Collaborative Research: Controls on the Isotopic Composition of Fixed CO2 and Ecosystem-Respired CO2 in Southeastern Pine Forests

合作研究：东南松林固定二氧化碳和生态系统呼吸二氧化碳同位素组成的控制

• 批准号: 0343604
• 负责人: Jeffrey Chanton
• 金额: $ 37.34万
• 依托单位: Florida State University
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 2004
• 资助国家: 美国
• 起止时间: 2004-04-01 至 2008-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0343604&HistoricalAwards=false
• 关键词: Collaborative; Research; Controls; Isotopic; Composition

Ever since scientists linked human production of carbon dioxide with global warming, they have sought to quantify how much impact humans have had on climate. Half the CO2 produced by humans-mainly from the burning of fossil fuels-remains in the atmosphere. The other "missing half" is either adsorbed by the oceans or taken up by terrestrial plants during photosynthesis. Knowing how much goes where is a crucial link in understanding how human activity affects global climate and the global carbon cycle. A useful marker to trace the destination of CO2 is the ratio of 13C to 12C in CO2 in the air. Land plants preferentially take up 12C, enriching the air in 13C. The oceans don't discriminate when they take up CO2. So by measuring the ratio of 13C to 12C, scientists can tell whether the CO2 is going into land plants or into the ocean. But there is variation in how much 13C to 12C land plants take up, so the models that predict where human-produced CO2 winds up can have significant error. To limit the error, and develop better estimates of the fate of CO2, a new study will be conducted to examine southern pine forests, one of the largest carbon sinks in North America. The study will look at how climate variability affects the 13C/12C ratio of the CO2 that plants absorb and release during their respiration. The result may yield a significant recalculation of how important land plants are as a "sink" for human-produced CO2.The study will look at carbon isotope composition in leaf waxes and respired CO2. This will be used to improve estimates of the distribution and magnitude of the terrestrial carbon sink, a step in further understanding the importance of land plants as absorbers of CO2 produced by humans.

自从科学家将人类产生的二氧化碳与全球变暖联系起来以来，他们一直试图量化人类对气候的影响。人类产生的二氧化碳中有一半主要来自化石燃料的燃烧留在了大气中。另一个“缺失的一半”要么被海洋吸收，要么在光合作用过程中被陆地植物吸收。了解有多少流向何处是了解人类活动如何影响全球气候和全球碳循环的关键环节。 追踪CO2目的地的有用标记是空气中CO2中13 C与12 C的比率。陆地植物优先吸收12 C，使空气中的13 C富集。 海洋在吸收二氧化碳的时候并不歧视。 因此，通过测量13 C与12 C的比例，科学家们可以判断二氧化碳是进入陆地植物还是进入海洋。 但是，陆地植物吸收13 C到12 C的量存在差异，因此预测人类产生的二氧化碳最终去向的模型可能会有很大的误差。为了限制误差，并更好地估计二氧化碳的命运，将进行一项新的研究，以检查南部松树林，北美最大的碳汇之一。该研究将研究气候变化如何影响植物在呼吸过程中吸收和释放的CO2的13 C/12 C比率。这一结果可能会对陆地植物作为人类产生的二氧化碳的“汇”的重要性进行重大的重新计算。这项研究将着眼于叶蜡和呼吸的二氧化碳中的碳同位素组成。这将用于改进对陆地碳汇分布和规模的估计，这是进一步了解陆地植物作为人类产生的二氧化碳吸收剂的重要性的一步。