海洋学研究 ›› 2020, Vol. 38 ›› Issue (1): 20-26.DOI: 10.3969/j.issn.1001-909X.2020.01.003

• 研究论文 • 上一篇    下一篇

海底表层土导热系数变化规律的试验研究

何旭涛1, 林晓波1, 徐建良1, 李世强1, 杨婧荷2, 徐海宁1   

  1. 1.国网浙江省电力有限公司 舟山供电公司,浙江 舟山 316021;
    2.自然资源部 第二海洋研究所,浙江 杭州 310012
  • 收稿日期:2019-04-19 出版日期:2020-03-15 发布日期:2022-11-14
  • 作者简介:何旭涛(1973-),男,浙江省舟山市人,高级工程师,主要从事海洋输电技术研究。E-mail:hxt0580@163.com
  • 基金资助:
    国家自然科学基金项目资助(5167090521);浙江省电力有限公司基金项目资助(5211ZS16000C)

Experimental study on variation of thermal conductivity of superficial submarine soils

HE Xutao1, LIN Xiaobo1, XU Jianliang1, LI Shiqiang1, YANG Jinghe2, XU Haining1   

  1. 1. State Grid Zhejiang Electric Power Company Zhoushan Branch, Zhoushan 316021, China;
    2. Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012,China
  • Received:2019-04-19 Online:2020-03-15 Published:2022-11-14

摘要: 基于热探针法原理,测试了在杭州湾以东陆架区取得的28个海底表层柱状样0.2、1.0和1.8 m处的导热系数,结合激光粒度分析结果,比较了研究区6种土导热系数的大小,发现含砂量大于10%的粗粒土拥有较大的导热系数。土质类型相同时,含水量和干密度对其导热系数影响显著。杭州湾沉积区、混合沉积区,陆架砂质沉积区表层土导热系数的平均值分别是:1.25、1.45 和1.46 W·m-1·K-1,呈现出由近岸向外海增大的趋势。而土样导热系数在垂向的变化表明:水深、埋深等空间分布因素对海洋土的热物性没有直接影响。

关键词: 海洋土, 导热系数, 含砂量, 空间分布

Abstract: From the continental shelf at the east of Hangzhou Bay, 28 sample columns were acquired. The thermal conductivities of soils at different depths (0.2 m,1.0 m and 1.8 m) from these cores were tested by thermal probe. Correspondingly, particle size of the soils were also tested. Through the comparison between six kinds of soils in the study area, It was found that those with higher sand content (>10%) have bigger thermal conductivities. Besides, water content and dry density have significant effect on thermal conductivities of certain type of soil. Average value of thermal conductivity for superficial soils in Hangzhou Bay area,mixed deposit area and shelf sandy area are respectively 1.25 W·m-1·K-1, 1.45 W·m-1·K-1 and 1.46 W·m-1·K-1, which indicates that thermal conductivities increase from the coast to open waters. On the other hand, vertical variation of thermal conductivities shows that spatial factors including water depth and buried depth have no direct effect on the thermophysical properties of seabed soils.

Key words: marine soils, thermal conductivity, sand content, spatial distribution

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