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汉江流域不同土地利用方式下土壤反硝化率及其控制因素研究
引用本文:S. P. JUNG,Y. J. KIM,H. KANG. 汉江流域不同土地利用方式下土壤反硝化率及其控制因素研究[J]. 土壤圈, 2014, 24(4): 516-528. DOI: 10.1016/S1002-0160(14)60038-2
作者姓名:S. P. JUNG  Y. J. KIM  H. KANG
基金项目:Supported by the National Research Foundation of Korea (No. 2013056833)
摘    要:Land-use patterns can affect various nutrient cycles in stream ecosystems, but little information is available about the effects of urban development on denitrification processes at the watershed scale. In the presented study, we investigated the controlling factors of denitrification rates within the streams of the Han River Basin, Korea, with different land-use patterns, in order to enhance the effectiveness of water resource management strategies. Ten watersheds were classified into three land-use patterns (forest, agriculture and urban) using satellite images and geographic information system techniques, and in-situ denitrification rates were determined using an acetylene blocking method. Additionally, sediment samples were collected from each stream to analyze denitrifier communities and abundance using molecular approaches. In-situ denitrification rates were found to be in the order of agricultural streams (289.6 mg N20-N m-2 d-1) 〉 urban streams (157.0 mg N20-N m-2 d-1) 〉 forested streams (41.9 mg N20-N m-2 d-l). In contrast, the average quantity of denitrifying genes was the lowest in the urban streams. Genetic diversity of denitrifying genes was not affected by watershed land-use pattern, but exhibited stream-dependent pattern. More significance factors were involved in denitrification in the sites with higher denitrification rates. Multiple linear regression analysis revealed that clay, dissolved organic carbon and water contents were the main factors controlling denitrification rate in the agricultural streams, while dissolved organic carbon was the main controlling factor in the urban streams. In contrast, temperature appeared to be the main controlling factor in the forested streams.

关 键 词:土地利用模式  反硝化速率  森林溪流  汉江流域  影响因素  地理信息系统技术  多元线性回归分析  分子生物学方法
收稿时间:2013-10-29

Denitrification rates and their controlling factors in streams of the Han River Basin with different land-use patterns
S. P. JUNG,Y. J. KIM and H. KANG. Denitrification rates and their controlling factors in streams of the Han River Basin with different land-use patterns[J]. Pedosphere, 2014, 24(4): 516-528. DOI: 10.1016/S1002-0160(14)60038-2
Authors:S. P. JUNG  Y. J. KIM  H. KANG
Affiliation:1School of Civil and Environmental Engineering, Yonsei University, Seoul 120-749 (Korea)2River and Coastal Research Division, Korea Institute of Construction Technology, Goyang 211-712 (Korea)
Abstract:Land-use patterns can affect various nutrient cycles in stream ecosystems, but little information is available about the effects of urban development on denitrification processes at the watershed scale. In the presented study, we investigated the controlling factors of denitrification rates within the streams of the Han River Basin, Korea, with different land-use patterns, in order to enhance the effectiveness of water resource management strategies. Ten watersheds were classified into three land-use patterns (forest, agriculture and urban) using satellite images and geographic information system techniques, and in-situ denitrification rates were determined using an acetylene blocking method. Additionally, sediment samples were collected from each stream to analyze denitrifier communities and abundance using molecular approaches. In-situ denitrification rates were found to be in the order of agricultural streams (289.6 mg N2O-N m-2 d-1) > urban streams (157.0 mg N2O-N m-2 d-1) > forested streams (41.9 mg N2O-N m-2 d-1). In contrast, the average quantity of denitrifying genes was the lowest in the urban streams. Genetic diversity of denitrifying genes was not affected by watershed land-use pattern, but exhibited stream-dependent pattern. More significance factors were involved in denitrification in the sites with higher denitrification rates. Multiple linear regression analysis revealed that clay, dissolved organic carbon and water contents were the main factors controlling denitrification rate in the agricultural streams, while dissolved organic carbon was the main controlling factor in the urban streams. In contrast, temperature appeared to be the main controlling factor in the forested streams.
Keywords:denitrifier communities   denitrifying genes   nutrient cycle   stream ecosystem
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