中国东部沙区表层沉积物粒度特征

沈亚萍; 张春来; 李庆; 贾文茹; 李姣; 田金鹭

doi:10.7522/j.issn.1000-694X.2015.00278

中国沙漠 >

2016 , Vol. 36 >Issue 1: 150 - 157

DOI: https://doi.org/10.7522/j.issn.1000-694X.2015.00278

沙漠与沙漠化

中国东部沙区表层沉积物粒度特征

沈亚萍 ,
张春来 ,
李庆 ,
贾文茹 ,
李姣 ,
田金鹭

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北京师范大学地表过程与资源生态国家重点实验室/防沙治沙教育部工程研究中心, 北京 100875

沈亚萍(1990-),女,四川省彭州人,硕士研究生,风沙地貌研究方向。E-mail:603462941@qq.com

收稿日期: 2015-11-23

修回日期: 2015-12-11

网络出版日期: 2016-01-20

基金资助

国家自然科学基金项目(41330746);中央高校基本科研业务费专项(2012LZD13)

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Grain-size Characteristics of Surface Sediments in the Eastern Desert Regions of China

Shen Yaping ,
Zhang Chunlai ,
Li Qing ,
Jia Wenru ,
Li Jiao ,
Tian Jinlu

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State Key Laboratory of Earth Surface Processes and Resource Ecology/MOE Engineering Research Center of Desertification and Blown-sand Control, Beijing Normal University, Beijing 100875, China

Received date: 2015-11-23

Revised date: 2015-12-11

Online published: 2016-01-20

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摘要

通过分析中国东部沙区表层沉积物粒度特征及其与风力、植被覆盖的相关性,探讨了东部沙区现代风沙沉积环境及其区域差异性。结果显示:东部沙区各沙漠/沙地粒径级配相对一致,均以细沙、中沙为主,粒度分布整体呈单峰形态,中等分选,粒度分布和分选性均与西部沙区有较大不同。风力和植被覆盖状况的差异决定了各沙地所处的风沙环境性质和风沙活动强度不同,导致东部沙区表层沉积物粒度特征存在明显的区域差异性。其中,库布齐沙漠粒度特征与该区风蚀、搬运、堆积过程频繁交替的风沙活动方式密切关联;呼伦贝尔沙地粒度特征反映了风蚀主导的风沙环境;科尔沁沙地、浑善达克沙地,毛乌素沙地粒度特征和风沙活动方式相对复杂,与这3个沙地内部风蚀主导区和沙尘沉降主导区镶嵌分布的格局有关。东部沙区表层沉积物平均粒径和分选系数均与沙地年均风速和植被总盖度双因素之间具有显著的非线性相关性。

关键词： 东部沙区; 粒度; 风沙环境; 区域差异

本文引用格式

沈亚萍 , 张春来 , 李庆 , 贾文茹 , 李姣 , 田金鹭 . 中国东部沙区表层沉积物粒度特征[J]. 中国沙漠, 2016 , 36(1) : 150 -157 . DOI: 10.7522/j.issn.1000-694X.2015.00278

Abstract

By analyzing grain-size characteristics of surface sediments as related to wind force and vegetation cover in the eastern sand area of China, this paper discussed the modern aeolian sedimentary environment and the regional differences. The results show that with a unimodal distribution pattern the grain-size of the surface sediments of each desert and sandy land in the eastern desert regions is similar. All of the surface sediments are mainly composed of fine sand and medium sand and moderately sorted. Both grain-size composition and sorting differ from those of the western deserts. Controlled by the properties of the aeolian environment and the intensity of aeolian activities that were determined mainly by wind force and vegetation cover, grain-size characteristics of the surface sediments exhibit regional difference in the eastern desert regions. Specifically, grain-size in the Hobq Desert implies a typical desert environment that is characterized by frequent alternating processes of wind erosion, particle transportation and deposition; In the Hulunbeir Sandy Land, it is characterized by a wind erosion dominated aeolian environment; In the Otindag Sandy Land, Horqin Sandy Land and Mu Us Sandy Land, grain-size and aeolian activities are relatively complex, which is related to the mosaic distribution pattern of wind erosion dominated areas and aeolian deposition dominated areas. Statistics shows that both the mean grain-size and the sorting of the surface sediments significantly correlated to the annual average wind speed and the total vegetation coverage in the eastern desert regions.

Key words： eastern desert regions; grian-size; aeolian environment; regional difference

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