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沙漠-黄土南北样带土壤物理性质区域分异特征
引用本文:杨岩岩,刘连友,曹恒武,贾振杰.沙漠-黄土南北样带土壤物理性质区域分异特征[J].中国沙漠,2013,33(1):146-152.
作者姓名:杨岩岩  刘连友  曹恒武  贾振杰
作者单位:北京师范大学 减灾与应急管理研究院, 北京 100875
基金项目:国家自然科学基金项目(41071331)资助
摘    要:采集了沙漠-黄土南北样带从北到南的沙漠区、过渡区、黄土区的土壤样品,测量和分析了不同区域土壤容重(D)、粒度特征。结果表明:①D沙漠区>D过渡区>D黄土区,土壤容重的平均值依次为1.53 g·cm-3、1.51 g·cm-3、1.41 g·cm-3,过渡性明显;②沙漠区以中砂和细砂为主,过渡区以细砂为主,黄土区以细砂和粉砂为主。从沙漠区到黄土区,土壤颗粒逐渐变细,粘粒含量增加,分选性变差,偏度均属正偏,且在增大,峰态从常峰态向窄峰态类型变化,过渡区和黄土区属于双峰态,沙漠区属于单峰态。

关 键 词:沙漠-黄土过渡区    容重    粒度  
收稿时间:2012-06-28;
修稿时间:2012-07-27

Change of Soil Physical Properties from Desert Area to Loess Area in China
YANG Yan-yan,LIU Lian-you,CAO Heng-wu,JIA Zhen-jie.Change of Soil Physical Properties from Desert Area to Loess Area in China[J].Journal of Desert Research,2013,33(1):146-152.
Authors:YANG Yan-yan  LIU Lian-you  CAO Heng-wu  JIA Zhen-jie
Institution:Academy of Disaster Reduction and Emergency Management, Beijing Normal University, Beijing 100875, China
Abstract:Through collecting the soil samples from desert area, desert-loss transitional area, and loss area, which are located in a meridional desert-loess transition zone in north Loess Plateau, we analyzed the soil bulk density and grain-size. The results showed that: (1) Ddesert>Ddesert-loss>Dloss, and the average soil bulk densities were 1.53 g·cm-3, 1.51 g·cm-3, 1.41 g·cm-3 for the three sub-areas, respectively, which had a transitional trend. (2) Medium and fine sand were higher in the desert area, fine sand was higher in the desert-loess transitional zone, while fine and silty sand were higher in the loess area. From the desert area to the loess area, the soil grain size became smaller; the content of clay particle increased; the sorting gets worse; the skewness belonged to a right skewness but having an increasing trend; the kurtosis changed from mesokurtic to leptokurtic. It was single-kurtosis in the desert area, and it is double-kurtosis in the transitional zone and loess zone.
Keywords:desert-loess transitional zone  soil bulk density  grain size
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