On the solubility of whitlockite, Ca9Mg(HPO4)(PO4)6, in aqueous solution at 298.15 K

Whitlockite was assigned the ideal formula Ca 9 Mg(HPO 4 )(PO 4 ) 6 , but the synthesis of a solid phase with this exact composition is very difficult. One of the reasons arises from the fact that there are no accurate values published for its solubility constant and/or other thermodynamic parameter...

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Published inMonatshefte für Chemie Vol. 149; no. 2; pp. 253 - 260
Main Authors Magalhães, M. Clara F., Costa, M. Odete G.
Format Journal Article
LanguageEnglish
Published Vienna Springer Vienna 01.02.2018
Springer Nature B.V
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Abstract Whitlockite was assigned the ideal formula Ca 9 Mg(HPO 4 )(PO 4 ) 6 , but the synthesis of a solid phase with this exact composition is very difficult. One of the reasons arises from the fact that there are no accurate values published for its solubility constant and/or other thermodynamic parameters. These could help to delineate a stability field in relation to the most common solid calcium and magnesium phosphates which normally co-occur with whitlockite. Calcium magnesium phosphates with the structure of whitlockite containing various n Mg / n Ca ratios were synthesized from aqueous solution of pH between 5.0 and 6.0, with the ratio of the concentrations of magnesium and calcium between 0.4 and 1.5, and excess of total calcium and magnesium over total phosphate. Those solids were used to determine the solubility of whitlockite with the ideal formula [lg K s (whitlockite, solid, 298.15 K) = − 113.75 ± 2.18], which was used to determine its standard molar Gibbs energy of formation. This value, together with the previously published values for the standard molar Gibbs energy of formation of the relevant calcium and magnesium solid phosphates and other species at equilibrium, allowed the construction of a phase diagram containing all the relevant solid calcium and magnesium phosphates. Graphical abstract
AbstractList Whitlockite was assigned the ideal formula Ca9Mg(HPO4)(PO4)6, but the synthesis of a solid phase with this exact composition is very difficult. One of the reasons arises from the fact that there are no accurate values published for its solubility constant and/or other thermodynamic parameters. These could help to delineate a stability field in relation to the most common solid calcium and magnesium phosphates which normally co-occur with whitlockite. Calcium magnesium phosphates with the structure of whitlockite containing various nMg/nCa ratios were synthesized from aqueous solution of pH between 5.0 and 6.0, with the ratio of the concentrations of magnesium and calcium between 0.4 and 1.5, and excess of total calcium and magnesium over total phosphate. Those solids were used to determine the solubility of whitlockite with the ideal formula [lg Ks(whitlockite, solid, 298.15 K) = − 113.75 ± 2.18], which was used to determine its standard molar Gibbs energy of formation. This value, together with the previously published values for the standard molar Gibbs energy of formation of the relevant calcium and magnesium solid phosphates and other species at equilibrium, allowed the construction of a phase diagram containing all the relevant solid calcium and magnesium phosphates.Graphical abstract
Whitlockite was assigned the ideal formula Ca 9 Mg(HPO 4 )(PO 4 ) 6 , but the synthesis of a solid phase with this exact composition is very difficult. One of the reasons arises from the fact that there are no accurate values published for its solubility constant and/or other thermodynamic parameters. These could help to delineate a stability field in relation to the most common solid calcium and magnesium phosphates which normally co-occur with whitlockite. Calcium magnesium phosphates with the structure of whitlockite containing various n Mg / n Ca ratios were synthesized from aqueous solution of pH between 5.0 and 6.0, with the ratio of the concentrations of magnesium and calcium between 0.4 and 1.5, and excess of total calcium and magnesium over total phosphate. Those solids were used to determine the solubility of whitlockite with the ideal formula [lg K s (whitlockite, solid, 298.15 K) = − 113.75 ± 2.18], which was used to determine its standard molar Gibbs energy of formation. This value, together with the previously published values for the standard molar Gibbs energy of formation of the relevant calcium and magnesium solid phosphates and other species at equilibrium, allowed the construction of a phase diagram containing all the relevant solid calcium and magnesium phosphates. Graphical abstract
Author Costa, M. Odete G.
Magalhães, M. Clara F.
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Issue 2
Keywords Calcium–magnesium phosphate
Whitlockite
Phase diagram
Solubility constant
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  doi: 10.1038/sj.ki.5002028
  contributor:
    fullname: S Verberckmoes
– volume: 8
  start-page: 634
  year: 2014
  ident: 2129_CR3
  publication-title: ACS Nano
  doi: 10.1021/nn405246h
  contributor:
    fullname: HL Jang
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Snippet Whitlockite was assigned the ideal formula Ca 9 Mg(HPO 4 )(PO 4 ) 6 , but the synthesis of a solid phase with this exact composition is very difficult. One of...
Whitlockite was assigned the ideal formula Ca9Mg(HPO4)(PO4)6, but the synthesis of a solid phase with this exact composition is very difficult. One of the...
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SubjectTerms Analytical Chemistry
Aqueous solutions
Calcium
Chemistry
Chemistry and Materials Science
Chemistry/Food Science
Energy of formation
Free energy
Heat of formation
Inorganic Chemistry
Magnesium
Organic Chemistry
Original Paper
Phosphates
Physical Chemistry
Solids
Solubility
Theoretical and Computational Chemistry
Title On the solubility of whitlockite, Ca9Mg(HPO4)(PO4)6, in aqueous solution at 298.15 K
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https://www.proquest.com/docview/2005112300/abstract/
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