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dc.contributor.authorRao, A.
dc.contributor.authorVásquez-Quitral, P.
dc.contributor.authorFernández, M.
dc.contributor.authorBerg, J.
dc.contributor.authorSánchez, M.
dc.contributor.authorDrechsler, M.
dc.contributor.authorNeira-Carrillo, A.
dc.contributor.authorArias, J.
dc.contributor.authorGebauer, Denis
dc.contributor.authorCölfen, H.
dc.date.accessioned2017-04-28T13:56:53Z
dc.date.available2017-04-28T13:56:53Z
dc.date.created2017-04-28T09:06:17Z
dc.date.issued2016
dc.identifier.citationRao, A. and Vásquez-Quitral, P. and Fernández, M. and Berg, J. and Sánchez, M. and Drechsler, M. and Neira-Carrillo, A. et al. 2016. PH-Dependent Schemes of Calcium Carbonate Formation in the Presence of Alginates. Crystal Growth & Design. 16 (3): pp. 1349-1359.
dc.identifier.urihttp://hdl.handle.net/20.500.11937/51923
dc.identifier.doi10.1021/acs.cgd.5b01488
dc.description.abstract

© 2016 American Chemical Society.From recent studies on bone and shell formation, the importance of polysaccharides in biomineralization processes is gradually being recognized. Through ion-complexation and self-assembly properties, such macromolecules have remarkable effects on mineralization. However, their influences on the different regimes of crystallization including the interactions with precursor species are unclear. The present study therefore addresses calcium carbonate mineralization in the presence of alginates, a class of linear copolymeric saccharides composed of ß-1,4 linked d-mannuronic and l-guluronic acid. During mineralization, this biopolymer is found to exert pH-dependent control over mineralization pathways in terms of the stability of prenucleation clusters, inhibitory effect toward nucleation and initially formed postnucleation products. Remarkably in the presence of this macromolecular additive, either amorphous or crystalline vaterite particles can be selectively nucleated in a pH-dependent manner. This is validated by electron microscopy wherein vaterite particles are intimately associated with alginate assemblies after nucleation at pH 9.75. At lower pH, aggregates of amorphous particles are formed. Thus, in addition to the general focus on biochemical properties of additives, solution pH, a physiologically fundamental parameter significantly alters the scheme of mineralization.

dc.publisherAmerican Chemical Society
dc.titlePH-Dependent Schemes of Calcium Carbonate Formation in the Presence of Alginates
dc.typeJournal Article
dcterms.source.volume16
dcterms.source.number3
dcterms.source.startPage1349
dcterms.source.endPage1359
dcterms.source.issn1528-7483
dcterms.source.titleCrystal Growth & Design
curtin.departmentDepartment of Chemistry
curtin.accessStatusFulltext not available


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