SUMMARY
This discussion focuses on calculating the change in volume when transitioning granite from a solid to a liquid state. The user has determined the solid density of granite at approximately 2.617 g/cm³, derived from its mineral composition: 60% orthoclase, 30% quartz, 5% hornblende, and 5% biotite. The user seeks a general equation or ratio to estimate the liquid density of granite, as specific data is scarce. The conversation suggests that experimentation may be necessary to obtain accurate values for the liquid state.
PREREQUISITES
- Understanding of phase changes in materials
- Knowledge of mineral composition and density calculations
- Familiarity with specific heat capacities of minerals
- Basic principles of thermodynamics
NEXT STEPS
- Research methods for calculating liquid densities from solid densities
- Explore the concept of phase change and its impact on volume
- Investigate specific heat capacities of granite's mineral components
- Consider experimental approaches to measure the density of molten granite
USEFUL FOR
Hobbyists, students, and anyone interested in the thermodynamic properties of minerals, particularly those studying phase changes in geological materials.