2001
DOI: 10.1016/s0309-1708(00)00047-6
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Lanczos method for the solution of groundwater flow in discretely fractured porous media

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Cited by 18 publications
(17 citation statements)
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“…Standard Galerkin method is applied to discretize the weak forms with appropriate boundary conditions (Zimmerman and Bodvarsson 1996;Woodbury and Zhang 2001).…”
Section: Finite Element Methods Formulationmentioning
confidence: 99%
“…Standard Galerkin method is applied to discretize the weak forms with appropriate boundary conditions (Zimmerman and Bodvarsson 1996;Woodbury and Zhang 2001).…”
Section: Finite Element Methods Formulationmentioning
confidence: 99%
“…The continuum medium approach has proven to be inadequate in describing large scale regions since it has to oversimplify the fractured formation as a homogeneous zone [125]. The DFN approach cannot produce the detailed set of the geometrical parameters for individual fractures, while requiring extensive computational time for large scale simulations [126,127]. The third approach can be considered more efficient since it combines the advantages of both continuum and discrete methods.…”
Section: Direct Applications Of Hydraulic Fracturing Studiesmentioning
confidence: 99%
“…Now let us return to the original case of model reduction for systems (1.1.4)-(1.1.8). From a control theory viewpoint we term it single input-complete outputconvection partial differential equation, then the Krylov subspace (1.1.31) with s o 0 is a very good choice for the lower dimensional subspace in Equation (1.1.6) [8,9,[37][38][39][40][41][42][43]. In this case, the model reduction step (1.1.8) can be viewed as an approximate solution of the original system (1.1.4), because it is possible to recover the solution for all of the original unknowns by means of Equation (1.1.6).…”
Section: Approximating a Transfer Function By Padé And Padé-type Apprmentioning
confidence: 99%
“…They mostly deal with the SICO case discussed above. Here, model reduction is at the beginning stage if we compare the number of papers in which model reduction is used to the total number of papers on the solution of advection-diffusion PDEs: advection dispersion equation for groundwater flow [37,38], mass transport in hydrogeological environments [39], photon diffusion (optical tomography) problem [40], radionuclide decay-chain transport in porous media [41], groundwater flow in dual-porosity media [42], radionuclide decay chain transport in dual-porosity media [43], groundwater flow in discretely fractured porous media [8] and diffusion and convection dominated flow [9].…”
Section: Approximating a Transfer Function By Padé And Padé-type Apprmentioning
confidence: 99%
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