4.6 Article

An extended numerical manifold method for unsaturated soil-water interaction analysis at micro-scale

Publisher

WILEY
DOI: 10.1002/nag.3211

Keywords

capillary water; microscopic analysis; numerical manifold method; soil‐ water interaction; unsaturated soil

Funding

  1. National Key Research and Development Program of China [2017YFC1501302]
  2. National Natural Science Foundation of China [42077246, 41772309, 41941018]
  3. OutstandingYouth Foundation of Hubei Province, China [2019CFA074]
  4. China ScholarshipCouncil [201906270145]

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This study investigates unsaturated soil-water interaction at the micro-scale using an extended numerical manifold method (NMM) and validates the proposed capillary water solving framework. The results suggest that the extended method is a potential tool to explore unsaturated soil behaviors at the micro-scale.
To investigate unsaturated soil-water interaction at micro-scale, this study extends the numerical manifold method (NMM) by incorporating a soil-water coupling model considering specific capillary water distribution and capillary force calculation. The soil skeleton is constructed by a soil skeleton generation algorithm with random polygons. To more realistically capture the interaction between soil grains and capillary water, a capillary mechanics-based geometric algorithm is proposed to iteratively calculate the capillary water distribution. The capillary forces corresponding to the capillary water distribution are calculated based on the Young-Laplace equation. The proposed capillary water solving framework is first verified by reproducing the soil-water characteristic curve and the capillary water distribution of an ideal contact-disk model against analytical solutions. To further validate the ability of the capillary water solving framework to predict hydraulic behavior of the real soil, a laboratory test on the Toyoura sand is reproduced numerically. Then an ideal direct shear test is performed to further validate the two-way soil-water coupling procedure, in which a comparison between the numerical and analytical results regarding the shear strength and matric suction is presented. Finally, microscopic hydraulic and compression tests are conducted on two soil specimens with the same porosity and mean grain diameter but different uniformity coefficients. The results elucidate that the extended method is a potential tool to explore unsaturated soil behaviors at micro-scale.

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