DISSERTATION RESEARCH: Will Ecosystem Recovery From Acid Precipitation Jeopardize Soil Carbon Storage?

论文研究：酸沉淀中的生态系统恢复是否会危及土壤碳储存？

• 批准号: 1701920
• 负责人: Emily Bernhardt
• 金额: $ 2.05万
• 依托单位: Duke University
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2017
• 资助国家: 美国
• 起止时间: 2017-06-01 至 2019-05-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1701920&HistoricalAwards=false
• 关键词: DISSERTATION; RESEARCH; Will; Ecosystem; Recovery

While acid rain has significantly decreased across the United States over the past thirty years, many forested ecosystems are only beginning to recover, with full recovery expected to take decades to centuries. Recent evidence suggests that, while forests will grow better as they recover from acid rain, the soil in forests may also lose a substantial amount of the carbon and nutrients. In this Doctoral Dissertation Improvement Grant (DDIG) project, the student is working to understand the mechanisms by which forest recovery from acid rain may increase the vulnerability of soil organic matter that contains soil carbon and nutrients. The investigators are particularly interested in understanding how rising soil acidity and calcium content may alter the solubility and lability (decomposability) of soil carbon. The project will test this by studying the physical, chemical and microbiological properties of soils in response to changing acidity. This research is necessary to predict future trends of forest growth and carbon storage throughout the Northeastern United States. To facilitate and inform evidence-based management decisions, this research will be incorporated into a web-based application that is geared toward letting the general public explore and understand long-term ecological data. To examine the mechanisms by which ecosystem recovery from acid rain may alter soil organic matter (SOM) dynamics, the researchers will perform a long-term greenhouse mesocosm experiment. Soils will be collected from Hubbard Brook Experimental Forest, a Northeastern hardwood forest that is impacted by acid rain. The team will reconstruct soil mesocosms by horizon, both with and without sugar maple seedlings, a co-dominant species in the forest where the soils were obtained. Soils will be experimentally amended to increase soil pH and Ca in a fully factorial design. The student will measure SOM solubility and microbial respiration of SOM to determine the responses of SOM pools to these treatments. In addition, researchers will measure proximate mechanisms of SOM dynamics (Aluminum-SOM complexation, soil exoenzyme activity, bacterial:fungal microbial biomass ratios, etc.) that may drive changes to SOM solubility and microbial respiration. These measurements will be compared between planted and unplanted mesocosm to identify possible plant-mediated effects on SOM dynamics.

虽然过去三十年来美国各地的酸雨显着减少，但许多森林生态系统才刚刚开始恢复，预计完全恢复需要几十年到几个世纪的时间。最近的证据表明，虽然森林从酸雨中恢复后会生长得更好，但森林中的土壤也可能会损失大量的碳和养分。 在这个博士论文改进资助（DDIG）项目中，学生正在努力了解酸雨森林恢复可能增加含有土壤碳和养分的土壤有机质的脆弱性的机制。研究人员特别感兴趣的是了解土壤酸度和钙含量的上升如何改变土壤碳的溶解度和不稳定性（可分解性）。 该项目将通过研究土壤对酸度变化的物理、化学和微生物特性来测试这一点。 这项研究对于预测整个美国东北部森林生长和碳储存的未来趋势是必要的。为了促进和告知基于证据的管理决策，这项研究将被纳入一个基于网络的应用程序，旨在让公众探索和理解长期生态数据。为了研究酸雨生态系统恢复可能改变土壤有机质（SOM）动态的机制，研究人员将进行长期温室中生态实验。土壤将从哈伯德布鲁克实验森林收集，这是一个受酸雨影响的东北阔叶林。该团队将按地平线重建土壤中生态系统，包括有或没有糖枫树苗，糖枫树苗是获得土壤的森林中的共同优势物种。将通过全因子设计对土壤进行实验性修改，以提高土壤 pH 值和钙含量。学生将测量 SOM 溶解度和 SOM 微生物呼吸，以确定 SOM 库对这些处理的反应。此外，研究人员还将测量 SOM 动力学的近似机制（铝-SOM 络合、土壤外酶活性、细菌：真菌微生物生物量比率等），这些机制可能会驱动 SOM 溶解度和微生物呼吸的变化。这些测量结果将在种植和未种植的中生态系统之间进行比较，以确定植物介导的对 SOM 动态可能的影响。