物探与化探
物探與化探
물탐여화탐
GEOPHYSICAL AND GEOCHEMICAL EXPLORATION
2014年
4期
737-741
,共5页
朱崇利%董云%王延平%周佃刚%孙文%何兆容
硃崇利%董雲%王延平%週佃剛%孫文%何兆容
주숭리%동운%왕연평%주전강%손문%하조용
网格剖分%反演%博斯蒂克%非线性共轭梯度
網格剖分%反縯%博斯蒂剋%非線性共軛梯度
망격부분%반연%박사체극%비선성공액제도
grid subdivision%inversion%Bostick%nonlinear conjugate gradient
网格剖分的合适与否,影响着反演结果的精度。用不同模型、不同反演方法,对比验证粗细两种不同的网格对反演精度的影响。研究结果表明,从整体上看两种不同网格剖分方式,粗网格在深部比细网格模拟精度高,但是近地表开始阶段,粗网格与细网格波动幅度都较大,都脱离正常值,粗网格模拟精度不如细网格;粗网格的整体变化幅度比细网格缓和,其中对低阻异常体反演精度较好,但对高阻异常体反演精度较差,与真实值相去甚远。
網格剖分的閤適與否,影響著反縯結果的精度。用不同模型、不同反縯方法,對比驗證粗細兩種不同的網格對反縯精度的影響。研究結果錶明,從整體上看兩種不同網格剖分方式,粗網格在深部比細網格模擬精度高,但是近地錶開始階段,粗網格與細網格波動幅度都較大,都脫離正常值,粗網格模擬精度不如細網格;粗網格的整體變化幅度比細網格緩和,其中對低阻異常體反縯精度較好,但對高阻異常體反縯精度較差,與真實值相去甚遠。
망격부분적합괄여부,영향착반연결과적정도。용불동모형、불동반연방법,대비험증조세량충불동적망격대반연정도적영향。연구결과표명,종정체상간량충불동망격부분방식,조망격재심부비세망격모의정도고,단시근지표개시계단,조망격여세망격파동폭도도교대,도탈리정상치,조망격모의정도불여세망격;조망격적정체변화폭도비세망격완화,기중대저조이상체반연정도교호,단대고조이상체반연정도교차,여진실치상거심원。
The problem whether the grid subdivision is suitable or not constitutes a prerequisite for the accuracy of the inversion results. Using different models and different inversion methods, the authors made a comparative study to detect the effects of two different grids on the accuracy of inversion. The employment of the two different ways of grid subdivision shows that, on the whole, the coarse grid has higher simulation precision than the fine grid in the depth, but at the starting stage of near-surface, the amplitude of fluctuation of the coarse grid and that of the fine grid are both relatively large, i.e., both obviously deviate from the normal value. The simulation accura-cy of the fine grid is better than that of the coarse grid. The overall change in the coarse grid is more smooth than the fine grid, and the inversion accuracy of the coarse grid for the anomalous body of low resistance is better;nevertheless, for abnormal body of high resist-ance, the inversion accuracy is poorer, and the value widely deviates from the real value.