2013
DOI: 10.18268/bsgm2013v65n1a10
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Analysis and simulation of regional subsidence accompanying groundwater abstraction and compaction of susceptible aquifer systems in the USA

Abstract: Regional aquifer-system compaction and land subsidence accompanying groundwater abstraction in susceptible aquifer systems in the USA is a challenge for managing groundwater resources and mitigating associated hazards. Developments in the assessment of regional subsidence provide more information to constrain analyses and simulation of aquifer-system compaction. Current popular approaches to simulating vertical aquifer-system deformation (compaction), such as those embodied in the aquitard drainage model and t… Show more

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Cited by 36 publications
(18 citation statements)
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References 63 publications
(57 reference statements)
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“…In general, thick, coarse-grained sediment layers (i.e., aquifers) are the primary space for storing groundwater; fine-grained sediment layers are impermeable and often preclude recharging of the aquifer as well as the locations where consolidation is likely to occur (i.e., land subsidence) due to excessive withdrawal of groundwater (Galloway and Sneed 2013). In general, thick, coarse-grained sediment layers (i.e., aquifers) are the primary space for storing groundwater; fine-grained sediment layers are impermeable and often preclude recharging of the aquifer as well as the locations where consolidation is likely to occur (i.e., land subsidence) due to excessive withdrawal of groundwater (Galloway and Sneed 2013).…”
Section: Introductionmentioning
confidence: 99%
“…In general, thick, coarse-grained sediment layers (i.e., aquifers) are the primary space for storing groundwater; fine-grained sediment layers are impermeable and often preclude recharging of the aquifer as well as the locations where consolidation is likely to occur (i.e., land subsidence) due to excessive withdrawal of groundwater (Galloway and Sneed 2013). In general, thick, coarse-grained sediment layers (i.e., aquifers) are the primary space for storing groundwater; fine-grained sediment layers are impermeable and often preclude recharging of the aquifer as well as the locations where consolidation is likely to occur (i.e., land subsidence) due to excessive withdrawal of groundwater (Galloway and Sneed 2013).…”
Section: Introductionmentioning
confidence: 99%
“…Based on the theory, simulations of groundwater induced surface motions have been validated to be useful by comparing with GPS and InSAR data. Groundwater rise will uplift the surface, whereas groundwater depletion will induce land subsidence (Galloway et al, 1999;Bawden et al, 2001;King et al, 2007;Ji et al, 2012;Galloway et al, 2013), which means GPS observations keeps consistent with the groundwater variation. Figure 7 is a conceptualization of this process.…”
Section: Comparison Of Annual Water Variationsmentioning
confidence: 76%
“…These specially occur in carbonate rocks, and may have a variety of sizes and are morphologically expressed as a function of its evolution mechanisms. In the present world, sinkholes (SH) are among the most significant geo-hazards of karsts areas of various countries, with significant negative consequences for society in terms of economic losses (Galloway & Sneed, 2013). Subsidence, based on the morphology of the failure and the triggering agent, may be termed as Sinkhole or ground subsidence, though these two are entirely different on morphology and process of their evolution.…”
Section: Introductionmentioning
confidence: 99%