华北科技学院学报
華北科技學院學報
화북과기학원학보
JOURNAL OF NORTH CHINA INSTITUTE OF SCIENCE AND TECHNOLOGY
2014年
5期
15-19
,共5页
李飞%谭强%刘德民%张景钢%潘建旭
李飛%譚彊%劉德民%張景鋼%潘建旭
리비%담강%류덕민%장경강%반건욱
矿井瞬变电磁%镜像模型%全空间%反演
礦井瞬變電磁%鏡像模型%全空間%反縯
광정순변전자%경상모형%전공간%반연
Mine Transient Electromagnetic Method%Mirror model%Whole space%Inversion
常规的瞬变电磁反演用半空间响应乘以全空间响应系数来拟合观测数据,具有一定的局限性;直接进行全空间反演,瞬变电磁场的空间不可分性会导致反演结果的不稳定。针对以上问题,提出了基于镜像模型的矿井瞬变电磁全空间反演方法,编制了反演程序。对低阻模型、受巷道后方高阻影响的低阻模型、受巷道后方低阻影响的低阻模型进行了反演试算,结果表明:基于镜像模型的全空间反演方法能够准确反演出掘进工作面前方的低阻地质异常体,巷道后方的高阻体不会影响对前方低阻地质异常体的判断。
常規的瞬變電磁反縯用半空間響應乘以全空間響應繫數來擬閤觀測數據,具有一定的跼限性;直接進行全空間反縯,瞬變電磁場的空間不可分性會導緻反縯結果的不穩定。針對以上問題,提齣瞭基于鏡像模型的礦井瞬變電磁全空間反縯方法,編製瞭反縯程序。對低阻模型、受巷道後方高阻影響的低阻模型、受巷道後方低阻影響的低阻模型進行瞭反縯試算,結果錶明:基于鏡像模型的全空間反縯方法能夠準確反縯齣掘進工作麵前方的低阻地質異常體,巷道後方的高阻體不會影響對前方低阻地質異常體的判斷。
상규적순변전자반연용반공간향응승이전공간향응계수래의합관측수거,구유일정적국한성;직접진행전공간반연,순변전자장적공간불가분성회도치반연결과적불은정。침대이상문제,제출료기우경상모형적광정순변전자전공간반연방법,편제료반연정서。대저조모형、수항도후방고조영향적저조모형、수항도후방저조영향적저조모형진행료반연시산,결과표명:기우경상모형적전공간반연방법능구준학반연출굴진공작면전방적저조지질이상체,항도후방적고조체불회영향대전방저조지질이상체적판단。
The conventional inversion method based on half -space response multiplied by whole spatial re-sponse factor has some limitations.The direct whole space inversion will lead to instability of the inversion re-sults.To solve the above problem , the paper presents mine transient electromagnetic whole -space inversion method based on mirror model.The inversion of low resistivity model , low resistivity model affected by high resistance and low resistivity model affected by low resistance show that:the method of mine transient electro-magnetic Whole-space inversion based on mirror model can inverse the geological low resistivity anomalies in the front of heading face accurately , and the high resistivity of rear of the roadway will not affect the judgment for geological low resistivity anomalies in the front of the roadway.