中文概要
目 的
综合使用 HYPROP 和 WP4C 两种仪器, 探索 采用蒸发法和冷镜露点法测量大吸力范围的水-土特征曲线, 并采用收缩曲线对土体变形进行修 正。
方 法
1. 方法, 在 0∼100 kPa 吸力范围内 测量土体的水-土特征曲线。 2. 当吸力大于 600 kPa 时, 采用WP4C 仪器, 测量土体的水-土 特征曲线。 3. 采用传统张力仪吸力板仪器, 在 0∼500 kPa 吸力范围内测量土体的水-土特征曲 线。 4. 采用 Satyanaga et al. (2017)公式, 对实验 数据进行拟合。 5. 采用 HYPROP 仪器直接测量土 体的非饱和渗透系数。 6. 采用蒸发法, 获取干缩 曲线。
结 论
1. 采用 Satyanaga et al. (2017)公式, 对实验数据进 行拟合, 拟合参数直接关联到进气值、拐点及方 差。拟合结果显示, 不同仪器所收集的水-土特征 曲线的数据相互吻合, 为水-土特征曲线的实验测 量提供了更大的吸力范围。 2. 采用 HYPROP 仪器 测量的非饱和渗透系数和采用传统改装的非饱 和三轴实验数据基本吻合, , 因此, HYPROP 可以 作为在低吸力范围内 (<100 kPa) 测量非饱和渗 透系数的有效仪器。 3. 当进气值小于 100 kPa 或 者大于 500 kPa 时, 综合采用 HYPROP 和 WP4C 可以有效缩短实验周期。
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Acknowledgements
The authors would like to acknowledge the assistance from Prof. Qian ZHAI from Key Laboratory for RC and PRC Structures of the Ministry of Education, Southeast University, China in providing the Chinese translation of the summary of the paper. The authors also acknowledge the assistances from Mr. Jeremy TAN and Ms. Yu-ying WANG during the collection of the data in this study.
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Measurement of a soil-water characteristic curve and unsaturated permeability using the evaporation method and the chilled-mirror method
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Satyanaga, A., Rahardjo, H., Koh, Z.H. et al. Measurement of a soil-water characteristic curve and unsaturated permeability using the evaporation method and the chilled-mirror method. J. Zhejiang Univ. Sci. A 20, 368–374 (2019). https://doi.org/10.1631/jzus.A1800593
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DOI: https://doi.org/10.1631/jzus.A1800593