Dissolution of magnetite in acidic oxalate solutions

Taxiarchou, M; Panias, D; Douni, I; Paspaliaris, I; Kontopoulos, A

dc.contributor.author	Taxiarchou, M	en
dc.contributor.author	Panias, D	en
dc.contributor.author	Douni, I	en
dc.contributor.author	Paspaliaris, I	en
dc.contributor.author	Kontopoulos, A	en
dc.date.accessioned	2014-03-01T01:13:42Z
dc.date.available	2014-03-01T01:13:42Z
dc.date.issued	1998	en
dc.identifier.issn	0371-9553	en
dc.identifier.uri	https://dspace.lib.ntua.gr/xmlui/handle/123456789/12664
dc.relation.uri	http://www.scopus.com/inward/record.url?eid=2-s2.0-0038477615&partnerID=40&md5=6eaa6ccdcdaaf8659249e090ab955e88	en
dc.subject.classification	Metallurgy & Metallurgical Engineering	en
dc.subject.classification	Mineralogy	en
dc.subject.classification	Mining & Mineral Processing	en
dc.subject.other	OXALIC-ACID	en
dc.subject.other	IRON-OXIDES	en
dc.subject.other	HEMATITE	en
dc.subject.other	ION	en
dc.title	Dissolution of magnetite in acidic oxalate solutions	en
heal.type	journalArticle	en
heal.language	English	en
heal.publicationDate	1998	en
heal.abstract	The dissolution of magnetite in acidic oxalate solutions has been studied under various experimental conditions. The effects of temperature, pH, oxalate and ferrous ion concentration in solution were extensively examined. The dissolution of the magnetite is highly dependent on temperature and the pH of the solution, but is practically independent of the oxalate concentration. The addition of ferrous ions in the solution has a positive effect on the dissolution rate, especially at lower temperatures and higher pH values. © The Institution of Mining and Metallurgy 1998.	en
heal.publisher	INST MINING METALLURGY	en
heal.journalName	Transactions of the Institutions of Mining and Metallurgy, Section C: Mineral Processing and Extractive Metallurgy	en
dc.identifier.isi	ISI:000078280000005	en
dc.identifier.volume	107	en
dc.identifier.issue	JAN/APR	en
dc.identifier.spage	C37	en
dc.identifier.epage	C41	en