实验力学
實驗力學
실험역학
JOURNAL OF EXPERIMENTAL MECHANICS
2009年
5期
459-466
,共8页
刘传孝%张加旺%张美政%张福俊
劉傳孝%張加旺%張美政%張福俊
류전효%장가왕%장미정%장복준
分级加卸载%应力-应变等时曲线%Gauss分布%相关系数%短时蠕变实验
分級加卸載%應力-應變等時麯線%Gauss分佈%相關繫數%短時蠕變實驗
분급가사재%응력-응변등시곡선%Gauss분포%상관계수%단시연변실험
step loading-unloading%isochronous stress-strain curves%Gauss distribution%correlative coefficient%short-term creep experiment
由单向抗压强度实验及8级加卸载短时蠕变实验,得到蠕变下限为27MPa的细砂岩试样典型的坚硬岩石脆性断裂特征.应力-应变等时曲线线性回归函数的相关系数均高于0.92,长期强度与瞬时强度之比达94.39%,证明细砂岩试样的整体蠕变特性不强.应力-轴向应变等时曲线线性回归函数的平均相关系数高出应力-径向应变等时曲线线性回归函数的平均相关系数3.92%,因此其轴向非线性蠕变特性相对于径向非线性蠕变特性更弱.随着时间延续,细砂岩试样的非线性蠕变特性总体服从负Gauss分布规律,具有明显的时间效应.随加载应力水平的提高,应力-轴向应变等时曲线和应力-径向应变等时曲线线性拟合函数的平均相关系数下降幅度分别为0.97%和0.67%,线性相关性普遍降低.所以细砂岩试样的非线性蠕变程度随加载应力水平的提高而提高,载荷效应明显.
由單嚮抗壓彊度實驗及8級加卸載短時蠕變實驗,得到蠕變下限為27MPa的細砂巖試樣典型的堅硬巖石脆性斷裂特徵.應力-應變等時麯線線性迴歸函數的相關繫數均高于0.92,長期彊度與瞬時彊度之比達94.39%,證明細砂巖試樣的整體蠕變特性不彊.應力-軸嚮應變等時麯線線性迴歸函數的平均相關繫數高齣應力-徑嚮應變等時麯線線性迴歸函數的平均相關繫數3.92%,因此其軸嚮非線性蠕變特性相對于徑嚮非線性蠕變特性更弱.隨著時間延續,細砂巖試樣的非線性蠕變特性總體服從負Gauss分佈規律,具有明顯的時間效應.隨加載應力水平的提高,應力-軸嚮應變等時麯線和應力-徑嚮應變等時麯線線性擬閤函數的平均相關繫數下降幅度分彆為0.97%和0.67%,線性相關性普遍降低.所以細砂巖試樣的非線性蠕變程度隨加載應力水平的提高而提高,載荷效應明顯.
유단향항압강도실험급8급가사재단시연변실험,득도연변하한위27MPa적세사암시양전형적견경암석취성단렬특정.응력-응변등시곡선선성회귀함수적상관계수균고우0.92,장기강도여순시강도지비체94.39%,증명세사암시양적정체연변특성불강.응력-축향응변등시곡선선성회귀함수적평균상관계수고출응력-경향응변등시곡선선성회귀함수적평균상관계수3.92%,인차기축향비선성연변특성상대우경향비선성연변특성경약.수착시간연속,세사암시양적비선성연변특성총체복종부Gauss분포규률,구유명현적시간효응.수가재응력수평적제고,응력-축향응변등시곡선화응력-경향응변등시곡선선성의합함수적평균상관계수하강폭도분별위0.97%화0.67%,선성상관성보편강저.소이세사암시양적비선성연변정도수가재응력수평적제고이제고,재하효응명현.
Based on experimental results of uniaxial compression and short-term creep using 8-step loading-unloading method, fine sandstone specimen, which lower creep limit is 27MPa, present typical brittle breakage properties of hard rock. The correlative coefficients of linear regression function for isochronous stress-strain curve are all higher than 0.92, and the ratio of long-term strength to instantaneous strength reaches 94.39%, which indicate that the whole creep of fine sandstone specimen is weak. The average correlative coefficients of linear regression function for isochronous stress- axial strain curve are 3.92% higher than that of average correlative coefficients of linear regression function for isochronous stress- radial strain curve, so nonlinear creep property of the fine sandstone specimen in axial direction is correspondingly weaker than that in radial direction. Negative Gauss distribution can be applied collectively to nonlinear creep of fine sandstone specimen, which has obvious time effect. With increasing loading, the reduction degrees of average correlative coefficients of linear fitting functions of isochronous stress-axial strain curve and isochronous stress-radial strain curve are 0.97% and 0.67% respectively, which indicates the linear correlation decreases commonly. Thus, the degree of nonlinear creep for fine sandstone specimen increases along with loading stress with obvious stress effect.