Numerical simulation on the performance of thermosyphon adopted to mitigate thaw settlement of embankment in sandy permafrost zone

被引:57
作者
Chen, Lin [1 ,3 ]
Yu, Wenbing [1 ,2 ]
Lu, Yan [1 ]
Liu, Weibo [1 ]
机构
[1] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Frozen Soil Engn, Lanzhou 730000, Gansu, Peoples R China
[2] Chongqing Jiaotong Univ, Coll Civil Engn, Chongqing 400074, Peoples R China
[3] Univ Montreal, Dept Geography, Cold Reg Geomorphol & Geotech Lab, Montreal, PQ H2V 2E8, Canada
关键词
Qinghai-Tibet Railway; Climate warming; Aeolian sand; Permafrost degradation; Crushed-rock layer; Thermosyphon; 2-PHASE CLOSED THERMOSIPHONS; QINGHAI-TIBETAN PLATEAU; CRUSHED-ROCK; COOLING PERFORMANCE; HIGHWAY EMBANKMENT; GROUNDWATER-FLOW; HEAT-EXCHANGER; REGIONS; TEMPERATURE; DESERTIFICATION;
D O I
10.1016/j.applthermaleng.2017.09.130
中图分类号
O414.1 [热力学];
学科分类号
摘要
Desertification and climate warming have affected the stability of the crushed-rock interlayer embankment of the Qinghai-Tibet Railway (QTR) in the permafrost zone. The two-phase closed thermosyphon (TPCT) is adopted to mitigate the problem in sandy permafrost zone. A composite heat transfer model, including air convection in the crushed-rock interlayer, the air-TPCT-soil coupled heat transfer for TPCTs system and the heat conduction with phase change in the soil layers, is developed based on the equivalent thermal resistance for the TPCf. And an increase in average air temperature by 0.04 degrees C a(-1) was also simulated. The numerical results indicate that TPCTs play rapidly a cooling effect and approach a thermal balance state after 10 years of construction. TPCfs installed at the embankment slope effectively ease the underlying permafrost degeneration and cool down permafrost. However, the cooling scope and magnitude of TPCTs largely depends on working duration after installation. If the mean average air temperature is still lower than -3.5 degrees C after considering climate warming, TPCTs installed at the 10th year of QTR operation can mitigate the negative effect of climate warming and sand accumulation in the sandy permafrost zone of the Qinghai Tibet Corridor. (C) 2017 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1624 / 1633
页数:10
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