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首页|期刊导航|干旱区研究|巴丹吉林沙漠周边沉积物粒度空间分异与粉尘释放源区识别

巴丹吉林沙漠周边沉积物粒度空间分异与粉尘释放源区识别

刘军 左合君 王海兵 张雪 廖承贤

干旱区研究2025,Vol.42Issue(9):1671-1680,10.
干旱区研究2025,Vol.42Issue(9):1671-1680,10.DOI:10.13866/j.azr.2025.09.11

巴丹吉林沙漠周边沉积物粒度空间分异与粉尘释放源区识别

Spatial variations in sediment size serve as a basis for the identification of dust emission source areas around the Badain Jaran Desert

刘军 1左合君 2王海兵 2张雪 3廖承贤3

作者信息

  • 1. 内蒙古农业大学沙漠治理学院,内蒙古呼和浩特 010011||内蒙古风沙物理与防沙治沙工程重点实验室,内蒙古呼和浩特 010011
  • 2. 内蒙古农业大学沙漠治理学院,内蒙古呼和浩特 010011||内蒙古风沙物理与防沙治沙工程重点实验室,内蒙古呼和浩特 010011||内蒙古农业大学,旱区水工程生态环境全国重点实验室,内蒙古呼和浩特 010011
  • 3. 内蒙古农业大学沙漠治理学院,内蒙古呼和浩特 010011
  • 折叠

摘要

Abstract

To elucidate the sediment grain size characteristics and identify potential dust emission sources in the regions of the Badain Jaran Desert,110 surface(0-2 cm)and subsurface(10-20 cm)sediment samples from sev-en typical areas(Wentugaole Gobi,Alatengaobao Gobi,Yabulai Gobi,Alatengchaoke Gobi,Dingxin-Dongfeng Gobi,Gurinai Dry Lake,and Juyanhai Dry Lake)surrounding the desert were collected in August 2023.Sieving and laser particle size analyses were combined to analyze the grain composition.A sediment erosion-deposition model was used to quantify the potential erosion-deposition and emission rates of PM10.The findings are summa-rized as follows.(1)Surface sediments exhibited triple peaking distributions dominated by fine sand(2-3 Φ),fine gravel(-3--1 Φ),and very fine silt(8-9 Φ)due to the superimposition of hydraulic processes and eolian ero-sion.The subsurface layers had quadruple peaking distributions with an additional coarse silt particle peak.The fraction of sand(58.23%-84.60%)in the surface layers significantly exceeded that in the subsurface layers(30.87%-81.20%)as the sand content increased,while the proportions of gravel,silt,and clay declined from the Dingxin-Dongfeng Gobi to the Yabrai Gobi.(2)The surface fine-particle loss in the Dingxin-Dongfeng Gobi and Gurinai Dry lakes was the most pronounced,with the highest values in the potential erosion-deposition rates(7.82%)and emission rates of PM10(4.01%).In contrast,Yabulai Gobi exhibited the lowest values(0.15%and 0.02%for those traits,respectively.(3)The dry lake areas were dominated by fine-grained deposits from the lake,whereas the Gobi regions were influenced by alluvial-proluvial processes that lacked sorting.The Dingxin-Dong-feng Gobi,a high-wind-energy zone,exhibited surface coarsening due to the high intensity of spatially heteroge-neous eolian erosion.In summary,the Dingxin-Dongfeng Gobi and Gurinai Dry lakes were considered the prima-ry potential dust emission sources around the Badain Jaran Desert.Moreover,land conservation in these areas is critical for regional sand control and dust transport between regions.

关键词

粒度特征/粉尘释放潜力/潜在蚀积率/沉积环境/巴丹吉林沙漠

Key words

grain size characteristics/dust emission potential/potential erosion-deposition rate/sedimentary en-vironment/Badain Jaran Desert

引用本文复制引用

刘军,左合君,王海兵,张雪,廖承贤..巴丹吉林沙漠周边沉积物粒度空间分异与粉尘释放源区识别[J].干旱区研究,2025,42(9):1671-1680,10.

基金项目

国家自然科学基金项目(42261002,41861001) (42261002,41861001)

内蒙古农业大学实验教学仪器设备研制与标本制作项目(YZ2024013) (YZ2024013)

干旱区研究

OA北大核心

1001-4675

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