THE SILT SOLUTIONS OF THE FRESH WATER BODIES IN THE FLAT TERRAIN OF UKRAINE

The poral sediment solutions of fresh water basins are considered as a separate type of natural water that forms a transition zone between surface water and under ground water. They are characterized by reduction conditions, a specific chemical content and an increased matter of some components (hyd...

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Збережено в:
Бібліографічні деталі
Дата:2015
Автор: Sukhorebriy, A.A.
Формат: Стаття
Мова:Українська
Опубліковано: Institute of Geological Sciences, NAS of Ukraine 2015
Теми:
Онлайн доступ:http://geojournal.igs-nas.org.ua/article/view/139063
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Назва журналу:Geological journal

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Geological journal
Опис
Резюме:The poral sediment solutions of fresh water basins are considered as a separate type of natural water that forms a transition zone between surface water and under ground water. They are characterized by reduction conditions, a specific chemical content and an increased matter of some components (hydrogen sulfide, ammonium, ferrum). There are the repfesented results of the fult-scale study on the poral sediment solutions of some fresh water bodies of Ukraine (rivers, lakes, reservoirs).