2001
DOI: 10.1016/s0022-1694(00)00379-6
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Prediction of optimal safe ground water yield and land subsidence in the Los Banos-Kettleman City area, California, using a calibrated numerical simulation model

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Cited by 106 publications
(38 citation statements)
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“…From 1940, California over-exploited 1.8 million m 3 of water every year with the exploitation depth of 305-754 m. Land subsidence affected farmland of more than 9000 km 2 . After water transfer, land subsidence was effectively prevented, and soil and water were conserved (Poland, 1981;Larsona et al, 2001). …”
Section: Positive Impacts On Water Recipient Basinsmentioning
confidence: 99%
“…From 1940, California over-exploited 1.8 million m 3 of water every year with the exploitation depth of 305-754 m. Land subsidence affected farmland of more than 9000 km 2 . After water transfer, land subsidence was effectively prevented, and soil and water were conserved (Poland, 1981;Larsona et al, 2001). …”
Section: Positive Impacts On Water Recipient Basinsmentioning
confidence: 99%
“…There was about 8 m settlement due to the uncontrolled exploitation of groundwater for agricultural use. Until 1994 the amount of subsidence increased to 10-meter for 50-meter water level drop in the region [4]. Such phenomenon has been observed in many parts of the world such as Mexico, Thailand, Japan, America [5], Shanghai [6] and other parts of the China in the past years [7].…”
Section: History Of Subsidencementioning
confidence: 99%
“…Este problema se presenta en depósitos de sedimentos recientes arcillosos, a causa de la disminución de la presión intersticial o bien colapsos locales si hay cavidades kársticas o sifonamiento y arrastre de arenas. La ST puede ser de extensión regional cuando es causada por bombeo muy excesivo y continuo de AS y combinado con el peso de las construcciones civiles (Larson et al, 2001;LoboGuerrero Uscátegui, 2003;Carreón-Freyre et al, 2005;Ochoa-González y Carreón-Freyre, 2006;Abidin et al, 2008). La ST es gradual, repentina o con la presencia de grietas, que se deben al movimiento y deformación del material del subsuelo por extracción de petróleo, gas o descenso del AS.…”
Section: Subsidencia Del Terrenounclassified