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The changing process and trend of ground temperature around tower foundations of Qinghai-Tibet Power Transmission line

机译:青藏输电线路塔基周围地温变化过程及趋势

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摘要

After the construction of Qinghai-Tibet Highway and Railway,the Qinghai-Tibet Power Transmission(QTPT)line is another major permafrost engineering project with new types of engineering structures.The changing process and trend of ground temperature around tower foundations are crucial for the stability of QTPT.We analyzed the change characteristics and tendencies of the ground temperature based on field monitoring data from 2010 to 2014.The results reveal that soil around the tower foundations froze and connected with the artificial permafrost induced during the construction of footings after the first freezing period,and the soil below the original permafrost table kept freezing in subsequent thawing periods.The ground temperature lowered to that of natural fields,fast or slowly for tower foundations with thermosyphons,while for tower foundations without thermosyphons,the increase in ground temperature resulted in higher temperature than that of natural fields.Also,the permafrost temperature and ice content are significant factors that influence the ground temperature around tower foundations.Specifically,the ground temperature around tower foundations in warm and ice-rich permafrost regions decreased slowly,while that in cold and ice poor permafrost regions cooled faster.Moreover,foundations types impacted the ground temperature,which consisted of different technical processes during construction and variant of tower footing structures.The revealed changing process and trend of the ground temperature is beneficial for evaluating the thermal regime evolution around tower foundations in the context of climate change.
机译:继青藏公路和铁路建设之后,青藏输电(QTPT)线路是另一项具有新型工程结构的多年冻土工程项目。塔基周围的地温变化过程和趋势对稳定性至关重要。根据2010年至2014年的实地监测数据,分析了地温的变化特征和趋势,结果表明塔基础周围的土壤冻结并与首次冻结后基础施工过程中引起的人工多年冻土有关。期间,原始冻土层下面的土壤在随后的解冻期中保持冻结。地温降至自然田地,装有热虹吸管的塔基础快或慢,而没有热虹吸的塔基础的地温升高导致高于自然领域的温度。此外,永久冻土温度温度和含冰量是影响塔基础周围温度的重要因素。特别是,温暖和富冰的多年冻土地区塔基础周围的地面温度下降缓慢,而寒冷和冰贫寒的冻土地区冷却速度更快。不同的类型会影响地面温度,这由建造过程中的不同技术过程以及塔式立脚结构的变化组成。揭示的地面温度变化过程和趋势有利于评估气候变化背景下塔基础周围的热状态演变。

著录项

  • 来源
    《寒旱区科学:英文版》 |2019年第001期|P.13-20|共8页
  • 作者单位

    [1]State Grid Qinghai Electric Power Research Institute,Xining,Qinghai 810008,China;

    [2]State Key Laboratory of Frozen Soil Engineering,Northwest Institute of Eco-environment and Resources,Chinese Academy of Sciences,Lanzhou,Gansu 730000,China;

    [2]State Key Laboratory of Frozen Soil Engineering,Northwest Institute of Eco-environment and Resources,Chinese Academy of Sciences,Lanzhou,Gansu 730000,China;

    [1]State Grid Qinghai Electric Power Research Institute,Xining,Qinghai 810008,China;

    [1]State Grid Qinghai Electric Power Research Institute,Xining,Qinghai 810008,China;

  • 收录信息 中国科学引文数据库(CSCD);
  • 原文格式 PDF
  • 正文语种 CHI
  • 中图分类 天文学、地球科学;
  • 关键词

    Qinghai-Tibet Power Transmission line; tower foundation; ground temperature change characteristic; trend;

    机译:青藏输电线路;塔基;地温变化特征;趋势;
  • 入库时间 2022-08-19 04:28:30
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