四川农业大学学报 ›› 2003, Vol. 21 ›› Issue (04): 322-327.doi: 10.16036/j.issn.1000-2650.2003.04.012

• 研究论文 • 上一篇    下一篇

西藏酸性土壤的分布和酸度特征

张宗锦, 刘世全, 张世熔, 邓良基, 蒲玉琳, 范宇   

  1. 四川农业大学 资源环境学院, 四川 雅安 625014
  • 收稿日期:2003-08-29 出版日期:2003-12-31 发布日期:2017-03-07
  • 基金资助:
    国家"863"计划项目资助(990140046)。

Distribution and Acidity Character of Acid Soil in Tibet

ZHANG Zong-jin, LIU Shi-quan, ZHANG Shi-rong, DENG Liang-ji, PU Yu-lin, FAN Yu   

  1. College of Resource and Environment, Sichuan Agricultural University, Yaan 625014, Sichuan, China
  • Received:2003-08-29 Online:2003-12-31 Published:2017-03-07

摘要: 根据西藏9个土类70个土壤剖面258层土样的分析资料,应用统计方法,探讨其酸性土的分布和酸度特征。西藏酸性土面积约占1/5,主要分布于藏东南地区。土壤pH主要决定于土壤潜性酸中的交换性酸,特别是其中占绝对优势的交换性Al3+,而受非交换性酸的影响较小。非交换性酸主要来源于腐殖质酸性功能团结合H、Al的解离。土壤pH与盐基饱和度呈非线性正相关,且主要受占优势的交换性Ca2+制约。

关键词: 西藏, 酸性土pH, 交换性酸, 非交换性酸, 交换性盐基

Abstract: There are 9 soils types which include 70 soils profiles and 258 layers in Tibet. Based on the analytic data of the nine soils types, the distribution and acidity characters of acid soils are discussed by analytic method. The 1/5 soils area is acid soils in Tibet. The soil is mainly distributed in the southeast of Tibet. The soil pH is mainly determined by the Exchangeable Acid in Potential Acid, especially, exchangeable Al3+. However, nonexchangeable Acid is less impact. The dispel of acid functional group, which combines H and Al, is the main source of nonexchangeable Acid. The soil pH is also significant positive correlation with Base Saturation, which is mainly restricted by Exchangeable Base Ca2+.

Key words: Tibet, acid soil, exchangeable acid, nonexchangeable acidity, exchangeable base

中图分类号: 

  • S153.1