Analytical solution for dissipation of excess pore water pressure
and soil consolidation settlement induced by tunneling under
the influence of long-term leakage
|更新时间:2026-06-25
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Analytical solution for dissipation of excess pore water pressure
and soil consolidation settlement induced by tunneling under
the influence of long-term leakage
ZHANG Zhi-guo, HUANG Mao-song, YANG Xuan. Analytical solution for dissipation of excess pore water pressure
and soil consolidation settlement induced by tunneling under
the influence of long-term leakage[J]. 2019, 40(8): 3135-3144.
DOI:
ZHANG Zhi-guo, HUANG Mao-song, YANG Xuan. Analytical solution for dissipation of excess pore water pressure
and soil consolidation settlement induced by tunneling under
the influence of long-term leakage[J]. 2019, 40(8): 3135-3144.DOI: 10.16285/j.rsm.2018.0913.
Analytical solution for dissipation of excess pore water pressure
and soil consolidation settlement induced by tunneling under
the influence of long-term leakage
Considering semi-permeable boundary condition and Terzaghi-Rendulic consolidation theory
the dissipation solution of excess pore water pressure and the ground surface consolidation settlement are obtained by using the conformal mapping and separation variable method. The analytical results are compared with the measured results from project cases
which shows good agreement. In addition
the influence laws of the soil consolidation settlement and the excess pore water pressure are obtained via the parameter analysis. The results show that the larger the permeable ratio of soil and lining is
the larger the initial rate of consolidation settlement is
but it has no influence on the final convergence value. The smaller the elastic modulus of soil is
the larger the final consolidation settlement is. The excess pore water pressure gradually increases with time
while it dissipates on a large scale in a short time after the excavation of the tunnel. The speed becomes slow when the value reaches to about one-tenth of the initial value. The longer the distance to the lining is
the smaller the initial excess pore water pressure is
and the slower the corresponding dissipation speed is.