高压埋地CO2管道泄漏土壤温度场分布研究

A study on soil temperature field distribution induced by leakage of buried high-pressure CO2 pipelines

  • 摘要:
    目的 碳捕集、利用与封存(CCUS)是实现大规模碳减排的核心技术路径,管道泄漏是制约其安全运行的主要原因之一。相较于架空管道,埋地管道泄漏受土壤环境的影响,扩散机理更复杂。超临界CO2泄漏产生的焦耳-汤姆孙效应会引发土壤温度骤降,进而诱发管材脆断、土壤冻胀等次生风险。
    方法 为揭示土壤含水率、泄漏方向及泄漏孔名义直径对埋地CO2管道泄漏扩散行为与土壤温度场演化的影响规律,依托工业规模埋地CO2管道泄漏实验平台开展11组实验。通过对土壤温度场进行全程动态监测,同步记录地表CO2射流形貌与冻土区参数。
    结果 土壤含水率与土壤低温区扩散范围呈正相关,低温区最大径向扩展距离随时间的演化曲线整体呈S形增长;高含水率工况下,管道周边冻土区形貌的非对称性显著增强。泄漏方向决定了低温CO2射流在土壤中的优先扩散路径,土壤环向温度场的温降峰值方位与射流初始方向一致。泄漏孔名义直径与土壤温降幅度呈负相关。
    结论 上述结果明确了土壤含水率、泄漏方向及泄漏孔名义直径对埋地超临界CO2管道泄漏后土壤温度场演化的影响规律,可为长输CO2管道泄漏监测点的优化布设、低温风险评估及应急防控方案制定提供实验依据与理论支撑。

     

    Abstract:
    Objective Carbon Capture, Utilization, and Storage (CCUS) is a critical technical pathway for large-scale carbon emission reduction, yet pipeline leakage remains a key constraint on its operational safety. Unlike aboveground pipelines, buried pipelines exhibit more complex leakage diffusion dynamics due to interactions with surrounding soil. Additionally, the Joule–Thomson effect during supercritical CO2 leakage causes rapid soil cooling, triggering secondary risks such as pipeline embrittlement and frost heave.
    Methods This study aims to reveal how soil water content, leakage direction, and leakage orifice nominal diameter affect the leakage-diffusion behavior of buried CO2 pipelines and the evolution of the soil temperature field. To this end, eleven test runs were conducted on an industrial-scale test platform for buried CO2 pipeline leakage. The soil temperature field is dynamically monitored throughout the test, while the surface CO2 jet morphology and frozen soil zone parameters are recorded simultaneously.
    Results Soil water content correlates positively with the diffusion range of the low-temperature soil zone. The evolution curve of the maximum radial extension distance of the low-temperature zone over time generally follows an S-shaped growth pattern. Under high soil water content, the morphological asymmetry of the frozen soil zone around the pipeline increases significantly. Leakage direction determines the preferential diffusion path of low-temperature CO2 jets in soil, and the peak temperature drop azimuth in the circumferential soil temperature field aligns with the initial jet direction. The nominal diameter of the leakage orifice correlates negatively with the magnitude of soil temperature drop.
    Conclusion These findings clarify how soil water content, leakage direction, and leakage orifice nominal diameter influence soil temperature field evolution following supercritical CO2 pipeline leaks. They provide experimental basis and theoretical support for optimizing leakage monitoring point placement, assessing low-temperature risks, and formulating emergency response strategies for long-distance CO2 pipelines.

     

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