CAI Han-cheng, MENG Jin-bao, ZHAO Xiang-qing, et al. Design method of the thermosyphon embankment in permafrost
region based on principle of heat balance[J]. 2020, 41(11): 3769-3776.
CAI Han-cheng, MENG Jin-bao, ZHAO Xiang-qing, et al. Design method of the thermosyphon embankment in permafrost
region based on principle of heat balance[J]. 2020, 41(11): 3769-3776.DOI: 10.16285/j.rsm.2020.0269.
Thermosyphon is one of the important measures for thermal protection of the embankment in permafrost region. But the design method of the thermosyphon embankment is not provided in relevant standards. Therefore
the design of the existing embankments with thermosyphon mainly depends on the past engineering experience. Through field monitoring and theoretical calculation
the characteristics of heat exchange balance for the embankment in frozen soil region were analyzed. It was found that the embankment absorbs heat in warm season
but releases heat in cold season
and it was in the endothermic state for the whole year. The essential reason of the embankment thawing settlement is that the heat absorption is greater than heat release. A new design method of thermosyphon embankment was proposed based on the theory of heat balance. Its basic principle is to ensure the thermosyphon annual heat transmission capacity which is not less than the embankment net heat absorption. Taking the highway engineering in permafrost region of Qinghai-Tibet Plateau as an example
the design method proposed in this paper was verified by field test. The results show that the settlement of the thermosyphon embankment designed using the proposed method was significantly less than that of the ordinary ones. The thermosyphon embankment has improved the stability of the underlying permafrost and mitigated the settlement of the foundation permafrost. That verified the correctness and rationality of the method proposed in this paper. This method has clear theory
simple parameter acquisition and strong engineering application value
which can be widely used in design of the thermosyphon embankment in permafrost region.