Collaborative Research: In Situ Examination of Hydrogen Peroxide Sources and Sinks in a Slightly Alkaline Stream

合作研究：微碱性流中过氧化氢源和汇的原位检查

• 批准号: 0720172
• 负责人: Durelle Scott
• 金额: $ 11.58万
• 依托单位: University of Nebraska-Lincoln
• 依托单位国家: 美国
• 项目类别: Standard Grant
• 财政年份: 2007
• 资助国家: 美国
• 起止时间: 2007-09-01 至 2009-03-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=0720172&HistoricalAwards=false
• 关键词: Collaborative; Research; Situ; Examination; Hydrogen

Photochemically produced hydrogen peroxide (H2O2) is ubiquitous in sunlit freshwater and may play a number of important biogeochemical roles. Of particular interest is that H2O2 may be the most important source of hydroxyl radical (OH) in surface waters via reduction of H2O2 by Fe(II). Oxidation by hydroxyl radical is an effective mechanism for converting refractory organic compounds, including contaminants and natural organic matter, to CO2 and microbial substrates. It is still unclear whether the sources and sinks of H2O2 identified in lakes and marine systems are the most important controls on H2O2 in streams. The role of reduction of H2O2, in particular, remains unexplored in all but very acidic streams. In addition, preliminary modeling of a theoretical reach-scale stream tracer injection experiment suggests that H2-18O2, used in conjunction with a conservative tracer, could be uniquely useful for addressing one of the main problems of modeling biogeochemical processes in streams (e.g. nitrogen cycling, contaminant biodegradation, sorption): the need for a tracer that can distinguish flowpaths involving transient storage in surface water pools from flowpaths through the hyporheic zone (subsurface). However, H2-18O2's application as a tracer requires a better understanding of the controls on H2-18O2 decomposition rates in surface and subsurface waters. The overall goal of the proposed work is to conduct the first comprehensive study of hydrogen peroxide cycling in a natural stream chosen to be broadly representative of agricultural headwater streams in the central U.S. Measurement of the fate of natural H2O2 and an injected isotope-labeled H2-18O2 tracer in mesocosms placed directly into stream sediments will be used to test our current understanding of H2O2 sources and sinks in sunlit stream water and the underlying sediment. Our results will show whether hydroxyl radical production from hydrogen peroxide could be a dominant mechanism of indirect photolysis of organic contaminants and natural organic matter in streams. Photolysis of natural organic matter is of significance because it produces bioavailable carbon substrates as well as carbon dioxide, and is thought to be an important control on ecosystem-scale carbon cycling. Our work could also lay the groundwork for developing methods to accelerate Fenton's reaction in systems such as agricultural headwaters, for the purpose of decreasing concentrations of contaminants such as atrazine. Finally, if hydrogen peroxide turns out to be a good tracer for distinguishing between surface and subsurface storage in streams, the proposed work will contribute to the development of better models of biogeochemical processes such as nitrogen cycling and biodegradation of contaminants in these environments. The proposed work is a joint effort between a new investigator (Durelle Scott) and a mid-level female scientist (Bettina Voelker), and will support one graduate student and one undergraduate researcher each at the Colorado School of Mines and at the University of Nebraska.

光化学产生的过氧化氢(H_2O_2)普遍存在于阳光充足的淡水中，并可能发挥许多重要的生物地球化学作用。特别令人感兴趣的是，通过Fe(II)还原H_2O_2，H_2O_2可能是地表水中羟基自由基(OH)的最重要来源。羟基自由基氧化是将难降解有机化合物(包括污染物和天然有机物)转化为二氧化碳和微生物底物的有效机制。目前尚不清楚湖泊和海洋系统中发现的过氧化氢的源和汇是否是对溪流中过氧化氢的最重要控制。尤其是在酸性很强的河流中，过氧化氢的还原作用仍未得到探索。此外，对理论范围内的河流示踪剂注入实验进行的初步模拟表明，H2-18O2与一种保守的示踪剂结合使用，对于解决对河流中的生物地球化学过程进行模拟的主要问题之一(例如氮循环、污染物生物降解、吸附)可能是唯一有用的：需要一种示踪剂，能够区分涉及地表水池中瞬时储存的流动路径和通过次表层(次表层)的流动路径。然而，H_2-18O_2的S示踪剂的应用需要更好地了解地表和次表层水中H_2-18O_2分解速率的控制。拟议工作的总体目标是对过氧化氢在天然溪流中的循环进行第一次全面研究，该天然溪流被选为广泛代表美国中部的农业水源溪流。测量天然过氧化氢的去向以及直接放置到水系沉积物中的注入同位素标记的H2-18O2示踪剂将用于测试我们目前对阳光充足的溪水和底层沉积物中的过氧化氢来源和汇的理解。我们的结果将表明，过氧化氢产生羟基自由基是否可能是河流中有机污染物和天然有机物间接光解的主要机制。天然有机物的光解具有重要意义，因为它产生了可生物利用的碳基质和二氧化碳，并被认为是生态系统规模碳循环的重要控制因素。我们的工作还可以为开发在农业源头等系统中加速Fenton反应的方法奠定基础，以降低阿特拉津等污染物的浓度。最后，如果过氧化氢被证明是区分河流表层和地下储存的良好示踪剂，拟议的工作将有助于开发更好的生物地球化学过程模型，例如这些环境中的氮循环和污染物的生物降解。这项拟议的工作是一名新的研究员(杜蕾尔·斯科特)和一名中级女科学家(贝蒂娜·沃克尔)的共同努力，将支持科罗拉多矿业学院和内布拉斯加大学的一名研究生和一名本科生研究员。