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Coseismic Groundwater Drawdown Along Crustal Ruptures During the 2016 Mw 7.0 Kumamoto Earthquake
Ist Teil von
Water resources research, 2019-07, Vol.55 (7), p.5891-5903
Ort / Verlag
Washington: John Wiley & Sons, Inc
Erscheinungsjahr
2019
Link zum Volltext
Quelle
Wiley-Blackwell Journals
Beschreibungen/Notizen
Groundwater‐level changes after earthquakes provide insight into changes in hydrogeological properties such as permeability and pore pressure. Quantifying such changes, both their location and magnitude, is usually hindered by limited data. Using extensive high‐resolution water‐level monitoring records, we provide direct evidence of significant groundwater drawdown (4.74‐m maximum) over a 160‐km2 area along crustal ruptures after the Mw 7.0, 2016, Kumamoto earthquake. Approximately 106 m3 of water disappeared within 35 min after the main shock. The loss of water was not caused by static‐strain driven pore‐pressure decrease nor by releasing of water through structural pathways, but most likely by water transfer downwards through open cracks. Such changes may impact the security of water resources, the safety of underground waste repositories, and contaminant transport in seismically active areas.
Key Points
Groundwater levels changed immediately after the 2016 Mw 7.0 Kumamoto earthquake
Surface and aquifer waters were transferred into the deeper crust through rupture systems
Proposed water drawdown model may be transferrable globally to other aquifer systems