Heat of Dissolution Equation:
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Heat of dissolution (ΔH) is the enthalpy change when one mole of a substance dissolves in a solvent at constant pressure. For water, it represents the heat absorbed or released when a solute dissolves in water.
The calculator uses the heat of dissolution equation:
Where:
Explanation: The equation calculates the enthalpy change per mole of solute dissolved in water, indicating whether the process is endothermic (positive ΔH) or exothermic (negative ΔH).
Details: Calculating heat of dissolution is important for understanding solubility, predicting temperature changes during dissolution, and designing industrial processes involving dissolution.
Tips: Enter the heat absorbed or released in kJ and the number of moles of solute. Both values must be positive numbers greater than zero.
Q1: What does a positive ΔH value indicate?
A: A positive ΔH indicates an endothermic process where heat is absorbed from the surroundings during dissolution.
Q2: What does a negative ΔH value indicate?
A: A negative ΔH indicates an exothermic process where heat is released to the surroundings during dissolution.
Q3: How is heat (q) measured experimentally?
A: Heat is typically measured using a calorimeter, which detects temperature changes in the solution during dissolution.
Q4: Does this calculation apply to all solvents?
A: While the equation is general, this calculator is specifically designed for dissolution in water as the solvent.
Q5: How does temperature affect heat of dissolution?
A: Heat of dissolution can vary with temperature, though for many substances it's relatively constant over moderate temperature ranges.