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39'K 409'K 0 0.5 11) 15 2a a. Figure4. Effective diffusiviiy vs. loading forn-heptone/5A;-Equotion (8), ---Equation (1 1).
π SIMILAR VOLUMES
Computer experiments for diffusion and dispersion in a capillary tube have been used to learn something of the functional dependence of the dispersion vector, ($), and the dispersion coefficient, K. At short times we find the latter to be a function of time and strongly dependent on the concentratio
Withers, R.J. and Nyland, E., 1976 . Theory for the rapid solution of ground subsidence near reservoirs on layered and porous media. In: W.G. Milne (Editor), Induced Seismicity. Eng. Geol., 10(2--4): 169--185. The use of two-dimensional fourier transforms of reservoir topography allows substantial
## Abstract The dyadic Green's function in spherically layered media is considered by assuming that source and field points can be located anywhere. After manipulations from the expression of the dyadic Green's function based on the reflections and transmissions of the scalar waves, the dyadic Gree