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Research on conductive mechanism and saturation model of the volcanic reservoir with complex pore structure |
Yu-Fei FAN1( ), Bao-Zhi PAN1, Fang ZHANG2 |
1.College of Geo-exploration Science and Technology,Jilin University,Changchun 130026,China 2.Daqing Oilfield Drilling Engineering Company,Songyuan 138000,China |
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Abstract The complex lithology and pore system in volcanic reservoir result in the complex conductive features of the strata.The authors applied the electric conduction model proposed by Herrick and Kennedy to the volcanic reservoir in Wangfu area based on the theory of pore geometry.The parameters of the model were determined with core litho-electric experimental data in the volcanic rocks of Wangfu area,and a new electrical efficiency model suitable for the volcanic reservoir of complex pore structures was established.Using the new model to deal with the actual well data has achieved very good results.
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Received: 13 July 2016
Published: 20 February 2018
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岩样编号 | 岩性 | 孔隙度/% | 渗透率/10-3μm2 | m(a=1) | n | b | A-1 | 粗安质角砾熔岩 | 9.45 | 3.94 | 1.62 | 0.92 | 1.10 | A-2 | 粗安质角砾熔岩 | 9.88 | 9.90 | 1.55 | 1.64 | 1.07 | A-3 | 粗安质角砾熔岩 | 8.81 | 29.09 | 1.37 | 1.68 | 1.04 | A-4 | 粗安质凝灰熔岩 | 8.67 | 1.59 | 1.30 | 1.58 | 1.14 | B-1 | 沉角砾岩 | 7.87 | 0.88 | 1.41 | 0.74 | 0.98 | B-2 | 沉角砾岩 | 7.64 | 0.46 | 1.59 | 1.04 | 0.97 | B-3 | 沉角砾岩 | 7.36 | 1.01 | 1.39 | 1.31 | 0.91 | B-4 | 沉角砾岩 | 9.48 | 0.30 | 1.60 | 1.78 | 0.96 | B-5 | 沉角砾岩 | 6.59 | 0.53 | 1.52 | 0.99 | 0.96 |
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拟合关系式(x代表φ,y代表E0) | R2 | y=0.9539x0.4571 | 0.7358 | y=0.7494x+0.2483 | 0.9154 | y=0.2738e1.2887 | 0.776 | y=0.2678ln(x)+0.9785 | 0.881 | y=0.1613x2+0.5492x+0.2895 | 0.8523 |
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岩样编号 | 回归分析类型 | 多项式 | 指数 | 线性 | 对数 | 幂 | A-1 | 0.8456 | 0.1619 | 0.1572 | 0.237 | 0.2418 | A-2 | 0.9643 | 0.858 | 0.8489 | 0.7928 | 0.8056 | A-3 | 0.9463 | 0.906 | 0.8998 | 0.8784 | 0.8868 | A-4 | 0.9124 | 0.9129 | 0.8847 | 0.8585 | 0.8949 | B-1 | 0.8746 | 0.8622 | 0.8661 | 0.8544 | 0.8479 | B-2 | 0.7024 | 0.001 | 0.0012 | 0.000001 | 0.00002 | B-3 | 0.7923 | 0.0451 | 0.0439 | 0.0258 | 0.0267 | B-4 | 0.9629 | 0.8295 | 0.8368 | 0.8611 | 0.8548 | B-5 | 0.9258 | 0.4495 | 0.4383 | 0.5157 | 0.5278 |
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岩样编号 | 拟合关系式(x代表et,y代表Sw) | R2 | A-1 | y=1.2177x2-1.7832x+1.5466 | 0.8456 | A-2 | y=2.0815x2-2.5517x+1.4824 | 0.9643 | A-3 | y=2.1276x2-2.9126x+1.7791 | 0.9463 | A-4 | y=1.0922x2-0.9954x+0.8597 | 0.9124 | B-1 | y=-0.3355x2+0.2075x+1.1387 | 0.8746 | B-2 | y=-3.159x2+5.4833x-1.3321 | 0.7024 | B-3 | y=-3.2155x2+5.3145x-1.1174 | 0.7923 | B-4 | y=-4.344x2+8.4964x-3.1482 | 0.9629 | B-5 | y=-2.8973x2+4.8027x-0.906 | 0.9258 |
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