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Absorption and fluorescence of hydrophobic components of dissolved organic matter in several Karelian lakes with stratified structures

机译:具有分层结构的若干卡尔湖中溶解有机物疏水成分的吸收和荧光

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Hydrophobic components of cromophoric dissolved organic matter (CDOM) extracted from water samples and sediments taken in several relic basins located on Karelian shoreline of the White Sea were analyzed using spectroscopic techniques. Those water reservoirs exist at various stages of isolation from the White Sea and represent complex stratified systems of fresh and marine water layers not completely mixing trough the year. Basins separating from the White Sea are the unique natural objects for investigations of properties CDOM, its transformation in the process of turning the marine ecosystem into freshwater environment. CDOM occurring in all types of natural water represents a significant reservoir of organic carbon and plays a key role in the carbon cycle on the Earth. However, aquatic CDOM and nonliving organic matter in sediments from relic separating basins still have not been studied. The target of this work was to study absorption and fluorescence spectra of hydrophobic components of aquatic CDOM from different water depth and sediments in several separated basins of the Kandalaksha Gulf of the White Sea located near the N.A. Pertsov White Sea Biological Station.
机译:使用光谱技术分析了从水样中提取的克罗姆莫溶解有机物质(CDOM)的疏水组分,从而在几种遗物盆地中采取的几种遗物盆地进行分析。这些水库存在于来自白海的各个隔离阶段,并代表复杂的新鲜和海洋水层的分层系统,而不是完全混合槽。与白海分离的盆地是属性CDOM调查的独特自然对象,它在将海洋生态系统转化为淡水环境的过程中的转变。在所有类型的天然水中发生的CDOM代表了有机碳的重要储层,并在地球上的碳循环中起着关键作用。然而,仍未研究遗传分离盆地沉积物中的水生CDom和非生物有机物。这项工作的目标是研究来自位于N.A.Pertsov白海生物站附近的白海的康达岛海湾的几个分离盆地的不同水深和沉积物的水生CDOM疏水分量的吸收和荧光光谱。

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