首页> 外文会议>International Conference on Advances in Energy and Environmental Research >ANALYSIS OF THE THERMOPHYSICAL PROPERTIES AND INFLUENCING FACTORS OF VARIOUS ROCK TYPES FROM THE GUIZHOU PROVINCE
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ANALYSIS OF THE THERMOPHYSICAL PROPERTIES AND INFLUENCING FACTORS OF VARIOUS ROCK TYPES FROM THE GUIZHOU PROVINCE

机译:贵州省各种岩石类型热物理特性及影响因素分析

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A series of analyses have been carried out on a number of rock types from the Guizhou Province to investigate their thermophysical properties. A total of 433 samples from 14 types of rock were collected, tested and analyzed. It was found that in this province, the average thermal conductivity of the samples ranged between 1.516±0.264 and 5.066±0.521 W/(m.K), the average specific heat capacity varied from 0.272±0.042 to 0.603±0.096 kJ/(kg?°C), and the average thermal diffusion coefficients were from 0.752±0.331 to 2.854±0.368 MJ/(m~3?K). The older rocks always had higher thermal conductivity and thermal diffusion. Thermal conductivity and thermal diffusion of rocks are positively correlated with the mineral content of high thermal conductivity species, but the situation for the specific heat capacity is the opposite. With increasing mineral particle size, the thermal conductivity and thermal diffusion coefficient also increase, but the relationship with specific heat capacity is not obvious. The thermal conductivity and thermal diffusion coefficient of rocks increases under water saturated conditions compared to dry conditions, but the specific heat capacity decreases.
机译:一系列的分析已经在一些岩石类型从贵州省考察其热物理性质进行。从14种类型的岩石总共433个样品收集,测试和分析。据发现,在此省,样品的平均热导率1.516±0.264和5.066±0.521 W /(mK的),平均比热容量从0.272±0.042变化到0.603±0.096千焦/(千克?°之间的范围内C),和平均热扩散系数为0.752,从±0.331至2.854±0.368 MJ /(米3〜?K)。较老的岩石总是有更高的导热性和热扩散。热导率和岩石的热扩散具有正高导热性物质的矿物质含量相关,但对于特定的热容量的情况是相反的。随着矿物颗粒的尺寸,热导率和热扩散系数也增加,但具有比热容量的关系不明显。热导率和相比,干燥的条件下用水饱和的条件下增加的岩石的热扩散系数,但具体的热容量而降低。

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