植物生态学报 ›› 2006, Vol. 30 ›› Issue (3): 441-449.DOI: 10.17521/cjpe.2006.0059

所属专题: 青藏高原植物生态学:植物-土壤-微生物

• 研究论文 • 上一篇    下一篇

三江源地区主要草地类型土壤碳氮沿海拔变化特征及其影响因素

王长庭1,2, 龙瑞军1,3,*(), 曹广民1, 王启兰1, 丁路明1, 施建军4   

  1. 1中国科学院西北高原生物研究所,西宁 810008
    2中国科学院研究生院,北京 100039
    3甘肃农业大学草业学院,兰州 730070
    4青海省畜牧兽医科学院草原所,西宁 810003
  • 接受日期:2005-12-06 发布日期:2006-05-30
  • 通讯作者: 龙瑞军
  • 作者简介:*E-mail: longuijun@sina.com
  • 基金资助:
    中国科学院”百人计划”项目;国家自然科学基金项目(30371021);国家自然科学基金项目(40471133);中国科学院野外台站基金项目

SOIL CARBON AND NITROGEN CONTENTS ALONG ELEVATION GRADIENTS IN THE SOURCE REGION OF YANGTZE, YELLOW AND LANTSANG RIVERS

WANG Chang-Ting1,2, LONG Run-Jun1,3,*(), CAO Guang-Min1, WANG Qi-Lan1, DING Lu-Ming1, SHI Jian-Jun4   

  1. 1Northwest Plateau Institute of Biology, Chinese Academy of Sciences, Xining 810008, China
    2Graduate School of Chinese Academy of Sciences, Beijing 100039, China
    3Grassland Science College of Gansu Agriculture University, Lanzhou 730070, China
    4Grassland institute, Qinghai Academy of Animal and Veterinary Science, Xining 810003, China
  • Accepted:2005-12-06 Published:2006-05-30
  • Contact: LONG Run-Jun

摘要:

以三江源地区主要草地类型为研究对象,分析了不同草地类型土壤有机碳和全氮的变化特征及其与环境因子、土壤特征等的相互关系。结果表明:沿着海拔的逐渐升高,土壤有机碳和全氮含量均呈现出 “V"字形变化规律,即土壤有机碳氮含量在海拔最高处(5 120 m)和最低处(4 176 m)比较高,而在中间海拔梯度较低,土壤有机碳与全氮含量极显著相关( r=0.905)且高寒草甸土壤碳、氮含量高于高山草原土壤碳、氮含量;土壤中有机碳含量和全氮含量均随着土壤含水量的增加而增加,偏相关分析结果表明:对0~30 cm土层中土壤有机碳和土壤全氮影响最大的是土壤含水量,偏相关系数为0.946 5、0.905 9(p<0.01);土壤有机碳含量和全氮含量与植被盖度和草地生产力存在正相关趋势;土壤有机碳含量和全氮含量与土壤pH值和全盐量存在负相关趋势。

关键词: 三江源地区, 土壤有机碳, 土壤全氮, 草地, 影响因素

Abstract:

Soil is an important component of the terrestrial ecosystem and plays a critical role in global carbon cycle. Better understanding the distribution pattern of soil carbon storage along environmental gradients will facilitate the projection of global change on terrestrial C cycling. This study was conducted to examine soil organic carbon and nitrogen contents in major grassland types along elevation gradients in the source region of Yangtze, Yellow and Lantsang Rivers. Soil organic carbon and nitrogen contents were greater at the highest (5 120 m a.s.l.) and lowest (4 176 m a.s.l.) sites and lower at middle site. Soil organic carbon and nitrogen contents increased with soil moisture along the altitudinal gradient. Partial correlation analysis showed that spatial variability of soil organic carbon and nitrogen contents at 0-30 cm soil layers could be primarily explain by soil moisture with partial correlation coefficients of 0.946 5、0.905 9 (p<0.01), respectively. In addition, soil organic carbon and nitrogen contents showed positive linear correlations with plant cover and productivity and negative correlation trend with soil pH and total salt content.

Key words: The source region of Yangtze, Yellow and Lantsang Rivers, Soil organic carbon, Soil total nitrogen, Grassland, Impact factors