长江流域资源与环境 >> 2014, Vol. 23 >> Issue (02): 287-.doi: 10.11870/cjlyzyyhj201402019

• 生态环境 • 上一篇    下一篇

三峡库区消落带土壤N2O排放及反硝化研究

方芳|孙志伟|高红涛|郭劲松|李哲   

  1. (1.重庆大学城市建设与环境工程学院|重庆 400045;2.中国科学院重庆绿色智能技术研究院|重庆 401122)
  • 出版日期:2014-02-20

N2O EMISSION AND DENITRIFICATION IN THE SOILS OF WATERLEVELFLUCTUATION ZONE IN THE THREE GORGES RESERVOIR AREA

FANG Fang1,SUN Zhiwei1,GAO Hongtao1,GUO Jinsong1,2,LI Zhe1   

  1. (1.Faculty of Urban Construction and Environmental Engineering,Chongqing University,Chongqing 400045,China;
    2.Chongqing Institute of Green and Intelligent Technology,Chinese Academy of Sciences,Chongqing 401122,China)
  • Online:2014-02-20

摘要:

应用C2H2抑制原状土柱培养法研究了三峡库区腹地忠县境内两种不同土地利用方式和不同高程消落带土壤N2O排放及反硝化速率的变化及特征。结果表明:研究区域消落带土壤N2O排放速率和反硝化速率具有明显的时空差异,农耕区消落带土壤N2O排放速率均值为2371±3161 g N/hm2·d,为人工植被恢复区土壤N2O排放速率均值的348倍,农耕区反硝化速率均值为10551±12660 g N/hm2·d,为人工植被恢复区反硝化速率均值的539倍,二者反硝化速率差异显著(p<005)。不同高程消落带土壤N2O排放速率和反硝化速率差异不显著(p>005),但低高程消落带土壤反硝化作用相对较强。相关性分析表明,农耕区消落带N2O排放速率与土壤温度和Eh存在显著正相关(p<005),其反硝化速率与土壤温度存在正相关关系,表明消落带土壤N2O排放和反硝化作用受土壤温度影响明显。研究区域N2O/(N2O+N2)介于009~052,表明N2为消落带土壤反硝化作用的主要产物,但N2O的排放量也不容忽视。三峡库区消落带的土地利用方式对消落带土壤N2O排放和反硝化作用有重要影响,而耕种等人类活动可显著提高消落带N2O排放量和反硝化损失量

Abstract:

The intact soil coreacetylene inhibition technique was used to study the nitrous oxide (N2O) emission and the denitrification performance in the soils,with different land utilization and altitude,from the waterlevelfluctuation zone (WLFZ) in Zhongxian County in the Three Gorges Reservoir Area.The results indicated that the N2O emission and the denitrification rates in the soils of WLFZ varied spatiotemporally.The average N2O emission rate in the soils of cultivated area was 2371±3161 g N/hm2·d,with 3.48 times of artificial vegetation restoration area.The average denitrification rate of cultivated area was 10551±12660 g N/hm2·d,with 539 times of artificial vegetation restoration area,and the difference of denitrification rate was significant (p<005).There was no significant difference in N2O emission and denitrification rates in the soils of different altitude,while the denitrification rate in the soils of low altitude was relatively higher.Analysis indicated that the N2O emission rate in the soils of cultivated area was significantly and positively correlated with soil temperature and Eh(p<005),and its denitrification rate was positively correlated with soil temperature,implying that soil temperature played an important role in regulating N2O emission and denitrification in the soils of WLFZ.The ratio of N2O/(N2O+N2) ranged from 009 to 052 in the study area,suggesting that N2 was the main product of denitrification,but the N2O emission amount cannot be ignored.Land utilization types had a great impact on N2O emission and denitrification in the soils of WLFZ.Human activities,e.g.cultivation,significantly increased N2O emission amount and denitrification loss in the soils of WLFZ

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