Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature Conditions

The crystallization behaviour of jarosite and schwertmannite has been studied by precipitation-aging experiments performed using different parent-solution concentrations at acidic conditions and ambient temperature. Schwertmannite exhibits low crystallinity and is the only mineral identified during...

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Main Authors: Amalia Jiménez, Ana Hernández, Manuel Prieto
Format: Article
Language:English
Published: MDPI AG 2019-01-01
Series:Minerals
Subjects:
Online Access:http://www.mdpi.com/2075-163X/9/1/27
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spelling doaj-40652e9803b440b1a35f4244b082b1482020-11-24T21:35:55ZengMDPI AGMinerals2075-163X2019-01-01912710.3390/min9010027min9010027Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature ConditionsAmalia Jiménez0Ana Hernández1Manuel Prieto2Department of Geology, University of Oviedo, 33005 Oviedo, SpainDepartment of Geology, University of Oviedo, 33005 Oviedo, SpainDepartment of Geology, University of Oviedo, 33005 Oviedo, SpainThe crystallization behaviour of jarosite and schwertmannite has been studied by precipitation-aging experiments performed using different parent-solution concentrations at acidic conditions and ambient temperature. Schwertmannite exhibits low crystallinity and is the only mineral identified during low-concentration (LC) experiments. However, in high-concentration (HC) experiments, a relatively rapid Ostwald ripening process leads to the transformation of schwertmannite into natrojarosite. The presence of sodium modifies the morphology and stability of the obtained phases. TEM observations reveal that schwertmannite particles consist of disoriented nanodomains (~6 nm) spread in an amorphous mass. In contrast, natrojarosite particles exhibit a single-domain, highly crystalline core, with the crystallinity decreasing from core to rim. The thermal behaviour of these phases depends on both their composition and their degree of crystallinity. TG and DTG analyses show that, below 500 °C, the amount of structural water is clearly higher in schwertmannite than in natrojarosite. The present results highlight the role of the ripening processes in epigenetic conditions and could be important in interpreting the formation of jarosite in Earth and Martian surface environments.http://www.mdpi.com/2075-163X/9/1/27jarositeschwertmannitemorphologyprecipitationdecomposition behavioursupergene
collection DOAJ
language English
format Article
sources DOAJ
author Amalia Jiménez
Ana Hernández
Manuel Prieto
spellingShingle Amalia Jiménez
Ana Hernández
Manuel Prieto
Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature Conditions
Minerals
jarosite
schwertmannite
morphology
precipitation
decomposition behaviour
supergene
author_facet Amalia Jiménez
Ana Hernández
Manuel Prieto
author_sort Amalia Jiménez
title Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature Conditions
title_short Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature Conditions
title_full Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature Conditions
title_fullStr Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature Conditions
title_full_unstemmed Crystallization Behaviour of Iron-Hydroxide Sulphates by Aging under Ambient Temperature Conditions
title_sort crystallization behaviour of iron-hydroxide sulphates by aging under ambient temperature conditions
publisher MDPI AG
series Minerals
issn 2075-163X
publishDate 2019-01-01
description The crystallization behaviour of jarosite and schwertmannite has been studied by precipitation-aging experiments performed using different parent-solution concentrations at acidic conditions and ambient temperature. Schwertmannite exhibits low crystallinity and is the only mineral identified during low-concentration (LC) experiments. However, in high-concentration (HC) experiments, a relatively rapid Ostwald ripening process leads to the transformation of schwertmannite into natrojarosite. The presence of sodium modifies the morphology and stability of the obtained phases. TEM observations reveal that schwertmannite particles consist of disoriented nanodomains (~6 nm) spread in an amorphous mass. In contrast, natrojarosite particles exhibit a single-domain, highly crystalline core, with the crystallinity decreasing from core to rim. The thermal behaviour of these phases depends on both their composition and their degree of crystallinity. TG and DTG analyses show that, below 500 °C, the amount of structural water is clearly higher in schwertmannite than in natrojarosite. The present results highlight the role of the ripening processes in epigenetic conditions and could be important in interpreting the formation of jarosite in Earth and Martian surface environments.
topic jarosite
schwertmannite
morphology
precipitation
decomposition behaviour
supergene
url http://www.mdpi.com/2075-163X/9/1/27
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AT anahernandez crystallizationbehaviourofironhydroxidesulphatesbyagingunderambienttemperatureconditions
AT manuelprieto crystallizationbehaviourofironhydroxidesulphatesbyagingunderambienttemperatureconditions
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