DISSERTATION RESEARCH: Dynamics of labile organic matter fractions in arctic soils

论文研究：北极土壤中不稳定有机物组分的动态

• 批准号: 0909747
• 负责人: John Moore
• 金额: $ 1.32万
• 依托单位: Colorado State University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2009
• 资助国家: 美国
• 起止时间: 2009-09-01 至 2011-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0909747&HistoricalAwards=false
• 关键词: DISSERTATION; RESEARCH; Dynamics; labile; organic

The proposed doctoral dissertation research will determine the extent to which soil aggregates, a foundation of soils, provide stabilization for soil organic matter (SOM) in the Arctic. Warming has been linked to changes in carbon cycling in the Arctic. Cold temperatures and anoxic conditions inhibit microbial activity and reduce decomposition, resulting in an accumulation of carbon-rich organic matter, straining an already nitrogen-limited system. Nutrient additions have changed the plant community and depleted soil carbon; however, mechanisms behind carbon loss are not understood. It is not known which OM fractions are most susceptible to degradation in Arctic soils, and 2) where are they located within the soil matrix. These factors are important to understanding mechanisms behind carbon loss in Arctic soils, which may be due, in part, to shifts in the physical stability of soil aggregates. In other words, soils with greater proportions of macroaggregates contain more carbon.Soils have been collected from long-term nutrient addition experiments at the Arctic LTER site on the Alaskan North Slope, and were separated into four size classes of aggregates. These aggregates will be separated into sub-structural elements as well as free OM, which will reveal if SOM is protected within aggregates and which fractions are susceptible to degradation. The project will also link current conceptual models of soil carbon stabilization to the Arctic. The graduate student will interact with the K-12 community by providing research opportunities for teachers through existing workshops, internships, and a Teacher-in-Residence program.

拟议的博士论文研究将确定土壤团聚体（土壤的基础）在多大程度上为北极的土壤有机质（SOM）提供稳定作用。 变暖与北极碳循环的变化有关。低温和缺氧条件抑制微生物活动并减少分解，导致富含碳的有机物积累，使本已有限的氮系统变得紧张。养分的添加改变了植物群落并消耗了土壤碳；然而，碳损失背后的机制尚不清楚。目前尚不清楚哪些 OM 组分最容易在北极土壤中降解，2) 它们位于土壤基质中的什么位置。这些因素对于理解北极土壤碳流失背后的机制非常重要，这可能部分归因于土壤团聚体物理稳定性的变化。 换句话说，具有较大比例的大团聚体的土壤含有更多的碳。土壤是从阿拉斯加北坡北极 LTER 站点的长期养分添加实验中收集的，并分为四个尺寸等级的团聚体。 这些聚集体将被分为子结构元素和游离 OM，这将揭示 SOM 是否在聚集体中受到保护以及哪些部分容易降解。该项目还将当前土壤碳稳定的概念模型与北极联系起来。研究生将通过现有的研讨会、实习和驻校教师计划为教师提供研究机会，从而与 K-12 社区进行互动。