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Estimating pore volume compressibility by spheroidal pore modeling of digital rocks
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SUI Weibo,QUAN Zihan,HOU Yanan,CHENG Haoran
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Table 1 Aspect ratios and volume proportions of different types of pores in the spheroidal pore models of the 10 digital core samples.
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No. | Sample name | Prolate ellipsoidal pores | Oblate ellipsoidal pores | Spherical pores | Poro- sity/% | Volume proportion/% | Aspect ratio | Mean | Variance | Volume proportion/% | Aspect ratio | Mean | Variance | Volume proportion/% | 1 | Bentheimer sandstone | 54.19 | 1.11-7.96 | 2.07 | 0.440 | 45.76 | 0.16-0.90 | 0.54 | 0.020 | 0.04 | 23 | 2 | Doddington sandstone | 54.83 | 1.13-9.40 | 2.37 | 0.820 | 45.15 | 0.15-0.86 | 0.54 | 0.030 | 0.02 | 25 | 3 | Estaillades carbonate | 60.28 | 1.11-12.75 | 2.26 | 1.120 | 39.51 | 0.15-0.87 | 0.57 | 0.030 | 0.21 | 25 | 4 | Berea sandstone | 45.00 | 1.11-4.90 | 1.86 | 0.380 | 54.11 | 0.23-0.90 | 0.60 | 0.005 | 0.89 | 15 | 5 | Fountainebleau sandstone | 38.85 | 1.12-4.87 | 1.74 | 0.340 | 58.25 | 0.22-0.90 | 0.64 | 0.030 | 2.91 | 8 | 6 | Wilcox sandstone | 66.43 | 1.15-8.31 | 2.52 | 1.270 | 32.83 | 0.12-0.87 | 0.51 | 0.030 | 0.74 | 2 | 7 | Daqing sandstone | 57.71 | 1.11-9.58 | 2.43 | 0.830 | 42.23 | 0.11-0.88 | 0.50 | 0.020 | 0.06 | 13 | 8 | Tarim sandstone | 59.75 | 1.13-10.84 | 2.25 | 0.800 | 40.11 | 0.12-0.90 | 0.54 | 0.020 | 0.14 | 13 | 9 | Eastern South China Sea sandstone | 57.69 | 1.14-10.72 | 2.38 | 0.880 | 42.19 | 0.13-0.88 | 0.52 | 0.020 | 0.12 | 14 | 10 | Xinjiang sandstone | 60.91 | 1.14-12.12 | 2.34 | 0.860 | 38.97 | 0.12-0.88 | 0.52 | 0.020 | 0.12 | 12 |
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