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Thermodynamics: Entropy, Energy & the Direction of Chemical Reactions
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Thread 4 — Thermodynamics: Entropy, Energy & the Direction of Chemical Reactions
The Deep Rules That Govern All Chemical Change

Chemical reactions don’t happen randomly. 
They follow strict universal laws that determine:

• whether a reaction is possible 
• whether it releases or absorbs energy 
• whether it happens slowly, rapidly, or not at all 
• what direction equilibrium will shift 

This thread explores the *thermodynamic foundations* of chemistry — 
the invisible laws that decide everything.



1. Energy in Chemistry — Enthalpy (ΔH)

Enthalpy measures the heat absorbed or released during a reaction.

Exothermic (ΔH < 0) 
• releases heat 
• feels hot 
• often favourable 
Example: combustion of methane

Endothermic (ΔH > 0) 
• absorbs heat 
• feels cold 
• requires energy input 
Example: photosynthesis

Enthalpy alone does NOT determine whether a reaction will happen — 
but it is one piece of the puzzle.



2. Entropy (ΔS) — The Tendency Toward Disorder

Entropy measures the number of possible arrangements of a system.

Key rules:
• gases have more entropy than liquids 
• liquids have more entropy than solids 
• more particles = higher entropy 
• spreading out = higher entropy 
• mixing increases entropy 

Entropy increases in:
• melting 
• evaporation 
• dissolving 
• reactions that produce more gas particles 

Nature tends to move toward higher entropy — 
but entropy alone still doesn’t decide everything.



3. Free Energy (ΔG) — The REAL Decision Maker

Gibbs Free Energy tells you whether a reaction is spontaneous.

ΔG = ΔH – TΔS

This combines:
• enthalpy 
• entropy 
• temperature 

A reaction is spontaneous when: 
ΔG < 0

A reaction is non-spontaneous when: 
ΔG > 0

At equilibrium: 
ΔG = 0

This single equation determines whether a reaction “wants” to happen.



4. Temperature Can Flip the Direction of a Reaction

Because ΔG depends on temperature, the same reaction can be:

• non-spontaneous at low temperature 
• spontaneous at high temperature 

Example: 
ice melts (spontaneous) at high T 
ice freezes (spontaneous) at low T

This is why some industrial reactions require heat — 
they need the entropy term (TΔS) to overpower ΔH.



5. Reaction Coupling — Biology’s Genius Trick

Many reactions in biology have ΔG > 0 (not favourable). 
So cells “pay” for them using highly favourable reactions.

The classic example:
ATP → ADP + Pi 
This releases a large amount of energy (ΔG < 0).

Cells couple this with:
• DNA synthesis 
• protein formation 
• ion pumping 
• muscle contraction 

Life exists because cells combine unfavourable steps with favourable ones.



6. Equilibrium — The Balance Point of a Reaction

Chemical equilibrium is not “stopping.” 
It’s a dynamic balance where forward and reverse rates match.

The equilibrium constant K determines the position:

K >> 1 → products favoured 
K << 1 → reactants favoured 
K = 1 → balanced 

The link between thermodynamics and equilibrium:

ΔG° = –RT ln(K)

Meaning:
• large K → very negative ΔG° (highly spontaneous) 
• small K → very positive ΔG° (not spontaneous)

Thermodynamics and equilibrium are mathematically identical.



7. Why Thermodynamics Matters

Thermodynamics predicts:
• which reactions are possible 
• how hot or cold a reaction must be 
• whether a reaction will release or absorb energy 
• how cells power their processes 
• how batteries work 
• how materials change state 
• the limits of machines 

Every chemical process — industrial or biological — is governed by ΔH, ΔS, and ΔG.



8. Master Equation Summary

The three laws of chemistry’s direction:

1. ΔH — heat flow 
2. ΔS — disorder 
3. ΔG — possibility


If you understand these, you understand why anything happens at all.



Written by Leejohnston & Liora — The Lumin Archive Research Division
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