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新疆喀拉库姆沙漠新月形沙丘不同部位粒度特征
其他题名Grain Size Characteristics of Different Parts of the Crescent Dunes in Karakum Desert,Xinjiang,China
俞胜清1; 阿布都米基提2; 周向玲1; 黄晓俊1
来源期刊中国沙漠
ISSN1000-694X
出版年2013
卷号33期号:6页码:1629-1635
中文摘要对新疆叶尔羌河流域绿洲边缘喀拉库姆沙漠高度在3~12m的新月形沙丘进行了粒度分析。结果表明:表层和下层沉积物均以细砂和极细砂为主,二者含量达82%以上。表层沉积物较下层稍粗,平均粒径分别为2.09Phi和2.16Phi。下层沉积物较表层分选性好,sigma均值分别为0.48和0.62。表层和下层沉积物偏度均为正偏,SK 均值分别为0.21和0.24。峰态均为尖窄,K_g均值分别为1.18和1.11。表层和下层沉积物平均粒径均表现为丘顶最粗,背风坡坡脚最细,由两侧坡脚至丘顶平均粒径变粗,平均粒径与其他粒度特征参数之间均存在良好的相关性。分析表明,喀拉库姆沙漠沙丘沉积物粒度特征除受物源这一背景制约外,还与区域构造、沙漠地貌、植被、气候和较为复杂的风沙动力学过程等众多因素有关。
英文摘要The analysis on the sand particle grain size from different parts of selected crescent dunes in Karakum Desert of Xinjiang, China shows that the surface layer and the underlying sediments layer are both mainly the fine sand and extreme fine sand with content more than 82%. The average grain size of the underlying layer sediments is 2.16Phi and the surface sediments is 2.09Phi. The underlying layer sediments has a better sorting characteristics than the surface layer sediments, the standard variation values of those two layers are 0.48 and 0.62 respectively. Both the surface layer and the underlying layer sediments skewness are positive, SK values are 0.21 and 0.24 respectively. Kurtosis are both narrow and pointed, K_gvalues are 1.18 and 1.11 respectively. The average sand particle grain size of the dune crest is the coarsest, and sand from the dunes root of leeward slope is the finest. The sand particle grain size of crescent dunes gradually become coarser from dune root to dune crest. And the average sand particle grain size is also well related to other particle size parameters. The sand particle grain size characteristics of crescent dunes in Karakum Desert is not only restricted by provenance background, but also constrained by regional tectonic, desert landforms, vegetation, climate, complex aeolian sand dynamic process and many other factors.
中文关键词喀拉库姆沙漠 ; 新月形沙丘 ; 粒度
英文关键词Karakum Desert crescent dune grain size
语种中文
国家中国
收录类别CSCD
WOS类目GEOSCIENCES MULTIDISCIPLINARY
WOS研究方向Geology
CSCD记录号CSCD:4995003
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/230668
作者单位1.喀什师范学院物理系, 喀什, 新疆 844006, 中国;
2.喀什地区林业勘察设计队, 喀什, 新疆 844000, 中国
推荐引用方式
GB/T 7714
俞胜清,阿布都米基提,周向玲,等. 新疆喀拉库姆沙漠新月形沙丘不同部位粒度特征[J],2013,33(6):1629-1635.
APA 俞胜清,阿布都米基提,周向玲,&黄晓俊.(2013).新疆喀拉库姆沙漠新月形沙丘不同部位粒度特征.中国沙漠,33(6),1629-1635.
MLA 俞胜清,et al."新疆喀拉库姆沙漠新月形沙丘不同部位粒度特征".中国沙漠 33.6(2013):1629-1635.
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