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Boron and manganese fractions in dystrophic lake waters (Wigry National Park, NE Poland)

机译:营养不良的湖水中的硼和锰馏分(波兰东北部维格里国家公园)

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Physicochemical studies in four dystrophic lakes (Suchar Wielki, Suchar II, Suchar IV, and W?do?ek) were carried out in Wigry National Park, NE Poland. Total manganese concentrations oscillated within the range of 386.6-647.5 μg Mn dm-3, while those of soluble reactive manganese, 112.5-328.2 μg Mn dm-3. Fairly high boron contents were recorded in the studied lakes, which amounted to 0.09-2.20 mg B dm-3. The increase in dissolved reactive manganese (DRMn) and decrease in dissolved boron concentration with the lake depth were observed. Almost half (47%) of the total manganese pool was composed of dissolved reactive soluble fraction (DRMn), then dissolved organic form (DOMn, 41%), whereas the particulate fraction (PMn) made up the smallest share (12%). Microbial decomposition of lake organic matter disappears and requirements of authotrophic plankton for Mn2+ decreases when the water temperature drops, thus the fraction prevails. The following regularity was recorded in all analysed dystrophic lakes: iron concentration decreases along with the depth, hence boron content can also be observed due to precipitated borates to bottom sediments, where they are accumulated.
机译:在波兰内格里国家公园的四个营养不良湖泊(Suchar Wielki,Suchar II,Sucha IV和W?do?ek)中进行了理化研究。锰总浓度在386.6-647.5μgMn dm-3范围内波动,而可溶性反应性锰在112.5-328.2μgMn dm-3范围内波动。在所研究的湖泊中记录到相当高的硼含量,总计为0.09-2.20 mg B dm-3。观察到随着湖深,溶解性反应锰(DRMn)的增加和溶解硼浓度的降低。锰池中几乎一半(47%)由溶解性反应性可溶级分(DRMn)组成,然后是溶解有机物形式(DOMn,41%),而颗粒级分(PMn)占最小份额(12 %)。当水温下降时,湖泊有机物的微生物分解消失,对营养性浮游生物对Mn2 +的需求降低,因此占优势。在所有被分析的营养不良湖泊中记录了以下规律性:铁的浓度随着深度的增加而降低,因此,由于沉淀在底部沉积物中的硼酸盐的沉淀也可以观察到硼含量。

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