By Shlomo P. Neuman, Alberto Guadagnini, Monica Riva (auth.), Phoolendra K. Mishra, Kristopher L. Kuhlman (eds.)
This publication represents varieties of growth in hydrogeology, together with conceptualization adjustments, varied ways to simulating groundwater stream and delivery new hydrogeophysical equipment. each one bankruptcy extends or summarizes a up to date improvement in hydrogeology, with forward-looking statements concerning the demanding situations and strengths which are confronted. whereas the identify and scope is extensive, there are numerous sub-themes that attach the chapters. issues contain theoretical advances in conceptualization and modeling of hydrogeologic difficulties. Conceptual advances are additional tempered through insights coming up from observations from either box and laboratory work.
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2 Problem Formulations The present multiphase flow model is assumed to consist of a compressible media and three compressible fluid phases consisting of water, NAPL, and air The porosity is assumed constant in the simulation. Each phase is assumed to have an average property, since each phase contains one component in this investigation. These assumptions do not alter the key points to be addressed in this chapter. However, a model without these assumptions is under development to make it more applicable to real-world problems.
21) is workable only if the products of the scaling factor and capillary pressure head, (α32 hC32 ) and (α21 hC21 ), satisfy the constraint in Eq. 23). This constraint seems to have little physical relevance. , not due to physical justifications. 23). ’s model, the relative permeability as a function of the degree of saturation is proposed by Parker et al. 28) where S1 is the effective degree of saturation for water, S1r is the irreducible saturation of water and St is the effective degree of saturation for total liquid.
Geophys Res Lett 21(5):349–352 Neuman SP (2010a) Apparent/spurious multifractality of data sampled from fractional Brownian/L´evy motions. 7611 Neuman SP (2010b) Apparent/spurious multifractality of absolute increments sampled from truncated fractional Gaussian/L´evy noise. 1029/2010GL043314 Neuman SP (2011) Apparent multifractality and scale-dependent distribution of data sampled from self-affine processes. 7967 Neuman SP, Di Federico V (2003) Multifaceted nature of hydrogeologic scaling and its interpretation.
Advances in Hydrogeology by Shlomo P. Neuman, Alberto Guadagnini, Monica Riva (auth.), Phoolendra K. Mishra, Kristopher L. Kuhlman (eds.)