Revealing the evolution of freeze-thaw damage in soil-rock mixtures with different moisture contents using characteristic parameters of electrochemical conductivity pathway equivalent models
Guanglin Tian , Hongwei Deng , Taoying Liu , Jielin Li , Xin Xiong
Journal of Central South University ›› : 1 -21.
Understanding the intrinsic relationship between microstructure and macroscopic properties under freeze-thaw (F–T) cycles is of great significance for advancing knowledge of soil-rock mixtures (SRM) in low-temperature environments. This study conducted F–T cycles, electrochemical impedance spectroscopy (EIS), and uniaxial compression mechanical tests on SRM with varying moisture contents. An equivalent circuit model of conductive paths was proposed, and the microstructure was characterized using the parameters of these paths. The paper examined the effects of varying moisture contents and F–T cycles on the characteristics of conductive paths and mechanical properties, exploring the underlying mechanisms. The results indicated that the increasing moisture content enlarged the cross-sectional area of CP and DSRP and enhanced the double-layer effect, while simultaneously reducing the ion concentration within DSRP. F–T cycling induced pore expansion and interconnection, resulting in increased contact areas and shortened lengths of CPP and CP, as well as increased contact areas and numbers of DSRP. The uniaxial strength degradation model based on ΔCDSRP(t) can be used to evaluate the peak strength after different cycles. Under F–T cycling, the expansion of DSRP exerted a deleterious effect on peak strength. Water – ice phase transitions increased the contact area of soil – rock cemented interfaces of DSRP and enhanced the double-layer effect.
soil-rock mixture / moisture content / electrochemical impedance spectrometry / microscopic structure / mechanical properties / deterioration model
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Central South University
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