By Shlomo P. Neuman, Alberto Guadagnini, Monica Riva (auth.), Phoolendra K. Mishra, Kristopher L. Kuhlman (eds.)
This ebook represents kinds of growth in hydrogeology, together with conceptualization adjustments, diverse ways to simulating groundwater circulation and delivery new hydrogeophysical tools. every one bankruptcy extends or summarizes a contemporary improvement in hydrogeology, with forward-looking statements in regards to the demanding situations and strengths which are confronted. whereas the name and scope is huge, there are numerous sub-themes that attach the chapters. topics comprise theoretical advances in conceptualization and modeling of hydrogeologic difficulties. Conceptual advances are additional tempered by way of insights bobbing up from observations from either box and laboratory work.
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In multiphase flow simulations, the fractional flow-based approach is widely used due to two advantages. First, the primary variables in the fractional flowbased approach are degrees of saturation and total pressure. Therefore, the change of phase configuration, phase appearance, and phase disappearance are automated. For example, the number of simulated phases in a three-phase flow problem can degenerate from three to two or one and conversely extend from one to two or three (Suk and Yeh 2008).
7119 Zhang Q, Xu C-Y, Yu Z, Liu C-L, Chen YD (2009) Multifractal analysis of streamflow records of the east River basin (Pearl River), China. H. T. Yeh Abstract The purpose of this investigation is to implement a new constitutive law of saturation–capillary pressure into a fractional flow-based multiphase flow model to simulate compressible subsurface flow problems. Using the new constitutive law to describe the saturation–capillary pressure relations alleviates an undue constraint on pressure distributions inherent in a widely used law.
Carrano and yeh 1995; Christie et al. 1976). Other more robust numerical discretization methods may be employed, but that will not alter the key points addressed in this chapter. H. T. 26) B where [C1p ] is the mass matrix associated with total pressure for water saturation; [C1w ] is the mass matrix associated with water saturation; [C1t ] is the mass matrix associated with total liquid saturation for water saturation; [ADW1 ] is the advection and gravity matrix associated with water saturation; [ADT1 ] is the advection and gravity matrix associated with total liquid saturation; [DDW1 ] is the dispersion- 2 An Advanced Constitutive Law in Multiphase Flow Model for Simulations...