the time of large earthquakes during the swarm activity. The post-seismic water level rises, which can be fitted by an exponential function with a time constant of about six hours, are explained in terms of the horizontal pressure diffusion due to the pressure gradient in the aquifer induced by the coseismic static strain.[PUBLICATION ABSTRACT] |
| doi_str_mv | 10.1007/s00024-006-0041-2 |
| format | Article |
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| subjects | Aquifers Diffusion Earthquakes Groundwater Groundwater levels Peninsulas Pressure gradients Seismic activity Seismic engineering Seismic phenomena Strain |
| title | Groundwater-level Changes Due to Pressure Gradient Induced by Nearby Earthquakes off Izu Peninsula, 1997 |
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