(c) Gases in the atmosphere
- Syllabus
- 2024
- Topic
- —
- Level
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Dry air is a mixture dominated by nitrogen and oxygen. Its four most abundant gases have approximate percentages by volume that add to about 100%.
| Gas | Approximate percentage by volume in dry air |
|---|---|
| nitrogen, NX2 | 78% |
| oxygen, OX2 | 21% |
| argon, Ar | 0.9% (about 1%) |
| carbon dioxide, COX2 | 0.04% |
In a 100 cm3 sample of dry air, this corresponds approximately to 78 cm3 nitrogen and 21 cm3 oxygen, with less than 1 cm3 argon and a much smaller carbon dioxide volume.
'Dry air' excludes variable water vapour. The percentages are approximate: 78% nitrogen and 21% oxygen are not 79% nitrogen and 20% oxygen unless the question explicitly permits that rounding.
To determine the oxygen percentage, trap a known volume of air and react its oxygen completely with a substance while the other main gases remain unreacted. The decrease in gas volume represents the oxygen removed.
| Reactant | How oxygen is removed | Evidence reaction is complete |
|---|---|---|
| wet iron wool or filings | iron rusts and binds oxygen in a solid oxide | gas volume stops decreasing |
| heated copper | air is passed repeatedly over hot copper, forming black copper(II) oxide | repeated volume readings become constant |
| burning phosphorus | phosphorus consumes oxygen and forms a solid oxide | burning stops and the apparatus cools before the final reading |
\text{oxygen percentage}=\frac{\text{initial gas volume}-\text{final gas volume}}{\text{initial gas volume}}\times100
If the trapped air starts at 100 cm3 and ends at 79 cm3, the decrease is 21 cm3, so oxygen is 21/100×100=21% by volume.
Use the total initial air volume, including connecting tubes, when required. Compare readings at the same temperature and pressure after cooling; leaks, incomplete reaction or a hot final gas volume make the result unreliable.
Combustion in oxygen forms an oxide. Magnesium, hydrogen and sulfur give different observations and products, so each reaction must be identified precisely.
| Element | Observation in oxygen | Product |
|---|---|---|
| magnesium | intense bright white flame; white solid forms | magnesium oxide, MgO |
| hydrogen | pale blue flame; water vapour forms and may condense | water, HX2O |
| sulfur | blue flame; colourless choking gas forms | sulfur dioxide, SOX2 |
\ce{2Mg + O2 -> 2MgO}\qquad\ce{2H2 + O2 -> 2H2O}\qquad\ce{S + O2 -> SO2}
A white magnesium product is a solid or ash, not a precipitate. Hydrogen combustion forms water, not hydrogen peroxide; sulfur normally forms sulfur dioxide under these conditions.
Thermal decomposition breaks one compound into simpler substances by heating it. Many metal carbonates form a metal oxide and carbon dioxide.
\ce{metal carbonate ->[heat] metal oxide + carbon dioxide}
When green copper(II) carbonate is heated, it forms black copper(II) oxide and carbon dioxide: CuCOX3(s)heatCuO(s)+COX2(g).
| Evidence | Conclusion |
|---|---|
| green solid becomes black | copper(II) oxide has formed |
| gas turns limewater milky/cloudy | carbon dioxide has formed |
The gas is released because the carbonate decomposes; it is not combustion, because oxygen is not a reactant in the equation. 'Thermal' means heat is supplied, not that the reaction necessarily gives heat out.
Carbon dioxide is a greenhouse gas. It absorbs some infrared radiation emitted by Earth's surface and re-emits it, reducing the rate at which energy escapes to space.
If the amount of atmospheric carbon dioxide increases, more outgoing infrared radiation can be absorbed. This strengthens the greenhouse effect and may raise average global temperatures, contributing to climate change.
Climate change can alter rainfall patterns and increase the likelihood of some extreme conditions; warming also contributes to melting land ice and sea-level rise. These are consequences of a changing climate, not the definition of a greenhouse gas.
The natural greenhouse effect keeps Earth warm enough for life. The concern is an enhanced effect caused by increasing greenhouse-gas concentrations. Carbon dioxide may contribute to climate change; it is not correct to describe it as the sole influence on climate.
A practical way to estimate oxygen in air is to trap a measured column of air with wet iron wool. Water is required for rusting, and oxygen is removed from the trapped gas as solid rust forms.
| Stage | Action |
|---|---|
| 1 | Push wet iron wool into one end of a graduated tube and record the initial trapped-air length or volume. |
| 2 | Invert the open end in water so the air remains sealed; leave the apparatus until the reading becomes constant. |
| 3 | Record the final air length or volume at the same temperature and pressure. |
| 4 | Subtract final from initial; divide by the initial value and multiply by 100. |
\text{oxygen percentage}=\frac{84-69}{84}\times100=17.9%\approx18%
Use excess finely divided iron to provide enough surface area, make airtight connections and wait for a constant reading. A value below 21% may mean not all oxygen reacted; leaks, temperature or pressure changes, or inaccurate meniscus readings can shift the result.
Wear eye protection and handle rusty or sharp iron wool with tools. Keep the apparatus stable and do not force a sealed plunger; the volume change is caused by oxygen removal, not by nitrogen being produced.