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[外源氮输入对不同土地利用方式下沟渠沉积物反硝化及一氧化氮排放的影响]

[Impact of Exogenous Nitrogen Import on Sediment Denitrification and NO Emissions in Ditches Under Different Land Uses].

作者信息

She Dong-Li, Chen Xin-Yi, Gao Xue-Mei, Zhang Wen-Juan, 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 Agricultural 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. 2018 Aug 8;39(8):3689-3695. doi: 10.13227/j.hjkx.201709100.

Abstract

Farmland drainage ditch soil can consume part of the agricultural non-point nitrogen through nitrification-denitrification processes. Paddy fields, vegetable land, and orchards are the main types of land uses in the Taihu Lake region, and many drainage ditches are distributed across these lands. The way exogenous nitrogen is imported to drain ditches under different land uses differs significantly, which can directly affect the nitrogen consumption ability of the channels. A soil incubation experiment was conducted under laboratory conditions to study the denitrification loss and NO emissions of drainage ditch soil under different land uses. In this study, drainage ditch sediment was collected from orchards, paddy fields, and vegetable land in the Taihu Lake region. Five different NO-N content import levels were set:0, 0.5, 1.0, 5.0, and 10 mg·L, which were denoted as N, N, N, N, and N, respectively. The results showed that exogenous nitrogen input stimulated sediment denitrification in the drainage ditches. The sediment denitrification rates of the three types of channels increased significantly with the increase of input NO-N concentration (<0.05). There was a significant linear positive correlation between the cumulative denitrification loss and input NO-N concentration (>0.75). Excluding for the vegetable land sediment, the NO emission rate and cumulative emissions did not increase significantly with the increase of input NO-N concentration (>0.05). There was no significant difference in the denitrification and NO emissions among the three kinds of channel sediment, with no or low exogenous nitrogen input (Nand N) (>0.05). As the input NO-N concentration increased, especially under the condition of high exogenous nitrogen input (Nand N), the nitrogen consumed via denitrification in orchard and paddy field sediment was significantly higher than that in vegetable land sediment (<0.05), whereas the NO emissions of drainage ditch sediment from the vegetable land was significantly higher than that of the other two channel sediments (<0.05). The mineralization rate of ditch soil organic carbon had a positive correlation with denitrification rate (=15), and microbial mineralization (CO-C) promoted the nitrification and denitrification of the drainage ditch soils.

摘要

农田排水沟土壤可通过硝化-反硝化过程消耗部分农业面源氮。稻田、菜地和果园是太湖地区主要的土地利用类型,这些土地上分布着许多排水沟。不同土地利用方式下外源氮进入排水沟的方式差异显著,这会直接影响沟渠的氮消耗能力。在实验室条件下进行了土壤培养实验,以研究不同土地利用方式下排水沟土壤的反硝化损失和一氧化氮排放。本研究中,从太湖地区的果园、稻田和菜地里采集了排水沟沉积物。设置了5种不同的一氧化氮-氮含量输入水平:0、0.5、1.0、5.0和10毫克·升,分别记为N₀、N₁、N₂、N₃和N₄。结果表明,外源氮输入刺激了排水沟沉积物的反硝化作用。三种类型沟渠的沉积物反硝化速率随输入一氧化氮-氮浓度的增加而显著增加(P<0.05)。累积反硝化损失与输入一氧化氮-氮浓度之间存在显著的线性正相关(R²>0.75)。除菜地沉积物外,一氧化氮排放速率和累积排放量并未随输入一氧化氮-氮浓度的增加而显著增加(P>0.05)。在无或低外源氮输入(N₀和N₁)时,三种沟渠沉积物的反硝化和一氧化氮排放无显著差异(P>0.05)。随着输入一氧化氮-氮浓度的增加,特别是在外源氮高输入(N₃和N₄)条件下,果园和稻田沉积物中通过反硝化消耗的氮显著高于菜地沉积物(P<0.05),而菜地排水沟沉积物的一氧化氮排放量显著高于其他两种沟渠沉积物(P<0.05)。沟渠土壤有机碳的矿化率与反硝化速率呈正相关(R²=0.15),微生物矿化(CO₂-C)促进了排水沟土壤的硝化和反硝化作用。

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