Pore-throat sizes in sandstones, siltstones, and shales: Reply

Philip H. Nelson

doi:10.1306/12141010159

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Pore-throat sizes in sandstones, siltstones, and shales: Reply

Philip H. Nelson

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Abstract

In his discussion of my article (Nelson, 2009), W. K. Camp takes issue with the concept that buoyancy is not the dominant force in forming and maintaining the distribution of gas in tight-gas accumulations (Camp, 2011). I will restrict my response to the issues he raised regarding buoyant versus nonbuoyant drive and to a few comments regarding water saturation and production. I claim that the pressure generated in petroleum source rocks (P g ), instead of the buoyancy pressure (P b ), provides the energy to charge most tight sandstones with gas. The arguments are fourfold: (1) buoyant columns of sufficient height seldom exist in low-permeability sand-shale sequences, (2) tight-gas systems display a pressure profile that declines instead of increases upward, (3) gas is pervasive in overpressured systems, and (4) source rocks can generate pore pressures sufficiently high to charge tight sandstones.

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Philip H. Nelson. 2011. Pore-throat sizes in sandstones, siltstones, and shales: Reply. https://doi.org/10.1306/12141010159

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