Synthesis-identification of hematite and bentonite-hematite (b-h) system

dc.contributor.author	Dimirkou, A	en
dc.contributor.author	Ioannou, A	en
dc.contributor.author	Kalliannou, Ch	en
dc.date.accessioned	2014-06-06T06:43:04Z
dc.date.available	2014-06-06T06:43:04Z
dc.date.issued	1996	en
dc.identifier.issn	00103624	en
dc.identifier.uri	http://62.217.125.90/xmlui/handle/123456789/985
dc.relation.uri	http://www.scopus.com/inward/record.url?eid=2-s2.0-0030483043&partnerID=40&md5=b346bf37132689fddac98697e1eecc7a	en
dc.title	Synthesis-identification of hematite and bentonite-hematite (b-h) system	en
heal.type	journalArticle	en
heal.publicationDate	1996	en
heal.abstract	Iron and aluminium are common in soils as the weathering product of soil-forming minerals. Iron occurs as coating on silicate clay minerals and significantly influence the physico-chemical properties of clay mineral. In this study hydrogen saturated bentonite was coated with 16 mequivalents of iron as hematite/g of clay in suspension of pH 6.0. The influence of hematite on the physico-chemical properties of bentonite was studied on the synthetic hematite-bentonite (h-b) system, by X-ray, NMR, FT-IR spectroscopy, specific surface area, magnesium exchange capacity (Mg.E.C.) of hematite, hydrogen-saturated bentonite and bentonite-hematite (b-h) system. Copyright © 1996 by Marcel Dekker, Inc.	en
heal.journalName	Communications in Soil Science and Plant Analysis	en
dc.identifier.issue	5-8	en
dc.identifier.volume	27	en
dc.identifier.spage	1055	en
dc.identifier.epage	1069	en