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芦苇湿地土壤有机碳和全氮含量的垂直分布特征

吕国红1;周莉2;赵先丽1;贾庆宇1;谢艳兵1;周广胜1,2   

  1. 1中国气象局沈阳大气环境研究所,沈阳110016;2中国科学院植物研究所植被数量生态学重点实验室,北京 100093
  • 收稿日期:2005-04-21 修回日期:2005-11-10 出版日期:2006-03-18 发布日期:2006-03-18

Vertical distribution of soil organic carbon and total nitrogen in reed wetland

LU Guohong1;ZHOU Li2;ZHAO Xianli1;JIA Qingyu1;XIE Yanbing1;ZHOU Guangsheng1,2   

  1. 1Institute of Atmospheric Environment,China Meteorological Administration,Shenyang 110016,China; 2Laboratory of Quantitative Vegetation Ecology,Institute of Botany,Chinese Academy of Sciences,Beijing 100093,China

  • Received:2005-04-21 Revised:2005-11-10 Online:2006-03-18 Published:2006-03-18

摘要: 利用元素分析仪,测定了芦苇湿地不同层次土壤有机碳和全N的变化.结果表明,土壤有机碳、全N及C/N随土壤深度的增加呈下降趋势.对不同月份(7、8、9和10月)而言,有机碳、全N及C/N比累积峰位于不同的土层中.土壤温度、水分及芦苇生长状况是引起分异的重要因子.7、8和10月份芦苇湿地不同层次土壤有机碳与全N呈显著相关(R2=0.73、0.73、0.71),而9月份芦苇湿地不同层次土壤有机碳与全N之间的相关性相对较差(R2=0.41).土壤C/N与土壤有机碳、全N均呈负相关,但C/N与全N的相关性强于土壤有机碳,说明C/N的大小主要决定于全N含量.

关键词: 干沉降通量, 干沉降速率, 臭氧干沉降, 沉降阻力

Abstract: With element analyzer,this paper measured the variation of organic carbon and total nitrogen in different soil depths of reed wetland.The results showed that soil organic carbon,total nitrogen,and C/N ratio were decreased gradually with increasing soil depth,and their accumulation peaks were differed with soil layers and months.Soil temperature and moisture and the growth status of reed were the main factors caused the differences.Soil organic carbon was strongly positively correlated with soil total nitrogen content in July,August and October,the R2 being 0.73,0.73 and 0.71 respectively,but weakly correlated in September.Soil C/N ratio was negatively correlated to soil organic carbon and total nitrogen,but the correlativity was higher with soil total nitrogen than with soil organic carbon,suggesting that soil C/N ratio was more determined by the content of soil total nitrogen.

Key words: ozone dry deposition flux, ozone deposition resistance., ozone deposition, ozone dry deposition rate