8.5 - Compounds of Groups 1 and 2
- 1Solubility trends of group 2 compounds
- 2Reactions of oxides and hydroxides of groups 1 and 2
- 3Thermal stability trends of the carbonates and nitrates of groups 1 and 2
- 4Testing for carbonate, hydrogencarbonate and sulfate ions
Opposite solubility trends for group 2 hydroxides and sulfates
The solubility of group 2 metal hydroxides and sulfates follows opposite trends down the group:
- Group 2 metal hydroxides become more soluble down the group.
- Group 2 metal sulfates become less soluble down the group.
This is summarised in the table below:
| Group 2 element | Solubility of hydroxide | Solubility of sulfate |
|---|---|---|
| Magnesium | Insoluble | Soluble |
| Calcium | Sparingly soluble | Sparingly soluble |
| Strontium | Soluble | Insoluble |
| Barium | Soluble | Insoluble |
Reactions of group 1 and 2 oxides with water
Group 1 and group 2 metal oxides are basic oxides and readily react with water to alkaline solutions.
For group 1 oxides:
- M2O(s) + H2O(l) ➔ 2MOH(aq)
For group 2 oxides
- MO(s) + H2O(l) ➔ M(OH)2(aq)
These reactions release hydroxide ions (OH-) making the solutions strongly alkaline. The ionic equation is:
- O2-(aq) + H2O(l) ➔ 2OH-(aq)
Reactions of group 1 and 2 oxides and hydroxides with acid
The oxides and hydroxides of group 1 and group 2 react with dilute acids in neutralisation reactions to form salts and water.
Group 1 examples:
Lithium oxide and lithium hydroxide react with hydrochloric acid to form lithium chloride and water:
- Li2O(s) + 2HCl(aq) ➔ 2LiCl(aq) + H2O(l)
- LiOH(s) + HCl(aq) ➔ LiCl(aq) + H2O(l)
Group 2 examples:
Calcium oxide and calcium hydroxide react with sulfuric acid acid to form calcium sulfate and water:
- CaO(s) + H2SO4(aq) ➔ CaSO4(aq) + H2O(l)
- Ca(OH)2(s) + H2SO4(aq) ➔ CaSO4(aq) + 2H2O(l)
Thermal decomposition of carbonates and nitrates
Group 1 compounds
Group 1 carbonates are very stable and don't decompose with Bunsen burner heating.An exception is lithium carbonate which decomposes to form lithium oxide and carbon dioxide:
- Li2CO3(s) ➔ Li2O(s) + CO2(g)
Group 1 nitrates (MNO3) decompose to nitrites and oxygen, for example:
-
2NaNO3(s) ➔ 2NaNO2(s) + O2(g) An exception is lithium nitrate which decomposes to form lithium oxide, nitrogen dioxide and oxygen:
-
2LiNO3(s) ➔ Li2O(s) + 2NO2(g) + 1⁄2O2(g)
Group 2 compounds
Group 2 carbonates (MCO3) decompose to oxides and carbon dioxide, for example:
- CaCO3(s) ➔ CaO(s) + CO2(g)
Group 2 nitrates, (M(NO3)2) decompose to oxides, nitrogen dioxide and oxygen, for example:
- 2Ca(NO3)2(s) ➔ 2CaO(s) + 4NO2(g) + O2(g)
Thermal stability of carbonates and nitrates
The thermal stability of carbonates and nitrates increases as we move down both group 1 and group 2. To understand this trend, we first need to introduce two key concepts:
- Ion polarisation - The distortion of an anion's electron cloud by a nearby cation.
- Polarising power - A cation's ability to distort an anion's electron cloud.

The trend in thermal stability can be explained by considering two main factors:
- Cation size:
- As we move down the group, cations become larger.
- Larger cations have lower charge density (charge spread over a larger area).
- This results in lower polarising power, causing less anion distortion.
- Less distortion leads to stronger C-O and N-O bonds, increasing stability.
- Cation charge:
- Group 2 cations (+2) have higher charge than group 1 cations (+1).
- Higher charge results in greater polarising power.
- This makes group 2 compounds generally less stable than their group 1 counterparts.
Testing the thermal stability of carbonates and nitrates
- Group 2 carbonates - Measure the time taken to produce enough CO2 gas to turn limewater cloudy.
- Group 1 nitrates - Measure the time taken to produce enough O2 gas to relight a glowing splint.
- Group 2 nitrates - In a fume cupboard, measure the time taken to produce brown NO2 gas.
Identifying carbonate and hydrogencarbonate ions
To confirm the presence of carbonate (CO32-) or hydrogencarbonate (HCO3-) ions:
- Add dilute nitric acid (HNO3) dropwise to a sample containing an unknown ion.
- Observe carefully for effervescence caused by bubbles of carbon dioxide (CO2) gas being evolved: CO32-(aq) + 2H+(aq) ➔ CO2(g) + H2O(l)
HCO3-(aq) + H+(aq) ➔ CO2(g) + H2O(l)
Confirm the presence of CO2 by passing bubbles of the gas through limewater (calcium hydroxide solution), in a connecting test tube. If CO2 is present, the limewater will turn cloudy due to the formation of a white calcium carbonate precipitate, confirming the original presence of carbonate ions in the sample:
CO2(g) + Ca(OH)2(aq) ➔ CaCO3(s) + H2O(l)
Identifying sulfate ions
To confirm the presence of sulfate (SO42-) ions:
- Add dilute nitric acid (HNO3) dropwise to a sample containing an unknown ion.
- Add a few drops of a solution containing aqueous Ba2+ ions, such as barium chloride (BaCl2) or barium nitrate (Ba(NO3)2), to the sample.
- Observe carefully for the formation of a white precipitate of barium sulfate (BaSO4): Ba2+(aq) + SO42-(aq) ➔ BaSO4(s)