泥水盾构排浆管土石团聚体床层运移特性及堵塞防控对策

Transport characteristics of soil-rock agglomerates bed load in slurry shield discharge pipelines and countermeasures for blockage prevention

  • 摘要: 泥水盾构穿越黏砾互层时,易形成大块土石团聚体,严重影响掘进效率与安全。为揭示土石团聚体在排渣管内的运移规律及沉积堵塞机制,依托芜湖长江隧道工程,构建固液两相流耦合模型,系统分析团聚体尺寸、泥浆密度与流速对排渣性能的影响。结果表明:团聚体在管内以床层推移形式运动,并呈现显著的速度分层特征;当团聚体尺寸由3.0 cm增至4.5 cm时,床层推移速度呈线性下降,局部泥浆压力增加35.5%;提升泥浆密度与流速可显著增强携渣运移能力,当泥浆密度由1.05 g/cm3增至1.35 g/cm3时,床层推移速度提升26.2%;泥浆流速由2.3 m/s增至3.3 m/s时,床层推移速度增加136.8%,增大泥浆流速是抑制团聚体沉积堵塞的高效措施。工程实践中,在舱底增加高压冲刷管路后,每环实际出渣量由210 m3增加到345~350 m3,舱底淤积与堵塞风险显著降低。

     

    Abstract: Large soil-rock agglomerates are easily generated during slurry shield tunnelling through interbedded clay-gravel strata, significantly affecting excavation efficiency and operational safety. To investigate their transport and blockage mechanisms, a solid-liquid two-phase flow coupled model was developed based on the Wuhu Yangtze River Tunnel. Results indicate that agglomerates migrate in the form of bed load transport with distinct velocity stratification. When the agglomerate size increases from 3.0 to 4.5 cm, the bed velocity decreases linearly while local slurry pressure increases by 35.5%. Enhancing slurry density (from 1.05 to 1.35 g/cm3) and flow velocity (from 2.3 to 3.3 m/s) significantly increases the bed velocity by 26.2% and 136.8%, respectively, indicating that increasing slurry velocity is an effective measure for suppressing agglomerate deposition and blockage. Field applications confirmed that installing high-pressure flushing pipes at the chamber bottom effectively improved mucking efficiency, increasing the actual discharge volume from 210 m3 to 345~350 m3 per ring and substantially mitigating deposition and blockage risks.

     

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