Using estimated thermodynamic properties to model accessory phases: the case of tourmaline
Accessory phases and minor components in minerals are commonly ignored in thermodynamic modelling. Such an approach seems unwarranted, as accessory phases can represent a significant element reservoir and minor components can substantially change their host mineral's stability field. However, a...
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| Format: | Journal article |
| Language: | English |
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2007
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| _version_ | 1826306908064055296 |
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| author | Van Hinsberg, V Schumacher, J |
| author_facet | Van Hinsberg, V Schumacher, J |
| author_sort | Van Hinsberg, V |
| collection | OXFORD |
| description | Accessory phases and minor components in minerals are commonly ignored in thermodynamic modelling. Such an approach seems unwarranted, as accessory phases can represent a significant element reservoir and minor components can substantially change their host mineral's stability field. However, a lack of thermodynamic data prohibits assessment of these effects. In this contribution, the polyhedron method is used to estimate the thermodynamic properties of tourmaline, a common and widespread accessory phase, stable over a range of P-T-X conditions. The polyhedron method allows Δ H, S, V, Cp and Vm (T, P) properties to be estimated from a linear stoichiometric summation over the fractional properties of its polyhedron constituents. To allow for estimates of tourmaline, fractional thermodynamic properties for B III and B IV polyhedra were derived. Mixing contributions to molar volume were evaluated and symmetrical mixing parameters derived for Al-Mg, Al-Fe and Al-Li interaction on tourmaline's Y-site and T-site Al-Si interaction. Evaluation of the estimated properties using experimental and natural equilibria between tourmaline and melts, minerals and hydrothermal fluids, shows that reliable semi-quantitative results are obtained. The boron contents in fluids coexisting with tourmaline are calculated to within an order of magnitude of measured content, and where anchor-points are available, agreement improves to within a factor of 2. Including tourmaline in petrogenetic modelling of metamorphic rocks indicates that its presence leads to disappearance of staurolite and garnet, among others, and modifies the XMg of coexisting phases, in line with observations on natural rocks. © 2007 Blackwell Publishing Ltd. |
| first_indexed | 2024-03-07T06:55:01Z |
| format | Journal article |
| id | oxford-uuid:fdd7b21a-0537-49a8-85e9-6d01f89e6f17 |
| institution | University of Oxford |
| language | English |
| last_indexed | 2024-03-07T06:55:01Z |
| publishDate | 2007 |
| record_format | dspace |
| spelling | oxford-uuid:fdd7b21a-0537-49a8-85e9-6d01f89e6f172022-03-27T13:31:48ZUsing estimated thermodynamic properties to model accessory phases: the case of tourmalineJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:fdd7b21a-0537-49a8-85e9-6d01f89e6f17EnglishSymplectic Elements at Oxford2007Van Hinsberg, VSchumacher, JAccessory phases and minor components in minerals are commonly ignored in thermodynamic modelling. Such an approach seems unwarranted, as accessory phases can represent a significant element reservoir and minor components can substantially change their host mineral's stability field. However, a lack of thermodynamic data prohibits assessment of these effects. In this contribution, the polyhedron method is used to estimate the thermodynamic properties of tourmaline, a common and widespread accessory phase, stable over a range of P-T-X conditions. The polyhedron method allows Δ H, S, V, Cp and Vm (T, P) properties to be estimated from a linear stoichiometric summation over the fractional properties of its polyhedron constituents. To allow for estimates of tourmaline, fractional thermodynamic properties for B III and B IV polyhedra were derived. Mixing contributions to molar volume were evaluated and symmetrical mixing parameters derived for Al-Mg, Al-Fe and Al-Li interaction on tourmaline's Y-site and T-site Al-Si interaction. Evaluation of the estimated properties using experimental and natural equilibria between tourmaline and melts, minerals and hydrothermal fluids, shows that reliable semi-quantitative results are obtained. The boron contents in fluids coexisting with tourmaline are calculated to within an order of magnitude of measured content, and where anchor-points are available, agreement improves to within a factor of 2. Including tourmaline in petrogenetic modelling of metamorphic rocks indicates that its presence leads to disappearance of staurolite and garnet, among others, and modifies the XMg of coexisting phases, in line with observations on natural rocks. © 2007 Blackwell Publishing Ltd. |
| spellingShingle | Van Hinsberg, V Schumacher, J Using estimated thermodynamic properties to model accessory phases: the case of tourmaline |
| title | Using estimated thermodynamic properties to model accessory phases: the case of tourmaline |
| title_full | Using estimated thermodynamic properties to model accessory phases: the case of tourmaline |
| title_fullStr | Using estimated thermodynamic properties to model accessory phases: the case of tourmaline |
| title_full_unstemmed | Using estimated thermodynamic properties to model accessory phases: the case of tourmaline |
| title_short | Using estimated thermodynamic properties to model accessory phases: the case of tourmaline |
| title_sort | using estimated thermodynamic properties to model accessory phases the case of tourmaline |
| work_keys_str_mv | AT vanhinsbergv usingestimatedthermodynamicpropertiestomodelaccessoryphasesthecaseoftourmaline AT schumacherj usingestimatedthermodynamicpropertiestomodelaccessoryphasesthecaseoftourmaline |