The Clausius-Clapeyron equation gives the slope at a curve in:
P-T diagram
The Clausius-Clapeyron equation is a fundamental thermodynamic relationship used to describe how the pressure ($P$) of a substance changes with temperature ($T$) during a phase transition, such as melting, boiling, or sublimation. It specifically relates the slope of the phase equilibrium curve on a phase diagram to the properties of the substance undergoing the transition.
The equation itself provides a way to calculate the slope ($\frac{dP}{dT}$) of the coexistence curve (the line separating two phases) on a pressure-temperature (P-T) diagram. The commonly used form of the Clausius-Clapeyron equation is:
$$ \frac{dP}{dT} = \frac{\Delta H_{tr}}{T \Delta V} $$
Where:
A P-T diagram plots pressure against temperature. Lines on this diagram represent conditions where two phases can coexist in equilibrium. The Clausius-Clapeyron equation directly calculates the slope ($ \frac{dP}{dT} $) of these equilibrium lines. For example, it describes the slope of the vaporization curve (liquid-gas equilibrium) and the sublimation curve (solid-gas equilibrium).
Therefore, the Clausius-Clapeyron equation specifically defines the slope of a curve found on a P-T diagram, representing the relationship between pressure and temperature during phase changes.
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A system that does NOT allow exchange of heat with its surrounding is called
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