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Evaluation of Temperature Trend In Contaminated Tidal Flat In The Ariake Sea, Japan | Science Publications

机译:日本有明海受污染的滩涂温度趋势评估科学出版物

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> Thermal environment of the tidal flat is one of the major parts of the contaminated geo-environment of the Ariake Sea. The activities of marine ecosystem in tidal flats depend strongly on the thermal environment. In order to get a clear idea about the thermal environment of the tidal flats of the Ariake Sea, two study areas, Iida and Higashiyoka tidal flats were selected. By installing five nos. of thermocouple (Tokyo Sokki co., Model no.: N004853) at different specified depths ( 0.10 m,0.20 m,0.50 m,1.0 m and 2.0 m) connected with data logger (TDS-530) were used to observe diurnal variation of temperature during the 1st April to 8th April, 2006 at Higashiyoka tidal flat. The measured temperature was stored automatically at 1 h interval in the data logger. To observe seasonal variation of temperature in different depths , temperature was measured by inserting the thermocouple at 0.10 m depths interval in the last week of every month at both study areas in the Ariake sea tidal flat. The diurnal temperature variation was more visible near the surface (0.10 m and 0.20 m) indicating the influence of solar radiation in that portion, however in the deeper region (1.0 m and 2.0 m depth) the temperature was dominated by thermal properties of the mud. From seasonal variation of temperature it was seen that during spring and summer heat was transferred from subsurface to the deeper area but during winter and autumn opposite phenomenon was observed. A correlation is proposed to get the temperature profile in the tidal flat in different seasons.
机译: >潮滩的热环境是有明海受污染的地质环境的主要部分之一。潮滩中海洋生态系统的活动在很大程度上取决于热环境。为了对有明海的滩涂的热环境有一个清晰的认识,我们选择了两个研究区域,饭田和东横冈。通过安装五个编号。使用连接数据记录器(TDS-530)的不同指定深度(0.10 m,0.20 m,0.50 m,1.0 m和2.0 m)的热电偶(Tokyo Sokki co。,型号:N004853)观察温度的日变化东yoka潮滩2006年4月1日至4月8日的温度。测得的温度每隔1小时自动存储在数据记录仪中。为了观察不同深度处温度的季节性变化,在有明海潮滩两个研究区的每个月的最后一周,以每隔0.10 m的深度插入热电偶来测量温度。昼夜温度变化在地表(0.10 m和0.20 m)附近更明显,表明该部分受到太阳辐射的影响,但是在更深的区域(1.0 m和2.0 m深度),温度受泥浆的热性质支配。从温度的季节变化可以看出,春季和夏季热量从地下转移到更深的区域,而在冬季和秋季则观察到相反的现象。提出了相关性以获取不同季节的潮滩温度曲线。

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