| 察尔汗盐湖沙漠沙丘沉积物粒度特征分析 |
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| 引用本文： | 鲍锋,董治宝.察尔汗盐湖沙漠沙丘沉积物粒度特征分析[J].水土保持通报,2014(6):355-359. |
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| 作者姓名： | 鲍锋 董治宝 |
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| 作者单位： | 陕西师范大学 旅游与环境学院, 陕西 西安 710062;西安文理学院 文化与旅游学院, 陕西 西安 710065;陕西师范大学 旅游与环境学院, 陕西 西安 710062;中国科学院 寒区旱区环境与工程研究所 沙漠与沙漠化重点实验室, 甘肃 兰州 730000 |
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| 基金项目： | 教育部"长江学者"特聘教授项目(801813);国家重大科学研究计划(2013CB95600);国家自然科学基金项目(41130533;411710107) |
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| 摘 要： | 在对柴达木盆地沙漠地区两次野外实地调查的基础上,选取察尔汗盐湖沙漠盛行风向沿线的线形沙丘和新月形沙丘沉积物样品进行了粒度特征分析。结果表明,研究区沙区沙粒度组成以细沙和中沙占优,粉沙和黏土含量明显,粒度变化遵循沿盛行风向粒径变细的规律;粒度参数特征表现出沉积物平均粒径较国内其他沙漠偏粗,分选较差,呈正偏-近对称形分布,线形沙丘成熟度比新月形沙丘偏高;沉积物累计概率曲线特征指示研究区沙区沙的沉积环境以跃移搬运为主,存在明显的悬移搬运和微弱的滚动搬运。
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| 关 键 词： | 线形沙丘 新月形沙丘 粒度特征 柴达木盆地 |
| 收稿时间： | 2011/10/8 0:00:00 |
| 修稿时间： | 2014/9/30 0:00:00 |
Grain Size Characteristics of Sediments from Typical Sand Dunes in Chaerhan Salt Lake |
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| BAO Feng and DONG Zhi-bao.Grain Size Characteristics of Sediments from Typical Sand Dunes in Chaerhan Salt Lake[J].Bulletin of Soil and Water Conservation,2014(6):355-359. |
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| Authors: | BAO Feng and DONG Zhi-bao |
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| Institution: | College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China;College of Tourism and Culture Science, Xi'an University, Xi'an, Shaanxi 710065, China;College of Tourism and Environment Science, Shaanxi Normal University, Xi'an, Shaanxi 710062, China;Key Laboratory of Desert and Desertification, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou, Gansu 730000, China |
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| Abstract: | Based on the two field studies in Qaidam Basin Desert, sediments of linear dune and barchans dune that are distributed along the prevailing wind in Chaerhan Salt Lake were collected as samples. Then, the grain size of the selected samples was analyzed. The results showed that fine and medium sand was dominant in the sand, sandy clay and fine silt was also detected in a large quantity. The grain size changed from coarse to fine along the prevailing wind. Moreover, the grain size parameters implied that the mean diameter of the samples was higher than those collected from the other deserts in China, which indicated a higher maturity values of linear dune over those of barchans dune. Finally, the cumulative frequency curve demonstrated that the sandy area under research was primarily deposited by saltation and suspension population. |
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| Keywords: | linear dune barchan dune grain size characteristics Qaidam Basin |
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