Використання осаду сполук феруму (ІІІ) як каталізатора у процесі деферизації води

Abstract

In the sandy-clay and carbonate deposits of the upper horizons of many artesian basins where oxygen is absent, underground waters with a high concentration of total Ferum (up to 100 mg / dm 3) are formed, in which the Ferrum compounds (IIІ) predominate. The use of such water is dangerous for a person, since the excess of this element in it causes liver disease and allergic reactions.