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对在冻土条件下的雅库茨克热电厂的长期(2008~2011年)研究进行分析。对沿着建筑物和墙壁邻近地区的36个水井地下4~16 m温度进行测量。目前融化区域下所有的建筑,利用循环泵站和东北的水墙附近的锅炉设备可以观测到最高年平均气温(12~13℃)和不冻层厚度(23~25 m)。根据化学水处理东部解冻较早的土壤冻结从顶部到8.0~9.5m。解冻层保留较深,其中在2011年10~11 m深度年平均气温下降到0.3~0.6℃。在雅库茨克热电厂的大部分地区仍然是永久冻结地区。在主楼下方4~10 m的深度的年平均气温为0~-4.1℃。近年来,筑物地温逐步恢复的基础依据已经发生变化。
The long-term (2008-2011) study of Yakutsk thermal power plants in frozen earth conditions was analyzed. Measurements were taken at a depth of 4 to 16 m below the surface of 36 wells along the buildings and adjacent walls. At present, all the buildings under the melting area can observe the highest annual average temperature (12-13 ° C) and the thickness of the anti-freeze layer (23-25 m) by using circulating pump stations and boiler equipment near the water wall in the northeast. According to the chemical water treatment east thaw earlier soil freezing from the top to 8.0 ~ 9.5m. The thawing layer remains relatively deep, with annual mean temperature of 10 ~ 11 m in 2011 decreasing to 0.3 ~ 0.6 ℃. Most areas of the Yakutsk thermal power plant remain permanently frozen. In the main building 4 ~ 10 m depth of the annual average temperature of 0 ~ -4.1 ℃. In recent years, the basis for the gradual restoration of building geothermal has changed.