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农业氮淋溶和径流间接 NO 排放因子的综述,以更新 IPCC 默认值。

A review of indirect NO emission factors from agricultural nitrogen leaching and runoff to update of the default IPCC values.

机构信息

State Key Laboratory of Subtropical Silviculture, Zhejiang A & F University, Hangzhou, 311300, China; Institute for Agro-Environmental Sciences, National Agriculture and Food Research Organization, 3-1-3, Kannondai, Tsukuba, Ibaraki, 305-8604, Japan.

Institute for Agro-Environmental Sciences, National Agriculture and Food Research Organization, 3-1-3, Kannondai, Tsukuba, Ibaraki, 305-8604, Japan.

出版信息

Environ Pollut. 2019 Feb;245:300-306. doi: 10.1016/j.envpol.2018.11.016. Epub 2018 Nov 9.

Abstract

Indirect NO emissions from agricultural nitrogen (N) leaching and runoff in water bodies contribute significantly to the global atmospheric NO budget. However, considerable uncertainty regarding this source remains in the bottom-up NO inventory. Indirect NO emission factor associated with N leaching and runoff (EF; kg NON per kg of NO-N) incorporate three components for groundwater and surface drainage (EF), rivers (EF), and estuaries (EF). The 2006 IPCC default EF value was based on a small number of studies available at the time. Here we present the synthesis of 254 measurements of EF, dissolved NO, and nitrate from 106 studies. Our results do not support the further downward revision of EF by the IPCC and suggest an upward revision of EF of 0.0060. The emission factors for groundwater and springs (0.0079) was higher than that for surface drainage (0.0040). The emission factor for lakes, ponds, and reservoirs was 0.0012, whereas that for rivers was 0.0030, and a combined EF was 0.0026. Estimated EF and EF (0.0026) values from the study were close to the current IPCC default values (0.0025 each). We estimated an updated default EF value of 0.01 for the refinement of IPCC guidelines.

摘要

水体中农业氮(N)淋溶和径流导致的间接 NO 排放对全球大气 NO 预算有重要贡献。然而,在自下而上的 NO 清单中,这种来源仍然存在相当大的不确定性。与 N 淋溶和径流相关的间接 NO 排放因子(EF;kg NON 每 kg 的 NO-N)包含地下水和地表排水(EF)、河流(EF)和河口(EF)的三个组成部分。2006 年 IPCC 默认的 EF 值是基于当时可用的少数几项研究。在这里,我们综合了来自 106 项研究的 254 项 EF、溶解 NO 和硝酸盐测量值。我们的结果不支持 IPCC 进一步下调 EF,并建议将 EF 上调 0.0060。地下水和泉水的排放因子(0.0079)高于地表排水(0.0040)。湖泊、池塘和水库的排放因子为 0.0012,而河流的排放因子为 0.0030,综合排放因子为 0.0026。从这项研究中估计的 EF 和 EF(0.0026)值接近当前 IPCC 默认值(各为 0.0025)。我们估计了一个更新的默认 EF 值 0.01,用于完善 IPCC 指南。

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