朱超祁, 周蕾, 张红, 程升, 焦欣然, 姜君, 申志聪, 贾永刚. 2017: 南海北陆架坡表面沉积物的物理力学性质初探. 工程地质学报, 25(6): 1566-1573. DOI: 10.13544/j.cnki.jeg.2017.06.020
    引用本文: 朱超祁, 周蕾, 张红, 程升, 焦欣然, 姜君, 申志聪, 贾永刚. 2017: 南海北陆架坡表面沉积物的物理力学性质初探. 工程地质学报, 25(6): 1566-1573. DOI: 10.13544/j.cnki.jeg.2017.06.020
    ZHU Chaoqi, ZHOU Lei, ZHANG Hong, CHENG Sheng, JIAO Xinran, JIANG Jun, SHEN Zhicong, JIA Yonggang. 2017: PRELIMINARY STUDY OF PHYSICAL AND MECHANICAL PROPERTIES OF SURFACE SEDIMENT IN NORTHERN SOUTH CHINA SEA. JOURNAL OF ENGINEERING GEOLOGY, 25(6): 1566-1573. DOI: 10.13544/j.cnki.jeg.2017.06.020
    Citation: ZHU Chaoqi, ZHOU Lei, ZHANG Hong, CHENG Sheng, JIAO Xinran, JIANG Jun, SHEN Zhicong, JIA Yonggang. 2017: PRELIMINARY STUDY OF PHYSICAL AND MECHANICAL PROPERTIES OF SURFACE SEDIMENT IN NORTHERN SOUTH CHINA SEA. JOURNAL OF ENGINEERING GEOLOGY, 25(6): 1566-1573. DOI: 10.13544/j.cnki.jeg.2017.06.020

    南海北陆架坡表面沉积物的物理力学性质初探

    PRELIMINARY STUDY OF PHYSICAL AND MECHANICAL PROPERTIES OF SURFACE SEDIMENT IN NORTHERN SOUTH CHINA SEA

    • 摘要: 南海北部陆坡工程地质环境复杂,并分布有大量油气资源,对该区海底沉积物的物理力学性质的研究是不可缺少的研究工作。本文利用2015年6月于"实验3"号科考船南海北部航次获得的箱式样和柱状样样品,在室内进行了含水率、天然密度、比重、微型扭力十字板以及微型贯入试验和压缩试验,获得了该处沉积物的粒度分布特征及物理力学性质参数。研究表明,南海北陆坡架表层沉积物类型以粉砂质黏土和黏土质粉砂为主,具有较高的含水率和较低的湿密度,抗剪强度、贯入阻力、压缩性等力学性质较差。沉积物的各项土工参数随深度呈现一定规律性的变化,且沉积环境、粒度成分和沉积年代等因素对其存在一定影响。

       

      Abstract: The geological environment of the northern South China Sea is complex and rich in oil and gas resources. It is necessary to examine the physical and mechanical properties of seafloor sediments. Hence, this paper reports a preliminary study of the geological environment. In this study, a series of tests to determine various factors including water content, density, and specific gravity, are conducted in conjunction with miniature vane shear, micro penetration, and compression tests on samples collected in June 2015. The study includes investigating types of seafloor sediments and index parameters of the physical and mechanical properties of soil in the northern South China Sea. The results of the investigation indicate that the surficial seafloor sediment in the study area is mainly composed of silty clay and clayey silt with high moisture content, low density, and low mechanical strength. The variation in the fore-mentioned parameters is generally correlated with the depth of the seabed. Additionally, sedimentary environment, grain size composition, and age are determined as important factors controlling the properties of the sediments to a significant extent.

       

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