The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns

<p>Storage caverns are increasingly located in heterogeneous salt deposits and filled with various fluids. The knowledge of phase behaviour in heterogeneous systems of salt, liquid and gas and the requirements for reliable analytical techniques is, therefore, of growing interest. A method t...

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Main Authors: B. Strauch, M. Zimmer, A. Zirkler, S. Höntzsch, A. M. Schleicher
Format: Article
Language:English
Published: Copernicus Publications 2018-08-01
Series:Advances in Geosciences
Online Access:https://www.adv-geosci.net/45/227/2018/adgeo-45-227-2018.pdf
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spelling doaj-9c12bd137e49433986eb4cacb7e057912020-11-25T00:40:28ZengCopernicus PublicationsAdvances in Geosciences1680-73401680-73592018-08-014522723310.5194/adgeo-45-227-2018The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical cavernsB. Strauch0M. Zimmer1A. Zirkler2S. Höntzsch3A. M. Schleicher4GFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyGFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, GermanyK+S Aktiengesellschaft, Bertha-von-Suttner-Straße 7, 34131 Kassel, GermanyK+S Windsor Salt Ltd., 30 Prospect Avenue, Windsor, ON, CanadaGFZ German Research Centre for Geosciences, Telegrafenberg, 14473 Potsdam, Germany<p>Storage caverns are increasingly located in heterogeneous salt deposits and filled with various fluids. The knowledge of phase behaviour in heterogeneous systems of salt, liquid and gas and the requirements for reliable analytical techniques is, therefore, of growing interest. A method that allows for the continuous monitoring of mineral compositions at distinct humidity and gas content using XRD measurements is presented here. Various saliniferous mineral compositions have been investigated in pure CO<sub>2</sub>, N<sub>2</sub> or CH<sub>4</sub> atmospheres with varying humidity in a closed chamber. All mineral compositions experience dissolution and/or mineral conversion reaction accompanied by volume loss. Dissolution-recrystallization reactions of complex mineral assemblages involving halite, sylvite, kieserite, carnallite and kainite were observed using this method. For carnallite-rich mineral assemblages, the mineral conversion from carnallite to sylvite was observed when humidity exceeded 50&thinsp;%&thinsp;RH. In the presence of CO<sub>2</sub>, acidification of the aqueous phase occurs which enhances the dissolution rate and reaction kinetics.</p>https://www.adv-geosci.net/45/227/2018/adgeo-45-227-2018.pdf
collection DOAJ
language English
format Article
sources DOAJ
author B. Strauch
M. Zimmer
A. Zirkler
S. Höntzsch
A. M. Schleicher
spellingShingle B. Strauch
M. Zimmer
A. Zirkler
S. Höntzsch
A. M. Schleicher
The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns
Advances in Geosciences
author_facet B. Strauch
M. Zimmer
A. Zirkler
S. Höntzsch
A. M. Schleicher
author_sort B. Strauch
title The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns
title_short The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns
title_full The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns
title_fullStr The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns
title_full_unstemmed The influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns
title_sort influence of gas and humidity on the mineralogy of various salt compositions – implications for natural and technical caverns
publisher Copernicus Publications
series Advances in Geosciences
issn 1680-7340
1680-7359
publishDate 2018-08-01
description <p>Storage caverns are increasingly located in heterogeneous salt deposits and filled with various fluids. The knowledge of phase behaviour in heterogeneous systems of salt, liquid and gas and the requirements for reliable analytical techniques is, therefore, of growing interest. A method that allows for the continuous monitoring of mineral compositions at distinct humidity and gas content using XRD measurements is presented here. Various saliniferous mineral compositions have been investigated in pure CO<sub>2</sub>, N<sub>2</sub> or CH<sub>4</sub> atmospheres with varying humidity in a closed chamber. All mineral compositions experience dissolution and/or mineral conversion reaction accompanied by volume loss. Dissolution-recrystallization reactions of complex mineral assemblages involving halite, sylvite, kieserite, carnallite and kainite were observed using this method. For carnallite-rich mineral assemblages, the mineral conversion from carnallite to sylvite was observed when humidity exceeded 50&thinsp;%&thinsp;RH. In the presence of CO<sub>2</sub>, acidification of the aqueous phase occurs which enhances the dissolution rate and reaction kinetics.</p>
url https://www.adv-geosci.net/45/227/2018/adgeo-45-227-2018.pdf
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