Articles | Volume 27, issue 2
https://doi.org/10.5194/hess-27-401-2023
https://doi.org/10.5194/hess-27-401-2023
Research article
 | 
19 Jan 2023
Research article |  | 19 Jan 2023

The origin of hydrological responses following earthquakes in a confined aquifer: insight from water level, flow rate, and temperature observations

Shouchuan Zhang, Zheming Shi, Guangcai Wang, Zuochen Zhang, and Huaming Guo

Viewed

Total article views: 2,949 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,055 809 85 2,949 208 76 90
  • HTML: 2,055
  • PDF: 809
  • XML: 85
  • Total: 2,949
  • Supplement: 208
  • BibTeX: 76
  • EndNote: 90
Views and downloads (calculated since 22 Sep 2022)
Cumulative views and downloads (calculated since 22 Sep 2022)

Viewed (geographical distribution)

Total article views: 2,949 (including HTML, PDF, and XML) Thereof 2,832 with geography defined and 117 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 30 Aug 2025
Download
Short summary
We documented the step-like increases of water level, flow rate, and water temperatures in a confined aquifer following multiple earthquakes. By employing tidal analysis and a coupled temperature and flow rate model, we find that post-seismic vertical permeability changes and recharge model could explain the co-seismic response. And co-seismic temperature changes are caused by mixing of different volumes of water, with the mixing ratio varying according to each earthquake.
Share