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首页> 外文期刊>Journal of Geochemical Exploration: Journal of the Association of Exploration Geochemists >A method for the definition of the carbon oxidation number in the gases dissolved in waters and the redox variations using an elemental analyser (FlashEA 1112). Preliminary data from a stratified lake
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A method for the definition of the carbon oxidation number in the gases dissolved in waters and the redox variations using an elemental analyser (FlashEA 1112). Preliminary data from a stratified lake

机译:一种使用元素分析仪(FlashEA 1112)定义溶于水的气体中的碳氧化数和氧化还原变化的方法。分层湖的初步数据

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摘要

Obtaining meaningful redox potential determinations is questionable in disequilibrium solutions, like surface waters and groundwater. However, identifying redox processes in a natural ecosystem is a key factor to characterize the chemical quality and, consequently, the sustainability of that environment. To do that, the determination of an exact redox potential is not needed and on many cases it is more important to describe how and if the redox state of a system changes. In particular, the redox status of aqueous systems is assigned based on analysis of samples for redox-sensitive compounds. In general, these analyses do not include measurements of gases dissolved in the waters. Here, we present an innovative method to underline in an easy way changes in redox state of a system using the elemental composition (C, H, S) measured in the headspace gas after the equilibration with water phase. The results allow denning the empirical formula of the gas, the mean number of oxidation of the carbon and the molar ratio between C:H:S. The method is applied to investigate the redox condition in a stratified lake, San Rocchino (Northern Tuscany, Italy) using an instrument (Thermo Scientific FlashEA 1112) equipped for headspace gas analysis. Samples of waters and dissolved gases were collected at five different depths along a vertical profile. Such analytical system is used to determine the mean oxidation number of the carbon gaseous phase in the headspace, which allows distinguishing relatively oxidizing from relatively reducing condition. Further information on the redox state is reached considering the molar ratio C/H and C/S. This innovative method is simple and rapid, and the instrument is robust and it needs low maintenance. Moreover, it could be applied to other research and exploratory fields, such as geothermic and volcanic monitoring, polluted aquifer and contaminated sites.
机译:在地表水和地下水等不平衡溶液中,获得有意义的氧化还原电势测定存在疑问。但是,识别自然生态系统中的氧化还原过程是表征化学质量以及因此环境可持续性的关键因素。为此,不需要确定确切的氧化还原电位,并且在许多情况下,描述系统的氧化还原状态如何以及是否发生变化更为重要。具体而言,基于对氧化还原敏感化合物的样品分析来分配水性系统的氧化还原状态。通常,这些分析不包括溶解在水中的气体的测量值。在这里,我们提出了一种创新的方法,该方法使用水平衡后在顶空气体中测得的元素组成(C,H,S)以简单的方式强调系统氧化还原状态的变化。结果可以确定气体的经验公式,碳的平均氧化数和C:H:S之间的摩尔比。该方法通过配备用于顶空气体分析的仪器(Thermo Scientific FlashEA 1112)用于研究分层湖San Rocchino(意大利北托斯卡纳)中的氧化还原条件。在垂直剖面的五个不同深度处收集了水和溶解气体的样品。这种分析系统用于确定顶部空间中碳气相的平均氧化数,这可以区分相对氧化条件和相对还原条件。考虑到摩尔比C / H和C / S,获得了有关氧化还原状态的更多信息。这种创新的方法既简单又快速,并且仪器坚固耐用且维护成本低。此外,它还可以应用于其他研究和探索领域,例如地热和火山监测,受污染的含水层和受污染的地点。

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