Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates

Structural characteristics of iron (III) oxide/silica co-precipitates were investigated. The association between these materials is relevant to practically all natural aqueous systems due to the prevalence of iron and silicon in the earth’s crust. Crystallographic information is very difficult to ob...

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Main Authors: Dyer, Laurence, Chapman, K., English, P., Saunders, M., Richmond, William
Format: Journal Article
Published: Mineralogical Society of America 2012
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/32419
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author Dyer, Laurence
Chapman, K.
English, P.
Saunders, M.
Richmond, William
author_facet Dyer, Laurence
Chapman, K.
English, P.
Saunders, M.
Richmond, William
author_sort Dyer, Laurence
building Curtin Institutional Repository
collection Online Access
description Structural characteristics of iron (III) oxide/silica co-precipitates were investigated. The association between these materials is relevant to practically all natural aqueous systems due to the prevalence of iron and silicon in the earth’s crust. Crystallographic information is very difficult to obtain from these precipitates due to the nanocrystalline nature of ferrihydrite and the amorphous structure of precipitated silica. Several previously undetermined key insights were gained into the structure of iron oxide/silica co-precipitates through this examination. The distribution of iron and silicon throughout co-precipitate particles is illustrated along with the influence of their association. Evidence to the governing factor behind differences in apparent crystallinity is also presented. This information culminates in the formulation of a precipitation pathway, displaying the formation of the co-precipitates.
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institution Curtin University Malaysia
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publishDate 2012
publisher Mineralogical Society of America
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spelling curtin-20.500.11937-324192017-10-02T02:28:10Z Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates Dyer, Laurence Chapman, K. English, P. Saunders, M. Richmond, William pair distribution function silica co-precipitation Ferrihydrite Structural characteristics of iron (III) oxide/silica co-precipitates were investigated. The association between these materials is relevant to practically all natural aqueous systems due to the prevalence of iron and silicon in the earth’s crust. Crystallographic information is very difficult to obtain from these precipitates due to the nanocrystalline nature of ferrihydrite and the amorphous structure of precipitated silica. Several previously undetermined key insights were gained into the structure of iron oxide/silica co-precipitates through this examination. The distribution of iron and silicon throughout co-precipitate particles is illustrated along with the influence of their association. Evidence to the governing factor behind differences in apparent crystallinity is also presented. This information culminates in the formulation of a precipitation pathway, displaying the formation of the co-precipitates. 2012 Journal Article http://hdl.handle.net/20.500.11937/32419 10.2138/am.2011.3874 Mineralogical Society of America restricted
spellingShingle pair distribution function
silica
co-precipitation
Ferrihydrite
Dyer, Laurence
Chapman, K.
English, P.
Saunders, M.
Richmond, William
Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates
title Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates
title_full Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates
title_fullStr Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates
title_full_unstemmed Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates
title_short Insights into the crystal and aggregate structure of Fe3+ oxide/silica co-precipitates
title_sort insights into the crystal and aggregate structure of fe3+ oxide/silica co-precipitates
topic pair distribution function
silica
co-precipitation
Ferrihydrite
url http://hdl.handle.net/20.500.11937/32419