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Soil Thermal Conductivity Study in Western Coastal Zone of Taiwan

机译:台湾西部沿海地区土壤热导率研究

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摘要

The thermal conductivity which governs the flow of heat through the soil is defined as the quantity of heat that flows through a unit area in a unit time under a unit temperature gradient. This characteristic of soil is usually concerned by power cable designer because of copper resistance during power transitions in both underground and submarine circumstance.rnThe study employed field needle shaped probe to measure 4 points on the beach in Penghuo Island of Taiwan and conduct 12 laboratory tests to measure the thermal conductivity. The soil of beach was categorized to be middle-fine sand with coral skeleton. For simulating the situation of water content of soil on beach varied with the tidal level and the run up of wave, the needle probe instead of micro variation to measure the average thermal conductivity. The results of filed investigation varied from 0.8W/mK to 1.17W/mK, under 27 degree Celsius of circumstance and being similar to Nidal's measurement of sand ranged from 0.58 to 1.94.
机译:控制通过土壤的热流的热导率定义为在单位温度梯度下在单位时间内在单位时间内流过单位面积的热量。电力电缆设计人员通常会因为在地下和海底情况下电源转换过程中的铜电阻而担心土壤的这种特性。该研究采用野外针形探头在台湾澎湖岛的海滩上测量了4个点,并进行了12次实验室测试测量热导率。海滩的土壤被分类为具有珊瑚骨架的中细砂。为了模拟海滩上土壤的水分含量随潮汐水平和波的上升而变化的情况,用针式探头代替微变化来测量平均导热率。现场调查的结果是在27摄氏度的环境下,从0.8W / mK到1.17W / mK不等,与Nidal测得的沙相似,范围从0.58到1.94。

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