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果园排水沉积物中不同碳输入导致的反硝化损失和一氧化氮排放

[Denitrification Loss and NO Emission from Different Carbon Inputs in Orchard Drains Sediments].

作者信息

Gao Xue-Mei, She Dong-Li, Yan Xiao-Yuan, Xia Yong-Qiu

机构信息

Key Laboratory of Efficient Irrigation-Drainage and Agricultural Soil-Water Environment in Southern China, Ministry of Education, College of Water Conservancy and Hydropower Engineering, Hohai University, Nanjing 210098, China.

State Key Laboratory of Soil and Sustainable Agriculture, Institute of Soil Science, Chinese Academy of Sciences, Nanjing 210008, China.

出版信息

Huan Jing Ke Xue. 2016 Jul 8;37(7):2731-2737. doi: 10.13227/j.hjkx.2016.07.041.

Abstract

The orchard is an important economic crop in Taihu Lake region. Heavy nitrogen application in orchard results in great nitrogen loss to drainage ditch, and unbalanced carbon nitrogen ratio. Therefore, carbon might be an important limiting factor for sediment nitrification and denitrification. A soil incubation experiment controlled by the acetylene inhibition method was conducted under laboratory conditions to study the denitrification loss and NO emissions of orchard drainage ditch soil. We designed five carbon input levels of 0, 5, 25, 50 and 100 mg·L, which were noted as C, C, C, C and C, respectively, meanwhile there was 5 mg·L net nitrogen input in the form of KNO in each treatment. The results showed that carbon inputs could stimulate both denitrification rates () and NO emission rates. Carbon and nitrogen ratio had a significant effect on NO emission rates and denitrification loss rates (<0.05). When the carbon and nitrogen ratio was 10:1, total cumulative denitrification losses and NO emissions were both highest (319.26 μg·kg and 6.20 μg·kg, respectively) among the treatments, which accounted for 1.28% and 0.02% of net nitrogen input, respectively. This result indicated that the carbon and nitrogen ratio of 10:1 was most favorable for NO emissions and denitrification process in sediments.

摘要

果园是太湖地区重要的经济作物。果园中大量施用氮肥导致氮素大量流失到排水沟中,且碳氮比失衡。因此,碳可能是沉积物硝化作用和反硝化作用的重要限制因素。在实验室条件下,采用乙炔抑制法进行土壤培养试验,研究果园排水沟土壤的反硝化损失和一氧化氮排放情况。我们设计了0、5、25、50和100 mg·L的五个碳输入水平,分别记为C₀、C₁、C₂、C₃和C₄,同时每个处理中以硝酸钾的形式有5 mg·L的净氮输入。结果表明,碳输入可以刺激反硝化速率()和一氧化氮排放速率。碳氮比对一氧化氮排放速率和反硝化损失速率有显著影响(P<0.05)。当碳氮比为10:1时,总累积反硝化损失和一氧化氮排放均为各处理中最高(分别为319.26 μg·kg和6.20 μg·kg),分别占净氮输入的1.28%和0.02%。这一结果表明,碳氮比为10:1最有利于沉积物中一氧化氮的排放和反硝化过程。

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