首页> 外文期刊>Exploration Geophysics >On airborne IP effects in standard AEM systems: tightening model space with data space
【24h】

On airborne IP effects in standard AEM systems: tightening model space with data space

机译:关于标准AEM系统中的机载IP效果:通过数据空间收紧模型空间

获取原文
获取原文并翻译 | 示例
           

摘要

IP effects in AEM data are subject of current research around the world. There have been successstories and it is now practical to model AIP. It is widely accepted that failure to account for IPeffects, when present, will produce artefacts in the resistivity model. However there still is a needto study more accurately the boundaries of the effect on AEM data and of its relevance, beyondcommon past acceptance. This paper provides a clear and extensive overview of detectable AIPeffects in the data space, without imposing simplistic assumptions (e.g. fixing some parametersto arbitrary values or limited boundaries), beside using a 1D approach. We produce forwardresponses with dispersive resistivity for hundreds of thousands of combinations of Cole–Colemodel parameters (different rock types) and AEM system transfer functions. The results are analysedusing various metrics (e.g. sum of negative voltages, exponential fitting), presented with aseries of 3D plots that capture different AIP signatures in the transients. Experiments include halfspaces, 2 and 3 layer models, combined with different waveforms, Rx types (dB/dt and B), Tx-Rxgeometries, flying heights, base frequencies. The results allow a clear assessment of the differentaspects of AIP effects over a wide range of geological and geophysical situations. MeasuredAIP effects are mostly focused in the range ofτ from 10~(−2) s to 10~(−4) s. Measurable AIP effectsdepend on AEM system’s specs, are often unpredictable, can originate from chargeable layers atconsiderable depth, are heavily affected by layering and can occur over a wide range of situations.Deeper chargeable layers do not necessarily produce fainter AIP anomalies. What can begeneralised is that AIP effects are increased most often by the presence of a resistive bedrock,often using slow turn-off of the waveform, are generally better observed with B field instead ofdB/dt and lowering base frequencies. They can vary abruptly, due to the rapidly changing relativecontribution of pure EM and pure IP responses. AIP effects can occur more often than previouslythought and should not be discarded a-priori from any AEM survey.
机译:AEM数据中的IP效果是世界各地当前研究的主题。成功了故事,现在是模拟AIP的实际情况。它被广泛接受,未能考虑IP当存在时,效果将在电阻率模型中产生人工制品。然而,仍然需要更准确地学习对AEM数据的影响和其相关性的影响常见的过去验收。本文提供了明确而广泛的可检测AIP概述在数据空间中的效果,而不会施加简单的假设(例如,修复一些参数在使用1D方法旁边的任意值或有限的边界。我们前进对多数千组合的COLE-COLE组合的反应模型参数(不同摇滚类型)和AEM系统传输功能。结果分析了使用各种度量(例如负电压,指数拟合),提出捕获瞬态中不同AIP签名的3D图系列。实验包括一半空格,2和3层模型,与不同的波形,Rx类型(DB / DT和B),TX-Rx组合几何,飞行高度,基频。结果允许对不同的评估进行明确评估AIP效应的各个方面在广泛的地质和地球物理情况下效应。测量AIP效应主要集中在10〜(2)S至10〜(4)秒的范围内。可测量的AIP效果依靠AEM系统的规格,通常是不可预测的,可以源自可充电的层相当大的深度,受到分层的严重影响,并且可以发生在各种情况下。更深的可充电层不一定会产生微弱的虹膜异常。什么可以概括的是通过电阻基岩的存在,均衡效果最常增加,通常使用波形的慢关闭,通常使用B字段更好地观察到DB / DT和降低基频。由于相对不断变化,它们可以突然变化纯EM和纯IP响应的贡献。 AIP效果可能比以前更频繁地发生思想,不应从任何AEM调查中丢弃先验。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号