dc.contributor.author |
Xenidis, A |
en |
dc.contributor.author |
Kontopoulos, A |
en |
dc.date.accessioned |
2014-03-01T02:47:50Z |
|
dc.date.available |
2014-03-01T02:47:50Z |
|
dc.date.issued |
1988 |
en |
dc.identifier.uri |
https://dspace.lib.ntua.gr/xmlui/handle/123456789/33387 |
|
dc.relation.uri |
http://www.scopus.com/inward/record.url?eid=2-s2.0-0023845019&partnerID=40&md5=98d05b0c0c00c2b5bb1648f5b40d2b28 |
en |
dc.subject.other |
IRON ORE TREATMENT - Solvent Extraction |
en |
dc.subject.other |
STATISTICAL METHODS |
en |
dc.subject.other |
IRON COMPLEXES |
en |
dc.subject.other |
ORGANIC PHASE |
en |
dc.subject.other |
NICKEL ORE TREATMENT |
en |
dc.title |
DETERMINATION OF THE ORGANIC PHASE COMPLEXES FORMED DURING THE EXTRACTION OF Fe(III) FROM Fe-Ni-Co SULFATE SOLUTIONS WITH D2EHPA. |
en |
heal.type |
conferenceItem |
en |
heal.publicationDate |
1988 |
en |
heal.abstract |
The classical slope analysis and a statistical technique were used in order to determine the iron complexes formed in the organic phase during the extraction of Fe(III) from Fe-Ni-Co sulfate solutions with Di-(2-ethylhexyl) phosphoric acid (D2EHPA) in kerosene. Equilibrium constants for the extraction based on these complexes were also calculated. The complexes determined were of the general form (Fe(OH)//3// minus //nR//n does not equal sHR)//x, where n varied between 1 and 2. 5 and s between 0 and 3, and both were found to be decreasing as the iron loading in the organic phase increased. Values of 1, 2 and 3 were generally found for x, indicating that the complexes were monomers, dimers and trimers. |
en |
heal.publisher |
Soc of Mining Engineers of AIME, Littleton, CO, USA |
en |
heal.journalName |
Preprint - Society of Mining Engineers of AIME |
en |