Reactivity of the calcite-water-interface, from molecular scale processes to geochemical engineering

Research output: Contribution to journalReview articleResearchpeer review

Authors

  • Frank Heberling
  • Dirk Bosbach
  • Jörg Detlef Eckhardt
  • Uwe Fischer
  • Jens Glowacky
  • Michael Haist
  • Utz Kramar
  • Steffen Loos
  • Harald S. Müller
  • Thomas Neumann
  • Christopher Pust
  • Thorsten Schäfer
  • Jan Stelling
  • Marko Ukrainczyk
  • Victor Vinograd
  • Marijan Vučak
  • Björn Winkler

External Research Organisations

  • Karlsruhe Institute of Technology (KIT)
  • Forschungszentrum Jülich
  • Rheinkalk Akdolit GmbH and Co. KG
  • Schaefer Kalk GmbH and Co. KG
  • Ruder Boskovic Institute
  • Goethe University Frankfurt
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Details

Original languageEnglish
Pages (from-to)158-190
Number of pages33
JournalApplied geochemistry
Volume45
Early online date26 Mar 2014
Publication statusPublished - Jun 2014
Externally publishedYes

Abstract

Surface reactions on calcite play an important role in geochemical and environmental systems, as well as many areas of industry. In this review, we present investigations of calcite that were performed in the frame of the joint research project "RECAWA" (reactivity of calcite-water-interfaces: molecular process understanding for technical applications). As indicated by the project title, work within the project comprised a large range of length scales. The molecular scale structure of the calcite (104)-water-interface is refined based on surface diffraction data. Structural details are related to surface charging phenomena, and a simplified basic stern surface complexation model is proposed. As an example for trace metal interactions with calcite surfaces we review and present new spectroscopic and macroscopic experimental results on Selenium interactions with calcite. Results demonstrate that selenate (SeO42-) shows no significant interaction with calcite at our experimental conditions, while selenite (SeO32-) adsorbs at the calcite surface and can be incorporated into the calcite structure. Atomistic calculations are used to assess the thermodynamics of sulfate (SO42-), selenate (SeO42-), and selenite (SeO32-) partitioning in calcite and aragonite. The results show that incorporation of these oxo-anions into the calcite structure is so highly endothermic that incorporation is practically impossible at bulk equilibrium and standard conditions. This indicates that entrapment processes are involved when coprecipitation is observed experimentally. The relevance of nano-scale surface features is addressed in an investigation of calcite growth and precipitation in the presence of phosphonates, demonstrating the influence of phosphonates on the morphology of growth spirals and macroscopic growth rates. It is investigated how physical properties of limestone containing cement suspensions may influence the workability of the cement suspensions and thus the efficacy of limestone in industrial applications. The largest scale is reached in iron filtration experiments in a water-purification-pilot-plant using limestone as filter material, which appeared to be highly effective for removing iron from drinking water. Investigations presented cover a whole series of methods to study the calcite-water-interface. Many calcite related topics are addressed, demonstrating how broad the field of calcite-water-interface research is and how manifold the applications are, for which calcite-water-interface phenomena are of major relevance.

ASJC Scopus subject areas

Cite this

Reactivity of the calcite-water-interface, from molecular scale processes to geochemical engineering. / Heberling, Frank; Bosbach, Dirk; Eckhardt, Jörg Detlef et al.
In: Applied geochemistry, Vol. 45, 06.2014, p. 158-190.

Research output: Contribution to journalReview articleResearchpeer review

Heberling, F, Bosbach, D, Eckhardt, JD, Fischer, U, Glowacky, J, Haist, M, Kramar, U, Loos, S, Müller, HS, Neumann, T, Pust, C, Schäfer, T, Stelling, J, Ukrainczyk, M, Vinograd, V, Vučak, M & Winkler, B 2014, 'Reactivity of the calcite-water-interface, from molecular scale processes to geochemical engineering', Applied geochemistry, vol. 45, pp. 158-190. https://doi.org/10.1016/j.apgeochem.2014.03.006
Heberling, F., Bosbach, D., Eckhardt, J. D., Fischer, U., Glowacky, J., Haist, M., Kramar, U., Loos, S., Müller, H. S., Neumann, T., Pust, C., Schäfer, T., Stelling, J., Ukrainczyk, M., Vinograd, V., Vučak, M., & Winkler, B. (2014). Reactivity of the calcite-water-interface, from molecular scale processes to geochemical engineering. Applied geochemistry, 45, 158-190. https://doi.org/10.1016/j.apgeochem.2014.03.006
Heberling F, Bosbach D, Eckhardt JD, Fischer U, Glowacky J, Haist M et al. Reactivity of the calcite-water-interface, from molecular scale processes to geochemical engineering. Applied geochemistry. 2014 Jun;45:158-190. Epub 2014 Mar 26. doi: 10.1016/j.apgeochem.2014.03.006
Heberling, Frank ; Bosbach, Dirk ; Eckhardt, Jörg Detlef et al. / Reactivity of the calcite-water-interface, from molecular scale processes to geochemical engineering. In: Applied geochemistry. 2014 ; Vol. 45. pp. 158-190.
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abstract = "Surface reactions on calcite play an important role in geochemical and environmental systems, as well as many areas of industry. In this review, we present investigations of calcite that were performed in the frame of the joint research project {"}RECAWA{"} (reactivity of calcite-water-interfaces: molecular process understanding for technical applications). As indicated by the project title, work within the project comprised a large range of length scales. The molecular scale structure of the calcite (104)-water-interface is refined based on surface diffraction data. Structural details are related to surface charging phenomena, and a simplified basic stern surface complexation model is proposed. As an example for trace metal interactions with calcite surfaces we review and present new spectroscopic and macroscopic experimental results on Selenium interactions with calcite. Results demonstrate that selenate (SeO42-) shows no significant interaction with calcite at our experimental conditions, while selenite (SeO32-) adsorbs at the calcite surface and can be incorporated into the calcite structure. Atomistic calculations are used to assess the thermodynamics of sulfate (SO42-), selenate (SeO42-), and selenite (SeO32-) partitioning in calcite and aragonite. The results show that incorporation of these oxo-anions into the calcite structure is so highly endothermic that incorporation is practically impossible at bulk equilibrium and standard conditions. This indicates that entrapment processes are involved when coprecipitation is observed experimentally. The relevance of nano-scale surface features is addressed in an investigation of calcite growth and precipitation in the presence of phosphonates, demonstrating the influence of phosphonates on the morphology of growth spirals and macroscopic growth rates. It is investigated how physical properties of limestone containing cement suspensions may influence the workability of the cement suspensions and thus the efficacy of limestone in industrial applications. The largest scale is reached in iron filtration experiments in a water-purification-pilot-plant using limestone as filter material, which appeared to be highly effective for removing iron from drinking water. Investigations presented cover a whole series of methods to study the calcite-water-interface. Many calcite related topics are addressed, demonstrating how broad the field of calcite-water-interface research is and how manifold the applications are, for which calcite-water-interface phenomena are of major relevance.",
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note = "Funding Information: The authors gratefully acknowledge funding by the German Federal Ministry of Education and Research (Bundesministerium f{\"u}r Bildung und Forschung, BMBF) and the German Research Foundation (Deutsche Forschungsgemeinschaft, DFG) through the joint research project RECAWA in framework of the research program GEOTECHNOLOGIEN. ",
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TY - JOUR

T1 - Reactivity of the calcite-water-interface, from molecular scale processes to geochemical engineering

AU - Heberling, Frank

AU - Bosbach, Dirk

AU - Eckhardt, Jörg Detlef

AU - Fischer, Uwe

AU - Glowacky, Jens

AU - Haist, Michael

AU - Kramar, Utz

AU - Loos, Steffen

AU - Müller, Harald S.

AU - Neumann, Thomas

AU - Pust, Christopher

AU - Schäfer, Thorsten

AU - Stelling, Jan

AU - Ukrainczyk, Marko

AU - Vinograd, Victor

AU - Vučak, Marijan

AU - Winkler, Björn

N1 - Funding Information: The authors gratefully acknowledge funding by the German Federal Ministry of Education and Research (Bundesministerium für Bildung und Forschung, BMBF) and the German Research Foundation (Deutsche Forschungsgemeinschaft, DFG) through the joint research project RECAWA in framework of the research program GEOTECHNOLOGIEN.

PY - 2014/6

Y1 - 2014/6

N2 - Surface reactions on calcite play an important role in geochemical and environmental systems, as well as many areas of industry. In this review, we present investigations of calcite that were performed in the frame of the joint research project "RECAWA" (reactivity of calcite-water-interfaces: molecular process understanding for technical applications). As indicated by the project title, work within the project comprised a large range of length scales. The molecular scale structure of the calcite (104)-water-interface is refined based on surface diffraction data. Structural details are related to surface charging phenomena, and a simplified basic stern surface complexation model is proposed. As an example for trace metal interactions with calcite surfaces we review and present new spectroscopic and macroscopic experimental results on Selenium interactions with calcite. Results demonstrate that selenate (SeO42-) shows no significant interaction with calcite at our experimental conditions, while selenite (SeO32-) adsorbs at the calcite surface and can be incorporated into the calcite structure. Atomistic calculations are used to assess the thermodynamics of sulfate (SO42-), selenate (SeO42-), and selenite (SeO32-) partitioning in calcite and aragonite. The results show that incorporation of these oxo-anions into the calcite structure is so highly endothermic that incorporation is practically impossible at bulk equilibrium and standard conditions. This indicates that entrapment processes are involved when coprecipitation is observed experimentally. The relevance of nano-scale surface features is addressed in an investigation of calcite growth and precipitation in the presence of phosphonates, demonstrating the influence of phosphonates on the morphology of growth spirals and macroscopic growth rates. It is investigated how physical properties of limestone containing cement suspensions may influence the workability of the cement suspensions and thus the efficacy of limestone in industrial applications. The largest scale is reached in iron filtration experiments in a water-purification-pilot-plant using limestone as filter material, which appeared to be highly effective for removing iron from drinking water. Investigations presented cover a whole series of methods to study the calcite-water-interface. Many calcite related topics are addressed, demonstrating how broad the field of calcite-water-interface research is and how manifold the applications are, for which calcite-water-interface phenomena are of major relevance.

AB - Surface reactions on calcite play an important role in geochemical and environmental systems, as well as many areas of industry. In this review, we present investigations of calcite that were performed in the frame of the joint research project "RECAWA" (reactivity of calcite-water-interfaces: molecular process understanding for technical applications). As indicated by the project title, work within the project comprised a large range of length scales. The molecular scale structure of the calcite (104)-water-interface is refined based on surface diffraction data. Structural details are related to surface charging phenomena, and a simplified basic stern surface complexation model is proposed. As an example for trace metal interactions with calcite surfaces we review and present new spectroscopic and macroscopic experimental results on Selenium interactions with calcite. Results demonstrate that selenate (SeO42-) shows no significant interaction with calcite at our experimental conditions, while selenite (SeO32-) adsorbs at the calcite surface and can be incorporated into the calcite structure. Atomistic calculations are used to assess the thermodynamics of sulfate (SO42-), selenate (SeO42-), and selenite (SeO32-) partitioning in calcite and aragonite. The results show that incorporation of these oxo-anions into the calcite structure is so highly endothermic that incorporation is practically impossible at bulk equilibrium and standard conditions. This indicates that entrapment processes are involved when coprecipitation is observed experimentally. The relevance of nano-scale surface features is addressed in an investigation of calcite growth and precipitation in the presence of phosphonates, demonstrating the influence of phosphonates on the morphology of growth spirals and macroscopic growth rates. It is investigated how physical properties of limestone containing cement suspensions may influence the workability of the cement suspensions and thus the efficacy of limestone in industrial applications. The largest scale is reached in iron filtration experiments in a water-purification-pilot-plant using limestone as filter material, which appeared to be highly effective for removing iron from drinking water. Investigations presented cover a whole series of methods to study the calcite-water-interface. Many calcite related topics are addressed, demonstrating how broad the field of calcite-water-interface research is and how manifold the applications are, for which calcite-water-interface phenomena are of major relevance.

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DO - 10.1016/j.apgeochem.2014.03.006

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JO - Applied geochemistry

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