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軟巖流變的尺寸效應

Scale effect of soft rock rheology

  • 摘要: 巖體內隨機分布結構面對軟巖流變的影響主要表現為尺寸效應.通過對四種不同尺寸砂質頁巖試件的分級增量循環加、卸載單軸壓縮蠕變實驗,揭示了該類軟巖的流變可以用薩烏斯托維奇模型來描述,模型的三個本構參數EH(線彈性參數)、EK(黏彈性參數)和ηK(黏性系數)值隨軟巖試件尺寸增大而不斷減小并最終趨于一定值,這一規律可用具有極值條件的非線性回歸方程來表達.由此獲得了求解結構面隨機分布條件下工程巖體連續微元尺寸的外推方法,利用該法可通過對室內不同尺寸巖石試件的流變力學實驗確定在連續性概化范圍內工程巖體的流變模型及其力學參數值.

     

    Abstract: The influence of random-distributing structure surfaces in rock mass on the soft rock rheology is mainly expressed by scale effect. Multi-step incremental cycling loading and unloading uniaxial compression creep tests on 4 different sizes of sand-shale specimens showed that soft rock rheology could be described by the Salustowicz model and the values of its constitutive parameters of E H(linear elastic parameter), EK(viscoelastic parameter) and ηK(viscous parameter) would decrease and tend towards being constant as the specimen size increased, which might be expressed by nonlinear regressive equations with extremum conditions. Then an extrapolation method was gained to determine the dimension of the continuous micro element of engineering rock mass with randomly distributing structure surfaces. It may be used to gain the rheological model and its mechanical parameters of engineering rock mass in the continuity schematization range by rheological tests on the different sizes of rock specimens in the laboratory.

     

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