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李凯崇, 蒋富强, 薛春晓, 刘贺业, 葛盛昌. 兰新铁路猛进东地区风沙运动特征研究[J]. 岩土工程学报, 2011, 33(zk1): 223-226.
引用本文: 李凯崇, 蒋富强, 薛春晓, 刘贺业, 葛盛昌. 兰新铁路猛进东地区风沙运动特征研究[J]. 岩土工程学报, 2011, 33(zk1): 223-226.
LI Kai-chong, JIANG Fu-qiang, XUE Chun-xiao, LIU He-ye, GE Sheng-chang. Characteristics of wind-blown sand motion in Mengjindong area of Lanzhou-Urumqi Railway[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(zk1): 223-226.
Citation: LI Kai-chong, JIANG Fu-qiang, XUE Chun-xiao, LIU He-ye, GE Sheng-chang. Characteristics of wind-blown sand motion in Mengjindong area of Lanzhou-Urumqi Railway[J]. Chinese Journal of Geotechnical Engineering, 2011, 33(zk1): 223-226.

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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