首页> 外文会议>2010 International Conference on Electromagnetics in Advanced Applications >Airborne electromagnetic sensing of shallow seawater using a helicopter time-domain system — Applications for bathymetric mapping and characterizing the seafloor
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Airborne electromagnetic sensing of shallow seawater using a helicopter time-domain system — Applications for bathymetric mapping and characterizing the seafloor

机译:使用直升机时域系统对浅海水进行机载电磁感应—水深测绘和表征海底的应用

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摘要

A helicopter time-domain airborne electromagnetic (AEM) system is under development for investigating the use of AEM for bathymetric mapping. Bathymetry and sediment thickness is computed from 1D inversion of the EM response based on a crude two-layer model (seawater/sediment) overlying resistive basement. The primary focus of this study is to test the accuracy of AEM for bathymetric mapping. A secondary objective is to map sediment thickness by determining the depth to bedrock. The AEM method senses the upper geo-electrical layers of the marine environment and is not sensitive to water turbidity and surf zone conditions because the optical opacity and presence of bubbles does not significantly affect the bulk electrical conductivity of seawater. The survey areas contain shallow waters (< 25 m) overlying paleovalleys infilled with unconsolidated sediment, and reef areas. Water depth accuracy of 1–2 m was achieved in water shallower than 25 m. This study shows that the AEM method is suited as a reconnaissance technique for rapid bathymetric mapping in turbid and surf-zone waters.
机译:直升机时域机载电磁(AEM)系统正在开发中,以研究将AEM用于测深图的使用。根据覆盖电阻基底的原始两层模型(海水/沉积物),通过EM响应的一维反演来计算测深法和沉积物厚度。这项研究的主要重点是测试用于测深图的AEM的准确性。第二个目标是通过确定基岩深度来绘制沉积物厚度。 AEM方法可感测海洋环境的上部地电层,并且对水混浊度和冲浪区条件不敏感,因为光学不透明性和气泡的存在不会显着影响海水的总体电导率。调查区域包含浅水区(<25 m)和覆盖礁石区,浅水区覆盖了充满未固结沉积物的古卵。在小于25 m的水中,实现了1-2 m的水深精度。这项研究表明,AEM方法适合作为在浑浊和海浪水域中进行快速测深测绘的侦察技术。

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