4.6 Article

Soil-Water Characteristics and Creep Deformation of Unsaturated Expansive Subgrade Soil: Experimental Test and Simulation

Journal

FRONTIERS IN EARTH SCIENCE
Volume 9, Issue -, Pages -

Publisher

FRONTIERS MEDIA SA
DOI: 10.3389/feart.2021.783273

Keywords

subgrade engineering; expansive soil; soil-water characteristics; creep behavior; numerical simulation

Funding

  1. National Natural Science Foundation of China [51908562]
  2. Standardization Project of Hunan Province
  3. Research Foundation of Education Bureau of Hunan Province [19B581]
  4. Natural Science Foundation of Hunan Province, China [2020JJ5987]
  5. Natural Science Foundation of Chongqing, China [cstc2018jcyjAX0640]

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The study focused on the stability of unsaturated expansive soil subgrade considering rainfall and creep behavior. Results showed that the compaction degree and stress state of the soil were closely related to its water holding capacity. The nonlinearity of creep behavior became increasingly obvious with time and stress level.
The creep deformation of expansive soil has been considered as a vital threat to the safety in engineering construction because it may cause serious slope diseases in geological engineering. Meanwhile, since expansive soil usually remains in unsaturated state, its mechanical property is significantly affected by the seasonal environment. Therefore, the nonlinear deformation of expansive soil has received increasing attention, especially the humidity-dependent creep properties. This study focused on the stability of the unsaturated expansive soil subgrade considering rainfall and the creep behavior. Pressure plate extractor and direct shear tests were performed to investigate the hydro-mechanical and creep characteristics of the unsaturated expansive soil. Both the Van-Genuchten and Burgers models were applied to analyze the test results and inserted into the numerical model of the slope under rainfall infiltration. Results show that the compaction degree and the stress state was closely related to the water holding capacity of the expansive soil. The nonlinearity of the creep behavior became increasingly obvious with the increase of time and the stress level. The safety factor of the slope decreased as the rainfall time increased, and the most dangerous slide of the slope moved toward the foot of the slope. Considering the long-term creep process, there was a period of rapid growth in horizontal displacement that is detrimental to the stability of the slope. Besides, the rainfall infiltration could accelerate the slope failure before and after this creep process.

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