Step 1 — Free energy of one substance depends on its pressure.
For 1 mole of an ideal gas at constant T, dG=VdP (from dG=VdP−SdT, with dT=0).
Using V=RT/P:
dG=PRTdP⇒∫P∘PdG=RT∫P∘PPdPG(P)=G∘+RTlnP∘PWhy this step? Chemical potential grows logarithmically with pressure — squeezing gas costs free energy, and the cost is RTln(ratio). Write μ=μ∘+RTlna where a=P/P∘ is the activity.
Step 2 — Build ΔG for a reaction. For aA+bB⇌cC+dD:
ΔG=∑νiμi=(cμC+dμD)−(aμA+bμB)
Substitute each μi=μi∘+RTlnai:
ΔG=ΔG∘(cμC∘+dμD∘−aμA∘−bμB∘)+RT(clnaC+dlnaD−alnaA−blnaB)
The log terms collapse using lnxn=nlnx and lnx+lny=lnxy:
ΔG=ΔG∘+RTlnQaAaaBbaCcaDdWhy this step? This is just algebra collecting all the logs into one quotient Q — the exact shape of the equilibrium expression.
Step 3 — Impose equilibrium. At equilibrium the system has no tendency to change, so ΔG=0 and Q=K:
0=ΔG∘+RTlnK⇒ΔG∘=−RTlnKWhy this step?ΔG is the slope of G vs extent of reaction. At the minimum of G (equilibrium) the slope is zero. That single physical fact is what pins ΔG∘ to K.
Recall Predict before you check (Forecast-then-Verify)
If T doubles at fixed ΔG∘<0, does K move toward 1 or away? (Answer: lnK=−ΔG∘/RT shrinks in magnitude ⇒ K moves toward 1.)
What is the relation between ΔG∘ and K?
ΔG∘=−RTlnK (equivalently K=e−ΔG∘/RT).
Difference between ΔG and ΔG∘?
ΔG = at actual composition (depends on Q); ΔG∘ = all species in standard states, a constant tied to K.
General equation linking ΔG, Q, ΔG∘?
ΔG=ΔG∘+RTlnQ.
Why is ΔG=0 at equilibrium?
G is minimum vs extent of reaction, so its slope (=ΔG) is zero.
Sign of ΔG∘ when K>1?
Negative (lnK>0).
Can a reaction with ΔG∘>0 proceed forward?
Yes, if Q<K so that ΔG<0.
What decides the actual direction of a real mixture?
Comparing Q with K (i.e. the sign of ΔG), not ΔG∘.
Base-10 form of the relation?
ΔG∘=−2.303RTlogK.
Why is K dimensionless?
It is built from activities (P/P∘, c/c∘), which are unitless.
Where does the RTln term come from physically?
From μ=μ∘+RTlna, i.e. dG=VdP=RTdP/P integrated.
Recall Feynman: explain to a 12-year-old
Imagine a ball rolling in a valley. The bottom of the valley is where the reaction "settles" — that's equilibrium. ΔG∘ tells you how deep and where the bottom is: a very deep valley on the "products" side means the reaction almost completely turns into products (huge K). If the valley bottom is more toward "reactants," you get a small K. The formula ΔG∘=−RTlnK is just the mathematical rule linking "how deep/where the valley sits" to "how much product you end with."
Dekho, thermodynamics mein sabse important rishta yahi hai: ΔG∘=−RTlnK. Iska matlab simple hai — reaction ka standard free energy change humein bata deta hai ki equilibrium par products zyada banenge ya reactants. Agar ΔG∘ bahut negative hai, to K bahut bada hoga, yaani reaction almost poora products mein convert ho jaayega. Agar ΔG∘ positive hai, to K chhota, matlab mostly reactants hi bache rahenge.
Ek cheez hamesha yaad rakho: ΔG aur ΔG∘ alag hain. ΔG∘ ek fixed constant hai (jab saare species standard state mein ho), jabki ΔG current mixture par depend karta hai — uska formula hai ΔG=ΔG∘+RTlnQ. Equilibrium par ΔG zero ho jaata hai (kyunki G ki valley ka bottom aa gaya, slope zero), aur tab Q=K ho jaata hai — bas yahin se ΔG∘=−RTlnK nikalta hai.
Bahut students yeh galti karte hain ki ΔG∘>0 dekhte hi bol dete hain "reaction hoga hi nahi". Galat! Agar starting mein product kam hai (yaani Q<K), to ΔG negative ban sakta hai aur reaction forward chalega. Direction hamesha Q aur K compare karke decide hota hai, sirf ΔG∘ se nahi.
Practical tip: numbers plug karte waqt units match karo — ΔG∘ ko Joule mein le lo (kJ ko ×1000) taaki R=8.314 ke saath sahi bethe. Aur K hamesha dimensionless hota hai kyunki wo activities (P/P∘) se banta hai. Yeh ek formula tumhare equilibrium aur spontaneity dono chapters ko jod deta hai — isliye ratta nahi, derivation samajh lo.