Thermal and hydrological processes in permafrost slope wetlands affect thermosyphon embankment stability

IF 6.4 1区 地球科学 Q1 ENVIRONMENTAL SCIENCES Advances in Climate Change Research Pub Date : 2024-08-01 DOI:10.1016/j.accre.2024.07.010
Bo-Wen Tai , Qing-Bai Wu , Xiao-Ming Xu
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Abstract

To ensure the long-term service performance of infrastructure such as railways, highways, airports and oil pipelines built on permafrost slope wetland sites, it is imperative to systematically uncover the long-term heat‒water changes of soil in slope wetlands environment under climate warming. More specifically, considering valuable field data from 2001 to 2019, the long-term heat and water changes in active layers of the slope wetland site along the Qinghai–Xizang Railway (QXR) are illustrated, the effect of thermosyphon measures in protecting the permafrost environment is evaluated, and the influences of climate warming and hydrological effects on the stability of slope wetland embankments are systematically discussed. The permafrost at the slope wetland site is rapidly degrading, demonstrating a reduction in active layer thickness of >3.7 cm per year and a permafrost temperature warming of >0.006 °C per year. The thermosiphon embankment developed by QXR has a specific cooling period; thus, to mitigate the long-term impacts of climate warming on the thermal stability of permafrost foundation, it is essential to implement strengthening measures for the thermosiphon embankment, such as adding a crushed-rock layer or sunshade board on the slope of thermosiphon embankment to creating a composite cooling embankment. Short-term seasonal groundwater seepage intensifies frost damage to the slope wetland embankment, while long-term seasonal supra-permafrost water and groundwater seepage exacerbates uneven transverse deformation of slope wetland embankment. Long-term climate warming and slope effects have altered the surface water and groundwater hydrological processes of slope wetlands, potentially leading to an increased occurrence of slope embankment instability. These results are crucial for improving our understanding of heat and water variation processes in the active layer of slope wetland sites located in permafrost regions and ensuring long-term service safety for the QXR.

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永久冻土斜坡湿地的热过程和水文过程对热流堤稳定性的影响
为确保建在冻土坡地湿地上的铁路、公路、机场、输油管道等基础设施的长期服役性能,系统揭示气候变暖条件下坡地湿地环境土壤的长期水热变化势在必行。具体而言,结合2001年至2019年的宝贵野外资料,阐述了青藏铁路沿线坡面湿地场地活动层的长期水热变化,评价了温水喷雾措施在保护冻土环境方面的效果,系统讨论了气候变暖和水文效应对坡面湿地堤坝稳定性的影响。坡地湿地的永久冻土正在迅速退化,活动层厚度每年减少 3.7 厘米,永久冻土温度每年升高 0.006 °C。QXR 开发的热虹吸堤具有特定的降温期,因此,为减轻气候变暖对冻土地基热稳定性的长期影响,必须对热虹吸堤采取加固措施,如在热虹吸堤坡面上增加碎石层或遮阳板,形成复合降温堤。短期的季节性地下水渗流加剧了坡面湿地堤坝的冻害,长期的季节性上冻水及地下水渗流加剧了坡面湿地堤坝的不均匀横向变形。长期的气候变暖和坡度效应改变了坡地湿地的地表水和地下水水文过程,可能导致坡地堤坝失稳的发生率增加。这些结果对于提高我们对位于永久冻土地区的坡地湿地活动层的热量和水量变化过程的认识以及确保 QXR 的长期服务安全至关重要。
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来源期刊
Advances in Climate Change Research
Advances in Climate Change Research Earth and Planetary Sciences-Atmospheric Science
CiteScore
9.80
自引率
4.10%
发文量
424
审稿时长
107 days
期刊介绍: Advances in Climate Change Research publishes scientific research and analyses on climate change and the interactions of climate change with society. This journal encompasses basic science and economic, social, and policy research, including studies on mitigation and adaptation to climate change. Advances in Climate Change Research attempts to promote research in climate change and provide an impetus for the application of research achievements in numerous aspects, such as socioeconomic sustainable development, responses to the adaptation and mitigation of climate change, diplomatic negotiations of climate and environment policies, and the protection and exploitation of natural resources.
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