1949
DOI: 10.2118/949224-g
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Some Examples of Fluid Flow Mechanism in Limestone Reservoirs

Abstract: The properties of limestone reservoir rocks such as the distribution anddegree of continuity of the pore systems, and the relative volumes andpermeabilities of the systems making up the complex cause large variationsbetween performance of individual limestone reservoirs and their susceptibilityto secondary recovery methods. The effects of these factors on the mechanism offluid flow cannot be adequately evaluated with presently developed concepts, laboratory data, and geological information. The observance and … Show more

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“…Since this discussion is concerned with formation evaluation primarily from a logging standpoint, the carbonate rocks will be divided into two very general classifications of porosity: (1) primary porosity, which is porosity formed at the time of deposition of the rock and determined by the geometrical properties and sedimentation; and (2) secondary porosity, in which the porosity is usually the result of the solution of the rock by the action of ground waters. In addition, a rock in which the porosity consists of a fracture network will also be classified as having secondary porosity.…”
Section: Physical Characteristics Of Carbonate Rocksmentioning
confidence: 99%
“…Since this discussion is concerned with formation evaluation primarily from a logging standpoint, the carbonate rocks will be divided into two very general classifications of porosity: (1) primary porosity, which is porosity formed at the time of deposition of the rock and determined by the geometrical properties and sedimentation; and (2) secondary porosity, in which the porosity is usually the result of the solution of the rock by the action of ground waters. In addition, a rock in which the porosity consists of a fracture network will also be classified as having secondary porosity.…”
Section: Physical Characteristics Of Carbonate Rocksmentioning
confidence: 99%
“…where: ---ae S<I = 1>A aS d e (2) which states that the rate of advance of a plane of constant saturation in displacing fluid (Sd) is proportional to the change in composition of the flowing stream caused by a small change in saturation of the displacing fluid. The "rate of advance" equation, (2), was derived for a linear system, but m~y be adapted to a radial system by multiplying the expresr sion by the ratio __ w -, where T w is the well bore radius and Tw + u u is the radial distance from the bore face.…”
Section: Appendixmentioning
confidence: 99%
“…The "rate of advance" equation, (2), was derived for a linear system, but m~y be adapted to a radial system by multiplying the expresr sion by the ratio __ w -, where T w is the well bore radius and Tw + u u is the radial distance from the bore face. The expression then becomes, for a radial system:…”
Section: Appendixmentioning
confidence: 99%