干旱区生态环境知识资源中心(Arid): 生物土壤结皮对库布齐沙漠北缘土壤粒度特征的影响

Arid

	生物土壤结皮对库布齐沙漠北缘土壤粒度特征的影响
其他题名	Effect of Biological Soil Crusts on Features of Grain Size in the Northern Margin of Hobq Desert
	肖巍强; 董治宝; 陈颢; 邵天杰; 崔徐甲; 李超; 宋绍鹏; 肖南; 李露露
来源期刊	中国沙漠
ISSN	1000-694X
出版年	2017
卷号	37 期号:5 页码:970-977
中文摘要	对库布齐沙漠北缘不同发育阶段的生物土壤结皮及其下层土壤粒度特征进行分析。结果表明:流动沙地和藻类结皮表层均以细砂和中砂成分为主,藓类结皮表层以细砂和极细砂为主。生物土壤结皮表层的中粉砂至黏土、粗粉砂和极细砂含量均高于其下层土壤。两种结皮样地均属于分选性较差等级,但结皮下层土壤分选性中等, 3类曲线均不对称,属于正偏-极正偏等级,藓类结皮和藻类结皮表层的峰形均属于中等尖锐水平,而流动沙地的曲线尖窄。生物土壤结皮的成土作用随着结皮的发育阶段和土层深度的增加而表现出差异性和复杂性。
英文摘要	Grain size features of biological soil crusts and its subsoil in the northern margin of Hobq Desert at different developmental stages are studied by the method of particle-size analysis in this article.The fine sand and medium sand dominate the drifting sand and algal crust surface,and the fine sand and very fine sand prevail on the surface of moss crusts.The content of clay,medium silt,coarse silt and very fine sand on the crust surface are much more than that of same samples under the crust.The moss and algal crusts are very poor in sorting feature,however,soil under the crust is medium.Moreover,curves of drifting sand,moss crust and algal crust are all asymmetric in positive skewed distribution.The peaky curves of moss crust and algal crust are moderate,but that of drifting sand is very sharp.Therefore,soil formation effect of biological crust displays the difference and complexity at the different developmental stages and depth of the soil.
中文关键词	粒度特征 ; 生物土壤结皮 ; 库布齐沙漠
英文关键词	grain size biological soil crusts Hobq Desert
语种	中文
国家	中国
收录类别	CSCD
WOS类目	AGRICULTURE MULTIDISCIPLINARY
WOS研究方向	Agriculture
CSCD记录号	CSCD:6093705
来源机构	陕西师范大学
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/237143
作者单位	陕西师范大学地理科学与旅游学院, 西安, 陕西 710062, 中国
推荐引用方式 GB/T 7714	肖巍强,董治宝,陈颢,等. 生物土壤结皮对库布齐沙漠北缘土壤粒度特征的影响[J]. 陕西师范大学,2017,37(5):970-977.
APA	肖巍强.,董治宝.,陈颢.,邵天杰.,崔徐甲.,...&李露露.(2017).生物土壤结皮对库布齐沙漠北缘土壤粒度特征的影响.中国沙漠,37(5),970-977.
MLA	肖巍强,et al."生物土壤结皮对库布齐沙漠北缘土壤粒度特征的影响".中国沙漠 37.5(2017):970-977.