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Thermal Stability Analysis under Embankment with Asphalt Pavement and Cement Pavement in Permafrost Regions

机译:沥青地区沥青路面堤坝下的热稳定性分析

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The permafrost degradation is the fundamental cause generating embankment diseases and pavement diseases in permafrost region while the permafrost degradation is related with temperature. Based on the field monitoring results of ground temperature along G214 Highway in high temperature permafrost regions, both the ground temperatures in superficial layer and the annual average temperatures under the embankment were discussed, respectively, for concrete pavements and asphalt pavements. The maximum depth of temperature field under the embankment for concrete pavements and asphalt pavements was also studied by using the finite element method. The results of numerical analysis indicate that there were remarkable seasonal differences of the ground temperatures in superficial layer between asphalt pavement and concrete pavement. The maximum influencing depth of temperature field under the permafrost embankment for every pavement was under the depth of 8 m. The thawed cores under both embankments have close relation with the maximum thawed depth, the embankment height, and the service time. The effective measurements will be proposed to keep the thermal stabilities of highway embankment by the results.
机译:多年冻土的降解是多年冻土区域产生堤防疾病和路面疾病的根本原因,同时永久冻土降解与温度有关。基于高温多年冻土区G214公路的地下温度的现场监测结果,浅谈浅层浅层浅层底层的平均温度,用于混凝土路面和沥青路面。通过使用有限元方法,还研究了混凝土路面和沥青路面堤下下的最大温度场深度。数值分析的结果表明沥青路面与混凝土路面之间的浅表层浅季节性差异。每个人行道的永久冻土路堤下的最大温度场的最大影响深度在8米的深度下。两个堤坝下的解冻核心与最大解冻深度,路堤高度和服务时间具有密切的关系。将提出有效测量以通过结果保持高速公路堤防的热稳定性。

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