珠江口-南海北部陆架与温州港-东海中部陆架表层沉积物物理力学性质研究

    PHYSICAL AND MECHANICAL PROPERTIES OF SURFACE SEDIMENTS FROM THE PEARL RIVER ESTUARY-THE NORTHERN SOUTH CHINA SEA AND WENZHOU PORT-THE CENTRAL EAST CHINA SEA

    • 摘要: 明晰海底沉积物物理力学性质是海洋工程结构设计的前提和基础。本文针对我国珠江口-南海北部陆架和温州港-东海中部陆架所取的表层沉积物,开展基本物理性质试验,获得了天然含水量、比重、液塑限、颗粒级配等参数指标;进行一维压缩、K0固结试验以及渗透试验,探究了沉积物的固结及渗透特性;进行电镜扫描测试,分析了沉积物的微观结构特征。试验结果表明,两海域沉积物均属于低液限黏土(CL);东海沉积物主要由细粒土(粒径小于0.075 mm)构成,基本物理力学性质相近;而南海沉积物各项参数指标随空间分布呈规律性变化,液限、黏粒含量、压缩系数随离岸距离的增大而增加,固结系数随离岸距离的增大而减小。

       

      Abstract: It is necessary to clarify the physical and mechanical properties of seabed sediments before designing offshore engineering structures. Basic physical property tests were carried out on surface sediments collected from the Pearl River Estuary in the northern South China Sea and from Wenzhou Port to the central East China Sea. Parameters related to natural water content, specific gravity,Atterberg limits, and particle size distribution were obtained. In addition, one-dimensional compression tests,K0 consolidation tests, and permeability tests were conducted to investigate the consolidation and permeability characteristics of the sediments. Finally, scanning electron microscopy tests were performed to analyze the microstructure of the surface sediments. Experimental results show that the sediments in both sea areas are low-liquid-limit clays. The sediments in the East China Sea are mainly composed of fine-grained soil(particle size <0.075 mm), and their basic physical and mechanical properties are relatively uniform. In contrast, for the sediments in the South China Sea, the parameters characterizing physical and mechanical properties exhibit a clear variation with spatial distribution. The liquid limit, clay content, and compression coefficient increase with increasing distance from the coast, while the consolidation coefficient decreases with increasing offshore distance.

       

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