Quantitative investigation of the interaction between surface water and groundwater relies on the determination of transience of streambed hydraulic conductivity (K sb). The commonly …
Aquitard hydraulic conductivity (K), specific storage (S s) and porosity (ϕ) are critical to the modeling of flow and mass and heat transport in groundwater systems, yet comprehensive …
JJ Díaz-Nigenda, E Morales-Casique… - Water Resources …, 2023 - Springer
Groundwater management models have been widely applied to obtain optimal pumping strategies for land subsidence control, but most of them do not explicitly incorporate land …
The problem of land subsidence due to groundwater pumping in highly compressible, randomly heterogenous aquitards with stress-dependent parameters is analyzed through …
Abstract The Mexico City aquifer is a complex mix of alluvial deposits and volcanic rocks overlapped by an aquitard composed of lacustrine deposits. To characterize this …
Extensometers provide long-term records of deformation over a depth interval of interest. An overconsolidated aquitard usually undergoes elastic deformation if the hydraulic head within …
C Zhuang, L Yan, Z Zhou, J Wang, Z Dou - Water Science and Engineering, 2021 - Elsevier
Darcy's law has been widely used to study the groundwater drainage process within an aquitard. However, non-Darcy flow is frequently encountered in laboratory and in situ …
M Huang, D Li - Geofluids, 2019 - Wiley Online Library
Land subsidence resulting from the withdrawal of groundwater is one of the problems of major importance to geosciences and geomechanics. In order to analyze the phenomena of …
En esta investigación se evaluó el proceso de subsidencia en México mediante el uso de técnicas de geodesia satelital complementadas con información de los censos (2010 y …