Analysis of monitoring microseism in areas controlled by faults near powerhouse in Dagangshan hydropower station

被引:0
|
作者
Zhang Bo-hu [1 ,2 ]
Deng Jian-hui [1 ]
Zhou Zhi-hui [1 ]
Lu Hong-xu [1 ]
Wu Ji-chang [3 ]
Wu Si-hao [3 ]
机构
[1] Sichuan Univ, State Key Lab Hydraul & Mt River Engn, Chengdu 610065, Sichuan, Peoples R China
[2] Southwest Petr Univ, Sch Civil Engn & Architecture, Chengdu 610500, Sichuan, Peoples R China
[3] Dadu River Dagangshan Hydropower Dev Co Ltd, Shimian 625409, Sichuan, Peoples R China
关键词
microseismic monitoring; hydropower project; underground powerhouse; collapse empty area; fault; stability;
D O I
暂无
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Many faults propagate near the underground powerhouse of Dagangshan power station. Rockmass stability of the underground powerhouse is controlled by two steep angle faults which are extended through the middle and rear parts of the powerhouse. The collapse area near the fault was found when the fault extended through the vault was excavated. So it is necessary to monitor the stability of the powerhouse and collapse area near the faults. The integrated seismic system(ISS) of South Africa is established to monitor the area in October 2010. The unattended system run automatically, which also can be controlled and diagnosed remotely. Four methods such as spatiotemporal distribution method, magnitude level method, energy index method and dislocation method are used to analyze the stability of the collapse area, side walls and the rock mass near the structure plane. The research results show that the underground plant is overall stable and safe. Few seismic events and low magnitude near the collapse area can be got from seismic monitoring data. Two side walls are stable because the number of the seismic events and dislocation slip of the rock mass are small. The slide displacement between the structural planes is scattered and small. And the rock of the fault plane is inactive. Therefore, the stability of collapse area is increased and less influenced by faults after the rock is reinforced by the anchor. It is of guide significance to use microseismic monitoring to assess the stability of power house during the running and construction stages.
引用
收藏
页码:213 / 218
页数:6
相关论文
共 16 条
  • [1] [李庶林 Li Shulin], 2005, [岩石力学与工程学报, Chinese Journal of Rock Mechanics and Engineering], V24, P2048
  • [2] [陈炳瑞 Chen Bingrui], 2011, [岩石力学与工程学报, Chinese Journal of Rock Mechanics and Engineering], V30, P275
  • [3] Dong L., 2011, CHINESE J ROCK MECH, V30, P2058
  • [4] Violent failure of a remnant in a deep South African gold mine
    Durrheim, RJ
    Haile, A
    Roberts, MKC
    Schweitzer, JK
    Spottiswoode, SM
    Klokow, JW
    [J]. TECTONOPHYSICS, 1998, 289 (1-3) : 105 - 116
  • [5] [唐礼忠 Tang Lizhong], 2010, [岩石力学与工程学报, Chinese Journal of Rock Mechanics and Engineering], V29, P1818
  • [6] Lu Z.H., 1989, EARTHQUAKE, V10, P32
  • [7] Mendecki A.J., 1997, SEISMIC MONITORING M, P87
  • [8] Characteristics of microseismic events induced during hydraulic fracturing experiments at the Hijiori hot dry rock geothermal energy site, Yamagata, Japan
    Sasaki, S
    [J]. TECTONOPHYSICS, 1998, 289 (1-3) : 171 - 188
  • [9] Precursory monitoring of impending rockbursts in Kolar gold mines from microseismic emissions at deeper levels
    Srinivasan, C
    Arora, SK
    Benady, S
    [J]. INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1999, 36 (07): : 941 - 948
  • [10] [唐礼忠 TANG Lizhong], 2011, [岩石力学与工程学报, Chinese Journal of Rock Mechanics and Engineering], V30, P1168