ZHOU Qi-jian, MA De-cui, DENG Rong-gui, et al. Experimental study on mechanical properties of red-layer soft
rock in geothermal systems[J]. 2020, 41(10): 3333-3342.
DOI:
ZHOU Qi-jian, MA De-cui, DENG Rong-gui, et al. Experimental study on mechanical properties of red-layer soft
rock in geothermal systems[J]. 2020, 41(10): 3333-3342.DOI: 10.16285/j.rsm.2020.0035.
Experimental study on mechanical properties of red-layer soft
rock in geothermal systems
Geothermal energy is the development trend of green building. However
it is not clear about the relationship between the problems of building foundation impairment and the geothermal system in red-layer soft rock areas. Based on an accident investigation project of building clusters in Chengdu
the engineering characteristics of mudstone and gypsum rock with or without geothermal system were studied
and the macro-mechanical and micro-structural characteristics of rock under different heating methods
different temperatures and different soaking times were studied as well. The results show that: 1) At the same site
there is little influence of geothermal system on rock mechanical properties
but when geothermal system is in place
the number of fissures and the cumulative opening has an obvious increase. 2) With the increase of soaking time
the maximum water content of mudstone can reach more than 30%
the water content of gypsum can not exceed 15%
the water softening effect of mudstone is more obvious than that of gypsum
and the mechanical index of mudstone decreases with the increase of water content. 3) In the natural state
the gypsum rock is brittle and the mudstone is ductile; the water-rock interface of the gypsum rock has a significant effect of dissolution
and the dissolution of the gypsum rock is intensified from the surface to the interior. 4) In the temperature ranges from 20 °C to 50 °C
the compressive strength of gypsum rock parabolically changes with temperature
while that of mudstone monotonously increases. 5) The loose filling between geothermal pipe and rock mass is easy to form seepage pathway and change the hydrodynamic condition. Under the action of flowing water
the rock mass at the crack of gypsum rock and the weak interlayer dissolves
forming big cavity and inducing building subsidence.
Experimental study of mechanical characteristics of coal-serial mudstone under different temperatures
Experimental study of high embankment culvert treated by imperfect ditch covered with a geogrid layer
Experimental study of vertical bearing behaviors of super-long prestressed high-strength concrete pipe pile in soft clay
Experimental study of seismic behavior of prestressed pipe pile
Experimental study of the structural parameter of unsaturated loess
Related Author
ZHA Wen-hua
SONG Xin-long
WU Teng-fei
LI Xue
MA Qiang
ZHENG Jun-jie
ZHANG Jun
JIANG Zhen-chun
Related Institution
Key Laboratory of Safety and High-efficiency Coal Mining Constructed by Anhui Province and Ministry of Education, Anhui University of Science and Technology
School of Energy Resources and Safety, Anhui University of Science and Technology
School of Civil Engineering and Architecture, Hubei University of Technology
Institute of Geotechnical and Underground Engineering, Huazhong University of Science and Technology
Technical Management Office of Naval Defence Engineering