Computational Subsurface Hydrology: Fluid Flows by Yeh Gour-Tsyh

By Yeh Gour-Tsyh

Computational Subsurface Hydrology: Fluid Flows deals working towards engineers and scientists a theoretical heritage, numerical tools, and desktop codes for the modeling of fluid flows in subsurface media. it is going to additionally function a textual content for senior and graduate classes on fluid flows in subsurface media in disciplines akin to civil and environmental engineering, agricultural engineering, geosciences, soil sciences, and chemical engineering.
Computational Subsurface Hydrology: Fluid Flows provides a scientific derivation of governing equations and boundary stipulations of subsurface fluid stream. It discusses various numerical equipment, expounds designated strategies for developing finite point equipment, and describes specified implementation of computing device codes as they're utilized to subsurface flows.
4 laptop codes to simulate vertically built-in horizontal flows (FEWA), saturated flows with relocating phreatic surfaces in 3 dimensions (3DFEWA), variably saturated flows in dimensions (FEMWATER), and variable flows in 3 dimensions (3DFEMWATER) are hooked up to this e-book. those 4 desktop codes are designed for commonly used purposes to either examine and sensible difficulties. they can be used to simulate many of the functional, real-world box difficulties.
if you'd like a replica of the diskettes containing the 4, simple common function desktop codes mentioned in Computational SubsurfaceHydrology: Fluid Flows, please electronic mail Gour-Tsyh Yeh on the following handle : gyeh@mail.ucf.edu

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2nd Ed. New York: Wiley. 2 NUMERICAL METHODS APPLIED TO SUBSURFACE HYDROLOGY Numerical methods, as shall be described in this book, are merely tools used to enable one to replace differential equations governing the subsurface processes with approximation sets of algebraic equations or matrix equations, which are subsequently solved using the methods of linear algebra and requiring the manipulation of computers (Fig. 1). If the differential equations were solved exactly by analytic procedures, the solution would appear as some combination of mathematical functions.

Gupta, and R. N. Bhattacharya. 1979. Foundation theories of solute transport in porous media: a critical review. Advances in Water Resources. 2:59-68. Todd, D. K. 1980. Groundwater Hydrology. 2nd Ed. New York: Wiley. 2 NUMERICAL METHODS APPLIED TO SUBSURFACE HYDROLOGY Numerical methods, as shall be described in this book, are merely tools used to enable one to replace differential equations governing the subsurface processes with approximation sets of algebraic equations or matrix equations, which are subsequently solved using the methods of linear algebra and requiring the manipulation of computers (Fig.

New York: McGraw-Hill. Bird, R. , W. E. Stewart, and E. N. Lightfoot. 1960. Transport Phenomena. New York: Wiley. Bowen, R. M. 1976. Theory of mixtures: In A. C. , Continuum Physics. Vol. 3, Pt. I. New York: Acadernic Press. Fick, A. E. 1855. Philosophical Magazine. 10:30. Gray, W. G. 1983. General conservation equations for multi-phase systems: 4. Constitutive theory including phase change. Advances in Water Resources 6: 130-140. Gray, W. G. and P. C. Y. Lee. 1977. On the theorems for local volume averaging of multiphase systems.

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