Research Article

Numerical Simulation of Flood Control Levee Deformation by Shield Tunnel Excavation through the Liuyang River: A Case Study

Table 1

Properties of the stratum.

Name of stratumCompositionDistribution locationAverage thickness

Plain fill <1-1>ClayHorizontal distribution of partially exposed surface3.50 m
Miscellaneous fill <1-2>Sandy gravel, concrete blocks, and other types of construction wasteHorizontal distribution of surface exposure2.76 m
Silty clay <1-6>Viscous siltBelow Liuyang River embankment3.33 m
Silt <1-7>Silty fine sandDiscontinuously distributed on the west side of the Liuyang River2.82 m
Silty fine sand <1-8>Fine sand and siltDiscontinuously distributed on the west side of the Liuyang River1.50 m
Rounded gravel <1-11>Siliceous rock and quartzLiuyang Riverbed3.16 m
Silty clay <2-1>Clay and powderDistributed on the east side of the Liuyang River3.44 m
Rounded gravel <2-6>Silicate, medium sand, and coarse sandHorizontal distribution in the east of the Liuyang River3.72 m
Highly weathered argillaceous siltstone <7-2>Muddy siltstoneMainly distributed under flood control levees and riverbeds8.71 m