Chenglong Liu

TL;DR: In this article, the authors used the well water-level response to earth tides and atmospheric pressure to study the changes in hydraulic properties in an aquifer and an overlying confining layer in Beijing, China, following the 11 March 2011 Tohoku earthquake in Japan.

TL;DR: In this article, Zhao et al. found that both the magnitude and the sign of water level changes are inconsistent with those predicted by the coseismic strain hypothesis in the near-field and in the intermediate-field.

TL;DR: In this article, the authors compared the static strain predicted by dislocation theory with the volumetric strain calculated by the tide effect of the groundwater based on poroelastic theory, and they roughly estimate that the effect range of the static stress is approximately 300 kilometres for the Wenchuan earthquake, and the dynamic stresses dominate beyond this epicenter distance.

TL;DR: In this paper, multi environmental tracers (hydrochemical parameters, stable hydrogen and oxygen isotopes and radioactive 222Rn) were employed to investigate the interaction between groundwater and surface water along two rivers (Tiangeli River and Nomhon River) in the Nomhon area, southeast of the arid Qaidam Basin, northwest China.

TL;DR: Hydrochemical and stable and radium and stable isotopic approaches were employed to study the hydrochemical and isotopic characteristics of groundwater and surface water to identify the places where groundwater discharged into Poyang Lake and the groundwater discharge sources and showed that the groundwater discharged area was extensive during the dry season.