爆破
爆破
폭파
BLASTING
2014年
4期
11-15,53
,共6页
殷秀红%钟冬望%黄小武%司剑锋%何理
慇秀紅%鐘鼕望%黃小武%司劍鋒%何理
은수홍%종동망%황소무%사검봉%하리
水下钻孔爆破%数值模拟%应力响应%多物质ALE算法
水下鑽孔爆破%數值模擬%應力響應%多物質ALE算法
수하찬공폭파%수치모의%응력향응%다물질ALE산법
underwater blasting%numerical simulation%stress response%multi-material ALE algorithm
结合连续介质力学和动力非线性有限元理论知识,通过ANSYS/LS-DYNA建立20 m水深和无水两种情况下的钻孔爆破模型,采用多物质ALE算法,模拟得出了从孔底起爆时爆炸冲击波引起的应力响应,并根据岩石破碎机理判断出粉碎区、裂隙区和弹性振动区,在5~8倍的药柱半径范围内,由冲击波压碎岩石形成粉碎区,临界径向压应力为207 MPa左右,在10~14倍的药柱半径范围内,岩石被割裂形成裂隙区,且切向拉应力起主导作用,其临界值为16.1 MPa左右,对比分析两种模型的计算结果可知,水介质的存在会减缓冲击波与爆轰气体的衰减速率。
結閤連續介質力學和動力非線性有限元理論知識,通過ANSYS/LS-DYNA建立20 m水深和無水兩種情況下的鑽孔爆破模型,採用多物質ALE算法,模擬得齣瞭從孔底起爆時爆炸遲擊波引起的應力響應,併根據巖石破碎機理判斷齣粉碎區、裂隙區和彈性振動區,在5~8倍的藥柱半徑範圍內,由遲擊波壓碎巖石形成粉碎區,臨界徑嚮壓應力為207 MPa左右,在10~14倍的藥柱半徑範圍內,巖石被割裂形成裂隙區,且切嚮拉應力起主導作用,其臨界值為16.1 MPa左右,對比分析兩種模型的計算結果可知,水介質的存在會減緩遲擊波與爆轟氣體的衰減速率。
결합련속개질역학화동력비선성유한원이론지식,통과ANSYS/LS-DYNA건립20 m수심화무수량충정황하적찬공폭파모형,채용다물질ALE산법,모의득출료종공저기폭시폭작충격파인기적응력향응,병근거암석파쇄궤리판단출분쇄구、렬극구화탄성진동구,재5~8배적약주반경범위내,유충격파압쇄암석형성분쇄구,림계경향압응력위207 MPa좌우,재10~14배적약주반경범위내,암석피할렬형성렬극구,차절향랍응력기주도작용,기림계치위16.1 MPa좌우,대비분석량충모형적계산결과가지,수개질적존재회감완충격파여폭굉기체적쇠감속솔。
Combining with the principles of continuum mechanics with dynamical nonlinear finite element theo-ry,the ANSYS/LS-DYNA was used to build the drilling blast model with 20 m deep water and without water,by u-sing the method of multi-material Arbitrary Lagrange Eulerian finite. The stress response caused by explosive shock wave from the bottom initiation was simulated,which determined the crushing zone,fissure zone and elastic vibration zone by the rock-cracking mechanism. Furthermore,within 5 to 8 times of the radius of charge,the rock was crushed by shock wave and the critical radial compressive stress was about 207 MPa;within 10 to 14 times of the radius of charge,the rock was torn and the fissure zone came into being,where the tangential tensile stress played a leading role and critical value was about 16. 1 MPa. Results showed that the water decreased the decay rate of stress wave and detonation wave.