煤田地质与勘探
煤田地質與勘探
매전지질여감탐
COAL GEOLOGY & EXPLORATION
2014年
1期
40-44
,共5页
黄晖%贾海宾%韩必武%朱昌淮%刘可胜
黃暉%賈海賓%韓必武%硃昌淮%劉可勝
황휘%가해빈%한필무%주창회%류가성
井筒%非采动破坏%影响因素%数值模拟%破坏预测
井筒%非採動破壞%影響因素%數值模擬%破壞預測
정통%비채동파배%영향인소%수치모의%파배예측
shaft%damage induced by non-mining disturbance%influencing factors%numerical simulation%failure prediction
立井井筒的非采动变形破坏是出现在华东厚表土层矿区的一种特殊矿山地质灾害,底部含水层失水压缩变形产生的附加应力是造成这一地质灾害的主要原因。在总结井筒发生非采动变形破坏的地质条件和破坏特征基础之上,通过建立三维数值模拟模型,分析了不同影响因素作用下井筒外壁所受附加应力的大小和变化规律,并根据模拟结果,利用弹性力学厚壁圆筒解建立井筒变形破坏应力状态与底部含水层水头降之间的对应关系,得到井筒变形破坏极限状态下对应的底部含水层水头降为89.5 m。
立井井筒的非採動變形破壞是齣現在華東厚錶土層礦區的一種特殊礦山地質災害,底部含水層失水壓縮變形產生的附加應力是造成這一地質災害的主要原因。在總結井筒髮生非採動變形破壞的地質條件和破壞特徵基礎之上,通過建立三維數值模擬模型,分析瞭不同影響因素作用下井筒外壁所受附加應力的大小和變化規律,併根據模擬結果,利用彈性力學厚壁圓筒解建立井筒變形破壞應力狀態與底部含水層水頭降之間的對應關繫,得到井筒變形破壞極限狀態下對應的底部含水層水頭降為89.5 m。
립정정통적비채동변형파배시출현재화동후표토층광구적일충특수광산지질재해,저부함수층실수압축변형산생적부가응력시조성저일지질재해적주요원인。재총결정통발생비채동변형파배적지질조건화파배특정기출지상,통과건립삼유수치모의모형,분석료불동영향인소작용하정통외벽소수부가응력적대소화변화규률,병근거모의결과,이용탄성역학후벽원통해건립정통변형파배응력상태여저부함수층수두강지간적대응관계,득도정통변형파배겁한상태하대응적저부함수층수두강위89.5 m。
Non-mining disturbance-induced deformation and failure in shaft is a special mine geological hazard in mining areas with thick alluvium layer in East China. Additional stress induced by water loss and compression de-formation in bottom aquifer is the major cause for the geological hazard. On the basis of summarizing the geologi-cal conditions and characteristics of deformation and failure induced by non-mining disturbance in shaft, the paper analyzes the amplitude and variation regularities of the additional stress in outer wall of shaft under action of dif-ferent influencing factors through 3-D numerical modeling. On the basis of the modeling results and using elastic mechanics to solve the shaft with thick wall, the relationship between stress condition of deformation and failure and water head drop in bottom aquifer was established, it was indicated that the corresponding water head drop under limit state of deformation and failure in shaft was 89.5 m.