Open Access Review Article

The Root of Silica Scale Formation and Its Remedy

Mai Al Saadi* and Naser Al Haddabi

Mechanical Engineering department, Al Musana College of Technology, Oman

Corresponding Author

Received Date: September 25, 2019;  Published Date: October 03, 2019

Abstract

Naturally, silica present in water feed in the range of 1-100 ppm. It is existed as silicic acid (H2SiO3) which is a weak acid and dissociated at or below neutral pH [1,2]. The presence of silicic acid lead to form silica colloidal in water at neutral pH. But when pH exceeds the neutral, silicic can be dissociated and form silicate anion (SiO3 2-), which can react with positive ions like calcium, magnesium, iron, manganese and aluminum to form insoluble silicates [3].

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