水下MASW和声学方法在沙特曼尼法堤施工前海底条件评估中的应用

Symposium on the Application of Geophysics to Engineering and Environmental Problems 2018 Pub Date : 2017-10-12 DOI:10.1190/ICEG2017-053

K. Sayers, T. Fechner, C. Park, A. Verweerd

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引用次数: 1

摘要

众所周知，近海海湾地区在海床以下0-5米的地面上有盖层。它的厚度从几厘米到两三米不等。盖层主要是海湾地区的区域现象，形成于有小潮汐运动和水循环的浅海地区。它是一种典型的胶结灰岩硬石膏，基质为小贝壳和方解石。

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Application of Underwater MASW and Acoustic Methods in the Assessment of Sub-seabed Conditions Prior to Construction of the Manifa Causeway, Saudi Arabia

The offshore Gulf Region is known to have caprock layer within the first 0-5m of ground below the seabed. It varies in thickness from a few centimetres to two or three metres in thickness. Caprock is predominantly a Gulf regional phenomenon forming in shallow coastal areas where there are small tidal movements and water circulation. It is typically a cemented Limestone anhydrite with a matrix of small shells and calcarenite.

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Symposium on the Application of Geophysics to Engineering and Environmental Problems 2018

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