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Fluorides in Surface and Underground Waters of Southeastern Coast and in Parts of Navigable Channels of Azov Sea

机译:东南海岸地下水域和地下水的氟化物以及亚佐夫海的通航渠道

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The concentration of fluorides in the surface and underground waters of the studied areas of the Azov sea does not exceed the maximum permissible concentrations. In the direction of the Eastern region of the Taganrog Bay → Central area →West Bay area → East Azov Sea, the concentration of fluorides in the water of the coastal zone increases. In the same direction, their concentration in underground aquifers increases. It is shown that the tributaries may he one of the main sources of fluoride inflow into the coastal zone of the sea, while the role of groundwater is secondary. In the areas of dredging and dumping soil, a slight excess of fluoride concentrations was revealed, compared with their concentrations in the water of the background sites, which may indicate the local influence of the functioning of navigable channels on the formation of the concentration of fluorides in the sea water.
机译:Azov海的研究区域的表面和地下水中的氟化物浓度不超过最大允许浓度。在Taganrog湾的东部地区的方向→中央区→西湾区→东艾佐海,沿海地区水中的氟化物浓度增加。在同一方向,他们在地下含水层中的浓度增加。结果表明,支流可以将氟化物流入的主要来源之一进入大海沿海地区,而地下水的作用是次要的。在疏浚和倾倒土壤的区域中,揭示了略微过量的氟化物浓度,与其在背景部位的水中的浓度相比,这可能表明可导航通道功能对氟化物浓度的形成的局部影响在海水中。

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