Collaborative Research: An Integrated Study of the Fractionation of Natural Dissolved Organic Matter Upon Sorption to Mineral Surfaces

合作研究：天然溶解有机物在矿物表面吸附后分馏的综合研究

• 批准号: 9628166
• 负责人: Yu-Ping Chin
• 金额: $ 6.01万
• 依托单位: Ohio State University Research Foundation -DO NOT USE
• 依托单位国家: 美国
• 项目类别: Continuing Grant
• 财政年份: 1996
• 资助国家: 美国
• 起止时间: 1996-09-01 至 2000-08-31
• 项目状态: 已结题
• 来源: https://www.nsf.gov/awardsearch/showAward?AWD_ID=9628166&HistoricalAwards=false
• 关键词: Collaborative; Research; Integrated; Study; Fractionation

9628166 Chin Natural organic matter (NOM) is an important component of soils, streams, lakes, ground waters, and estuarine waters, and it plays a key role in such diverse environmental phenomena as mineral growth and dissolution, cycling of trace metals, and the global biogeochemical C budget. Perhaps most importantly, NOM plays a crucial, though complex, role in the transport of organic and inorganic pollutants through porous media. On the one hand, NOM that is bound to mineral surfaces may remove trace metals, nonpolar organic compounds (NOCs ) and other pollutants from the water column. On the other hand, NOM that remains free or in colloidal form within the water column may increase the mobility of pollutants. Hence, understanding and quantifying the bulk partitioning of NOM between solid and dissolved phases is fundamental to a wide range of pollutant transport phenomena. Moreover, because NOM consists of a variety of hydrophobic and hydrophilic molecules with variable structure, functionality, and reactivity, we need to understand not only how NOM partitions but also how it fractionates upon sorption to mineral surfaces. For example, preferential sorption of the more hydrophobic components may increase the retardation of NOCs through porous media. Numerous field and laboratory studies have suggested that NOM fractionates upon sorption, and provided clues to fractionation processes. Nevertheless, many questions remain regarding the effects of NOM composition, solution characteristics, mineral surface properties and kinetic considerations on fractionation. Additionally, little is known about the effects of mineral dissolution, metal complexation, and NOM coagulation on apparent fractionation. Finally, much of our current understanding of fractionation is based on largely indirect evidence. For example, although observed kinetic effects on fractionation have been attributed by some to changes in conformations of sorbed NOM molecules, this hypothesis has not been tes ted directly. To better understand NOM fractionation processes, we propose a 3-year interdisciplinary research effort combining field sampling at a carefully chosen freshwater wetland watershed, McDonalds Branch basin in the New Jersey Pinelands, with newly developed molecular-level methodologies, to study NOM sorption and fractionation in a far more direct manner than previously has been possible. NOM samples will be collected from surface waters, soils, and shallow and deep ground waters in carefully documented recharge and discharge zones. Fractionation on sorption of McDonalds Branch and standard NOM samples will be quantified by characterizing solutions prior to and following adsorption, using a combination of analytical techniques, including: 13C NMR and 1H NMR; UV-Vis, fluorescence, and attenuated fourier transform infra-red (ATR-FTIR) spectroscopies; high pressure size exclusion chromatography (HPSEC); total organic carbon analysis (TOC); vapor pressure osmometry; potentiometric titration's; and elemental analysis. Scanning-tunneling and atomic-force microscopy (STM and AFM), including the new tapping mode AFM, will be used to determine the structure of sorbed organic molecules, and the role of structural changes in sorption and fractionation. High pressure liquid chromatogrphy (HPLC) and AA will be used to study oxide dissolution and NOM-metal binding phenomena. Surface FTIR will assist in deterring sorption mechanisms, and how they influence fractionation. We believe that this project is fundamental to many areas of water quality research, and that we have chosen a true end-member natural laboratory watershed to conduct the field investigation. The combination of state-of-the-art laboratory techniques listed above will allow us to tackle this problem in a far more quantitative, mechanistric manner than previously has been possible. Over the course of this research, new techniques of metal-complexation analysis will be refined, new methods of STM/AFM imaging of sorbed organic molecules will be furthered, and a new approach to integrating laboratory and field investigations of NOM structure, composition, and reactivity will be fostered. The proposed research will lay a strong foundation for a broad spectrum of additional research. For example, the approach may be expanded to encompass sampling at a greater diversity of watershed types, with different NOM characteristics. We anticipate that this research will enable a wide range of future studies of how NOM fractionation influences the transport of hydrophobic and hydrophilic pollutants. Finally, given the importance of freshwater wetlands, and the rapidity with which they are disappearing from our landscape, we feel that investigations involving NOM evolution in wetlands are crucial to further our understanding of such complex but fragile ecosystems.

天然有机质（NOM）是土壤、河流、湖泊、地下水和河口水体的重要组成部分，在矿物生长和溶解、微量金属循环、全球生物地球化学碳收支等多种环境现象中起着关键作用。也许最重要的是，NOM在有机和无机污染物通过多孔介质的运输中起着至关重要的作用，尽管它很复杂。一方面，与矿物表面结合的NOM可以去除水柱中的微量金属、非极性有机化合物（NOCs）和其他污染物。另一方面，在水柱内保持游离或胶体形式的NOM可能会增加污染物的流动性。因此，理解和量化NOM在固相和溶相之间的大块分配是广泛的污染物输送现象的基础。此外，由于NOM由多种具有可变结构、功能和反应性的疏水和亲水分子组成，我们不仅需要了解NOM是如何分区的，还需要了解它在吸附到矿物表面时是如何分选的。例如，疏水组分的优先吸附可能会增加noc通过多孔介质的缓凝性。许多现场和实验室研究表明，NOM在吸附过程中会发生分馏，并为分馏过程提供了线索。然而，关于NOM组成、溶液特性、矿物表面性质和动力学因素对分馏的影响仍存在许多问题。此外，对矿物溶解、金属络合和NOM混凝对表观分馏的影响知之甚少。最后，我们目前对分馏的理解很大程度上是基于间接证据。例如，虽然观察到的对分馏的动力学影响被一些人归因于吸附的NOM分子构象的变化，但这一假设尚未得到直接验证。为了更好地了解NOM的分离过程，我们提出了一项为期3年的跨学科研究工作，结合在精心选择的淡水湿地流域（新泽西州松林麦当劳分支盆地）进行实地采样，并采用新开发的分子水平方法，以比以前更直接的方式研究NOM的吸附和分离。NOM样品将从地表水、土壤以及仔细记录的补给和排放区的浅层和深层地下水中收集。麦当劳分支和标准NOM样品的吸附分馏法将通过吸附前后溶液的表征来定量，使用多种分析技术，包括：13C NMR和1H NMR；紫外-可见、荧光和衰减傅立叶变换红外光谱（ATR-FTIR）高压阻粒径色谱法；总有机碳分析；蒸汽压渗透法；电位滴定;元素分析。扫描隧道显微镜和原子力显微镜（STM和AFM），包括新的攻丝模式AFM，将用于确定吸附有机分子的结构，以及结构变化在吸附和分馏中的作用。高压液相色谱（HPLC）和AA将用于研究氧化物溶解和无机金属结合现象。表面FTIR将有助于阻止吸附机制，以及它们如何影响分馏。我们认为这个项目是许多水质研究领域的基础，我们选择了一个真正的末端自然实验室流域进行实地调查。上面列出的最先进的实验室技术的结合将使我们能够以比以前更定量、更机械的方式解决这个问题。在本研究的过程中，将完善金属络合分析的新技术，进一步发展吸附有机分子的STM/AFM成像的新方法，并培养一种将实验室和现场研究结合起来的新方法。拟议的研究将为广泛的其他研究奠定坚实的基础。例如，该方法可以扩大，以包括在具有不同NOM特征的更多样化的流域类型上进行采样。我们预计，这项研究将使未来更广泛地研究NOM分离如何影响疏水和亲水污染物的运输。最后，考虑到淡水湿地的重要性，以及它们从我们的景观中消失的速度，我们认为涉及湿地中NOM进化的研究对于进一步了解这种复杂而脆弱的生态系统至关重要。