Collaborative LTREB Renewal: Long-Term Ecosystem Response to Chronic Atmospheric Nitrate Deposition

LTREB 协作更新：生态系统对慢性大气硝酸盐沉积的长期响应

• 批准号: 1252841
• 负责人: Donald Zak
• 金额: $ 17.98万
• 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: 2013
• 资助国家: 美国
• 起止时间: 2013-09-01 至 2018-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=1252841&HistoricalAwards=false
• 关键词: Collaborative; LTREB; Renewal; Long; Term

As the Earth's climate warms over the next century, ecosystems throughout the northern hemisphere will be exposed to elevated rates of atmospheric nitrogen (N) deposition. Understanding this complex environmental change lies at the heart of our ability to anticipate the degree to which forests will sequester human-produced carbon dioxide from the atmosphere. An interdisciplinary team of scientists will investigate the interaction between climate warming and simulated atmospheric N deposition using a long-term, regional-based, field experiment located in a sugar maple-dominated forest ecosystem common over eastern North America. During the past 18 years, simulated atmospheric nitrogen deposition at rates expected to occur by 2050 have increased tree growth and slowed the decay of dead leaves and roots, increasing the amount of carbon stored in this wide-spread ecosystem. However, it is uncertain whether carbon storage will attain a higher equilibrium over the long-term as atmospheric nitrogen deposition increases or whether expected warming will counteract this effect. The proposed research will quantify the amounts of carbon stored in overstory trees, forest floor and soil over the next decade, allowing this team of scientists to test hypotheses regarding the interaction of climate warming and atmospheric nitrogen deposition on ecosystem carbon sequestration.Using NSF support, this team will continue conducting the annual Global Change Teachers Institute. Through lectures and field-based learning, middle and high school teachers will continue to develop an understanding of the causes and ecological impacts of global environmental change, thereby bringing this information into science curricula.

随着下个世纪地球气候变暖，整个北方的生态系统将暴露于大气氮（N）沉积速率的升高。 理解这种复杂的环境变化是我们预测森林将在多大程度上从大气中吸收人类产生的二氧化碳的能力的核心。 一个跨学科的科学家团队将研究气候变暖和模拟的大气氮沉降之间的相互作用，使用长期的，基于区域的，位于北美东部常见的糖枫主导的森林生态系统的实地实验。 在过去的18年里，模拟的大气氮沉降速度预计将在2050年发生，这增加了树木的生长，减缓了枯叶和树根的腐烂，增加了这个广泛分布的生态系统中储存的碳量。 然而，随着大气氮沉降的增加，碳储存是否会在长期内达到更高的平衡，或者预期的变暖是否会抵消这种影响，这是不确定的。 这项研究将量化未来十年中储存在上层树木，森林地面和土壤中的碳量，使这个科学家团队能够测试气候变暖和大气氮沉降对生态系统碳封存的相互作用的假设。在NSF的支持下，这个团队将继续进行年度全球变化教师研究所。 通过讲座和实地学习，初中和高中教师将继续了解全球环境变化的原因和生态影响，从而将这一信息纳入科学课程。