干旱区研究 ›› 2021, Vol. 38 ›› Issue (3): 875-881.doi: 10.13866/j.azr.2021.03.29

• 其他 • 上一篇    下一篇

3种低立式沙障内表层沉积物粒度特征研究

祁帅1(),汪季1,2(),党晓宏1,2,魏亚娟1,丁奋谦1   

  1. 1.内蒙古农业大学沙漠治理学院,中央与地方共建风沙物理重点实验室,内蒙古 呼和浩特010018
    2.内蒙古杭锦荒漠生态系统国家定位观测研究站,内蒙古 鄂尔多斯017400
  • 收稿日期:2020-07-03 修回日期:2020-11-06 出版日期:2021-05-15 发布日期:2021-06-17
  • 通讯作者: 汪季
  • 作者简介:祁帅(1995-),男,硕士研究生,主要从事水土保持与荒漠化防治研究. E-mail: 1182843101@qq.com
  • 基金资助:
    国家重点研发专项(2018YFC0507101)

Grain size characteristics of surface sediments in three low vertical sand barriers

QI Shuai1(),WANG Ji1,2(),DANG Xiaohong1,2,WEI Yajuan1,DING Fenqian1   

  1. 1. College of Desert Management, Inner Mongolia Agricultural University, Central and Local Key Laboratory of Wind and Sand Physics, Hohhot 010018, Inner Mongolia, China
    2. Inner Mongolia Hangjin Desert Ecosystem Observation and Research Station, Ordos 017400, Inner Mongolia, China
  • Received:2020-07-03 Revised:2020-11-06 Online:2021-05-15 Published:2021-06-17
  • Contact: Ji WANG

摘要:

以库布齐沙漠兴巴高速南铺设3 a的3种(PLA沙障、沙柳沙障、HDPE沙障)同种规格不同材料沙障为研究对象,通过采集沙障内表层0~2 cm沉积物样品,利用激光粒度仪测定样品机械组成,分析了平均粒径、标准偏差、偏度、峰态和分形维数等参数。结果表明:(1) 以中、细砂为主,其含量约为77.83%~98.00%,黏粒和粉粒的含量均不超过5%;沙丘迎风坡坡底PLA和HDPE沙障内表现为轻度风蚀,颗粒粒径偏粗;沙柳沙障自坡底到坡顶,障格内粒径逐渐增大,在坡顶处发生蚀积转换。(2) 整体上沙障内沉积物分选性较差,偏度向正偏或负偏发展,峰态向尖窄发展,分形维数在1.94~2.20,优势粒级向细砂转变。(3) 不同类型沙障对沉积物的影响具有一定差异性,HDPE沙障和PLA沙障内沉积颗粒分布更为广泛,而沙柳沙障则相对集中,且都趋于细化;对土壤颗粒组成优化表现为HDPE沙障>沙柳沙障>PLA沙障。

关键词: 低立式沙障, 迎风坡, 粒度特征, 分形维数, 库布齐沙漠

Abstract:

This research examines the inner surface (0-2 cm) of three types of sand barriers (PLA, Salix, HDPE) of the same specifications that have been laid for three years in the south of Xingba Expressway in the Kubuqi Desert. The mechanical composition of the samples was measured using a laser particle size analyzer, and parameters, such as average particle size, standard deviation, skewness, kurtosis, and fractal dimension, were analyzed. The study area was dominated by medium and fine sand (77.83%-98.00%), and the content of clay and powder particles did not exceed 5%. The PLA and HDPE sand barriers at the bottom of the windward slope of the dunes were manifested by mild wind erosion, and the particle size was relatively coarse. However, from the bottom to the top of the slope, the size of the sand willow sand barrier gradually increased, and there was a change from sedimentation to wind erosion at the top of the slope. Overall, the sediments in the sand barrier were poorly sorted, the skewness developed toward positive or negative deviation, kurtosis developed toward sharpness, the fractal dimension was 1.94-2.20, and the dominant grain size changed to fine sand. The impact of different types of sand barriers on sediments was different. The distribution of sediment particles in the HDPE and PLA sand barriers was more extensive, while the sand willow sand barrier was relatively concentrated and refined. The optimization of particle composition was HDPE> Salix> PLA sand barrier.

Key words: low vertical sand barrier, windward slope, granularity characteristics, fractal dimension, Kubuqi Desert