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中国沙漠 ›› 2013, Vol. 33 ›› Issue (1): 146-152.DOI: 10.7522/j.issn.1000-694X.2013.00021

• 生物与土壤 • 上一篇    下一篇

沙漠-黄土南北样带土壤物理性质区域分异特征

杨岩岩, 刘连友, 曹恒武, 贾振杰   

  1. 北京师范大学 减灾与应急管理研究院, 北京 100875
  • 收稿日期:2012-06-28 修回日期:2012-07-27 出版日期:2013-01-20 发布日期:2013-01-20

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   

  1. Academy of Disaster Reduction and Emergency Management, Beijing Normal University, Beijing 100875, China
  • Received:2012-06-28 Revised:2012-07-27 Online:2013-01-20 Published:2013-01-20

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

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.

Key words: desert-loess transitional zone, soil bulk density, grain size

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