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Summary This is an investigation of the absolute permeability of unconsolidated sand and consolidated sandstone cores to distilled water as a function of the temperature of the system, confining pressure on the core, and the pore pressure of the flowing fluid. The effects of flow rate and throughput are also discussed. In contrast to some previous investigations, no effect of temperature on permeability was found beyond experimental errors and effects caused by volumetric throughput. The probable causes of differing results in previous studies are also presented.
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Gobran et al. (1987) studied this question.
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