Sustained Changes in Well Water Levels Following a Large Earthquake: Possible Evidence of Permeability Decreases in a Shallow Groundwater System
Author:
Affiliation:
1. School of Water Resources and Environment China University of Geosciences Beijing China
2. School of Ecology and Environment Institute of Disaster Prevention Beijing China
Funder
National Natural Science Foundation of China
National Natural Science Foundation of China-Yunnan Joint Fund
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL090232
Reference17 articles.
1. A mechanism for sustained groundwater pressure changes induced by distant earthquakes
2. Hydrological effects of theMW7.1 Darfield (Canterbury) earthquake, 4 September 2010, New Zealand
3. Hydrodynamic response to strike- and dip-slip faulting in a half-space
4. Groundwater responses to the recent Canterbury earthquakes: a comparison
5. Post-earthquake ground movements correlated to pore-pressure transients
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