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Model Experimental Study on the Seepage and Failure Features of Tunnel under Wetting-Drying Alternation with Increasing Water Pressure
Geofluids ( IF 1.2 ) Pub Date : 2020-07-04 , DOI: 10.1155/2020/8845528
Haijian Su 1 , Yujie Feng 1 , Qingzhen Guo 1 , Hongwen Jing 1 , Wenxin Zhu 2
Affiliation  

Wetting-drying alternation caused by seasonal rainfall and water fluctuation has a negative effect on the rock mass. Model experiments were conducted in this paper to investigate the role of wetting-drying alternation on the seepage and failure features of a tunnel. Water-bearing structure was located in the lateral position of tunnel. The stratum thickness between the tunnel and water-bearing structure was ranged from 20 to 100 mm. The results showed that, with an increase in the wetting-drying alternation number, the pore water pressure increases gradually. The critical water pressure also increases gradually with the increasing thickness of water-resisting stratum. With the increase of the stratum thickness, the permeable area is gradually widened and the water storage capacity becomes stronger. The failure mode of water-resisting stratum under geostress and water pressure can be summarized as two types: fracture failure (thickness of 20 mm) and slippage failure (thickness between 40 and 100 mm), respectively.

中文翻译:

干湿交替下隧道渗流破坏特征模型试验研究

季节性降雨和水位波动引起的干湿交替对岩体有不利影响。本文通过模型试验研究干湿交替对隧道渗流破坏特征的影响。含水结构位于隧道横向位置。隧道与含水结构之间的地层厚度为20~100 mm。结果表明,随着干湿交替数的增加,孔隙水压力逐渐增加。临界水压也随着阻水地层厚度的增加而逐渐增加。随着地层厚度的增加,渗透面积逐渐扩大,蓄水能力增强。
更新日期:2020-07-04
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