Seasonal differences in seismic responses of embankment on a sloping ground in permafrost regions
Seasonal differences in seismic responses of embankment on a sloping ground in permafrost regions
复制标题
多年冻土区坡地路堤地震响应的季节差异
DOI:
10.1016/j.soildyn.2015.01.005
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发表时间:
2015
影响因子:
4
通讯作者:
Yu Wenbing
中科院分区:
文献类型:
--
作者:
Li Shuangyang;Lai Yuanming;Zhang Mingyi;Yu Wenbing
Because of its direct influence on the amount of unfrozen water and on the strength of intergranular ice in a frozen soil, temperature has a significant effect on all aspects of the mechanical behavior of the active layer in which temperature fluctuates above and below 0 °C. Hence seismic responses of engineering structures such as embankment on a sloping ground in permafrost regions exhibit obvious differences with seasonal alternation. To explore the distinctive seismic characteristics of a railway embankment on the sloping ground in permafrost regions, a coupled water-heat-dynamics model is built based on theories of heat transfer, soil moisture dynamics, frozen soil mechanics, soil dynamics, and so on. A well-monitored railway embankment on a sloping ground in Qinghai–Tibet Plateau is taken as an example to simulate seismic responses in four typical seasons in the 25th service year. The numerical results show that seismic acceleration, velocity and displacement responses are significantly different in four typical seasons, and the responses on October 15 are much higher among the four seasons. When the earthquake is over, there are still permanent differential deformations in the embankment and even severe damages on the left slope on October 15. Therefore, this position should be monitored closely and repaired timely to ensure safe operation. In addition, the numerical model and results may be a reference for maintenance, design and study on other embankments in permafrost regions.