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首页> 外文期刊>Marine Chemistry >Spatially resolved capture of hydrogen sulfide from the water column and sedimentary pore waters for abundance and stable isotopic analysis
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Spatially resolved capture of hydrogen sulfide from the water column and sedimentary pore waters for abundance and stable isotopic analysis

机译:从水柱和沉积孔隙水中空间分辨地捕获硫化氢,以进行丰度和稳定的同位素分析

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摘要

Sulfur cycling is ubiquitous in sedimentary environments, where it plays a major role in mediating carbon remineralization and impacts both local and global redox budgets. Microbial sulfur cycling is dominated by metabolic activity that either produces (e.g., sulfate reduction, disproportionation) or consumes (sulfide oxidation) hydrogen sulfide (H2S). As such, improved constraints on the production, distribution, and consumption of H2S in the natural environment will increase our understanding of microbial sulfur cycling. These different microbial sulfur metabolisms are additionally associated with particular stable isotopic fractionations. Coupling measurements of the isotopic composition of the sulfide with its distribution can provide additional information about environmental conditions and microbial ecology. Here we investigate the kinetics of sulfide capture on photographic films as a way to document the spatial distribution of sulfide in complex natural environments as well as for in situ capture of H2S for subsequent stable isotopic analysis. Laboratory experiments and timed field deployments demonstrate the ability to infer ambient sulfide abundances from the yield of sulfide on the films. This captured sulfide preserves the isotopic composition of the ambient sulfide, offset to slightly lower delta S-34 values by similar to 1.2 +/- 0.5 parts per thousand associated with the diffusion of sulfide into the film and subsequent reaction with silver to form Ag2S precipitates. The resulting data enable the exploration of cm-scale lateral heterogeneity that complement most geochemical profiles using traditional techniques in natural environments. Because these films can easily be deployed over a large spatial area, they are also ideal for real-time assessment of the spatial and temporal dynamics of a site during initial reconnaissance and for integration over long timescales to capture ephemeral processes.
机译:硫循环在沉积环境中无处不在,在那里它在介导碳再矿化中起主要作用,并影响本地和全球的氧化还原预算。微生物的硫循环以代谢活动为主导,该代谢活动产生(例如,硫酸盐还原,歧化)或消耗(硫化物氧化)硫化氢(H 2 S)。因此,在自然环境中对H2S的生产,分布和消耗的改善的约束将增加我们对微生物硫循环的理解。这些不同的微生物硫代谢还与特定的稳定同位素分馏有关。硫化物同位素组成及其分布的耦合测量可以提供有关环境条件和微生物生态学的其他信息。在这里,我们研究了在摄影胶片上捕获硫化物的动力学,以此作为记录硫化物在复杂自然环境中的空间分布以及就地捕获H2S进行后续稳定同位素分析的一种方法。实验室实验和定时现场部署证明了可以从薄膜上的硫化物产率推断周围硫化物丰度的能力。捕获的硫化物保留了周围硫化物的同位素组成,与硫化物扩散到薄膜中以及随后与银反应形成Ag2S沉淀物有关,偏移了稍低的δS-34值,接近每千分之1.2 +/- 0.5份。 。所得数据使得能够探索厘米级的横向异质性,从而在自然环境中使用传统技术对大多数地球化学剖面进行补充。由于这些胶片可以轻松地部署在较大的空间区域上,因此,它们对于在初始侦察期间实时评估站点的时空动态以及长时间集成以捕获短暂过程也是理想的选择。

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