Citation: | DENG Guohua, GAO Huyan, ZHENG Jianguo, YU Wenlong, KANG Jiawei. Calculation method of dewatering settlement in saturated loess stratum[J]. Hydrogeology & Engineering Geology, 2025, 52(3): 174-185. doi: 10.16030/j.cnki.issn.1000-3665.202312039 |
In the construction of underground engineering with complex surrounding environment, reasonable prediction and evaluation of the influence of precipitation on the surrounding environment is a key problem to control the feasibility of the project. At present, the calculation of dewatering-induced settlement using the layered summation method heavily relies on empirical coefficients, leading to significant variability in predictions and deviations from actual observations. To predict the precipitation settlement of loess reasonably and accurately, based on the analysis of the physical properties of saturated loess, the void ratio and liquid index were introduced as key indicators to characterize both deformation potential and the deformation’s difficulty in the dewatering process. The practical calculation method of dewatering settlement of saturated loess stratum was established, and settlement verification was carried out at multiple sites. The results show that depending on the overlying pressure and groundwater action mode, saturated loess can form uncompacted saturated loess and compact saturated loess. The physical properties and dewatering settlement deformation of the two types of loess are different. The main physical property indexes affecting dewatering deposition deformation are the porosity ratio and liquid property index in the initial state, reflecting the deformation potential and the difficulty of deformation of saturated loess, respectively. The comparison between the calculation and measurement of six sites shows that the dewatering subsidence in the loess area mainly occurs in compact saturated loess where the macroporous structure still exists. The proposed e-IL method, incorporating void ratio and liquid index, effectively captures the settlement behavior of saturated loess. This study provides effective technical method for designing and constructing dewatering engineering in the loess area.
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Formation of two types of saturated loess
Evolution of pore ratio of loess stratum in Xi’an area
Evolution curve of liquidity index of loess stratum in Xi’an area
Verification of site layout
Comparison of SEM images of soil layers with internal characteristics in loess strata
Correlation between Es and e of each characteristic soil layer within the dewatering range
Correlation between Es and IL of each characteristic soil layer within the dewatering range
Correlation between Es and e·IL index of each characteristic soil layer within the dewatering range
Schematic diagram of stratum and dewatering depth of six sites
Summary of surface settlement and deformation history curves at each site
Comparison between predicted water loss settlement values and field measured values of six sites
Normalization curve of precipitation settlement at each site location