Manure application magnifies methane emission from drainage ditch sediments

IF 4.3 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES
Biogeochemistry Pub Date : 2026-06-03 Epub Date: 2026-08-06 DOI:10.1007/s10533-026-01348-6
Quinten Struik, Madison Cicha, José R. Paranaíba, Sarian Kosten, Annelies J. Veraart
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引用次数: 0

Abstract

Agricultural drainage ditches have been recently identified as hotspots of methane (CH4), carbon dioxide (CO2), and nitrous oxide (N2O) emissions. Ditches often experience inputs of fertilizers from adjacent agricultural fields, which increases the availability of organic carbon and nutrients in ditch sediments, thereby fueling greenhouse gas (GHG) production. Here, we quantify the effects of two types of fertilizers (manure and artificial fertilizer) on GHG dynamics from agricultural drainage ditch sediments subjected to oxic and anoxic conditions. We first measured rates of potential sediment N2O production, CH4 production, and aerobic CH4 oxidation under different fertilizer doses. We observed that manure additions (expressed here as ammonium (NH4+) dose, referring to the resulting NH4+ concentration in a given bottle after addition) strongly stimulated CH4 and N2O production. Methane production rates increased approximately threefold as a result of manure additions, ranging from 18.4 to 61.7 µmol CH4 gDW−1 d−1, whereas N2O production rates increased approximately 16-fold, and varied from 0.1 to 1.6 µmol N2O gDW−1 d−1 across manure doses. Aerobic CH4 oxidation was also stimulated by manure addition, while at resulting NH4+ concentrations above 2 mmol L−1, oxidation rates declined. In contrast, artificial fertilizer caused immediate inhibition of CH4 and N2O production and aerobic CH4 oxidation, even at the lowest NH4+ concentration tested (0.05 mmol L−1). Focusing on the effects of manure on GHG emissions, we observed that under anoxic conditions, sediment cores receiving high manure inputs emitted approximately 3.5 times more GHGs (in CO2-equivalents) than anoxic controls (no manure) and about 5.5 times more than oxic controls. Methane was the dominant driver of increased emissions at higher manure doses. As fertilizer use continues to rise globally, these results highlight the importance of implementing climate-smart water and nutrient management strategies in ditches and adjacent grasslands to mitigate climate trade-offs.

施用粪肥增加了排水沟沉积物的甲烷排放。
农业排水沟最近被确定为甲烷(CH4)、二氧化碳(CO2)和氧化亚氮(N2O)排放的热点。沟渠经常从邻近的农田投入肥料,这增加了沟渠沉积物中有机碳和营养物质的可用性,从而助长了温室气体(GHG)的产生。在此,我们量化了两种类型的肥料(粪肥和人工肥料)在缺氧和缺氧条件下对农业排水沟沉积物温室气体动态的影响。我们首先测量了不同施肥剂量下潜在沉积物N2O生成速率、CH4生成速率和好氧CH4氧化速率。我们观察到,添加肥料(这里表示为铵(NH4 +)剂量,指添加后给定瓶中产生的NH4 +浓度)强烈刺激了CH4和N2O的产生。添加有机肥后,甲烷产率增加了约3倍,范围从18.4µmol CH4 gDW-1 d-1到61.7µmol CH4 gDW-1 d-1;添加有机肥后,N2O产率增加了约16倍,范围从0.1µmol N2O gDW-1 d-1到1.6µmol N2O gDW-1 d-1。添加肥料也能促进好氧CH4氧化,但当NH4 +浓度高于2 mmol L-1时,氧化速率下降。相比之下,即使在最低NH4 +浓度(0.05 mmol L-1)下,人工施肥也能立即抑制CH4和N2O的产生以及好氧CH4氧化。关注粪肥对温室气体排放的影响,我们观察到,在缺氧条件下,高粪肥投入的沉积物岩心排放的温室气体(以二氧化碳当量计)约为缺氧对照(无粪肥)的3.5倍,约为缺氧对照的5.5倍。在较高的肥料用量下,甲烷是温室气体排放量增加的主要驱动因素。随着全球化肥使用量的持续上升,这些结果强调了在沟渠和邻近草原实施气候智能型水和养分管理战略以减轻气候权衡的重要性。补充资料:在线版本包含补充资料,下载地址:10.1007/s10533-026-01348-6。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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