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)
2014年
2期
653-659
,共7页
王言章%杨蒙蒙%符磊%林君
王言章%楊矇矇%符磊%林君
왕언장%양몽몽%부뢰%림군
瞬变电磁%大定源回线%局部不均匀体%异常线圈%衰减曲线
瞬變電磁%大定源迴線%跼部不均勻體%異常線圈%衰減麯線
순변전자%대정원회선%국부불균균체%이상선권%쇠감곡선
TEM%large fixed loop%local non-homogeneous body%anomaly-loop%attenuation curve
根据瞬变电磁法基本原理,当大定源发射回线下方存在局部不均匀体时,由于不均匀体在接收线圈中产生的二次场方向不同,导致衰减曲线与均匀大地响应曲线偏离。为了分析浅层不均匀体对衰减曲线的影响,采用大定源回线装置发射电流为梯形波,回线面积为150 m×150 m,电流波形为梯形波,幅值为10 A,关断时间为176μs;对于时间常数分别为1、3、5 ms 的浅层不均匀体,利用多匝密绕的闭合线圈(即异常线圈模型)的电磁信号衰减规律,来模拟其响应衰减曲线。研究表明,当异常线圈位于发射回线下方或者是框边下方时,随着发射、异常、接收之间的相对位置的变化,三者之间的互感发生变化,引起异常线圈的响应可能为负值,致使接收到的综合响应衰减曲线出现过0情况。因此,大定源回线结构下存在不均匀体时,产生的负响应值在后续处理时需要引起注意。
根據瞬變電磁法基本原理,噹大定源髮射迴線下方存在跼部不均勻體時,由于不均勻體在接收線圈中產生的二次場方嚮不同,導緻衰減麯線與均勻大地響應麯線偏離。為瞭分析淺層不均勻體對衰減麯線的影響,採用大定源迴線裝置髮射電流為梯形波,迴線麵積為150 m×150 m,電流波形為梯形波,幅值為10 A,關斷時間為176μs;對于時間常數分彆為1、3、5 ms 的淺層不均勻體,利用多匝密繞的閉閤線圈(即異常線圈模型)的電磁信號衰減規律,來模擬其響應衰減麯線。研究錶明,噹異常線圈位于髮射迴線下方或者是框邊下方時,隨著髮射、異常、接收之間的相對位置的變化,三者之間的互感髮生變化,引起異常線圈的響應可能為負值,緻使接收到的綜閤響應衰減麯線齣現過0情況。因此,大定源迴線結構下存在不均勻體時,產生的負響應值在後續處理時需要引起註意。
근거순변전자법기본원리,당대정원발사회선하방존재국부불균균체시,유우불균균체재접수선권중산생적이차장방향불동,도치쇠감곡선여균균대지향응곡선편리。위료분석천층불균균체대쇠감곡선적영향,채용대정원회선장치발사전류위제형파,회선면적위150 m×150 m,전류파형위제형파,폭치위10 A,관단시간위176μs;대우시간상수분별위1、3、5 ms 적천층불균균체,이용다잡밀요적폐합선권(즉이상선권모형)적전자신호쇠감규률,래모의기향응쇠감곡선。연구표명,당이상선권위우발사회선하방혹자시광변하방시,수착발사、이상、접수지간적상대위치적변화,삼자지간적호감발생변화,인기이상선권적향응가능위부치,치사접수도적종합향응쇠감곡선출현과0정황。인차,대정원회선결구하존재불균균체시,산생적부향응치재후속처리시수요인기주의。
Based on the knowledge of the TEM theory,the secondary field direction generated by the heterogeneities in the position of the receive loop is different when the local heterogeneities exist below large fixed transmit loop,which may result in attenuation curve deviating from the response curve of the homogeneous body.In order to analyze the impact of heterogeneities to the attenuation curve,we adopts large fixed loop equipment whose area is 150 m×150 m and emission current is trapezoidal wave with the amplitude of 10 A and turn-off time of 176 μs.We use the electromagnetic signal attenuation rule of multi-turn and close-wound coil, namely anomaly loop to simulate the response curve of shallow heterogeneities whose time constant is respectively 1 ms,3 ms or 5 ms.When the anomaly loop is located below the transmit loop or its frame edge,with the different relative position between the transmit loop, anomaly loop and receive loop,that will change the mutual inductance of them and cause the response of the anomaly loop negatively and lead to the integrated response attenuation curve of the receive loop appearing zero-crossing condition.So we need to attract attention of the negative response in the subsequent processing when the heterogeneities exist below the large fixed loop.