Airborne electromagnetic sensing of shallow seawater using a helicopter time-domain system — Applications for bathymetric mapping and characterizing the seafloor

J. Vrbancich
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Abstract

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.
用直升机时域系统对浅海进行机载电磁传感。海底测深测绘和表征的应用
一种直升机时域机载电磁(AEM)系统正在开发中,用于研究AEM用于水深测绘的使用。水深和沉积物厚度是基于电阻基底上的粗糙双层模型(海水/沉积物)的电磁响应的一维反演来计算的。本研究的主要重点是测试AEM在水深测绘中的准确性。第二个目标是通过确定基岩的深度来绘制沉积物厚度图。AEM方法感知海洋环境的上层地电层,对水浊度和冲浪带条件不敏感,因为光学不透明性和气泡的存在不会显著影响海水的总体电导率。调查区域包括浅水(< 25 m)覆盖着未固结沉积物的古山谷和礁区。在浅于25 m的水域,水深精度达到1 ~ 2 m。研究表明,AEM方法适用于浑浊水域和冲浪带水域的快速测深测绘。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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