{"title":"Investigating Microbial Triggers of Nitrous Oxide Emissions in Agriculturally Influenced Aquatic Ecosystems","authors":"C Crundwell, Lori Phillips, Chris Weisener","doi":"10.3897/aca.6.e107604","DOIUrl":null,"url":null,"abstract":"The agricultural sector in Canada is responsible for approximately 9% of greenhouse gas (GHG) emissions in Canada, accounting for 54 MT of carbon dioxide (CO 2 ), as well as 31% of methane (CH 4 ) and 75% of national nitrous oxide (N 2 O) emissions in 2021 (Environment and Climate Change Canada 2021). However, these estimates do not include the indirect GHG emissions that occur in agriculturally impacted waterways. Ontario is home to over 45 000 kilometers of agricultural drainage ditches, with tile drains directly connecting terrestrial and aquatic environments. Microbial biogeochemical cycles in the causeways experience fluxes of nutrients leading to hotspots for GHG at the sediment-water interfaces. Along with fluxes of nutrients, the causeways are regularly disturbed by anthropogenic effects (e.g., dredging, removal of vegetative buffers) and increasing frequency of storm events. Previous studies have used static chambers to evaluate GHG emissions from aquatic systems (Mu et al. 2022, Xiao et al. 2016). However, this approach can be time consuming and labour intensive and is impractical in aquatic systems due potential extensive underestimation of fluxes from diffusion. To resolve driving factors contributing to GHG in these systems a detailed study investigating the activity of the microbial community is warranted. In this study we hypothesize microbial activity within the sediment will correlate with N 2 O emissions. To test the response of the microbial community a combination of molecular approaches (i.e., qPCR and Ion torrent) targeting archaeal and bacterial nitrifiers and denitrifies was used. These functional responses were evaluated with respect to N 2 O emissions, which were measured in the field at the time of sampling using Unisense N 2 O probes. In this study, N 2 O sensor response was calibrated to a functional gene index for rapid risk assessment of GHG hotspots.","PeriodicalId":101714,"journal":{"name":"ARPHA Conference Abstracts","volume":"16 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2023-10-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"ARPHA Conference Abstracts","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.3897/aca.6.e107604","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The agricultural sector in Canada is responsible for approximately 9% of greenhouse gas (GHG) emissions in Canada, accounting for 54 MT of carbon dioxide (CO 2 ), as well as 31% of methane (CH 4 ) and 75% of national nitrous oxide (N 2 O) emissions in 2021 (Environment and Climate Change Canada 2021). However, these estimates do not include the indirect GHG emissions that occur in agriculturally impacted waterways. Ontario is home to over 45 000 kilometers of agricultural drainage ditches, with tile drains directly connecting terrestrial and aquatic environments. Microbial biogeochemical cycles in the causeways experience fluxes of nutrients leading to hotspots for GHG at the sediment-water interfaces. Along with fluxes of nutrients, the causeways are regularly disturbed by anthropogenic effects (e.g., dredging, removal of vegetative buffers) and increasing frequency of storm events. Previous studies have used static chambers to evaluate GHG emissions from aquatic systems (Mu et al. 2022, Xiao et al. 2016). However, this approach can be time consuming and labour intensive and is impractical in aquatic systems due potential extensive underestimation of fluxes from diffusion. To resolve driving factors contributing to GHG in these systems a detailed study investigating the activity of the microbial community is warranted. In this study we hypothesize microbial activity within the sediment will correlate with N 2 O emissions. To test the response of the microbial community a combination of molecular approaches (i.e., qPCR and Ion torrent) targeting archaeal and bacterial nitrifiers and denitrifies was used. These functional responses were evaluated with respect to N 2 O emissions, which were measured in the field at the time of sampling using Unisense N 2 O probes. In this study, N 2 O sensor response was calibrated to a functional gene index for rapid risk assessment of GHG hotspots.
加拿大的农业部门约占加拿大温室气体(GHG)排放量的9%,占2021年二氧化碳(CO 2)的54公吨,以及31%的甲烷(CH 4)和75%的全国一氧化二氮(n2o)排放量(加拿大环境与气候变化2021年)。然而,这些估计不包括在受农业影响的水道中发生的间接温室气体排放。安大略省拥有超过45,000公里的农业排水沟,瓷砖排水沟直接连接陆地和水生环境。堤道中的微生物生物地球化学循环经历了养分的通量,导致沉积物-水界面的温室气体热点。随着营养物质的流动,堤道经常受到人为影响(如疏浚、移除植被缓冲)和风暴事件频率增加的干扰。以前的研究使用静态室来评估水生系统的温室气体排放(Mu et al. 2022, Xiao et al. 2016)。然而,这种方法可能是耗时和劳动密集型的,并且在水生系统中是不切实际的,因为可能广泛低估了扩散通量。为了解决这些系统中造成温室气体的驱动因素,有必要对微生物群落的活动进行详细的研究。在这项研究中,我们假设沉积物中的微生物活动与氮排放有关。为了测试微生物群落的反应,采用了针对古细菌和细菌硝化菌和反硝化菌的分子方法(即qPCR和离子流)的组合。这些功能响应是根据氮排放来评估的,氮排放是在采样时使用Unisense氮探针在现场测量的。本研究将氮氧传感器响应校准为一个功能基因指数,用于快速评估温室气体热点地区的风险。