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Chemistry · Ch 13 — General Principles and Processes of Isolation of Elements

Thermodynamic Principles of Metallurgy

13.4

Thermodynamic Principles of Metallurgy

Deciding how hot a reduction needs to run, and which reducing agent will actually do the job for a given metal oxide MxOyM_xO_y, isn't guesswork — it follows directly from Gibbs energy.

The basic criterion

For a thermal reduction to proceed at a given temperature, the Gibbs energy change of the reaction must be negative. Gibbs energy varies with temperature according to the familiar relation:

ΔG=ΔH−TΔS(6.14)\Delta G = \Delta H - T\Delta S \qquad(6.14)

where ΔH\Delta H is the enthalpy change and ΔS\Delta S is the entropy change of the process. A reaction only goes forward when ΔG\Delta G works out negative, and there are two distinct ways to engineer that:

  1. Raise the temperature, when ΔS\Delta S is positive. As TT increases, the TΔST\Delta S term grows, and once TΔST\Delta S overtakes ΔH\Delta H, ΔG\Delta G swings negative.
  2. Couple two reactions — an oxidation and a reduction — so that even if neither is favourable alone, their combined ΔG\Delta G is negative. This is the trick underlying almost every real metallurgical reduction.

The Ellingham diagram

Plotting ΔrG∘\Delta_r G^\circ against TT for the formation of metal oxides (per mole of O2O_2 consumed) gives what's called an Ellingham diagram (Fig. 6.4), first devised by H.J.T. Ellingham. It is the single most useful graphical tool for choosing a reducing agent.

Why the lines slope upward. The plotted reaction is 2xM(s)+O2(g)→2MxO(s)2xM(s) + O_2(g) \rightarrow 2M_xO(s). A gas is consumed in forming the oxide, so molecular randomness decreases — ΔS\Delta S is negative — which makes the −TΔS-T\Delta S term in equation 6.14 positive. So ΔrG∘\Delta_r G^\circ climbs upward (becomes less negative) as TT rises, giving most metal-oxide lines a positive slope.

Kinks mark phase changes. Each line is essentially straight except where the metal or its oxide changes phase (solid→liquid or liquid→gas) — at that temperature the slope visibly steepens on the positive side (the Zn/ZnO line, for instance, kinks where zinc melts).

The line crossing zero. As TT rises further, a line eventually crosses ΔrG∘=0\Delta_r G^\circ = 0. Below that crossing, the oxide is thermodynamically stable (ΔrG∘\Delta_r G^\circ negative); above it, ΔrG∘\Delta_r G^\circ turns positive and the oxide will spontaneously decompose.

Similar diagrams can be drawn for sulphides and halides, and they make it obvious why reducing MxSM_xS compounds is generally much harder than reducing the corresponding oxide.

Two limitations worth remembering:

  • The diagram only tells you whether reduction is thermodynamically possible, not how fast it happens — it says nothing about kinetics. It does, however, explain qualitatively why solid-state reactions are sluggish while reactions speed up once the ore melts (molecular randomness — and hence ΔS\Delta S — jumps at a phase change).
  • The ΔrG∘\Delta_r G^\circ values are derived via ΔG∘=−RTln⁡K\Delta G^\circ = -RT\ln K, which presumes reactants and products are at equilibrium. In an actual furnace, solids and gases are often in contact for only a short time, so this assumption doesn't strictly hold.

Coupling reduction and oxidation

During reduction, the metal oxide decomposes and the reducing agent carries the released oxygen away. For the reducing agent to succeed, its own oxidation must have a ΔrG∘\Delta_r G^\circ negative enough that the sum with the oxide's decomposition is negative overall.

Write the oxide's decomposition as:

MxO(s)→xM (solid or liquid)+12O2(g)[ΔrG∘(M,O,M)](6.15)M_xO(s) \rightarrow xM\ (\text{solid or liquid}) + \tfrac{1}{2}O_2(g) \qquad [\Delta_rG^\circ(M,O,M)] \qquad(6.15)

If carbon is the reducing agent, its oxidation can go two ways:

C(s)+12O2(g)→CO(g)[ΔrG∘(C,CO)](6.16)C(s) + \tfrac{1}{2}O_2(g) \rightarrow CO(g) \qquad [\Delta_rG^\circ(C,CO)] \qquad(6.16)

12C(s)+12O2(g)→12CO2(g)[12ΔrG∘(C,CO2)](6.17)\tfrac{1}{2}C(s) + \tfrac{1}{2}O_2(g) \rightarrow \tfrac{1}{2}CO_2(g) \qquad [\tfrac{1}{2}\Delta_rG^\circ(C,CO_2)] \qquad(6.17)

Coupling 6.15 with 6.16, or with 6.17, gives the two possible overall reduction reactions:

MxO(s)+C(s)→xM(s or l)+CO(g)(6.18)M_xO(s) + C(s) \rightarrow xM(s\ \text{or}\ l) + CO(g) \qquad(6.18)

MxO(s)+12C(s)→xM(s or l)+12CO2(g)(6.19)M_xO(s) + \tfrac{1}{2}C(s) \rightarrow xM(s\ \text{or}\ l) + \tfrac{1}{2}CO_2(g) \qquad(6.19)

If carbon monoxide itself is the reducing agent, the relevant oxidation is:

CO(g)+12O2(g)→CO2(g)[ΔrG∘(CO,CO2)](6.20)CO(g) + \tfrac{1}{2}O_2(g) \rightarrow CO_2(g) \qquad [\Delta_rG^\circ(CO,CO_2)] \qquad(6.20)

giving the overall reaction:

MxO(s)+CO(g)→xM(s or l)+CO2(g)(6.21)M_xO(s) + CO(g) \rightarrow xM(s\ \text{or}\ l) + CO_2(g) \qquad(6.21)

Reading the diagram to pick a reducing agent …

Figure 6.4Gibbs energy (ΔrG°) vs T plots (schematic) for the formation of some oxides per mole of oxygen consumed (Ellingham diagram)

What this figure shows. A graph with vertical axis 'ΔrG° kJ mol⁻¹' running from 0 at the top down to −1200 at the bottom, and a horizontal 'Temperature' axis with two aligned scales — °C (0, 400, 800, 1200, 1600, 2000) above K (273, 673, 1073, 1473, 1873, 2273) — with an arrow pointing right. Eight labelled, mostly-straight lines are plotted: '2Mg + O2 → 2MgO' is the lowest (most negative) line, starting near −1150 and rising to about −900, with a small red-dot kink partway (a phase-change break); '4/3Al + O2 → 2/3Al2O3' sits just above it, from about −900 rising to about −800, also with a red-dot kink; '2Zn + O2 → 2ZnO' starts near −480 with a red-dot kink where the slope changes (zinc's melting point) and then rises; '2Fe + O2 → 2FeO' starts near −480 too and rises gradually, roughly parallel to and just above the Zn line; '4Cu + O2 → 2Cu2O' starts near −280 (one of the highest/least-negative lines at low T) with two red-dot kinks and rises toward nearly 0 at high T; 'C + O2 → CO2' is drawn as an almost flat horizontal line at about −395 to −400 across the whole range; '2C + O2 → 2CO' starts near −400 but slopes steeply DOWNWARD (becoming more negative) as temperature rises, crossing beneath the metal-oxide lines, reaching about −700 by 2000°C; '2CO + O2 → 2CO2' starts near −500 and rises the most steeply of all, ending as the topmost (least negative) line near −100 by 2000°C. The upward-sloping metal lines (Mg, Al, Zn, Fe, Cu oxidation) crossing the downward-sloping C→C …