Colloid stability of iron compounds in groundwater of Western Siberia

10Citations
Citations of this article
8Readers
Mendeley users who have this article in their library.

This article is free to access.

Abstract

The paper reports on experimental modeling of the colloid system composition in natural groundwater. Iron hydroxide is found to be the main component of natural colloid systems. It is shown that silicon compounds and dissolved organic substances (DOS) stabilize iron hydroxide (III), forming a stable colloid system, and preclude coagulation. The presented results suggest that CaCl2 and AlCl3 electrolytes affect the coagulation stability of synthesized model colloid solutions. © 2014 Shiyan et al.; licensee Springer.

Cite

CITATION STYLE

APA

Shiyan, L. N., Tropina, E. A., Machekhina, K. I., Gryaznova, E. N., & An, V. V. (2014). Colloid stability of iron compounds in groundwater of Western Siberia. SpringerPlus, 3(1), 1–7. https://doi.org/10.1186/2193-1801-3-260

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free