Hydrologic influences on soil trace gas fluxes across complex terrain

水文对复杂地形土壤痕量气体通量的影响

• 批准号: 1114392
• 负责人: John Dore
• 金额: $ 32.39万
• 依托单位: Montana State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-09-15 至 2015-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1114392&HistoricalAwards=false
• 关键词: Hydrologic; influences; soil; trace; gas

The physical and microbiological processes governing nitrous oxide and methane fluxes to and from soil are highly variable in space and time and are controlled, directly and indirectly, by soil moisture content, which is largely governed by hydrologic processes. The goal of this project is to evaluate the impact of hydrological dynamics, in other words catchment scale water redistribution, on soil-atmosphere trace gas fluxes across a mountain landscape. A combination of nitrous oxide, methane and carbon dioxide flux determinations, soil water content and redistribution measurements, chemical assays of potential reactants, digital terrain analyses and hydrological monitoring will be used to assess the environmental controls on trace gas flux spatial and temporal dynamics in a forested Montana watershed. Relationships between trace gas sources and sinks and hydrologic properties in montane ecosystems will be uncovered. This project will test an existing topography analysis framework that uses hydrologic property based landscape units (slope position in relation to streams, aspect, drainage area, and so on) to translate point-scale trace gas measurements to the landscape scale. The project builds upon prior and ongoing NSF-funded research on hydrologic controls on carbon dioxide flux in montane ecosystems and uses existing field infrastructure and technical resources to advantage.Nitrous oxide and methane are, like carbon dioxide, radiatively active trace gases that contribute significantly to global warming. It is known that the montane forested ecosystems of North America are a significant carbon sink. However, the net impact of montane forested ecosystems on atmospheric warming potential is unclear because the net fluxes of other trace gases are not known. This is, in part, because effective approaches to translate point trace gas flux measurements to whole landscapes have yet to be developed for such systems. The approach that will be developed and tested in this project has the potential to improve net greenhouse gas emission estimates for montane forested ecosystems at the landscape scale ? the spatial scale considered in policymaking regarding greenhouse gas emissions. In addition, this research project will provide land-air carbon dioxide, nitrous oxide and methane flux data at multiple space and time scales that will be useful to scientists interested in benchmarking models. Hands-on field training opportunities in hydrology and biogeochemistry will be provided for graduate and undergraduate students from Montana State University.

控制一氧化二氮和甲烷流入和流出土壤的物理和微生物过程在空间和时间上变化很大，并直接或间接地受土壤含水量的控制，而土壤含水量主要受水文过程的控制。 该项目的目标是评估水文动力学的影响，换句话说，流域尺度的水再分配，对土壤-大气痕量气体通量在山区景观。 一氧化二氮，甲烷和二氧化碳通量测定，土壤水分含量和再分布测量，化学分析的潜在反应物，数字地形分析和水文监测相结合，将被用来评估环境控制微量气体通量的空间和时间动态在森林覆盖的蒙大拿州流域。 将揭示山地生态系统中痕量气体源和汇与水文特性之间的关系。 本项目将测试现有的地形分析框架，该框架使用基于水文属性的景观单元（与溪流、坡向、流域等相关的坡度位置），将点尺度痕量气体测量转换为景观尺度。该项目建立在国家科学基金会资助的关于山区生态系统中二氧化碳通量的水文控制的先前和正在进行的研究的基础上，并利用现有的实地基础设施和技术资源，一氧化二氮和甲烷与二氧化碳一样，是具有辐射活性的痕量气体，对全球变暖有重大影响。众所周知，北美山地森林生态系统是一个重要的碳汇。 然而，山地森林生态系统对大气升温潜能值的净影响尚不清楚，因为不知道其他痕量气体的净通量。这是，部分原因是，有效的方法来转换点示踪气体通量测量到整个景观尚未开发这样的系统。将在本项目中开发和测试的方法有可能在景观尺度上改进山地森林生态系统的净温室气体排放量估计？温室气体排放决策中考虑的空间尺度。此外，该研究项目将提供多个空间和时间尺度的陆地-空气二氧化碳、一氧化二氮和甲烷通量数据，这将有助于对基准模型感兴趣的科学家。将为蒙大拿州立大学的研究生和本科生提供水文学和地球化学方面的实地实践培训机会。