Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquifer

Abstract Crystallization of carbonates is a key process affecting the operation of geothermal facilities and aquifer heat storage systems. The crystals formed in an aquifer heat storage test in the Upper Jurassic carbonate aquifer were investigated at injection temperatures of $$65\,^{\circ }\hbox {...

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Main Authors: Martina Ueckert, Carina Wismeth, Thomas Baumann
Format: Article
Language:English
Published: SpringerOpen 2020-02-01
Series:Geothermal Energy
Subjects:
Online Access:https://doi.org/10.1186/s40517-020-0160-5
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spelling doaj-93509a6057e344a9a8f43edef06b5ea82021-02-07T12:26:49ZengSpringerOpenGeothermal Energy2195-97062020-02-018112310.1186/s40517-020-0160-5Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquiferMartina Ueckert0Carina Wismeth1Thomas Baumann2Institute of Hydrochemistry, Technical University of MunichInstitute of Hydrochemistry, Technical University of MunichChair of Hydrogeology, Technical University of MunichAbstract Crystallization of carbonates is a key process affecting the operation of geothermal facilities and aquifer heat storage systems. The crystals formed in an aquifer heat storage test in the Upper Jurassic carbonate aquifer were investigated at injection temperatures of $$65\,^{\circ }\hbox {C}$$ 65 ∘ C to $$110\,^{\circ }\hbox {C}$$ 110 ∘ C , with varying $$\hbox {CO}_{2}$$ CO 2 partial pressures, and varying Mg/Ca ratios. Water samples were directly filtrated, and analyzed by SEM/EDX. Complementary autoclave experiments were run. In the autoclave experiments with tap water, aragonite crystals dominated at all temperatures (45–110 $$\,^{\circ }\hbox {C}$$ ∘ C ). In the autoclave experiments with ultra-pure water, calcite crystals dominated at the same temperatures. In the field test, mainly calcite crystals were found up to temperatures of $$90\,^{\circ }\hbox {C}$$ 90 ∘ C . Only at very high temperatures of $$110\,^{\circ }\hbox {C}$$ 110 ∘ C aragonite crystallization prevailed. $$\hbox {CO}_{2}$$ CO 2 partial pressure varied especially between injection and production stages. Mg/Ca ratio varied through all stages, and depended on the dissolution of the rock matrix. Together with the autoclave experiments, this study suggest that temperature and Mg/Ca ratio had no influence on the crystallization, and only supersaturation affected the $$\hbox {CaO}_{3}$$ CaO 3 polymorphs. We further assume that we produced initially injected crystals back during the following production stage. That results in the assumption that existing particles can maintain an equilibrium in the dispersion, and reduce precipitation on surfaces like pipes and heat exchangers.https://doi.org/10.1186/s40517-020-0160-5$$\hbox {CaCO}_{3}$$ CaCO 3 polymorphsCalciteAragoniteCarbonate aquiferAutoclave experiments
collection DOAJ
language English
format Article
sources DOAJ
author Martina Ueckert
Carina Wismeth
Thomas Baumann
spellingShingle Martina Ueckert
Carina Wismeth
Thomas Baumann
Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquifer
Geothermal Energy
$$\hbox {CaCO}_{3}$$ CaCO 3 polymorphs
Calcite
Aragonite
Carbonate aquifer
Autoclave experiments
author_facet Martina Ueckert
Carina Wismeth
Thomas Baumann
author_sort Martina Ueckert
title Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquifer
title_short Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquifer
title_full Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquifer
title_fullStr Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquifer
title_full_unstemmed Crystallization of calcium carbonate in a large-scale push–pull heat storage test in the Upper Jurassic carbonate aquifer
title_sort crystallization of calcium carbonate in a large-scale push–pull heat storage test in the upper jurassic carbonate aquifer
publisher SpringerOpen
series Geothermal Energy
issn 2195-9706
publishDate 2020-02-01
description Abstract Crystallization of carbonates is a key process affecting the operation of geothermal facilities and aquifer heat storage systems. The crystals formed in an aquifer heat storage test in the Upper Jurassic carbonate aquifer were investigated at injection temperatures of $$65\,^{\circ }\hbox {C}$$ 65 ∘ C to $$110\,^{\circ }\hbox {C}$$ 110 ∘ C , with varying $$\hbox {CO}_{2}$$ CO 2 partial pressures, and varying Mg/Ca ratios. Water samples were directly filtrated, and analyzed by SEM/EDX. Complementary autoclave experiments were run. In the autoclave experiments with tap water, aragonite crystals dominated at all temperatures (45–110 $$\,^{\circ }\hbox {C}$$ ∘ C ). In the autoclave experiments with ultra-pure water, calcite crystals dominated at the same temperatures. In the field test, mainly calcite crystals were found up to temperatures of $$90\,^{\circ }\hbox {C}$$ 90 ∘ C . Only at very high temperatures of $$110\,^{\circ }\hbox {C}$$ 110 ∘ C aragonite crystallization prevailed. $$\hbox {CO}_{2}$$ CO 2 partial pressure varied especially between injection and production stages. Mg/Ca ratio varied through all stages, and depended on the dissolution of the rock matrix. Together with the autoclave experiments, this study suggest that temperature and Mg/Ca ratio had no influence on the crystallization, and only supersaturation affected the $$\hbox {CaO}_{3}$$ CaO 3 polymorphs. We further assume that we produced initially injected crystals back during the following production stage. That results in the assumption that existing particles can maintain an equilibrium in the dispersion, and reduce precipitation on surfaces like pipes and heat exchangers.
topic $$\hbox {CaCO}_{3}$$ CaCO 3 polymorphs
Calcite
Aragonite
Carbonate aquifer
Autoclave experiments
url https://doi.org/10.1186/s40517-020-0160-5
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