In chemistry, many solid crystal salts naturally trap water molecules inside their geometric structure. These are called 'Hydrated Salts' (e.g., blue Copper Sulfate crystals). A classic chemistry lab experiment involves heating these crystals to figure out exactly how many water molecules are trapped inside.
The trapped water molecules are officially called the 'Water of Crystallization'. They are responsible for giving the crystal its color and geometric shape.
Plaster of Paris ($CaSO_4 \cdot \frac{1}{2}H_2O$) is a famous hydrate used to cast broken bones. When you add water to it, it turns back into hard Gypsum ($CaSO_4 \cdot 2H_2O$).
A hydrated salt has the general formula: $Salt \cdot xH_2O$. Your goal is to find the value of x (the integer number of water molecules attached to one molecule of the salt). To do this, you must physically burn the water away and measure the weight difference.
Step A: Find the mass of the lost water
Step B: Convert both masses into Moles
Step C: Find the Ratio (The 'x' value)
Conclusion: The value of x is 5. The empirical formula of the hydrated salt is $CuSO_4 \cdot 5H_2O$ (Copper(II) sulfate pentahydrate).
If you don't heat it enough, some water will remain trapped in the salt. When you weigh the 'dry' salt, it will be heavier than it should be. This will make your final calculation for the number of water moles (x) incorrectly low.
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