2019
DOI: 10.1016/j.geomorph.2019.03.017
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Quantifying the contribution of multiple factors to land subsidence in the Beijing Plain, China with machine learning technology

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Cited by 67 publications
(51 citation statements)
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“…Figure 2 is the distribution map of the quaternary sediments (QS) and major faults, superimposed with compressible thickness (CT) contours and recorded epicenters around the study site. The quaternary sediments with good compressibility near the study area are about 150-250 m thick, which was proved to provide geological conditions for the generation and development of local land subsidence [42]. The Shunyi-liangxiang fault is one of the major faults crossing the study area, with a total length of 35 km and a trend of~30-40 NE.…”
Section: Study Sitementioning
confidence: 90%
“…Figure 2 is the distribution map of the quaternary sediments (QS) and major faults, superimposed with compressible thickness (CT) contours and recorded epicenters around the study site. The quaternary sediments with good compressibility near the study area are about 150-250 m thick, which was proved to provide geological conditions for the generation and development of local land subsidence [42]. The Shunyi-liangxiang fault is one of the major faults crossing the study area, with a total length of 35 km and a trend of~30-40 NE.…”
Section: Study Sitementioning
confidence: 90%
“…2020, 12, 457 3 of 22 reached 4000 km 2 . The areas affected by land subsidence comprise more than 60% of the Beijing Plain and form six land subsidence funnels [40][41][42][43][44].…”
Section: Study Areamentioning
confidence: 99%
“…The overexploitation of groundwater resulted in an obvious recession in the level of said groundwater in the BP from 2003 to 2014, as well as in an increase in effective stress, which led to the consolidation of aquifer systems, thus causing serious land subsidence [3,16]. Quaternary loose sediments are widely distributed in the BP, which provide basic geological conditions for land subsidence, although the thickness of compressible layers varies greatly [21]. As shown in Figure 1c, the thickness of compressible layers gradually increases from the top to the bottom of the alluvial plain [22].…”
Section: Study Areamentioning
confidence: 99%
“…Zamanirad et al [20] modeled land subsidence susceptibility by using boosted regression trees and also indicated that groundwater exploitation is the most important influencing factor for the occurrence of land subsidence. Zhou et al [21] quantified the contribution rate of the influencing factors of land subsidence to cumulative land subsidence. Compared to cumulative land subsidence, uneven subsidence may cause greater economic loss.…”
Section: Introductionmentioning
confidence: 99%