兰新铁路猛进东地区风沙运动特征研究

    Characteristics of wind-blown sand motion in Mengjindong area of Lanzhou-Urumqi Railway

    • 摘要: 通过对兰新铁路“百里风区”戈壁风沙流进行现场观测研究,得出“百里风区”的大风天气主要集中在每年的春夏两季,起沙风速远远高于沙漠 地区,约为 9 级风左右。大风携沙量的垂直分布十分明显,集沙量与高度显现 e 的负指数变化,高度越高集沙量越小; 2 m 以下区域是风沙灾害防护的重点区域,其大风携沙量占总携沙量的 80% 左右。集沙颗粒粒径分析则指出:在≤ 3 m 的高度范围内“百里风区”的风沙流运动形式主要以跃移和蠕移为主;当超过垂直高度 3 m 以后,则以悬移为主。

       

      Abstract: Based on the field observation of wind-blown sand mothion in "100-kilometer wind area" along the Lanzhou-Urumqi Railway, the fresh gales mainly concentrate in spring and summer. The speed of sand-raising wind is for larger than that in desert regions, approximately 9-class wind. The sand transport capacity increases with the height of the wind, which has a good agreement with the experimental results. The sand transport capacity is up to almost 80% of the total capacity below 2 meters. The results of sand particle size analysis show that the form of wind-blown sand motion is bound and peristalsis below 3 meters, and it is mostly suspending over 3 meters.

       

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