Ca-Zeolite and Mg-Zeolite are formed in natural hard water by exchanging Na
+ in Na-Zeolite with Ca
2+ and Mg
2+.
In this paper, the effect of these exchanged Zeolite on the deposition of particulate soil were investigated by using the artificially prepared Ca- and Mg-Zeolites from CaCl
2 and MgCl
2 solution (residual Na-Zeolite are estimated
ca. 30%).
Main results obtained are summarized as follows :
1) When Mg-Zeolite or Ca-Zeolite of the same exchange ratio was added to Ca-containinghard water, both Zeolites removed Ca
2+ ions and their removal efficiencies were in the order of Mg-Zeolite > Ca-Zeolite.
2) In aqueous Fe
2O
3 suspension (0°DH), the deposition of Fe
2O
3 on cloths depended on the kind of Zeolite, and the amount of deposition decreased in the order of Ca-Zeolite > Mg-Zeolite > Na-Zeolite.
3) In Ca-containing hard water less than 30°DH, the deposition amount of Fe
2O
3 decreased in the order of Ca-Zeolite >Mg-Zeolite >Na-Zeolite according to the kind of added Zeolite.
In Ca-containing hard water which exceeds the ion binding capacity of Na-Zeolite, the deposition of Fe
2O
3 increased remarkably.
This phenomenon suggests that the deposition of particulate soil is affected by the presence of exchanged Zeolite and the concentration of Ca
2+ ion.
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