Hydro-mechanically coupled finite-element analysis of the stability of a fractured-rock slope using the equivalent continuum approach: a case study of planned reservoir banks in Blaubeuren, Germany

被引:0
作者
Song, Jie [1 ]
Dong, Mei [2 ]
Koltuk, Serdar [3 ]
Hu, Hui [3 ]
Zhang, Luqing [1 ]
Azzam, Rafig [3 ]
机构
[1] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Engn Geomech, Beitucheng Western Rd 19, Beijing 100029, Peoples R China
[2] Zhejiang Univ, Engn Res Ctr Urban Underground Dev Zhejiang Prov, Coll Civil Engn & Architecture, Yuhangtang Rd 866, Hangzhou, Zhejiang, Peoples R China
[3] Rhein Westfal TH Aachen, Dept Engn Geol & Hydrogeol, Lochnerstr 4-20, D-52064 Aachen, Germany
基金
中国国家自然科学基金;
关键词
Numerical modeling; Fractured rocks; Equivalent continuum approach; Hydro-mechanically coupled finite element analysis; Germany; NETWORKS; LENGTH; FIELD; MODEL; FLOW; MASS;
D O I
10.1007/s10040-017-1694-x
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Construction works associated with the building of reservoirs in mountain areas can damage the stability of adjacent valley slopes. Seepage processes caused by the filling and drawdown operations of reservoirs also affect the stability of the reservoir banks over time. The presented study investigates the stability of a fractured-rock slope subjected to seepage forces in the lower basin of a planned pumped-storage hydropower (PSH) plant in Blaubeuren, Germany. The investigation uses a hydro-mechanically coupled finite-element analyses. For this purpose, an equivalent continuum model is developed by using a representative elementary volume (REV) approach. To determine the minimum required REV size, a large number of discrete fracture networks are generated using Monte Carlo simulations. These analyses give a REV size of 28 x 28 m, which is sufficient to represent the equivalent hydraulic and mechanical properties of the investigated fractured-rock mass. The hydro-mechanically coupled analyses performed using this REV size show that the reservoir operations in the examined PSH plant have negligible effect on the adjacent valley slope.
引用
收藏
页码:803 / 817
页数:15
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