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We would then have 1/KØ = 1/Kgrain. Øe. [(1-Øe)-c – 1] = c/Kgrain to a fair approximation. Or KØ = Kgrain / c where c can vary with Øe, thus KØ varies with Øc Appendix 2 Implications to Porosity Decline with Depth in case of Normal Compaction...