岩石力学与工程学报
巖石力學與工程學報
암석역학여공정학보
CHINESE JOURNAL OF ROCK MECHANICS AND ENGINEERING
2014年
2期
376-389
,共14页
岩土力学%岩土材料%强度准则%SMP准则%广义Mises准则
巖土力學%巖土材料%彊度準則%SMP準則%廣義Mises準則
암토역학%암토재료%강도준칙%SMP준칙%엄의Mises준칙
rock and soil mechanics%geomaterials%strength criterion%SMP criterion%generalized von Mises criterion
针对岩土材料的压剪耦合特性,将原广义非线性强度理论(GNST)扩展为可合理考虑岩土材料屈服与破坏特性的广义非线性屈服准则。在偏平面上,屈服准则表达式采用SMP准则与广义Mises准则的插值表达式;在子午面上,屈服准则表达式采用可考虑压剪耦合特性的封闭曲线表达式。由于在过渡空间中建立相应的屈服准则表达式,因此与已有的Matsuoka-Nakai准则与Lade-Duncan准则的插值准则(MNLD准则)相比,新准则描述屈服时采用非线性强度曲线,同时能够更合理地考虑静水压力对于偏平面以及子午面上屈服特性的影响,模型参数均具有物理意义,且通过常规试验可以确定。通过不同岩土材料的破坏以及屈服特性的试验预测对比,验证了新准则在描述岩土材料压剪耦合特性方面的合理性。
針對巖土材料的壓剪耦閤特性,將原廣義非線性彊度理論(GNST)擴展為可閤理攷慮巖土材料屈服與破壞特性的廣義非線性屈服準則。在偏平麵上,屈服準則錶達式採用SMP準則與廣義Mises準則的插值錶達式;在子午麵上,屈服準則錶達式採用可攷慮壓剪耦閤特性的封閉麯線錶達式。由于在過渡空間中建立相應的屈服準則錶達式,因此與已有的Matsuoka-Nakai準則與Lade-Duncan準則的插值準則(MNLD準則)相比,新準則描述屈服時採用非線性彊度麯線,同時能夠更閤理地攷慮靜水壓力對于偏平麵以及子午麵上屈服特性的影響,模型參數均具有物理意義,且通過常規試驗可以確定。通過不同巖土材料的破壞以及屈服特性的試驗預測對比,驗證瞭新準則在描述巖土材料壓剪耦閤特性方麵的閤理性。
침대암토재료적압전우합특성,장원엄의비선성강도이론(GNST)확전위가합리고필암토재료굴복여파배특성적엄의비선성굴복준칙。재편평면상,굴복준칙표체식채용SMP준칙여엄의Mises준칙적삽치표체식;재자오면상,굴복준칙표체식채용가고필압전우합특성적봉폐곡선표체식。유우재과도공간중건립상응적굴복준칙표체식,인차여이유적Matsuoka-Nakai준칙여Lade-Duncan준칙적삽치준칙(MNLD준칙)상비,신준칙묘술굴복시채용비선성강도곡선,동시능구경합리지고필정수압력대우편평면이급자오면상굴복특성적영향,모형삼수균구유물리의의,차통과상규시험가이학정。통과불동암토재료적파배이급굴복특성적시험예측대비,험증료신준칙재묘술암토재료압전우합특성방면적합이성。
A new generalized nonlinear yield criterion(GNYC) is proposed to describe the yield and failure behaviors of geomaterials,including the coupling behavior of shearing and compression,through extending the generalized nonlinear strength theory(GNST). The interpolation function between SMP criterion and generalized von Mises criterion is adopted as the yield function of the new criterion on deviatoric plane;while the closed curve function considering coupling behavior of shearing and compression is adopted as the yield function on meridian plane. As the yield function is established in the transitional stress space,the nonlinear power function is adopted as the failure curve in new yield criterion,which can be described using the proposed criterion compared to the MNLD criterion(interpolation criterion between Matsuoka-Nakai criterion and Lade-Duncan criterion). The influence of the variation of hydrostatic stress on yield behavior on deviatoric and meridian planes can also be described more reasonably by the new criterion. There are physical meanings for all parameters in the new criterion and the values of parameters can all be determined by conventional tests. The validity of the new criterion is confirmed by data from yield and failure tests of different geomaterials.