10.4 - Metal Oxides & Non-metal Oxides
- 1
The reactions of metal oxides and non-metal oxides with water
- 2
The amphoteric nature of aluminium oxide
- 3
The trend in acid-base properties across a period
- 4
The environmental impact of acid rain and ocean acidification
Metal oxides react with water to form bases
Metal oxides, particularly those of alkali and alkaline earth metals, react with water to form hydroxides, which are bases.
Alkali metal oxides react with water according to the general equation:
M2O(s) + H2O(l) ➔ 2MOH(aq)
Examples include:
Li2O(s) + H2O(l) ➔ 2LiOH(aq)
Na2O(s) + H2O(l) ➔ 2NaOH(aq)
Group 2 metal oxides also react with water to produce hydroxides:
MO(s) + H2O(l) ➔ M(OH)2(aq)
Examples include:
MgO(s) + H2O(l) ➔ Mg(OH)2(aq)
CaO(s) + H2O(l) ➔ Ca(OH)2(aq)
Non-metal oxides react with water to form acids
Non-metal oxides react with water to form acidic compounds.
Some examples of non-metal oxides reacting with water include:
CO2(g) + H2O(l) ➔ H2CO3(aq)
SO2(g) + H2O(l) ➔ H2SO3(aq)
SO3(l) + H2O(l) ➔ H2SO4(aq)
P4O10(s) + 6H2O(l) ➔ 4H3PO4(aq)
Amphoteric oxides
Some oxides, such as aluminium oxide (Al2O3), can react with both acids and bases. These oxides are called amphoteric oxides.
When reacting with a base like sodium hydroxide, Al2O3 reacts to form a salt:
Al2O3(s) + 2NaOH(aq) + 3H2O(l) ➔ 2NaAl(OH)4(aq)
On the other hand, when reacting with an acid such as hydrochloric acid, Al2O3 also forms a salt:
Al2O3(s) + 6HCl(aq) ➔ 2AlCl3(aq) + 3H2O(l)
Both of these reactions are examples of neutralisation, in which an acid and a base react to form a salt.
Trends in acid-base properties across a period
As you move from left to right across a period in the periodic table, the oxides of the elements exhibit a gradual change from basic to amphoteric to acidic. This trend is a consequence of the increasing covalent character of the bonds in the oxides.
- Metal oxides on the left side of the period (e.g., Na2O and MgO) have primarily ionic bonding, which results in their basic properties when reacting with water.
- Oxides of elements in the middle of the period, like Al2O3, display both ionic and covalent bonding, leading to their amphoteric behaviour.
- Non-metal oxides on the right side of the period (e.g., P4O10, SO3, and SO2) have covalent bonding, which accounts for their acidic properties in water.
This gradual change in acid-base properties across a period can be summarised as follows:
Basic metal oxides ➔ Amphoteric oxides ➔ Acidic non-metal oxides
The table below illustrates the trend in acid-base properties of some period 3 oxides:
| Formula of oxide | Acid or base? |
|---|---|
| Na_2_O | Basic |
| MgO | Basic |
| Al_2_O_3_ | Amphoteric |
| SiO_2_ | Acidic |
| P_4_O_10_ | Acidic |
| SO_3_ and SO_2_ | Acidic |
Acid rain
Acid rain is rainwater with a pH below 5.6, caused by the dissolution of nitrogen oxides (NOx) and sulfur dioxide (SO2) in the atmosphere. These gases can be released naturally from volcanoes and decaying vegetation or from human activities such as burning high-sulfur fossil fuels in industrial processes.
When sulfur dioxide dissolves in rainwater, it forms sulfurous acid:
SO2(g) + H2O(l) ➔ H2SO3(aq)
Similarly, when nitrogen dioxide dissolves in rainwater, it forms nitric and nitrous acids:
2NO2(g) + H2O(l) ➔ HNO3(aq) + HNO2(aq)
Atmospheric oxygen can further oxidise sulfurous and nitrous acids to sulfuric and nitric acids, respectively:
2H2SO3(aq) + O2(g) ➔ 2H2SO4(aq)
2HNO2(aq) + O2(g) ➔ 2HNO3(aq)
The increased acidity of acid rain can harm plants, aquatic life, and infrastructure.
Ocean acidification
Ocean acidification is the decrease in the pH of the Earth's oceans due to the absorption of large amounts of atmospheric carbon dioxide (CO2).
When CO2 dissolves in seawater, it forms carbonic acid:
CO2(g) + H2O(l) ➔ H2CO3(aq)