Correction to ‘Nodal domain integration model of unsaturated two-dimensional soil-water flow: Development’
نویسندگان
چکیده
منابع مشابه
two-dimensional time domain fundamental solution to dynamic unsaturated poroelasticity
this paper presents time domain fundamental solutions for the extended biot's dynamic formulations of two-dimensional (2d) unsaturated poroelasticity. unsaturated porous media is considered as a porous media in which the voids are saturated with two immiscible fluids, i.e. liquid and gas. at first, the corresponding explicit laplace transform domain fundamental solution is obtained in term...
متن کاملRegional Quasi-Three-Dimensional Unsaturated-Saturated Water Flow Model Based on a Vertical-Horizontal Splitting Concept
Yan Zhu 1, Liangsheng Shi 1, Jingwei Wu 1, Ming Ye 2, Lihong Cui 1 and Jinzhong Yang 1,* 1 State Key Laboratory of Water Resources and Hydropower Engineering Science, Wuhan University, Wuhan 430072, China; [email protected] (Y.Z.); [email protected] (L.S.); [email protected] (J.W.); [email protected] (L.C.) 2 Department of Scientific Computing, Florida State University, Tall...
متن کاملCorrection to ‘‘Fracture intersections as integrators for unsaturated flow’’
[1] In the paper ‘‘Fracture intersections as integrators for unsaturated flow’’ by Thomas R. Wood, Michael J. Nicholl, and Robert J. Glass (Geophys. Res. Lett., 29(24), 2191, 10.1029/2002GL015551, 2002) an error appears in paragraph [3] in the third sentence. The corrected sentence follows: At low flow, pulsed flow in the upper fracture was integrated by the intersection, and released into the ...
متن کاملGroundwater recharge simulation using a coupled saturated-unsaturated flow model
Abstract The coupled MODFLOW-HYDRUS software package was used to produce a saturated-unsaturated flow model for a Flood Spreading System (FSS) and its associated aquifer. The study aim to improve simulations of near-surface hydrological processes, including temporal and spatial variation in groundwater recharge rates. The coupled model was built with average RMSE=1.1 and 1.3 for calibration ...
متن کاملtwo-dimensional magma flow
exact solution for steady two-dimensional flow of an incompressible magma is obtained. themagmatic flow is studied by considering the magma as a second grade fluid. the governing partialdifferential equations are transformed to ordinary differential equations by symmetry transformations. resultsare discussed through graphs to understand the rheology of the flowing magma
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ژورنال
عنوان ژورنال: Water Resources Research
سال: 1982
ISSN: 0043-1397
DOI: 10.1029/wr018i002p00447