Midwestern N2O Emissions Linked at Regional Scales to Remotely Sensed Soil Moisture in a North American Inversion

IF 5.4 2区 地球科学 Q1 ENVIRONMENTAL SCIENCES
Cynthia Nevison, Lei Hu, Stephen M. Ogle, Alisa Keyser, Xin Lan, Kathryn McKain
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Abstract

The interactions between soil moisture (SM), agricultural practices, and microbially driven N2O emissions have been described in detail at the field scale. The relationships among those variables are investigated here at larger scales using Soil Moisture Active-Passive remote sensing data and a regional atmospheric inversion. In the atmospheric N2O data set used in the inversion, 13 large pulse events were observed during the crop growing season from 2015 to 2021 in the U.S. Midwest, mainly in Iowa. These events were linked to rapid changes in SM, either increasing from dry to wet conditions, or vice versa, within a week preceding the N2O pulse. However, no significant correlations were found between SM or soil temperature and posterior N2O fluxes from the inversion integrated over Iowa across the peak emission months of May–June. Analysis over the full growing season suggested compensating emissions, for example, higher than normal N2O fluxes in July following a dry June. These results suggest a relatively consistent ∼4% yield of N2O from anthropogenic N inputs to croplands in Iowa regardless of short-term variability in soil conditions. Net growing season N2O emissions in the DayCent biogeochemistry model were also not correlated to SM or temperature, although the model tended to underestimate interannual variability relative to the inversion. An expanded atmospheric observation network, together with an extended SM time series, would allow a better understanding of the relationship between variability in SM and N2O emissions at regional scales.

中西部地区N2O排放在区域尺度上与北美逆温遥感土壤湿度有关
土壤湿度(SM)、农业实践和微生物驱动的N2O排放之间的相互作用已在田间尺度上进行了详细描述。本文利用土壤湿度主被动遥感数据和区域大气反演在更大尺度上研究了这些变量之间的关系。在反演使用的大气N2O数据集中,2015 - 2021年在美国中西部以爱荷华州为主的作物生长期观测到13个大脉冲事件。这些事件与SM的快速变化有关,在N2O脉冲之前的一周内,SM要么从干燥增加到潮湿,要么反之亦然。然而,5 - 6月在爱荷华州上空反演得到的N2O后验通量与SM或土壤温度之间没有显著的相关性。对整个生长季节的分析表明,补偿排放,例如,在干燥的6月之后,7月的N2O通量高于正常水平。这些结果表明,无论土壤条件的短期变化如何,爱荷华州人为氮输入农田的N2O产量相对一致~ 4%。在DayCent生物地球化学模型中,净生长季N2O排放量也与SM或温度无关,尽管该模型相对于反演倾向于低估年际变化。一个扩大的大气观测网,加上一个扩大的平均气温时间序列,将使我们能够更好地了解区域尺度上平均气温变化与N2O排放之间的关系。
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来源期刊
Global Biogeochemical Cycles
Global Biogeochemical Cycles 环境科学-地球科学综合
CiteScore
8.90
自引率
7.70%
发文量
141
审稿时长
8-16 weeks
期刊介绍: Global Biogeochemical Cycles (GBC) features research on regional to global biogeochemical interactions, as well as more local studies that demonstrate fundamental implications for biogeochemical processing at regional or global scales. Published papers draw on a wide array of methods and knowledge and extend in time from the deep geologic past to recent historical and potential future interactions. This broad scope includes studies that elucidate human activities as interactive components of biogeochemical cycles and physical Earth Systems including climate. Authors are required to make their work accessible to a broad interdisciplinary range of scientists.
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