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中国沙漠 ›› 2022, Vol. 42 ›› Issue (4): 81-88.DOI: 10.7522/j.issn.1000-694X.2021.00224

• • 上一篇    下一篇

干涸尾闾湖盆区泥漠地表磨蚀释尘特征

曲书锋1,3,4,5(), 张国明2,6(), 刘连友1,3,4,5, 李力7, 肖雨婷1,3,4,5, 向明珠1,3,4,5, 孙煦然1,3,4,5, 韩旭娇1,5   

  1. 1.北京师范大学,环境演变与自然灾害教育部重点实验室,北京 100875
    2.北京师范大学,应急管理部教育部减灾与应急管理研究院,北京 100875
    3.北京师范大学,防沙治沙教育部工程研究中心,北京 100875
    4.北京师范大学,地理科学学部,北京 100875
    5.北京师范大学,国家安全与应急管理学院,北京 100875
    6.中国科学院西北生态环境资源研究院 中国科学院沙漠与沙漠化重点实验室,甘肃 兰州 730000
    7.长江水利委员会长江科学院,湖北 武汉 430010
  • 收稿日期:2021-11-11 修回日期:2021-12-22 出版日期:2022-07-20 发布日期:2022-08-29
  • 通讯作者: 张国明
  • 作者简介:张国明(E-mail: zgm@bnu.edu.cn
    曲书锋(1998—),男,山东烟台人,硕士研究生,研究方向为干旱区风蚀过程与地表粉尘排放。E-mail: 202121051171@mail.bnu.edu.cn
  • 基金资助:
    国家自然科学基金面上项目(41971120);中国科学院沙漠与沙漠化重点实验室开放课题(KLDD-2020-002);国家自然科学基金重点项目(41730639)

The surface abrasion and dust emission of mud desert in dry rump lake basin

Shufeng Qu1,3,4,5(), Guoming Zhang2,6(), Lianyou Liu1,3,4,5, Li Li7, Yuting Xiao1,3,4,5, Mingzhu Xiang1,3,4,5, Xuran Sun1,3,4,5, Xujiao Han1,5   

  1. 1.MOE Key Laboratory of Environmental Change and Natural Disaster /, Beijing Normal University,Beijing 100875,China
    2.Academy of Disaster Reduction and Emergency Management /, Beijing Normal University,Beijing 100875,China
    3.Engineering Research Center of Desertification and Blown-sand Control /, Beijing Normal University,Beijing 100875,China
    4.Faculty of Geographical Science /, Beijing Normal University,Beijing 100875,China
    5.College of National Safety and Emergency Management, Beijing Normal University,Beijing 100875,China
    6.Key Laboratory of Desert and Desertification,Northwest Institute of Eco-Environment and Resources,Chinese Academy of Sciences,Lanzhou 730000,China
    7.Changjiang River Scientific Research Institute of Changjiang Water Resources Commission,Wuhan 430010,China
  • Received:2021-11-11 Revised:2021-12-22 Online:2022-07-20 Published:2022-08-29
  • Contact: Guoming Zhang

摘要:

沙粒的表面磨蚀效应是地表产尘、释尘的重要机制,针对干湖盆泥漠地表开展磨蚀释尘实验研究,对理解干湖盆地表风蚀过程及盐碱尘暴形成机理具有重要意义。对采自西居延海干涸湖盆泥漠地表土样进行室内磨蚀模拟实验,研究了不同粒级(细、中、粗)沙粒不同落沙角度(30°,45°,60°)的磨蚀效应。结果表明:(1)泥漠地表磨蚀实验中能够产生明显释尘效应的沙粒粒级阈值为中沙(0.25 mm<Md<0.50 mm);(2)磨蚀粒径粒级相同时,磨蚀角度会对泥漠地表磨蚀释尘速率产生影响,磨蚀量的角度排序为60°>30°>45°,但同一粒级3种角度下的磨蚀释尘率差异不显著。(3)磨蚀角度为45°时,计算了泥漠地表的质量磨蚀率与能量磨蚀率,其中中沙为0.04 g·kg-1、0.43 g·J-1,粗沙为0.08 g·kg-1、0.74 g·J-1,极粗沙为0.26 g·kg-1、2.54 g·J-1;在磨蚀沙粒粒级倍增而磨蚀角度不变情况下,泥漠地表磨蚀释尘率与能量磨蚀率未发生正比例线性增长变化。

关键词: 干涸尾闾湖盆, 沙粒粒级, 泥漠地表, 磨蚀释尘

Abstract:

The bombardment effect of saltating sand particles on the erodible surface is an important mechanism of dust release. It is of great significance to study the aeolian abrasion process and dust release mechanism on the surface of dry lake bed to mitigate the hazards of saline-alkali dust storm. In this paper, samples from mud desert surface of dry lakebed in the West Juyan Lake were collected to conduct laboratory abrasion experiments to study the abrasion effect of sand grains at different impacting angles(30°, 45°, 60°). The results show that: (1) The threshold sand size of erosion and dust release on mud desert surface is medium (0.25 mm<Md<0.50 mm). (2) When the abrasive particle size is the same, the impacting angle exerts effects on the dust release rate of mud desert surface, and the ranking order from higher dust release rate is 60°>30°>45°, but the difference of the dust release rate is not significant under such conditions. (3) When the impacting angle is 45°, the mass erosion rate and energy erosion rate of medium sand, coarse sand and extremely coarse sand on mud desert surface are 0.04 g·kg-1 and 0.43 g·J-1, 0.08 g·kg-1 and 0.74 g·J-1, 0.26 g·kg-1 and 2.54 g·J-1, respectively. When the grain size of sand abrader double increases while remaining the impacting angle, there is no proportional linear change in growth between the dust release rate and energy abrasion rate.

Key words: dry rump lake basin, sand particle size, mud desert surface, dust emission by abrasion

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