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    格库铁路桥路过渡段风沙流场数值模拟

    Numerical simulation on wind-sand flow field at the bridge and roadbed transition section of Golmud-Korla Railway in northwestern China

    • 摘要:
        目的  为了探究桥梁与路基(桥路)过渡段和路基附近流场、水平风速和积沙特征的分布规律,揭示桥路过渡段沙害形成机理。
        方法  通过数值模拟的技术手段对不同来流风速下桥路过渡段和路基附近的流场变化和积沙特征进行研究,并将数值模拟的积沙分布情况与现场实际积沙情况对比,验证数值模拟结果的准确性。
        结果  当风沙流运动到桥路过渡段时,受到桥路过渡段的阻碍,产生速度分区,分别形成气流减速区、集流加速区、高速区、涡流回旋区和气流恢复区,且桥路过渡段背风侧减速区面积明显大于路基背风侧;桥路过渡段近地表处,气流速度先降低(负值)后升高再降低(负值),最后逐渐恢复至来流风速。距地表4.2 m高度处,速度变化基本呈V型分布,距地表4.4 m高度处,速度变化基本呈双V型分布。根据数值模拟结果,桥路过渡段迎风侧和背风侧积沙均较多,而桥下净空是良好的过沙断面,绝大部分沙粒被输送至桥梁背风侧,不会在梁底大量沉积;路基积沙主要发生在迎风侧,背风侧很少。
        结论  随着时间的推移,桥路过渡段附近积沙会慢慢向周边蔓延,一部分沉积在梁底,造成梁底积沙,另一部分跃过路基,进入道床。因此,桥路过渡段沙害防治不可忽视,必须定期清理积沙,防止沙粒进入道床和钢轨,危害行车安全。

       

      Abstract:
        Objective  This paper aims to explore the distribution law of the flow field, horizontal wind speed and sand accumulation characteristics in the transition section between the bridge and the roadbed (bridge-road) and near the roadbed, and reveal the formation mechanism of sand damage in the bridge-road transition section.
        Method  By means of numerical simulation, the flow field changes and the characteristics of sand accumulation in the bridge-road transition section and near the roadbed under different incoming wind speeds were studied. And use the numerical simulation of the sand distribution to compare with the actual on-site sand accumulation to verify the accuracy of the numerical simulation results.
        Result  When the wind-sand flow moved to the bridge-road transition section, it was hindered by the bridge-road transition section, resulting in speed divisions. Air flow deceleration zone, current collection acceleration zone, high speed zone, vortex cyclone zone and air flow recovery zone were formed, respectively, and the area of the deceleration zone on the leeward side of the bridge-road transition sectionwas significantly larger than that on the leeward side of the subgrade. Near the surface of the bridge-road transition section, the airflow velocity first decreased (negative value), then increased and then decreased (negative value), and finally returned to the incoming wind speed gradually. At a height of 4.2 m from the ground, the velocity change basically showed a V-shaped distribution, and at a height of 4.4 m from the ground, the velocity change basically showed a double-V-shaped distribution. According to the numerical simulation results, therewas more sand on the windward and leeward sides of the bridge-to-road transition section, and the clearance under the bridge was a good sand-crossing section. Most of the sand particles were transported to the leeward side of the bridge and will not deposit a lot on the bottom of the beam. Sand accumulation on the roadbed mainly occurred on the windward side and rarely on the leeward side.
        Conclusion  As time goes by, the sand near the transition section of the bridge and road will slowly spread to the surrounding area. One part is deposited at the bottom of the beam, causing sand at the bottom of the beam, and the other part jumps over the subgrade and enters the track bed. Therefore, the prevention and control of sand hazards in the transitional section of bridges and roads cannot be ignored. The accumulated sand must be cleaned regularly to prevent sand particles from entering the track bed and steel rails and endangering driving safety.

       

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