Flume tests and corresponding numerical simulation of hydraulic/mechanical behavior of Tangjiashan landslide dam subjected to seepage loading

被引:8
作者
Xiong, Xi [1 ]
Matsumoto, Tatsunori [1 ]
Shi, Zhenming [2 ,3 ]
Zhang, Feng [4 ]
机构
[1] Kanazawa Univ, Inst Sci & Engn, Fac Geosci & Civil Engn, Kanazawa 9201192, Japan
[2] Tongji Univ, Coll Civil Engn, Dept Geotech Engn, Shanghai 200092, Peoples R China
[3] Tongji Univ, Key Lab Geotech & Underground Engn, Minist Educ, Shanghai 200092, Peoples R China
[4] Nagoya Inst Technol, Dept Civil Engn, Nagoya 4668555, Japan
基金
中国国家自然科学基金; 日本学术振兴会;
关键词
Landslide dam; Unsaturated soil; Flume test; Heterogeneous strata; Soil-water-air coupling; Finite element method; PREMONITORY FACTORS; FAILURE; MODEL;
D O I
10.1016/j.sandf.2022.101200
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Landslide dams (LDs) are usually composed of natural debris materials and normally exhibit heterogeneous strata along both the depth and run-out directions. In addition, LDs usually have weaker structures than undisturbed ground and are more vulnerable to seepage loading. Considering that the surface layer of naturally packed LD materials is mostly in an unsaturated state, it is undoubtedly important to investigate the hydraulic/mechanical behavior of LDs with heterogeneous strata subjected to seepage loading. In this paper, a systematic flume test program was firstly conducted, in which the Tangjiashan LD was carefully referenced for its model design. Three different water level rising rates and two different stratal arrangements were considered in the flume tests. Then, soil-water-air coupled finite element analyses were conducted to simulate the flume tests, and all the material parameters of the LD materials were carefully determined based on the results of element tests. A comparison of the test and calculated results showed the possibility of using the pro-posed numerical method to predict the occurrence of dam breaching and to estimate the risk of LD failure. Moreover, the hydraulic/ mechanical behavior of the LD materials and the heterogeneous strata of the LD were proven to be very important to the stability of the LD. Finally, from an engineering viewpoint, the possibility of utilizing a naturally formed LD, and not destroying it after its for-mation, is also discussed.(c) 2022 Production and hosting by Elsevier B.V. on behalf of The Japanese Geotechnical Society. This is an open access article under the CC BY -NC-ND license (http://creativecommons.org/licenses/by-nc-nd/4.0/).
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页数:21
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共 35 条
  • [1] Asaoka A., 2000, Soils and Foundations, V40, P99, DOI [10.3208/SANDF.40.2_99, DOI 10.3208/SANDF.40.2_99]
  • [2] AWAL R., 2011, J JAPAN SOC CIVIL EN, V67, pI
  • [3] Simulation of the erosion process of landslide dams due to overtopping considering variations in soil erodibility along depth
    Chang, D. S.
    Zhang, L. M.
    [J]. NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2010, 10 (04) : 933 - 946
  • [4] Modeling of natural dam failure modes and downstream riverbed morphological changes with different dam materials in a flume test
    Chen, Su-Chin
    Lin, Tsung-Wen
    Chen, Chien-Yuan
    [J]. ENGINEERING GEOLOGY, 2015, 188 : 148 - 158
  • [5] Chengdu Hydroelectric Investigation and Design Institute (CHIDI) in China, 2008, REP STAB ASS TANGJ L
  • [6] COSTA JE, 1988, GEOL SOC AM BULL, V100, P1054, DOI 10.1130/0016-7606(1988)100<1054:TFAFON>2.3.CO
  • [7] 2
  • [8] The relationship among the premonitory factors of landslide dam failure caused by seepage: an experimental study
    Dhungana, Prakash
    Wang, Fawu
    [J]. GEOENVIRONMENTAL DISASTERS, 2019, 6 (01)
  • [9] Prediction of the behaviour of landslide dams using a geomorphological dimensionless index
    Ermini, L
    Gasagli, N
    [J]. EARTH SURFACE PROCESSES AND LANDFORMS, 2003, 28 (01) : 31 - 47
  • [10] Simulating dam-breach flood scenarios of the Tangjiashan landslide dam induced by the Wenchuan Earthquake
    Fan, X.
    Tang, C. X.
    van Westen, C. J.
    Alkema, D.
    [J]. NATURAL HAZARDS AND EARTH SYSTEM SCIENCES, 2012, 12 (10) : 3031 - 3044