Reactivity of Metals

Chemical Changes

Reactivity Series

When metals react with other substances the metal atoms form positive ions. The reactivity of a metal is related to its tendency to form positive ions. Metals can be arranged in order of their reactivity in a reactivity series. The metals potassium, sodium, lithium, calcium, magnesium, zinc, iron and copper can be put in order of their reactivity from their reactions with water and dilute acids.

The non-metals hydrogen and carbon are often included in the reactivity series.

The Reactivity Series

Reactions of Metals

All metals will react with substances differently, and even the same metal can be more or less reactive depending on what it is being reacted with. Rather than having multiple tables for each specific reaction, a diagram was created to show the average reactivity of metals with water and dilute acids.

The reactivity series can also be used to see the relative tendency for metal atoms to form cations - the higher up the series, the more likely it will form a positive ion.

Something similar can be said for a metal's resistance to oxidation - the higher up the series, the more easier it is to oxidise.

metal reaction with water reaction with dilute acid
potassium react with cold water to form hydrogen and a metal hydroxide react violently
sodium
calcium react to form hydrogen and a salt solution
magnesium react very slowly, if at all, with cold water - but will react with steam to form hydrogen and a metal oxide
aluminium
zinc
iron
copper react with cold water to form hydrogen and a metal hydroxide do not react
silver
gold

Displacement Reactions

A more reactive metal can displace a less reactive metal from a compound in solution. This is one way to extract metals. For example:

magnesium + copper sulfate → copper + magnesium sulfate
Mg + CuSO4 → Cu + MgSO4

Higher Tier

Ionic equations only show us the ions that change in a chemical reaction. This is useful as it shows what is oxidised and reduced. We can start by writing a balanced symbol equation for a reaction:

Mg(s) + CuSO4(aq) → Cu(s) + MgSO4(aq)

Then we can write out all the ions involved:

Cu²⁺(aq) + SO4²⁻(aq) + Mg(s) → Cu(s) + Mg²⁺(aq) + SO4²⁻(aq)

We can identify the ions that don't change, these are called the spectator ions. These are of no interest in the reaction, so we can ignore them and write out our ionic equation:

Mg(s) + Cu²⁺(aq) → Cu(s) + Mg²⁺(aq)

Once we have an ionic equation, we can take it one step further and look at half equations. These look at how the electrons behave. We can see there are only two different chemicals involved, and we can split our equation in half... to make half equations:

Cu²⁺ + 2e⁻ → Cu
Mg - 2e⁻ → Mg²⁺

By writing our equation in this way, we can immediately see that copper had to gain two electrons (reduced) in this reaction, and those electrons came from magnesium (oxidised).

Displacement of Copper from Copper Sulfate, by Magnesium

REDOX (Reduction and Oxidation)

Most metals do not exist naturally on their own, but combined with other elements, and compounds, as ores in the Earth's crust. Most ores contain oxygen, and so when a metal reacts with oxygen a metal oxide is formed. This is called oxidation.

Removing the oxygen from the compound to extract the metal is called reduction. To extract iron we need to reduce the ore. This means we take away the oxygen.

Iron is naturally found as iron oxide, so we can reduce the ore by heating it with a reducing agent. By adding carbon monoxide, we can remove the oxygen from the ore to make iron and carbon dioxide:

iron oxide + carbon monoxide → iron + carbon dioxide
Fe2O3 + CO → Fe + CO2

The metals right at the bottom of the reactivity series are unreactive, and are found as uncombined elements in the Earth's crust.

Knowledge of the blast furnace (shown here) is not needed, and is only shown to illustrate how carbon is used to extract iron.

Extracting Iron using a Blast Furnace