安徽理工大学学报(自然科学版)
安徽理工大學學報(自然科學版)
안휘리공대학학보(자연과학판)
JOURNAL OF ANHUI UNIVERSITY OF SCIENCE AND TECHNOLOGY(NATURAL SCIENCE)
2014年
1期
24-29
,共6页
鲁海峰%姚多喜%沈丹%温亮%王康
魯海峰%姚多喜%瀋丹%溫亮%王康
로해봉%요다희%침단%온량%왕강
层状岩体%数值模拟%压缩破坏%结构面
層狀巖體%數值模擬%壓縮破壞%結構麵
층상암체%수치모의%압축파배%결구면
layered rock mass%numerical simulation%compressive failure%structural plane
煤层底板岩体是沉积岩,具有显著的层状结构特点。为研究层状岩体压缩强度的结构面效应,通过FLAC3D数值软件,结合改进的遍布节理本构模型,建立层状岩体压缩数值模型,分析单轴、三轴压缩情况下的应力应变响应以及强度特征。研究结果表明:层状岩体压缩强度具有显著的结构面倾角效应。随着倾角的增大,层状岩体的压缩强度呈现先减小后增大的趋势。当结构面倾角为40°~80°时,岩体强度整体较低,破裂面主要沿结构面展开。数值试验和理论分析反映的岩体强度随结构面倾角变化规律一致。层状岩体弹性模量沿平行于结构面方向最大,而垂直于结构面方向最小,并随结构面与水平面之间夹角的增加而增大。
煤層底闆巖體是沉積巖,具有顯著的層狀結構特點。為研究層狀巖體壓縮彊度的結構麵效應,通過FLAC3D數值軟件,結閤改進的遍佈節理本構模型,建立層狀巖體壓縮數值模型,分析單軸、三軸壓縮情況下的應力應變響應以及彊度特徵。研究結果錶明:層狀巖體壓縮彊度具有顯著的結構麵傾角效應。隨著傾角的增大,層狀巖體的壓縮彊度呈現先減小後增大的趨勢。噹結構麵傾角為40°~80°時,巖體彊度整體較低,破裂麵主要沿結構麵展開。數值試驗和理論分析反映的巖體彊度隨結構麵傾角變化規律一緻。層狀巖體彈性模量沿平行于結構麵方嚮最大,而垂直于結構麵方嚮最小,併隨結構麵與水平麵之間夾角的增加而增大。
매층저판암체시침적암,구유현저적층상결구특점。위연구층상암체압축강도적결구면효응,통과FLAC3D수치연건,결합개진적편포절리본구모형,건립층상암체압축수치모형,분석단축、삼축압축정황하적응력응변향응이급강도특정。연구결과표명:층상암체압축강도구유현저적결구면경각효응。수착경각적증대,층상암체적압축강도정현선감소후증대적추세。당결구면경각위40°~80°시,암체강도정체교저,파렬면주요연결구면전개。수치시험화이론분석반영적암체강도수결구면경각변화규률일치。층상암체탄성모량연평행우결구면방향최대,이수직우결구면방향최소,병수결구면여수평면지간협각적증가이증대。
Coal seam floor rock mass is sedimentary rock and has obvious characteristics of layered structure .In order to study the structural plane effect on compressive strength of layered rock mass , the stress-strain response and strength characteristic of layered rock mass under uniaxial compression and triaxial compression were ana -lyzed by numerical simulation with FLAC 3D .The results showed that compressive strength of layered rock mass has remarkable effect of layer plane dip .The compressive strength of rock mass first decreases and then increases with the increase of structure plane dip angle .When the structure plane dip angle is 40 °~80 °, the strength of rock mass is low and the fracture plane develops in the structure plane .Numerical experiments and theoretical a-nalysis gave the consistent regularity of rock strength with structural plane dip variation .The maximum elastic modulus of layered rock mass is parallel to structural plane and the minimum in the direction perpendicular to the structural plane , and increases with the angle rise between the structural plane and the horizontal plane .