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Detection of Perfectly-Conducting Targets with Airborne Electromagnetic Systems.

机译:用机载电磁系统检测完美导电的目标。

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摘要

A significant problem with exploring for electrically conductive mineral deposits with airborne electromagnetic (AEM) methods is that many of the most valuable sulphide deposits are too conductive to be detected with conventional systems. High-grade sulphide deposits with bulk electrical conductivities on the order of 100,000 S/m can appear as “perfect conductors” to most EM systems because the decay of secondary fields (the “time constant” of the deposit) generated in the target by the system transmitter takes much longer than the short measuring time of EM systems. Their EM response is essentially undetectable with off-time measurements.;One solution is to make measurements during the transmitter on-time when the secondary field of the target produced by magnetic flux exclusion is large. The difficulty is that the secondary field must be measured in the presence of a primary field which is orders of magnitude larger. The goal of this thesis is to advance the methodology of making AEM measurements during transmitter on-time by analysing experimental data from three different AEM systems.;The first system analysed is a very large separation, two helicopter system where geometry is measured using GPS sensors. In order to calculate the primary field at the receiver with sufficient accuracy, the very large (nominally 400 m) separation requires geometry to be known to better than 1 m. Using the measured geometry to estimate and remove the primary field, I show that a very conductive target can be detected at depths of 200m using the total secondary field. I then used fluxgate magnetometers to correct for receiver rotation which allowed the component of the secondary field to be determined.;The second system I examined was a large separation fixed-wing AEM system. Using a towed receiver bird with a smaller (≈ 135m) separation, the geometry must be known much more accurately. In the absence of direct measurement of this geometry, I used a least-squares prediction approach using measurements of aircraft manoeuvres which allowed primary field contamination to be estimated. Subtracting this estimate from the recorded signal increased the maximum time constant observed in a field survey for conductive targets by a factor of seven.;Finally, a study of a nominally rigid helicopter EM system employing a bucking coil to cancel primary field showed that system geometry (specifically, the position of the receiver coil relative to the transmitter and bucking coils) must be known to better than 0.01 mm to detect deep targets. Again, direct measurements of system geometry were not available. A least-squares prediction filter using helicopter manoeuvre and system pitch and roll measurements was applied, but was not able to estimate primary field well enough to provide an accurate secondary on-time response. Direct measurements of relative motion of the system components might solve this problem.
机译:用航空电磁法(AEM)探索导电性矿床的一个重要问题是,许多最有价值的硫化物矿床导电性太强,无法用常规系统检测到。多数电导率约为100,000 S / m的高品位硫化物矿床可能会成为大多数EM系统的“完美导体”,因为靶在靶中产生的次级磁场(矿床的“时间常数”)会衰减。系统变送器比EM系统的短测量时间要长得多。它们的EM响应在关断时间测量中基本上是无法检测到的。一种解决方案是在发射器导通时间进行测量,此时由磁通量排斥产生的目标的次级磁场很大。困难在于,必须在存在更大数量级的主场的情况下测量次场。本文的目的是通过分析来自三个不同AEM系统的实验数据来改进在发射机准时进行AEM测量的方法。第一个分析的系统是一个非常大的分离,两个直升机系统,其中使用GPS传感器测量几何形状。为了以足够的精度计算接收器处的主场,非常大的距离(标称值为400 m)需要知道几何形状优于1 m。使用测得的几何形状来估计和消除一次场,我表明可以使用整个二次场在200m的深度处检测到非常导电的目标。然后,我使用磁通门磁力计校正接收器的旋转,从而确定了次级磁场的分量。我检查的第二个系统是大分离固定翼AEM系统。使用间隔较小(约135m)的拖曳接收器鸟,必须更准确地知道其几何形状。在没有直接测量这种几何形状的情况下,我使用了最小二乘预测方法,该方法使用了对飞机操纵的测量,从而可以估算一次场污染。从记录的信号中减去此估计值后,在实地调查中观察到的导电目标的最大时间常数增加了7倍。 (具体来说,接收器线圈相对于发送器和降压线圈的位置)必须知道大于0.01毫米才能检测到较深的目标。同样,无法直接测量系统几何形状。应用了使用直升机操纵和系统俯仰和横滚测量值的最小二乘预测滤波器,但它无法很好地估计主场,无法提供准确的次要准时响应。直接测量系统组件的相对运动可能会解决此问题。

著录项

  • 作者

    Smiarowski, Adam.;

  • 作者单位

    University of Toronto (Canada).;

  • 授予单位 University of Toronto (Canada).;
  • 学科 Geophysics.
  • 学位 Ph.D.
  • 年度 2012
  • 页码 229 p.
  • 总页数 229
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

  • 入库时间 2022-08-17 11:43:44

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