增水对青藏高原高寒草甸生态系统表层土壤碳氮的影响
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  • 英文篇名:The Effect of Precipitation Increase on Topsoil Carbon and Nitrogen in an Alpine Meadow Ecosystem on the Tibetan Plateau
  • 作者:李凤滋 ; 旭日
  • 英文作者:LI Fengzi;XU Ri;Key Laboratory of Alpine Ecology,Institute of Tibetan Plateau Research,Chinese Academy of Sciences;The School of Ecology and Environment,Inner Mongolia University;
  • 关键词:增水 ; 土壤碳 ; 土壤氮 ; 高寒草甸生态系统 ; 青藏高原
  • 英文关键词:precipitation increase;;soil carbon;;soil nitrogen;;alpine meadow;;Tibetan Plateau
  • 中文刊名:LYZY
  • 英文刊名:Forest Resources Management
  • 机构:中国科学院青藏高原研究所高寒生态重点实验室;内蒙古大学生态与环境学院;
  • 出版日期:2019-01-28 18:30
  • 出版单位:林业资源管理
  • 年:2018
  • 基金:中国科学院战略性先导科技专项(XDA20050102,XDA2005010202);; 国家自然科学基金(41175128; 41575152;41775161)
  • 语种:中文;
  • 页:LYZY201806016
  • 页数:7
  • CN:06
  • ISSN:11-2108/S
  • 分类号:101-107
摘要
通过人为多梯度增加降水的控制实验,观察高寒草甸生态系统中表层(-10cm)土壤碳(Total Carbon,TC)氮(Total Nitrogen,TN)对降水增加的响应。结果显示:3年5个梯度的增水处理未引起表层土壤碳氮产生显著的变化,但2014年和2015年在增水40%和增水80%处理下,土壤总碳、土壤总氮有一定增加(P>0. 05);表层土壤铵态氮总体有增加的趋势(P> 0. 05),硝态氮总体有减少的趋势(P> 0. 05)。表明短期的增水处理不会引起表层土壤碳氮发生显著变化。
        By control experiments of artificially increasing precipitation,we observe the response of topsoil(-10 cm) total carbon(TC) and total nitrogen(TN) to precipitation increasing in the alpine meadow ecosystem. The results showed that the experiment with three years of five gradient precipitation increase treatments had no significant effect on surface TC/TN,but TN and TC has increase with the precipitation increase treatment of 40% and 80% in 2014 and 2015(P > 0. 05). There was an overall increase in NH+4-N in the topsoil(P > 0. 05) while NO-3-N was decreased(P > 0. 05). The results showed that short term precipitation increase did not cause the significant change of TC/TN.
引文
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