dc.contributor.author |
Moirou, A |
en |
dc.contributor.author |
CHRISTIDIS, G |
en |
dc.contributor.author |
PASPALIARIS, I |
en |
dc.date.accessioned |
2014-03-01T01:49:27Z |
|
dc.date.available |
2014-03-01T01:49:27Z |
|
dc.date.issued |
2000 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/25785 |
|
dc.subject |
Acid Mine Drainage |
en |
dc.subject |
Cation Exchange Capacity |
en |
dc.subject |
Fourier Transform Infrared |
en |
dc.subject |
Free Energy |
en |
dc.subject |
Heavy Metal |
en |
dc.subject |
Ion Exchange |
en |
dc.subject |
Water Loss |
en |
dc.subject |
X Ray Diffraction |
en |
dc.title |
Ion Exchange of Zeolite Na-Pc with Pb2+, Zn2+, and Ni2+ Ions |
en |
heal.type |
journalArticle |
en |
heal.identifier.primary |
10.1346/CCMN.2000.0480509 |
en |
heal.identifier.secondary |
http://dx.doi.org/10.1346/CCMN.2000.0480509 |
en |
heal.publicationDate |
2000 |
en |
heal.abstract |
This paper examines the ion-exchange properties of synthetic zeolite Na-P0, which was pro- duced from perlite-waste fines and has a SiO2:A1203 ratio of 4.45:1 and a cation-exchange capacity (CEC) of 3.95 meq g ~. Although equilibrium is attained rapidly for all three metals, exchange is incomplete, with At(max) (maximum equilibrium fraction of the metal in the zeolite) being 0.95 for |
en |
heal.journalName |
Clays and Clay Minerals |
en |
dc.identifier.doi |
10.1346/CCMN.2000.0480509 |
en |