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使用硫酸铵作为硫肥:对氨挥发的影响。

Use of ammonium sulphate as a sulphur fertilizer: Implications for ammonia volatilization.

作者信息

Powlson David S, Dawson Chris J

机构信息

Department of Sustainable Agriculture Systems Rothamsted Research Harpenden Herts UK.

Chris Dawson and Associates Westover York UK.

出版信息

Soil Use Manag. 2022 Jan;38(1):622-634. doi: 10.1111/sum.12733. Epub 2021 Jul 2.

DOI:10.1111/sum.12733
PMID:35873863
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC9290479/
Abstract

Ammonium sulphate is widely used as a sulphur (S) fertilizer, constituting about 50% of global S use. Within nitrogen (N) management, it is well known that ammonium-based fertilizers are subject to ammonia (NH) volatilization in soils with pH > 7, but this has been overlooked in decision making on S fertilization. We reviewed 41 publications reporting measurements of NH loss from ammonium sulphate in 16 countries covering a wide range of soil types and climates. In field experiments, loss was mostly <5% of applied N in soils with pH (in water) <7.0. In soils with pH > 7.0, there was a wide range of losses (0%-66%), with many in the 20%-40% range and some indication of increased loss (ca. 5%-15%) in soils with pH 6.5-7.0. We estimate that replacing ammonium sulphate with a different form of S for arable crops could decrease NH emissions from this source by 90%, even taking account of likely emissions from alternative fertilizers to replace the N, but chosen for low NH emission. For every kt of ammonium sulphate replaced on soils of pH > 7.0 in temperate regions, NH emission would decrease from 35.7 to 3.6 t NH. Other readily available sources of S include single superphosphate, potassium sulphate, magnesium sulphate, calcium sulphate dihydrate (gypsum), and polyhalite (Polysulphate). In view of the large areas of high pH soils globally, this change of S fertilizer selection would make a significant contribution to decreasing NH emissions worldwide, contributing to necessary cuts to meet agreed ceilings under the Gothenburg Convention.

摘要

硫酸铵作为一种硫(S)肥被广泛使用,约占全球硫肥使用量的50%。在氮(N)管理方面,众所周知,在pH值>7的土壤中,铵基肥料会发生氨(NH₃)挥发,但在硫肥施用决策中这一点一直被忽视。我们查阅了41份出版物,这些出版物报告了在16个国家对硫酸铵中NH₃损失的测量,涵盖了广泛的土壤类型和气候条件。在田间试验中,在pH值(水中)<7.0的土壤中,损失大多低于施氮量的5%。在pH值>7.0的土壤中,损失范围很广(0%-66%),许多在20%-40%范围内,并且有迹象表明在pH值为6.5-7.0的土壤中损失有所增加(约5%-15%)。我们估计,用不同形式的硫替代硫酸铵用于耕地作物,即使考虑到替代氮肥可能产生的排放,但因其氨排放低而被选用,也可使该来源的NH₃排放量减少90%。在温带地区pH值>7.0的土壤上,每替换1千吨硫酸铵,NH₃排放量将从35.7吨降至3.6吨。其他容易获得的硫源包括过磷酸钙、硫酸钾、硫酸镁、二水硫酸钙(石膏)和杂卤石(多硫酸盐)。鉴于全球高pH值土壤面积广大,这种硫肥选择的改变将对全球减少NH₃排放做出重大贡献,有助于实现《哥德堡公约》商定的排放上限所需的减排。

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