使用拖曳、直流、电阻率阵列对海洋沉积物进行分类

D. Lavoie, E. Mozley, R. Corwin, D. Lambert, P. Valent
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引用次数: 1

摘要

模型研究表明,直流电阻率技术在沉积物分类和地层构造中是可行的。建立了一个原型阵列来测试这种技术可以在海洋环境中的航行模式中使用的假设。一个60米的反向阵列在海底上下拖曳,电极间距适合于海底以下10米的穿透深度。在密西西比海湾使用该阵列测量了三种不同的底部类型,即泥浆、气泥浆和砂。地面真相提供了声学海底分类系统、CTD(电导率、温度和深度)模型和大量沉积物岩心。数据分析使用SUBVERT,这是一种适用于IBM-PC AT的反演程序。
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The use of a towed, direct-current, electrical resistivity array for the classification of marine sediments
Model studies indicate that the DC electric resistivity technique is feasible for sediment classification and layer structuring. A prototype array was built to test the hypothesis that such a technique can be used in an underway mode in the marine environment. A 60-m, inverted array was towed both on and off the seafloor with electrode spacings appropriate for a penetration depth of 10 m below the seafloor. Three different bottom types, namely mud, gassy mud, and sand, were surveyed in the Mississippi Sound using the array. Ground truth was provided with an acoustic seafloor classification system, CTD (conductivity, temperature, and depth) casts, and numerous sediment cores. Data were analyzed using SUBVERT, an inversion routine adapted for an IBM-PC AT.<>
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