Experimental and Numerical Studies on Permeability Properties of Thermal Damaged Red Sandstone under Different Confining Pressures

Abstract

The stability and safety of underground rock mass engineering are closely related to the permeability process of fluids and permeability properties of rocks. To reveal the flow behavior of fluid in thermal damaged rock, first, a rock seepage testing system was applied to study the permeability properties of red sandstone specimens after different high-temperature treatments from 200 to 800°C under different confining pressures of 10 to 30 MPa. Meanwhile, the microstructures of the red sandstone specimens were characterized by the mercury intrusion porosimetry (MIP) and scanning electron microscopy (SEM). Then, the permeability process of pore water pressure and the flow form of fluid also were investigated by the numerical modeling method. The results show that the permeability properties of red sandstone specimens after high-temperature exposure follow linear Darcy’s law, and the relation between confining pressures and equivalent permeability coefficient ( K 0 ) can be described by a power function. Besides, the phenomenon that microscopic structural deterioration is intensified with increasing temperature and the average pore size and porosity of the red sandstone specimens are both power functions is related to the equivalent permeability coefficient. Furthermore, the results of numerical modeling indicated that the flow field within the range affected by confining pressures gradually becomes stable and orderly from disorder, and flow lines of the fluid become smooth and straight, and perpendicular to the isosurface of pore water pressure as time goes by. Moreover, the nonlinear correlation between pore water pressure and seepage path length changes to a linear correlation, which is consistent with linear Darcy’s law.

Engineering Characteristics and Application Analysis of Red Sandstone in the Lanzhou Metro

“…Sandstone. The general characteristic index dry density data was collated according to the Standard for Geotechnical Test Methods (GB/T50123-1999), Equations ( 15)- (17) are often used to calculate their arithmetic mean x̅ , standard deviation s, and coefficient of variation c v to discern their reliability.…”

“…Ma et al [16] concluded that clay minerals influence the disintegration process of red sandstone by analyzing the rock properties such as basic physical indicators and microstructural parameters of red sandstone slopes. Zhao et al [17] revealed the permeability characteristics of thermally damaged red sandstones under freeze-thaw cycles and different envelope pressures. Yin et al [18] concluded that red sandstone disintegration is caused by particle bonding fractures when encountering water.…”

Energy Evolution and Acoustic Emission Characteristics of Uniaxial Compression Failure of Anchored Layered Sandstone

“…The fractal dimension of acoustic emission events in rock failure process is a measure of the disorder of micro-cracks in rock, which can reflect the tendency of micro-damage evolution to macro-cracks (Liu et al, 2019;Ma et al, 2021;Zhao et al, 2021). Xie et al (2011) proposed a sphere-covering method and columncovering method to predict the spatial fractal distribution of rock acoustic emission events (Figure 11).…”