Decomposition and Measured Mass Loss

Inferring volatile product amount from a heated sample

Lesson 1136 of 4,500 · Stoichiometry and Mole Calculations

Learning objectives

Introduction

Heating a solid can release a gas or water vapour, leaving a lighter residue. If the apparatus retains the solid and the escaping product is identified, the measured mass difference gives the escaped product mass. Convert that mass to moles and then use the balanced decomposition equation to infer how much starting compound decomposed.

Core explanation

Calcium carbonate can decompose on sufficient heating: CaCO₃(s) → CaO(s) + CO₂(g). A sample losing 0.440 g, with no solid lost and CO₂ as the only escaping substance, released 0.440 g CO₂. Dividing by M(CO₂) ≈ 44.0 g mol⁻¹ gives 0.0100 mol CO₂. The 1:1 equation ratio says 0.0100 mol CaCO₃ decomposed. This corresponds to about 1.00 g CaCO₃. The initial sample might be larger if some carbonate remained or inert material was present; mass loss alone gives the decomposed amount under those assumptions.

The equation identifies what the lost mass represents. A hydrate can lose water rather than CO₂; copper(II) sulfate pentahydrate, for example, can be discussed as CuSO₄·5H₂O → CuSO₄ + 5H₂O under a specified dehydration step. If 0.900 g water is lost, that is about 0.0500 mol H₂O, corresponding to 0.0100 mol of the pentahydrate units for complete loss of five waters per unit. It would be wrong to interpret that mass as 0.900 g CuSO₄. An experimentally heated salt may undergo additional chemistry at excessive temperature, so the specified product and heating regime matter.

Mass should be measured after cooling the container as instructed. A hot crucible can disturb a balance reading and can also take up moisture during prolonged exposure to air. Repeated heat–cool–weigh cycles until a suitably constant mass support the claim that the targeted loss is complete. The lid may help prevent solid particles from escaping, but must permit vapour to leave. If powder spits out, the mass decrease is not all volatile product and the inferred gas amount is too high.

Mass conservation still holds: the apparently missing mass has moved into the surroundings. In a closed system, the mass of vessel, residue and trapped gas together would remain constant. An open-crucible result is a partial-system mass difference. This distinction prevents a misconception that a decomposition reaction destroys matter.

Some reactions gain solid mass on heating in air because oxygen combines with the sample, such as oxidation of a metal. A mass gain cannot be analyzed as a simple escaped-gas amount. Even for mass loss, two volatile products make the inverse problem underdetermined unless their individual amounts or another independent measurement is supplied. Check whether the experiment justifies treating the lost mass as one named substance.

Step-by-step reasoning

1. Subtract final dry residue-plus-container mass from initial sample-plus-container mass. 2. Identify the volatile product and check that no solid was lost. 3. Divide mass loss by that product's molar mass. 4. Use balanced coefficients to find decomposed starting-material moles. 5. Convert to requested mass or fraction, stating completion and purity assumptions.

Visual explanation

Picture a crucible before and after heating. Initial sample mass is 2.00 g; final dry residue is 1.56 g. An upward CO₂ arrow is labeled 0.44 g. A second arrow converts 0.44 g CO₂ to 0.010 mol and then to 0.010 mol decomposed CaCO₃.

Real-world analogy

If a wet towel becomes lighter after drying, the mass difference estimates evaporated water only if no fibers were lost. A heating experiment similarly assigns weight loss to an escaped product only when no solid was spilled and no other vapour contributed significantly.

Real-world example

A mineral sample containing calcium carbonate may be heated under controlled conditions. The CO₂ mass loss can estimate carbonate that decomposed. A reliable analysis must avoid loss of dust and distinguish other volatile components, such as water in the mineral, from carbonate-derived carbon dioxide.

Why?

Why use the difference between two solid masses rather than the final solid mass alone? The initial-to-final decrease isolates matter that left the weighed system. The residue mass includes whatever nonvolatile products and impurities remain, so it cannot by itself identify gas moles without a composition model.

Common misconception

“A loss of 0.44 g always means 0.44 g CO₂.” The value is merely total mass lost. It represents CO₂ only if that is the sole escaping material and no solid particles leave. Moisture, splashing or additional decomposition can invalidate the assignment.

Worked example

A 2.50 g sample of hydrated salt is heated until 1.60 g dry salt remains. Assume the sole loss is water and all formula water is removed. Water mass = 0.90 g, or 0.90/18.0 = 0.050 mol H₂O. If the anhydrous salt amount is 0.010 mol from its formula mass, the ratio is 0.050:0.010 = 5:1, so the hydrate has five waters per salt unit. This conclusion needs the anhydrous identity and complete dehydration, not just the mass difference.

Quick check

1. In CaCO₃ → CaO + CO₂, what CO₂ amount corresponds to a valid 0.880 g mass loss? Answer: Divide 0.880 g by 44.0 g mol⁻¹ to obtain 0.0200 mol CO₂.

Exam focus

Show the subtraction of two compatible masses, identify the escaped species and name assumptions. Convert loss to gas moles before using the equation ratio. If the problem mentions constant mass or spattering, discuss how that affects the interpretation.

Advanced insight

Thermogravimetric analysis measures sample mass continuously as temperature changes. Separate mass-loss steps can suggest different volatile products, but a step's mass alone rarely proves chemical identity. Pairing mass data with gas analysis or known phase chemistry strengthens the assignment of each loss.

Summary

Valid mass loss measures material leaving an open heated sample. When a single volatile product is identified and the solid remains contained, divide its mass by molar mass and use the decomposition coefficients. Incomplete reaction, moisture and physical loss of particles can all distort the inferred starting amount.

Practice questions

1. What is the mass loss from 2.00 g initial solid to 1.56 g residue? Answer: 0.44 g left the weighed solid system. 2. How many moles CO₂ is 0.44 g? Answer: About 0.010 mol using 44.0 g mol⁻¹. 3. How much CaCO₃ decomposed to make that amount of CO₂? Answer: About 0.010 mol, or 1.00 g, by the 1:1 equation ratio. 4. How does solid spattering affect an inferred gas amount? Answer: It increases measured mass loss without adding gas, so gas amount would be overestimated.