2008
DOI: 10.1016/j.ijrmms.2007.04.008
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Time-dependent deformation behaviors of weak sandstones

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Cited by 103 publications
(58 citation statements)
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“…Weak cataclastic rocks are widely used as the host rock medium in various applications of hydraulic engineering, such as dam foundation stability, tunnel support design, and hydraulic fracturing (Habimana et al 2002;Tsai et al 2008;Zhang et al 2013). Cataclastic rocks are a type of sedimentary rock with several fault zones (Elodie and Christopher 2010;Lori and James 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Weak cataclastic rocks are widely used as the host rock medium in various applications of hydraulic engineering, such as dam foundation stability, tunnel support design, and hydraulic fracturing (Habimana et al 2002;Tsai et al 2008;Zhang et al 2013). Cataclastic rocks are a type of sedimentary rock with several fault zones (Elodie and Christopher 2010;Lori and James 2012).…”
Section: Introductionmentioning
confidence: 99%
“…Furthermore, knowledge of the mechanical behavior of sandstone is important in geotechnical engineering (e.g., the design of waste repositories) and in petroleum geoscience (e.g., the prediction of reservoir deformation and fluid flow). For this reason, in the last few decades, many experimental studies have investigated the mechanical behavior of sandstone, including its strength, deformation behavior, failure characteristics and time-dependent behavior (Wong et al 1997;Baud et al 2000;Wu et al 2000;Klein et al 2001;Jeng et al 2002;Bésuelle et al 2003;Fortin et al 2006;Tembe et al 2008;Tsai et al 2008;Zorlu et al 2008;Heap et al 2009a, b;Tavallali and Vervoort 2010;Huang et al 2010;Yang and Jiang 2010;.…”
Section: Introductionmentioning
confidence: 99%
“…In addition to simulating immediate rock deformation, the time-dependent deformation (i.e., creep deformation) of rock is a major concern in engineering practice (Cristescu 1989;Hoxha et al 2005;Tomanovic 2006;Xie and Shao 2006;Sterpi and Gioda 2009;Weng et al 2010a, b). According to previous studies on creep deformation of sandstone (Tsai et al 2008;Weng et al 2010a), viscoplastic flows indicate that the viscoplastic potential surface has a similar shape to the plastic potential surface, but the size of the viscoplastic potential surface changes with time. The plastic potential surface has a time-independent size.…”
Section: Introductionmentioning
confidence: 88%
“…According to Jeng et al (2002), Weng et al (2005), and Tsai et al (2008), triaxial results show that the plastic potential surface of sandstone coincides with the yield surface in the prepeak stage. Therefore, the associated flow rule, n ¼ n gL=U and M f ¼ M g , can be used when formulating the constitutive model for sandstone.…”
Section: Dilatancy and Viscoplastic Flowmentioning
confidence: 94%