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ThermoCodegen Fo-SiO2 database

<p>ThermoCodegen v0.6.7 generated thermodynamic database for the Forsterite-SiO2 binary system developed by Lucy Tweed, 2021</p> <p>This system is described by a custom&nbsp;<strong>Thermodynamic Database</strong>&nbsp;consisting of four phases, constructed from five endmembers.</p> <p>The first phase is silicate&nbsp;<strong>Liquid</strong>&nbsp;constructed as an assymetric regular solution between two endmembers:</p> <ul> <li> <p>Forsterite (Mg<sub>2</sub>SiO<sub>4</sub><sup>lq</sup>)</p> </li> <li> <p>Qz4 (Si<sub>2</sub>O<sub>4</sub><sup>lq</sup>)</p> </li> </ul> <p>where Mg<sub>2</sub>SiO<sub>4</sub><sup>lq</sup>&nbsp;is the forsteritic xMelts model and Qz4 is an endmember constructed from two moles of an xMelts SiO<sub>2</sub><sup>lq</sup>&nbsp;model.</p> <p>The next three phases are pure phases each constructed from a single endmember</p> <ul> <li> <p>Olivine (endmember: Forsterite, Mg<sub>2</sub>SiO<sub>4</sub><sup>ol</sup>)</p> </li> <li> <p>Opx (endmember: Orthoenstatite, MgSiO<sub>3</sub><sup>opx</sup>)</p> </li> <li> <p>pQz (endmember: polymorphic SiO<sub>2</sub>, SiO<sub>2</sub><sup>qz</sup>)</p> </li> </ul> <p>where pQz is constructed from a single polymorphic endmember (see below). All of the mineral endmembers are from (Berman, 1988)</p>

ShareScore

12/100

Overall dataset sharing score

Score breakdown

These five areas show where the dataset supports — or may limit — practical reuse.

Stewardship
4
Harmonization
4
Access
0
Reuse readiness
0
Engagement
4