岩土力学
巖土力學
암토역학
ROCK AND SOIL MECHANICS
2009年
12期
3783-3787,3792
,共6页
鲁祖德%陈从新%陈建胜%童志怡%左保成%戴旭明
魯祖德%陳從新%陳建勝%童誌怡%左保成%戴旭明
로조덕%진종신%진건성%동지이%좌보성%대욱명
强风化角岩%边坡岩体%现场直接剪切试验%强度%应力-应变关系
彊風化角巖%邊坡巖體%現場直接剪切試驗%彊度%應力-應變關繫
강풍화각암%변파암체%현장직접전절시험%강도%응력-응변관계
heavily weathered hornstone%side slope rock mass%field shearing test%strength%stress-strain relationship
采用堆载法进行天然状态与饱和状态下强风化角岩边坡岩体的现场直接剪切试验,获得不同正应力水平下剪切应力-剪切变形关系曲线和剪切强度参数,对其剪切应力-剪切变形关系曲线特征和不同正应力作用下剪应力随正应力的变化规律以及水-力耦合作用对剪切强度与变形特性影响进行了分析.试验结果表明:岩体峰值剪切强度和屈服剪切强度均随正应力的增大而增大;天然状态和饱水状态下剪应力随不同正应力的变化趋势基本相同;岩体剪切强度随含水率的增大而减小,在低法向应力下尤其敏感;水对岩体强度参数中黏聚力c的弱化作用更加明显,同时加大了岩体变形量,延长了岩体变形过程;通过现场直剪试验测得的法向变形可以估算岩体的压缩模量,为边坡稳定性分析提供参数.
採用堆載法進行天然狀態與飽和狀態下彊風化角巖邊坡巖體的現場直接剪切試驗,穫得不同正應力水平下剪切應力-剪切變形關繫麯線和剪切彊度參數,對其剪切應力-剪切變形關繫麯線特徵和不同正應力作用下剪應力隨正應力的變化規律以及水-力耦閤作用對剪切彊度與變形特性影響進行瞭分析.試驗結果錶明:巖體峰值剪切彊度和屈服剪切彊度均隨正應力的增大而增大;天然狀態和飽水狀態下剪應力隨不同正應力的變化趨勢基本相同;巖體剪切彊度隨含水率的增大而減小,在低法嚮應力下尤其敏感;水對巖體彊度參數中黏聚力c的弱化作用更加明顯,同時加大瞭巖體變形量,延長瞭巖體變形過程;通過現場直剪試驗測得的法嚮變形可以估算巖體的壓縮模量,為邊坡穩定性分析提供參數.
채용퇴재법진행천연상태여포화상태하강풍화각암변파암체적현장직접전절시험,획득불동정응력수평하전절응력-전절변형관계곡선화전절강도삼수,대기전절응력-전절변형관계곡선특정화불동정응력작용하전응력수정응력적변화규률이급수-력우합작용대전절강도여변형특성영향진행료분석.시험결과표명:암체봉치전절강도화굴복전절강도균수정응력적증대이증대;천연상태화포수상태하전응력수불동정응력적변화추세기본상동;암체전절강도수함수솔적증대이감소,재저법향응력하우기민감;수대암체강도삼수중점취력c적약화작용경가명현,동시가대료암체변형량,연장료암체변형과정;통과현장직전시험측득적법향변형가이고산암체적압축모량,위변파은정성분석제공삼수.
By using the method of preloading as vertical reaction, the field shearing test of heavily weathered hornstone side slope rock mass are carried out under the natural and the saturated condition. the shear stress - shear deformation relation curves under different normal stress levels and shear strength parameters are obtained. Based on the results of field shearing test, the effect of strength and deformation on mechanical-hydro coupling process and the change rule of the shear stress along with different normal stresses and the shear stress-deformation relation curves characteristics are analyzed. The test results indicate that, the peak shear strength and the yield shear strength increase with the increase of the normal stress; and the change of water content has not influence on the change rule of the shear stress along with different normal stresses. The shear strength decreases with the increase of water content; and it is especially sensitive under the low normal stress. Attenuated function for cohesive force of water is more obvious, and simultaneously has enlarged the rock mass amount of deformation and lengthened the rock mass distortion process. Modulus of compression of rock mass can be estimated by vertical deformation tested in the field shearing test.