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渤海中部海域海底热扩散率及恒温层深度研究
引用本文:刘文通,徐德伦,候伟,宋珊.渤海中部海域海底热扩散率及恒温层深度研究[J].中国海洋大学学报(自然科学版),1994(4).
作者姓名:刘文通  徐德伦  候伟  宋珊
作者单位:青岛海洋大学,渤海石油公司
摘    要:利用渤海中部海域泥温实测资料,计算出该海域海底热扩散率及恒温层深度。结果表明,8#平台处的热扩散率为0.001~0.005cm2s-1,A(B)平台处为0.002~0.010cm2s-1。恒温层深度8#平台处为8m,A(B)平台处10m,也有差异。与陆地比较,海底恒温层深度较浅,且水深越深恒温层深度越浅。

关 键 词:渤海中部海域  泥温  热导率  海底热扩散率  恒温深度

STUDIES ON THE SEA-BED HEAT DIFFUSION RATE AND SOIL DEPTH OF CONSTANT TEMPERATURE IN CENTRAL BOHAI SEA
Liu Wentong, Xu Delun, Hou Wei.STUDIES ON THE SEA-BED HEAT DIFFUSION RATE AND SOIL DEPTH OF CONSTANT TEMPERATURE IN CENTRAL BOHAI SEA[J].Periodical of Ocean University of China,1994(4).
Authors:Liu Wentong  Xu Delun  Hou Wei
Institution:Liu Wentong; Xu Delun; Hou Wei(Physical Oceanography Laboratory)Song Shan(Bobal Petroleum Company)
Abstract:The heat diffusion rate and soil depth of constant temperature are calculated by using the measured soil temperatures at the sites No. 8 and A(B) in the central Bobal Sea. The results indicate that the heat diffusion rate K is equal to 0. 001- 0. 005cm2 s-1 and 0. 002-0. 010cm2s -1 at the two sites, respectively. The soil depth of constant temperature is sin at site No. 8 and 10m at site A(B). The soil depth of constant temperature in the sea-bed is shallower compared with that on land, and the deeper the sea water, the shallower is the soil depth of constant temperature.
Keywords:Soil temperature  heat diffusion rate  soil depth of constant temperature
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