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An Approach for the Numerical Computation of the Reduction of the Original Porosity due to Diagenetic and Compaction Processes in Sandstone Reserviors

机译:砂岩保留中的成岩和压实过程引起的原始孔隙减小的数值计算方法

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Proper analysis of the original intergranular porosity loss of sedimentary strata is an important tool to gain insight into the influence of diagenetic processes on the quality of hydrocarbon reserviors. With emergence and progress of numerical technologies for simulating diagenetic processes in sedimenraty formations, the changes in the original porosity of reserviors attributed to more diagenetic processes (e.g. dissolution processes and the stabilization from one mineral to another one) can also be quantitatively evaluated. This paper proposed a set of formulas for the numerical computation of the loss in the original intergranular porosity of sandstone reserviors by compactional processes (COPL) and by intergranular cemention processes (CEPL), which consider the gain in the intergranular porosity by dissolution processes (DIPL). Theoretical analysis based on the measured data of sandstone samples shows that the real COPL will be obviously underestimated if the COPL computed by the traditional point-count method is far below CEPL and dissolution processes generated the additional porosity. Comparably, the real CEPL will only be slightly over-estimated. The deviation in COPL resulting from a DIPL of 5.0% lies in the range 0.75% ~ 2.10%, whereas the deviation in CEPL is in the range between 0.4 and 1.6%.
机译:适当分析原始型沉积地层的沉积孔隙损失是一种重要的工具,可以深入了解成岩工艺对烃类保留器质量的影响。对于模拟沉淀物形成中的成岩过程的数值技术的出现和进展,还可以定量评价归因于更多成幅过程的储存器的原始孔隙率的变化(例如,从一种矿物到另一个矿物到另一个矿物质)。本文提出了一组公式,用于通过尺寸处理(COP1)和晶间钢筋处理(CEPL)对砂岩保留的原始晶体孔隙率损失的数值计算(CEPL),其通过溶解过程考虑晶体孔隙率的增益(DIPL )。基于砂岩样品的测量数据的理论分析表明,如果通过传统点计数方法计算的COPL远低于CEPL和溶出过程,则真正的COPL显然将明显低估,并且产生额外的孔隙率。相当,真正的CEPL只会略微过度估计。由5.0%的潜品引起的COPL的偏差位于0.75%〜2.10%的范围内,而CEPL的偏差在0.4和1.6%之间。

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