📄 gassmnk.m
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function k2=gassmnk(k1,kfl1,kfl2,k0,phi)%GASSMNK Gassmann's relation (moduli)%% Fluid substitution using Gassmann equation% K1: original bulk modulus of rock saturated with fluid of bulk modulus KFL1% K2: rock bulk modulus with new fluid of bulk modulus KFL2% K0: mineral modulus% PHI: porosity%% Giving the P-wave modulus in place of the bulk modulus does the approximate% Gassmann calculation.%% See also GASSMNV%Written by T. Mukerjia= k1./(k0-k1) - kfl1./(phi.*(k0-kfl1)) + kfl2./(phi.*(k0-kfl2)); k2= (k0.*a ./(1+a)).*(phi~=0) + k1.*(phi==0);
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