基于不同分形模型的冻融黄土孔隙特征研究
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陈鑫, 张泽, 李东庆
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Study on the pore features of freezing-thawing loess based on different fractal models
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Xin CHEN, Ze ZHANG, Dongqing LI
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表2 经历不同冻融次数后土样分形维数计算结果
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Table 2 Calculation results of fractal dimension of soil specimen after various freeze-thaw cycles
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FT/次 | 毛细管压力曲线法 | Menger海绵模型 | 热力学模型 |
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DS | R2 | P<0.59 MPa | P>0.59 MPa | DT | R2 |
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DM | R2 | DM | R2 |
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0 | 2.5203 | 0.8487 | 2.8578 | 0.9269 | 2.636 | 0.9716 | 2.8013 | 0.9979 | 4 | 2.4918 | 0.8605 | 3.4361 | 0.3255 | 2.544 | 0.9923 | 2.7489 | 0.9984 | 6 | 2.4716 | 0.8537 | 3.6415 | 0.264 | 2.567 | 0.9944 | 2.7452 | 0.9985 | 8 | 2.4626 | 0.8563 | 3.7707 | 0.0735 | 2.527 | 0.9961 | 2.7462 | 0.9981 | 10 | 2.4489 | 0.8243 | 3.7765 | 0.1002 | 2.529 | 0.9864 | 2.7363 | 0.9984 | 50 | 2.5269 | 0.8668 | 3.0759 | 0.5439 | 2.625 | 0.9874 | 2.76 | 0.9989 | 100 | 2.5413 | 0.8768 | 4.0419 | 0.0037 | 2.632 | 0.9789 | 2.7566 | 0.9986 |
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