物探化探计算技术
物探化探計算技術
물탐화탐계산기술
COMPUTING TECHNIQUES FOR GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2015年
2期
224-228
,共5页
李长江%李庆春%邵广周
李長江%李慶春%邵廣週
리장강%리경춘%소엄주
旋转交错网格%高阶有限差分%地下空洞%真空法%波场数值模拟
鏇轉交錯網格%高階有限差分%地下空洞%真空法%波場數值模擬
선전교착망격%고계유한차분%지하공동%진공법%파장수치모의
rotated staggered grid%high order finite difference%underground cavities%vacuum formulation%wave- field simulation
将真空法和旋转交错网格相结合,实现了地下空洞高阶旋转交错网格波场数值模拟,克服了旋转交错网格在模拟自由边界条件时只在空间二阶差分时稳定的不足。通过和已有普通交错网格下改进的真空法对比,验证了该方法的正确性和稳定性。为了减弱模型人工边界产生的反射,采用了吸收效果较好的完全匹配层技术。模拟了不同模型参数组合情况下的地震波传播以及地震波与地下空洞的相互作用,通过对比不同参数组合的地震记录和波场快照,以及包含空洞和不含空洞地震记录和波场快照,分析了地震波在地下存在空洞时的传播特征以及震源子波频率、地下空洞大小和埋深对地表地震记录的影响。
將真空法和鏇轉交錯網格相結閤,實現瞭地下空洞高階鏇轉交錯網格波場數值模擬,剋服瞭鏇轉交錯網格在模擬自由邊界條件時隻在空間二階差分時穩定的不足。通過和已有普通交錯網格下改進的真空法對比,驗證瞭該方法的正確性和穩定性。為瞭減弱模型人工邊界產生的反射,採用瞭吸收效果較好的完全匹配層技術。模擬瞭不同模型參數組閤情況下的地震波傳播以及地震波與地下空洞的相互作用,通過對比不同參數組閤的地震記錄和波場快照,以及包含空洞和不含空洞地震記錄和波場快照,分析瞭地震波在地下存在空洞時的傳播特徵以及震源子波頻率、地下空洞大小和埋深對地錶地震記錄的影響。
장진공법화선전교착망격상결합,실현료지하공동고계선전교착망격파장수치모의,극복료선전교착망격재모의자유변계조건시지재공간이계차분시은정적불족。통과화이유보통교착망격하개진적진공법대비,험증료해방법적정학성화은정성。위료감약모형인공변계산생적반사,채용료흡수효과교호적완전필배층기술。모의료불동모형삼수조합정황하적지진파전파이급지진파여지하공동적상호작용,통과대비불동삼수조합적지진기록화파장쾌조,이급포함공동화불함공동지진기록화파장쾌조,분석료지진파재지하존재공동시적전파특정이급진원자파빈솔、지하공동대소화매심대지표지진기록적영향。
We combined the improved vacuum formulation and the rotated staggered grid finite difference method to imple-ment the high order rotated staggered finite difference elastic wave-field simulation at the presence of underground cavities. Our method overcame the defect of rotated staggered finite difference when modeling the free surface condition which is only stable at second order spatial FD operators,through the comparison with existing vacuum formulation testifies our methods ac-curacy and stability.The perfectly Matched Layer (PML)absorbing boundary condition is applied to decrease the reflection from the edges of the numerical model.Different seismograms are calculated with models without voids and models contain voids with different size and depth under different source wavelet frequency.The effects of different cavity size and depth and the source wavelet frequency are evaluated from the snapshots and seismograms with and without the cavity.