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- W4307110897 abstract "<strong class=journal-contentHeaderColor>Abstract.</strong> Although many mechanisms of earthquake-induced hydrological response have been proposed in recent decades, the origins of these responses remain enigmatic, and a quantitative understanding of them is lacking. In this study, we quantitatively analyze the mechanism of coseismic response in water level and flow rate from an artesian well in southwestern China before and after multiple earthquakes and reveal the origin of the earthquake-induced hydrological response based on the monitoring data of water temperature. Water level and temperature always show coseismic step-like increases following earthquakes, which are independent of the earthquakes' epicentral distances and magnitudes. Tidal analysis finds changes in aquifer and aquitard permeability following these earthquakes, which corresponds to the post-seismic total discharge of 85â273âm<span class=inline-formula><sup>3</sup></span> in 20âd after earthquakes. Furthermore, we couple the flow rate and temperature data to model the mixing processes that occurred following each earthquake. The results indicate that coseismic temperature changes are the result of the mixing of different volumes of water from shallow and deep aquifers, with the mixing ratio varying according to each earthquake." @default.
- W4307110897 created "2022-10-27" @default.
- W4307110897 creator A5073761054 @default.
- W4307110897 date "2022-10-24" @default.
- W4307110897 modified "2023-10-18" @default.
- W4307110897 title "Reply on RC1" @default.
- W4307110897 doi "https://doi.org/10.5194/hess-2022-326-rc3" @default.
- W4307110897 hasPublicationYear "2022" @default.
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