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000062965 0247_ $$2DOI$$a10.1111/j.1745-6584.2007.00419.x
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000062965 084__ $$2WoS$$aGeosciences, Multidisciplinary
000062965 084__ $$2WoS$$aWater Resources
000062965 1001_ $$0P:(DE-HGF)0$$aLi, W.$$b0
000062965 245__ $$aThree-dimensional geostatistical inversion of flowmeter and pumping test data
000062965 260__ $$aOxford [u.a.]$$bWiley-Blackwell$$c2008
000062965 300__ $$a193 - 201
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000062965 520__ $$aWe jointly invert field data of flowmeter and multiple pumping tests in fully screened wells to estimate hydraulic conductivity using a geostatistical method. We use the steady-state drawdowns of pumping tests and the discharge profiles of flowmeter tests as our data in the inference. The discharge profiles need not be converted to absolute hydraulic conductivities. Consequently, we do not need measurements of depth-averaged hydraulic conductivity at well locations. The flowmeter profiles contain information about relative vertical distributions of hydraulic conductivity, while drawdown measurements of pumping tests provide information about horizontal fluctuation of the depth-averaged hydraulic conductivity. We apply the method to data obtained at the Krauthausen test site of the Forschungszentrum Jülich, Germany. The resulting estimate of our joint three-dimensional (3D) geostatistical inversion shows an improved 3D structure in comparison to the inversion of pumping test data only.
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000062965 650_2 $$2MeSH$$aModels, Statistical
000062965 650_2 $$2MeSH$$aVacuum Curettage
000062965 650_7 $$2WoSType$$aJ
000062965 7001_ $$0P:(DE-HGF)0$$aEnglert, A.$$b1
000062965 7001_ $$0P:(DE-HGF)0$$aCirpka, O. A.$$b2
000062965 7001_ $$0P:(DE-Juel1)129549$$aVereecken, H.$$b3$$uFZJ
000062965 773__ $$0PERI:(DE-600)2066386-9$$a10.1111/j.1745-6584.2007.00419.x$$gVol. 46, p. 193 - 201$$p193 - 201$$q46<193 - 201$$tGround water$$v46$$x0017-467X$$y2008
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000062965 9141_ $$y2008
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