岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2013年
8期
2143-2150
,共8页
宋东日%任伟中%黄诚%王安礼%张军
宋東日%任偉中%黃誠%王安禮%張軍
송동일%임위중%황성%왕안례%장군
岩质边坡%节理%分量式本构模型%剪胀%双安全系数
巖質邊坡%節理%分量式本構模型%剪脹%雙安全繫數
암질변파%절리%분량식본구모형%전창%쌍안전계수
rock slope%joint%component constitutive model%dilation%dual safety factors
在法向荷载和切向荷载的作用下岩体节理的剪切应力由抗剪断效应、剪胀效应和摩擦效应所引起的三部分应力构成,但三个组成部分在节理的剪切过程中并不是同时发挥其最大作用。在详细分析边坡岩体节理工程地质特性的基础上,提出一种节理分量式剪切本构模型,主要特征为(1)体现了剪胀与剪切之间的耦合效应;(2)采用分量式表达,物理意义更明确;(3)每一分量采用简单函数,避免了总量式分段构造函数的不足。在节理分量式本构模型基础上,提出应用于岩质节理边坡的双安全系数的概念和求解原则,双安全系数能够较好地反映岩体节理剪切破坏直至残余强度的物理过程。最后,通过双安全系数算例明确了各个分量对于边坡稳定性的贡献。
在法嚮荷載和切嚮荷載的作用下巖體節理的剪切應力由抗剪斷效應、剪脹效應和摩抆效應所引起的三部分應力構成,但三箇組成部分在節理的剪切過程中併不是同時髮揮其最大作用。在詳細分析邊坡巖體節理工程地質特性的基礎上,提齣一種節理分量式剪切本構模型,主要特徵為(1)體現瞭剪脹與剪切之間的耦閤效應;(2)採用分量式錶達,物理意義更明確;(3)每一分量採用簡單函數,避免瞭總量式分段構造函數的不足。在節理分量式本構模型基礎上,提齣應用于巖質節理邊坡的雙安全繫數的概唸和求解原則,雙安全繫數能夠較好地反映巖體節理剪切破壞直至殘餘彊度的物理過程。最後,通過雙安全繫數算例明確瞭各箇分量對于邊坡穩定性的貢獻。
재법향하재화절향하재적작용하암체절리적전절응력유항전단효응、전창효응화마찰효응소인기적삼부분응력구성,단삼개조성부분재절리적전절과정중병불시동시발휘기최대작용。재상세분석변파암체절리공정지질특성적기출상,제출일충절리분량식전절본구모형,주요특정위(1)체현료전창여전절지간적우합효응;(2)채용분량식표체,물리의의경명학;(3)매일분량채용간단함수,피면료총량식분단구조함수적불족。재절리분량식본구모형기출상,제출응용우암질절리변파적쌍안전계수적개념화구해원칙,쌍안전계수능구교호지반영암체절리전절파배직지잔여강도적물리과정。최후,통과쌍안전계수산례명학료각개분량대우변파은정성적공헌。
The shear stress of a rock joint is composed of three components triggered by anti-shear effect, dilatancy effect, and frictional effect under normal load and shear load; but the three components will not exert their maximum at the same point in the shear process of a rock joint. Firstly, the five main engineering geological properties of rock slope joints are analyzed in detail, which will provide engineering conditions for the component constitutive model. A component constitutive model of rock joints is presented and its characteristics are as follows: (1) The coupling effect between dilation and shearing is considered. (2) The component constitutive model has obvious physical meanings. (3) Each component is composed with a simple function, so segmental fitting functions are not needed. Furthermore, based on the component constitutive model of rock joints, the concept and solving principle of dual safety factors for jointed rock slope are put forward, which will directly show the physical process from shear failure to residual strength. The three components’ contribution to the slope stability is clarified by a calculation example.