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加强热带农业对氮素损失潜力的元分析。

Meta-analysis on the potential for increasing nitrogen losses from intensifying tropical agriculture.

机构信息

Department of Ecology, Evolution, and Environmental Biology, Columbia University, New York, NY, USA.

Gund Institute for Environment, University of Vermont, Burlington, VT, USA.

出版信息

Glob Chang Biol. 2020 Mar;26(3):1668-1680. doi: 10.1111/gcb.14951. Epub 2020 Jan 26.

Abstract

Fertilized temperate croplands export large amounts of reactive nitrogen (N), which degrades water and air quality and contributes to climate change. Fertilizer use is poised to increase in the tropics, where widespread food insecurity persists and increased agricultural productivity will be needed, but much less is known about the potential consequences of increased tropical N fertilizer application. We conducted a meta-analysis of tropical field studies of nitrate leaching, nitrous oxide emissions, nitric oxide emissions, and ammonia volatilization totaling more than 1,000 observations. We found that the relationship between N inputs and losses differed little between temperate and tropical croplands, although total nitric oxide losses were higher in the tropics. Among the potential drivers we studied, the N input rate controlled all N losses, but soil texture and water inputs also controlled hydrological N losses. Irrigated systems had significantly higher losses of ammonia, and pasture agroecosystems had higher nitric oxide losses. Tripling of fertilizer N inputs to tropical croplands from 50 to 150 kg N ha  year would have substantial environmental implications and would lead to increases in nitrate leaching (+30%), nitrous oxide emissions (+30%), nitric oxide (+66%) emissions, and ammonia volatilization (+74%), bringing tropical agricultural nitrate, nitrous oxide, and ammonia losses in line with temperate losses and raising nitric oxide losses above them.

摘要

施肥耕地会向环境中输出大量活性氮(N),这会降低水和空气质量,并导致气候变化。在热带地区,肥料的使用量可能会增加,因为那里普遍存在粮食不安全问题,需要提高农业生产力,但人们对增加热带地区 N 肥应用的潜在后果知之甚少。我们对硝酸盐淋溶、氧化亚氮排放、一氧化氮排放和氨挥发的热带田间研究进行了荟萃分析,这些研究的总观测次数超过了 1000 次。我们发现,尽管热带地区的总一氧化氮损失较高,但 N 输入与损失之间的关系在温带和热带耕地之间差异不大。在我们研究的潜在驱动因素中,N 输入率控制着所有 N 损失,但土壤质地和水分输入也控制着水文 N 损失。灌溉系统的氨损失明显更高,而草地农业生态系统的一氧化氮损失更高。将热带耕地的肥料 N 输入从 50 千克/公顷/年增加到 150 千克/公顷/年,将对环境产生重大影响,并导致硝酸盐淋溶(增加 30%)、氧化亚氮排放(增加 30%)、一氧化氮(增加 66%)排放和氨挥发(增加 74%)的增加,使热带农业的硝酸盐、氧化亚氮和氨损失与温带损失持平,并使一氧化氮损失超过温带。

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