Collaborative Research: Linking the chemical structure of black carbon to its biological degradation and transport dynamics in a northern temperate forest soil

合作研究：将黑碳的化学结构与其在北温带森林土壤中的生物降解和运输动态联系起来

• 批准号: 1127250
• 负责人: Knute Nadelhoffer
• 金额: $ 37.2万
• 依托单位: Regents of the University of Michigan - Ann Arbor
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2011
• 资助国家: 美国
• 起止时间: 2011-10-01 至 2017-09-30
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1127250&HistoricalAwards=false
• 关键词: Collaborative; Research; Linking; chemical; structure

Fire is a major controller of carbon (C) cycling in terrestrial ecosystems, by converting plant biomass to atmospheric CO2 and by contributing incompletely combusted biomass or "black carbon" (BC) to soils. The scientific understanding of the short- and long-term fates of BC in terrestrial ecosystems is incomplete, and a critical knowledge gap exists in our understanding of the fate of BC in the environment. BC, may significantly affect soil C stocks and rates of CO2 exchange of forests with the atmosphere. Through integrated field and laboratory studies, this research will improve understanding of fundamental biological, chemical and physical controls on BC degradation and transport processes in a northern forest soil. This research will link the charring temperature of BC materials to their chemical and physical structures and their resulting decay rates, activity of the main decomposers, enzyme activities, transport dynamics, and stabilization mechanisms in soil. The proposed experimental approach will use stable isotope-enriched (13C and 15N) BC materials produced over a range of temperatures (200 to 600ºC) and its precursor wood of jack pine, a fire-prone and abundant tree species in eastern North America, to elucidate the structures of BC materials and track the multiple fates of these materials when added to soil. This approach will permit a direct assessment of the biological turnover in soil using advanced molecular and spectroscopic techniques. This work will provide the first look at the roles of specific groups of microorganisms and soil fauna involved in the decomposition and movement of BC and wood in soils. To test the effects of plant species on BC chemical and physical structures, highly 13C- and 15N-enriched BC from red maple will be compared with the jack pine. Resulting data and knowledge will contribute to ongoing efforts to predict terrestrial C cycling, and will inform ecosystem and climate modelers and also land use managers.Most existing climate models predict that temperate and boreal forests will experience greater fire frequency under a warmer future climate, thereby increasing BC (black carbon) contributions to soils. In addition, substantial BC (or "biochar") production is expected from the energy industry. This research will characterize the key biological, chemical and physical controls on BC and wood degradation processes in soils, thereby substantially increasing our understanding of the mechanisms involved in C stabilization and sequestration in fire-prone forests. This will provide information needed to improve ecosystem and global C cycling models and their uses in characterizing forest soil C sinks in present and future climates. This research will inform a broad scientific, educational, land manager and agency community interested in ecosystem function, productivity and sustainability. In addition, the project will include involvement of a science teacher from a New York City minority-serving high school and the NY GLOBE Metro program to integrate applied environmental ecosystem science and geosciences into the high school biology and earth science curricula. Purdue University, in collaboration with Leech Lake Tribal College (LLTC), will integrate this research into an ethnobiology curriculum focusing on both modern principles of chemistry and Native American utilization of BC. The University of Michigan Biological Station and City University of New York will each train a postdoctoral researcher within the scope of this project and will use the field study as a resource for on-site university courses, its site-based undergraduate and graduate student research programs, and its science outreach.

火是陆地生态系统中碳循环的主要控制者，它将植物生物质转化为大气中的CO2，并向土壤中提供不完全燃烧的生物质或“黑碳”。对BC在陆地生态系统中的短期和长期命运的科学理解是不完整的，我们对BC在环境中的命运的理解存在着重要的知识差距。 BC，可能会显着影响土壤碳储量和森林与大气的CO2交换率。通过综合实地和实验室研究，这项研究将提高基本的生物，化学和物理控制BC的降解和运输过程中的北方森林土壤的理解。这项研究将把BC材料的炭化温度与它们的化学和物理结构及其产生的衰变率、主要分解剂的活性、酶活性、运输动力学和土壤中的稳定机制联系起来。拟议的实验方法将使用在一系列温度（200至600ºC）下产生的稳定同位素富集（13 C和15 N）BC材料及其前体杰克松木材，杰克松是北美东部一种易着火和丰富的树种，以阐明BC材料的结构，并跟踪这些材料在添加到土壤中时的多种命运。这种方法将允许使用先进的分子和光谱技术直接评估土壤中的生物周转。这项工作将提供第一次看到的作用，特定群体的微生物和土壤动物参与分解和移动的BC和木材在土壤中。为了测试植物种类对BC化学和物理结构的影响，将来自红枫的高度13 C-和15 N富集的BC与短叶松进行比较。由此产生的数据和知识将有助于正在进行的努力，以预测陆地碳循环，并将告知生态系统和气候建模和土地利用manager.Most现有的气候模型预测，温带和寒带森林将经历更大的火灾频率在未来气候变暖，从而增加BC（黑碳）的贡献土壤。此外，预计能源工业将大量生产BC（或“生物炭”）。这项研究将表征关键的生物，化学和物理控制BC和木材在土壤中的降解过程，从而大大增加我们的理解的机制，涉及在易发生火灾的森林中的碳稳定和封存。这将提供所需的信息，以改善生态系统和全球碳循环模型及其在表征森林土壤碳汇在当前和未来的气候中的用途。这项研究将为对生态系统功能、生产力和可持续性感兴趣的广大科学、教育、土地管理者和机构社区提供信息。此外，该项目还将邀请来自纽约市一所为少数族裔服务的高中的一名科学教师和纽约地球仪Metro计划参与，将应用环境生态系统科学和地球科学整合到高中生物学和地球科学课程中。普渡大学与利奇湖部落学院（LLTC）合作，将把这项研究纳入民族生物学课程，重点是现代化学原理和美洲原住民对BC的利用。密歇根大学生物站和纽约将在本项目范围内分别培训一名博士后研究人员，并将实地研究作为现场大学课程、基于现场的本科生和研究生研究计划及其科学推广的资源。