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Spectromicroscopy Mapping of Colloidal/Particulate Organic Matter in Lake Brienz, Switzerland

机译:瑞士布里恩茨湖的胶体/颗粒有机物的光谱显微镜图

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Transmission electron microscopy (TEM), soft X-ray scanning transmission X-ray microscopy (STXM), and μ-FTIR spectromicroscopy were used to map colloidal/ particulate material in an ultra-oligotrophic lake, Lake Brienz, Switzerland, with a special focus on organic functionality. Within the statistical margin of error and the uncertainties arising from the representativeness of the results, the research reveals that organic material was associated with potassium-rich inorganic colloids present in surface and deep water (depths of 1 and 100 m, respectively), which indicates a vertical transfer of aggregates by sedimentation.Pure organic colloids could only be detected in surface waters. In addition, correlation map analysis of synchrotron-based μ-FTIR and carbon K-edge STXM spectromicroscopic data using spectra from the Lutschine and Aare Rivers as target spectra revealed spectral similarities with organic components from both tributary rivers in deeper regions (100 m) of the lake. The results prove that STXM and μ-FTIR can characterize colloidal and paniculate organic material in low organic carbon systems.
机译:透射电子显微镜(TEM),软X射线扫描透射X射线显微镜(STXM)和μ-FTIR光谱显微镜用于绘制瑞士布里恩茨湖的超贫营养湖中的胶体/颗粒物质图有机功能。在统计误差范围内以及结果的代表性所带来的不确定性范围内,研究表明,有机物质与地表水和深水中(分别为1和100 m的深度)中存在的富钾无机胶体有关。纯的有机胶体只能在地表水中被检测到。另外,基于同步加速器的μ-FTIR和碳K边缘STXM光谱数据的相关图分析,使用Lutschine和Aare河的光谱作为目标光谱,揭示了与深部地区(100 m)的两条支流河的有机成分的光谱相似性。那个湖。结果证明,STXM和μ-FTIR可以表征低有机碳体系中的胶体和颗粒状有机物质。

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