(d) Calculate the temperature at which calcite and aragonite are at equilibrium under 1 bar. (e) Determine whether an increase in pressure at a fixed temperature will increase or decrease the thermodynamic stability of aragonite with respect to calcite.

Introduction to Chemical Engineering Thermodynamics
8th Edition
ISBN:9781259696527
Author:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Publisher:J.M. Smith Termodinamica en ingenieria quimica, Hendrick C Van Ness, Michael Abbott, Mark Swihart
Chapter1: Introduction
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Part d and e please
### Calcium Carbonate Polymorph Transition

**Problem Statement:**

Calcium carbonate (\( \text{CaCO}_3 \)) has two polymorphs, calcite and aragonite. The volume change for the calcite to aragonite transition is \( -2.784 \, \text{cm}^3/\text{mol} \) and is assumed to be independent of temperature and pressure. The chemical potential change for the calcite to aragonite transition as a function of temperature at \( 1 \, \text{bar} \) is given by:

\[ \Delta \mu = -210 + 4.2T \, (\text{J/mol}) \]

**Questions:**

(a) What is the molar heat of transition?

(b) What is the molar entropy change for the transition?

(c) Determine the stable phase at room temperature \( 298 \, \text{K} \) under \( 1 \, \text{bar} \).

(d) Calculate the temperature at which calcite and aragonite are at equilibrium under \( 1 \, \text{bar} \).

(e) Determine whether an increase in pressure at a fixed temperature will increase or decrease the thermodynamic stability of aragonite with respect to calcite.

**Notes and Diagrams:**

- **Volume Change**: The transition from calcite to aragonite involves a volume decrease of \( 2.784 \, \text{cm}^3/\text{mol} \).
- **Chemical Potential Change Function**: It describes how the chemical potential changes with temperature at constant pressure.
  
For educational purposes, students should analyze these equations and data to understand the interactions between temperature, pressure, and phase stability in mineralogy.
Transcribed Image Text:### Calcium Carbonate Polymorph Transition **Problem Statement:** Calcium carbonate (\( \text{CaCO}_3 \)) has two polymorphs, calcite and aragonite. The volume change for the calcite to aragonite transition is \( -2.784 \, \text{cm}^3/\text{mol} \) and is assumed to be independent of temperature and pressure. The chemical potential change for the calcite to aragonite transition as a function of temperature at \( 1 \, \text{bar} \) is given by: \[ \Delta \mu = -210 + 4.2T \, (\text{J/mol}) \] **Questions:** (a) What is the molar heat of transition? (b) What is the molar entropy change for the transition? (c) Determine the stable phase at room temperature \( 298 \, \text{K} \) under \( 1 \, \text{bar} \). (d) Calculate the temperature at which calcite and aragonite are at equilibrium under \( 1 \, \text{bar} \). (e) Determine whether an increase in pressure at a fixed temperature will increase or decrease the thermodynamic stability of aragonite with respect to calcite. **Notes and Diagrams:** - **Volume Change**: The transition from calcite to aragonite involves a volume decrease of \( 2.784 \, \text{cm}^3/\text{mol} \). - **Chemical Potential Change Function**: It describes how the chemical potential changes with temperature at constant pressure. For educational purposes, students should analyze these equations and data to understand the interactions between temperature, pressure, and phase stability in mineralogy.
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