| 地震尺度下碳酸盐岩储层的岩石物理建模方法(英文) |
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| 引用本文： | 李景叶,陈小宏.地震尺度下碳酸盐岩储层的岩石物理建模方法(英文)[J].应用地球物理,2013,10(1):1-13. |
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| 作者姓名： | 李景叶 陈小宏 |
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| 作者单位： | 中国石油大学(北京)油气资源与探测国家重点实验室;中国石油大学CNPC物探重点实验室 |
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| 基金项目： | sponsored jointly by the National Natural Science Foundation of China(No.41074098);the Key State Science and Technology Project(2011ZX05023-005-005);China University of Petroleum(Beijing) Fund(KYJJ2012-05-08) |
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| 摘 要： | 碳酸盐岩油藏的强非均质性以及孔隙结构的复杂性,使得作为连接油藏参数与地震参数重要桥梁的岩石物理模型,以及作为油藏预测和定量表征最有效工具的流体替换成为岩石物理建模的难点与重点。在碳酸盐岩储层复杂孔隙结构与地震尺度下碳酸盐岩储层非均质性分析基础上,研究采用岩石网格化方法,将地震尺度下非均质碳酸盐岩储层岩石划分为具有独立岩石参数的均质岩石子体,根据岩石孔隙成因与结构特征采用不同岩石物理模型分步计算岩石子块干岩石弹性模量,并根据不同孔隙连通性进行流体替换,计算饱和不同流体岩石弹性模量。基于计算的岩石子块弹性模量,采用Hashin-Shtrikman-Walpole弹性边界计算理论方法实现地震尺度下碳酸盐岩储层弹性参数计算。通过对含有不同类型孔隙组合碳酸盐岩储层模型的弹性模量进行计算与分析,明确不同孔隙对岩石弹性参数的影响特征,模拟分析结果与实际资料认识一致。
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| 关 键 词： | 地震尺度 流体替换 碳酸盐岩 岩石物理建模 非均匀 |
A rock-physical modeling method for carbonate reservoirs at seismic scale |
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Li Jing-Ye
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Chen Xiao-Hong.A rock-physical modeling method for carbonate reservoirs at seismic scale[J].Applied Geophysics,2013,10(1):1-13. |
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| Authors: | ,
Li Jing-Ye
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Chen Xiao-Hong |
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| Institution: | State Key Lab of Petroleum Resources and Prospecting, Beijing 102249, China;CNPC Key Lab of China University of Petroleum(Beijing), Beijing 102249, China |
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| Abstract: | Strong heterogeneity and complex pore systems of carbonate reservoir rock make its rock physics model building and fluid substitution difficult and complex. However, rock physics models connect reservoir parameters with seismic parameters and fluid substitution is the most effective tool for reservoir prediction and quantitative characterization. On the basis of analyzing complex carbonate reservoir pore structures and heterogeneity at seismic scale, we use the gridding method to divide carbonate rock into homogeneous blocks with independent rock parameters and calculate the elastic moduli of dry rock units step by step using different rock physics models based on pore origin and structural feature. Then, the elastic moduli of rocks saturated with different fluids are obtained using fluid substitution based on different pore connectivity. Based on the calculated elastic moduli of rock units, the Hashin-Shtrikman-Walpole elastic boundary theory is adopted to calculate the carbonate elastic parameters at seismic scale. The calculation and analysis of carbonate models with different combinations of pore types demonstrate the effects of pore type on rock elastic parameters. The simulated result is consistent with our knowledge of real data. |
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| Keywords: | Seismic scale fluid substitution carbonate rock rock physics modeling heterogeneity |
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