吉林大学学报(地球科学版)
吉林大學學報(地毬科學版)
길림대학학보(지구과학판)
JOURNAL OF JILIN UNIVERSITY(EARTH SCIENCE EDITION)
2015年
1期
282-292
,共11页
沈金松%汪轩%魏帅帅%李曼
瀋金鬆%汪軒%魏帥帥%李曼
침금송%왕헌%위수수%리만
浅水域%海洋可控源电磁勘探%鸣震近似%波场分离%空气波压制
淺水域%海洋可控源電磁勘探%鳴震近似%波場分離%空氣波壓製
천수역%해양가공원전자감탐%명진근사%파장분리%공기파압제
shallower water domain%marine controlled-source electromagnetic exploration%wave reverberations approximation%air wave separation%air wave mitigation
可控源海洋电磁(MCSEM)勘探中空气波对海底电磁响应的影响已为业界所重视,它是由水平电偶极子源发射的电磁信号沿空气海水界面传播与来自海底地层的有效信号相互作用产生的。在浅水域勘探时,空气波淹没来自地层的有效信号,使浅水域 MCSEM 实现油气层识别产生困难。基于层状介质模型,采用电磁场的模式分解理论导出了半空间电阻率模型的空气波表达式,利用该式将空气波在海水层的传播近似用海水空气界面与海底地层之间的多次鸣震表达。结合源和接收器两边电磁场的传播特征,导出了有限水深时空气波近似关系,用于近似模拟空气波响应。为了对比不同方法压制空气波的效果,基于上行波场和下行波场的分解方法,获得了含油气高阻储层上上行波的异常幅度增大数倍的结果,显示了波场分解方法压制空气波的良好效果。最后,利用不含油气层的背景模型和含油气储层模型电磁响应的数值模拟结果,比较空气波渐近表达和波场分离2种空气波压制方法可知:对于水平层状模型后者效果更好;前者可适用于崎岖海底地层的数据处理,后者只适用于水平海底地层。
可控源海洋電磁(MCSEM)勘探中空氣波對海底電磁響應的影響已為業界所重視,它是由水平電偶極子源髮射的電磁信號沿空氣海水界麵傳播與來自海底地層的有效信號相互作用產生的。在淺水域勘探時,空氣波淹沒來自地層的有效信號,使淺水域 MCSEM 實現油氣層識彆產生睏難。基于層狀介質模型,採用電磁場的模式分解理論導齣瞭半空間電阻率模型的空氣波錶達式,利用該式將空氣波在海水層的傳播近似用海水空氣界麵與海底地層之間的多次鳴震錶達。結閤源和接收器兩邊電磁場的傳播特徵,導齣瞭有限水深時空氣波近似關繫,用于近似模擬空氣波響應。為瞭對比不同方法壓製空氣波的效果,基于上行波場和下行波場的分解方法,穫得瞭含油氣高阻儲層上上行波的異常幅度增大數倍的結果,顯示瞭波場分解方法壓製空氣波的良好效果。最後,利用不含油氣層的揹景模型和含油氣儲層模型電磁響應的數值模擬結果,比較空氣波漸近錶達和波場分離2種空氣波壓製方法可知:對于水平層狀模型後者效果更好;前者可適用于崎嶇海底地層的數據處理,後者隻適用于水平海底地層。
가공원해양전자(MCSEM)감탐중공기파대해저전자향응적영향이위업계소중시,타시유수평전우겁자원발사적전자신호연공기해수계면전파여래자해저지층적유효신호상호작용산생적。재천수역감탐시,공기파엄몰래자지층적유효신호,사천수역 MCSEM 실현유기층식별산생곤난。기우층상개질모형,채용전자장적모식분해이론도출료반공간전조솔모형적공기파표체식,이용해식장공기파재해수층적전파근사용해수공기계면여해저지층지간적다차명진표체。결합원화접수기량변전자장적전파특정,도출료유한수심시공기파근사관계,용우근사모의공기파향응。위료대비불동방법압제공기파적효과,기우상행파장화하행파장적분해방법,획득료함유기고조저층상상행파적이상폭도증대수배적결과,현시료파장분해방법압제공기파적량호효과。최후,이용불함유기층적배경모형화함유기저층모형전자향응적수치모의결과,비교공기파점근표체화파장분리2충공기파압제방법가지:대우수평층상모형후자효과경호;전자가괄용우기구해저지층적수거처리,후자지괄용우수평해저지층。
In marine controlled-source electromagnetic (MCSEM)exploration,the influence on the EM response of the airwave has been paid great attention by the industry and the air wave is one kind of EM signal from the horizontal electric dipole (HED)source that is reflected from or travels along the air-sea interface and return back to receivers.In shallow water domains,the airwave dominates over the effective signal from seabed sediments, and makes it very difficult to identify the hydrocarbon reservoirs.On the basis of the layer model,we have derived airwave expression of half space resistivity model by using the mode decomposition theory of the EM field and the air wave in the sea water layer is approximately expressed as a series of wave reverberations that travel down and backward between the sea surface and the seabed.According to the propagations of EM field near sources and receivers,we have obtained airwave expression of a finite water layer.In order to compare the effectiveness of the various air wave mitigation methods,we have adopted the decomposition method of EM fields into upgoing and downgoing components,and have acuired larger anomaly of several times than that of the raw EM field above the resistive formation,and indicated the favorable effect of airwave attenuation by using of wave separation. Finally, simulation results of electromagnetic responses from different background and reservoir models have been used to check the effectiveness and adaptability of the two air wave mitigation methods of wave reverberations approximation and wave field decomposition,numerical results show that for model of horizontal layers,the latter is more effective,however,the former is applicable to rugged sea floor formation and the latter only fits for horizontal layers.