Graduate Degree Program in Ecology, Colorado State University, Fort Collins, Colorado, USA.
Department of Biology, Colorado State University, Fort Collins, Colorado, USA.
Glob Chang Biol. 2022 Jul;28(13):4163-4179. doi: 10.1111/gcb.16190. Epub 2022 May 4.
Nitrous oxide (N O) is a formidable greenhouse gas with a warming potential ~300× greater than CO . However, its emissions to the atmosphere have gone largely unchecked because the microbial and environmental controls governing N O emissions have proven difficult to manage. The microbial process N O consumption is the only know biotic pathway to remove N O from soil pores and therefore reduce N O emissions. Consequently, manipulating soils to increase N O consumption by organic carbon (OC) additions has steadily gained interest. However, the response of N O emissions to different OC additions are inconsistent, and it is unclear if lower N O emissions are due to increased consumption, decreased production, or both. Simplified and systematic studies are needed to evaluate the efficacy of different OC additions on N O consumption. We aimed to manipulate N O consumption by amending soils with OC compounds (succinate, acetate, propionate) more directly available to denitrifiers. We hypothesized that N O consumption is OC-limited and predicted these denitrifier-targeted additions would lead to enhanced N O consumption and increased nosZ gene abundance. We incubated diverse soils in the laboratory and performed a N O isotope pool dilution assay to disentangle microbial N O emissions from consumption using laser-based spectroscopy. We found that amending soils with OC increased gross N O consumption in six of eight soils tested. Furthermore, three of eight soils showed Increased N O Consumption and Decreased N O Emissions (ICDE), a phenomenon we introduce in this study as an N O management ideal. All three ICDE soils had low soil OC content, suggesting ICDE is a response to relaxed C-limitation wherein C additions promote soil anoxia, consequently stimulating the reduction of N O via denitrification. We suggest, generally, OC additions to low OC soils will reduce N O emissions via ICDE. Future studies should prioritize methodical assessment of different, specific, OC-additions to determine which additions show ICDE in different soils.
一氧化二氮(N2O)是一种强大的温室气体,其增温潜能是二氧化碳的约 300 倍。然而,由于控制 N2O 排放的微生物和环境控制因素难以管理,其向大气中的排放基本上未得到控制。微生物过程 N2O 消耗是唯一已知的从土壤孔隙中去除 N2O 的生物途径,因此可以减少 N2O 排放。因此,通过添加有机碳(OC)来增加土壤中 N2O 消耗的方法逐渐受到关注。然而,不同 OC 添加对 N2O 排放的响应不一致,并且不清楚较低的 N2O 排放是由于消耗增加、产生减少还是两者兼而有之。需要简化和系统的研究来评估不同 OC 添加对 N2O 消耗的效果。我们的目的是通过用更直接可被反硝化菌利用的 OC 化合物(琥珀酸盐、醋酸盐、丙酸盐)来处理土壤,从而改变 N2O 的消耗。我们假设 N2O 消耗受 OC 限制,并预测这些针对反硝化菌的添加将导致 N2O 消耗增加和 nosZ 基因丰度增加。我们在实验室中培养了不同的土壤,并进行了 N2O 同位素库稀释测定,使用基于激光的光谱技术来区分微生物 N2O 排放和消耗。我们发现,在测试的 8 种土壤中的 6 种中,用 OC 处理土壤会增加总 N2O 消耗。此外,8 种土壤中有 3 种显示出 N2O 消耗增加和排放减少(ICDE),这是我们在本研究中引入的一种 N2O 管理理想状态。这 3 种 ICDE 土壤的土壤 OC 含量都较低,这表明 ICDE 是对 C 限制放松的反应,其中 OC 添加会导致土壤缺氧,从而通过反硝化作用刺激 N2O 的减少。我们建议,一般来说,向低 OC 土壤中添加 OC 将通过 ICDE 减少 N2O 排放。未来的研究应该优先对不同的、具体的 OC 添加进行系统评估,以确定哪些添加在不同的土壤中表现出 ICDE。