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Simulation Analysis of the Refreezing Characteristics of Cast-in-Place Piles in Permafrost Regions on the Qinghai-Tibet Plateau

机译:青藏高原多年冻土地区铸造桩泄漏特征的仿真分析

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The stability of piles used for the Qinghai-Tibet Power Transmission Line (QTPTL) is important for the operation of the line because this type of foundation is generally used in areas with unfavorable geological conditions. Intensive heat influence of casting temperatures and hydration heat means that the refreezing of cast-in-place piles obviously affects the schedule and cost of the project. The refreezing process was simulated on a cast-in-place pile based at tower 1443 of QTPTL in the warm and ice-rich Touerjiu region, Qinghai-Tibet Plateau. The results show that the thermal energy, originating from the casting temperature and hydration heat of cement, dissipates mainly through lateral heat flux, resulting in the warming and thawing of surrounding soil. The stability of the pile will dramatically decrease during the process. It was also found that the dissipation of the thermal energy is affected by the heat conductivity and water/ice content of the surrounding soil. The refreezing process of a 1-m-diameter pile in Touerjiu region continues for about 67 days. The maximum thermal influence range is about 9.8 m for a single pile, and group pile effects exist for towers of QTPTL in Touerjiu region. The duration of the thermal impact of casting temperature and hydration heat of a single pile is about 630 days.
机译:用于青藏电力传输线(QTPTL)的桩的稳定性对于该线路的操作是重要的,因为这种类型的基础通常用于具有不利地质条件的区域。铸造温度和水化热量的密集热影响意味着铸造桩的泄漏显然会影响项目的时间表和成本。在QTPTL的QTPTL塔1443的QTPTL塔,富冰富塞地区,青藏高原的QTPTL塔的热桩上模拟了简推过程。结果表明,源自水泥浇铸温度和水化热的热能,主要通过横向热通量消散,导致周围土壤的升温和解冻。在该过程中,桩的稳定性会显着降低。还发现热能的耗散受到周围土壤的导热率和水/冰含量的影响。 Touerjiu地区1米直径桩的简便过程持续约67天。对于单一桩的最大热影响范围为约9.8米,并且在Touerjiu地区的QTPTL塔中存在组桩效应。铸造温度和单桩水合热的热冲击的持续时间约为630天。

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