2020
DOI: 10.3390/rs12152461
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Quantifying Ground Subsidence Associated with Aquifer Overexploitation Using Space-Borne Radar Interferometry in Kabul, Afghanistan

Abstract: Rapid population growth combined with recent drought events and decades of political instability have left the residents of Kabul facing water scarcity, significantly relying on groundwater. Groundwater overexploitation might have induced various magnitudes of ground subsidence, however, to date, no comprehensive study of ground subsidence in Kabul has been conducted. In this study, we investigated the spatio-temporal evolution of ground deformation phenomena and its main governing processes in Kabul from 2014… Show more

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Cited by 16 publications
(5 citation statements)
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“…Time dependent soil consolidation [83] due to dewatering or other groundwater regime disturbance could explain the continued subsidence after the completion of the crossover cavern excavation. The duration of continued subsidence would depend on the amount of clay within the drained sediments [10,[84][85][86][87][88], as clays are more compressible and possess a lower hydraulic conductivity than larger grain sizes [89]. There would also be potential for hydro-mechanically coupled ground rebound post groundwater table recovery [90].…”
Section: Discussionmentioning
confidence: 99%
“…Time dependent soil consolidation [83] due to dewatering or other groundwater regime disturbance could explain the continued subsidence after the completion of the crossover cavern excavation. The duration of continued subsidence would depend on the amount of clay within the drained sediments [10,[84][85][86][87][88], as clays are more compressible and possess a lower hydraulic conductivity than larger grain sizes [89]. There would also be potential for hydro-mechanically coupled ground rebound post groundwater table recovery [90].…”
Section: Discussionmentioning
confidence: 99%
“…6, the maximum decline in groundwater level is observed in the south-western part of Paghman-Darulaman aquifer and north-western part of Central Kabul aquifer (>60 m). The sharp drop of groundwater level in the aforementioned areas is most likely due to the lower storativity of the aquifer (Landell Mills 2020a; Meldebekova et al 2020). Figure 6 shows that during 13 years, groundwater levels declined all across the Kabul Plain, except in a small area in Bagrami district, where the water table rose about 2 m over the considered period.…”
Section: Water-table Fluctuationsmentioning
confidence: 97%
“…A complex geological environment is often an important factor that impacts land subsidence [41]. As mentioned earlier, almost all of the land subsidence occurred in the infilling area.…”
Section: Natural Drivers Of Subsidencementioning
confidence: 99%