img

官方微信

高级检索

中国沙漠 ›› 1989, Vol. 9 ›› Issue (1): 75-84.

• 论文 • 上一篇    下一篇

我国亚热带湿润地区风沙化土地的水分状况及化学性质——以江西省新建县厚田地区为例

张继贤   

  1. 中国科学院兰州沙漠研究所
  • 出版日期:1989-03-20 发布日期:1989-03-20

Moisture Conditions and Chemical Properties of Blownsand Land in Subtropic Humid Zone of China -Take Houtian Region, Xinjian County, Jiangxi Province as an Example

Zhang Jixian   

  1. Institute of Desert Research, Academia Sinica, Lanzhou
  • Online:1989-03-20 Published:1989-03-20

摘要: 厚田拙区的风沙化土地以风成沙丘、沙质风蚀坑、波状片状沙地、蔓荆子沙堆及河流沙质沉积阶地交错分布。河流沙质沉积阶地含量大于76.40%, 表层高达87.78%, 为该区土地风沙化提供了丰富的沙物质来源, 属潜在的风沙化土地。在河流沙质沉积阶地上形成的风成沙丘、波状片状沙地为严重的风沙化土地。文中以河流沙质沉积阶地及风成沙丘进行了水分状况及化学性质的对比分析, 以示由潜在的类型发展为严重风沙化的风成沙丘时, 水分条件, 养分、微量元素及矿物全量的分异情况。

Abstract: Blownsand land in Houtian region consists of sand dunes, sandy blownouts, undulated sand sheet, vegetated sand mound and sandy river terraces. As a rule, sandy river terraces contain more than 76.4% of sand, with the top layer reaching up to 87.78%, therefore, they can not only provide abundant sand sources but also serve as a potential blownsand land. In this paper the moisture conditions and chemical properties, of sandy river terraces were analysed, this greatly contributes to a better understanding of the differentiation of water, nutrients and trace elements when the potential sandy land turned into serious blowusand land.