Heterogeneous equilibria — pure solids - liquids excluded
2.6.6· Chemistry › Equilibrium
Core Concept
Mathematical Wajah: Exclusion Rule Derive Karna
First Principles se Shuru Karte Hain
Kisi bhi equilibrium ke liye, thermodynamic equilibrium constant hai:
Activity kya hoti hai? Activity woh "effective concentration" hai jo non-ideal behavior ko account karti hai:
jahan activity coefficient hai, concentration/pressure hai, aur standard state hai.
Alag-Alag Phases ke Liye:
- Gases: jahan bar
- Aqueous solutions: (dilute approximation)
- Pure solids/liquids: har waqt!
Pure substances ke liye kyun hota hai?
Pure solid ya liquid ke liye, standard state ko khud woh pure substance choose kiya jaata hai. Activity uss standard state ke ratio ke roop mein define hoti hai:
Lekin "actual" pure phase hi standard state hai. Uska molar concentration fixed rehta hai:
Kyunki numerator aur denominator same fixed quantity hain:
Zyada solid add karne se total amount badhti hai lekin density ya molar mass nahi badhta, isliye activity exactly 1 hi rehti hai.
Exclusion Ka Practical Use
Consider karo:
Poora expression:
Kyunki aur :

Include karo:
- Gases: ke liye partial pressures use karo ya ke liye concentrations
- Aqueous ions/molecules: molar concentrations use karo
Exclude karo:
- Pure solids
- Pure liquids (including dilute aqueous solutions mein paani)
- Solvents jo bahut zyada excess mein hain
Relationship: jahan
Worked Examples with Step Reasoning
Is equilibrium ke liye likho.
Step 1: Phases identify karo
- : solid → exclude
- : solid → exclude
- : gas → include
Yeh step kyun? Sirf CO₂ ka pressure independently vary kar sakta hai. Solids ki "concentrations" unki densities se fixed hoti hain.
Step 2: Sirf included species ke saath expression likho
Physical meaning: Ek given temperature par, limestone tab tak decompose hota rahega jab tak CO₂ ek specific pressure tak na pahunch jaaye. Agar CO₂ pump out kar do, aur zyada limestone decompose hoga. Agar se zyada CO₂ add kar do, toh CaO aur CO₂ react karke CaCO₃ banate hain.
Numerical: Approximately 1100 K par, atm. (Calcium carbonate sirf high temperatures par appreciably decompose hota hai, roughly 900 °C ≈ 1173 K, jahan 1 atm tak pahunchta hai.) Iska matlab hai limestone spontaneously decompose hota hai jab surrounding us temperature par equilibrium value se neeche ho.
(solubility product) likho.
Step 1: Phases identify karo
- : solid → exclude
- : aqueous → include
- : aqueous → include
Yeh step kyun? Undissolved AgCl pure solid hai. Sirf dissolved ions ke concentrations variable hote hain.
Step 2: Expression likho
Physical interpretation: humein bataata hai ki saturation par ion concentrations ka maximum product kya ho sakta hai. Chahe kitna bhi solid AgCl paani mein daalo, product kabhi se zyada nahi ho sakta.
Numerical: at 25°C. Pure water mein, agar ho, toh , isliye , jo deta hai M.
High temperature par likho.
Step 1: Phases identify karo
- : solid (graphite) → exclude
- , , : sab gases → include
Yeh step kyun? High T par, paani steam (gas) hota hai, liquid nahi. Solid carbon ki activity 1 hai.
Step 2: Expression likho
Key insight: Aur graphite add karne se equilibrium shift nahi hota—sirf gas partial pressures change karne se farq padta hai.
Numerical reasoning: Agar at 1000 K aur initially atm, :
- Maano = extent of reaction
- Equilibrium par: ,
- → → atm
Yeh step kyun? Hum positive root lete hain kyunki pressure positive honi chahiye; , isliye atm.
Kya iron catalyst mein appear karta hai?
Answer: Nahi. Catalysts dono forward aur reverse reactions ko equally speed up karte hain—yeh equilibrium position shift nahi karte. Chahe Fe solid ho, yeh reactant ya product bhi nahi hai, isliye yeh doubly excluded hai.
Yeh kyun important hai: Equilibrium tak pahunchne ki speed badhane ke liye tum tons catalyst add kar sakte ho, lekin final pressures sirf , T, aur initial amounts par depend karte hain.
Common Mistakes aur Steel-Manning
Kyun sahi lagta hai: Roz ki zindagi mein, zyada starting material → zyada product. Confusion isliye hoti hai kyunki hum solids ko gases ki tarah "use up" hone wala samajhte hain.
Sach: Jab tak koi bhi solid present hai, aur zyada add karne se equilibrium position nahi badlti. Solid ki activity pehle se hi apne maximum (1) par hai. Aise sochiye: solid surface reaction ke liye sites provide karta hai, lekin saari available sites pehle se hi use ho rahi hain. Zyada solid = zyada sites, lekin har site par same rate, isliye same equilibrium.
Sahi: Equilibrium par CO₂ ki amount sirf temperature par depend karti hai (jo determine karta hai), nahi iss par ki tumne kitna CaCO₃ liya tha—jab tak kuch CaCO₃ unreacted raha ho.
Caveat: Agar tum itna thoda CaCO₃ se start karo ki woh poora decompose ho jaaye, toh tumhare paas equilibrium nahi hai (solid phase bacha hi nahi). Yeh ek alag scenario hai—system ab heterogeneous nahi raha.
Kyun sahi lagta hai: Zyaatar aqueous chemistry mein (acids, bases, salts dissolving), paani solvent hota hai bahut zyada excess mein, isliye uski activity ≈ 1 rehti hai.
Sach: Paani tabhi exclude hota hai jab woh pure liquid ya solvent bahut zyada excess mein ho. Agar paani:
- Gas (steam) ho: include karo! Example: →
- Non-aqueous solution mein ho jahan uska concentration significantly vary karta hai: include karo!
- Apni initial quantity ke relative significant amount mein consume/produce ho raha ho: include karo!
Decision rule: Agar substance ki amount itni change hoti hai ki uski concentration/activity meaningfully affect ho, toh include karo. Agar yeh ek ocean hai jo barely ripple karta hai, toh exclude karo.
Kyun sahi lagta hai: Hum ratios ke aadi hain—agar main numerator double karunga, ratio change ho jaayega.
Sach: sirf temperature par depend karta hai. Yeh ek fundamental thermodynamic property hai. Solid add karne se na forward na reverse rate constants () change hote hain, aur kyunki , K same rehta hai.
Jo actually change hota hai: Equilibrium tak pahunchne ka time change ho sakta hai (zyada surface area → faster), lekin equilibrium position (final pressures/concentrations) identical hoti hai.
Analogy: ek "finish line" jaisa hai jo temperature set karta hai. Tum alag-alag raaste le sakte ho (alag initial amounts), lekin hamesha same jagah pahunchte ho.
Active Recall Practice
Recall Feynman: 12-saal ke bacche ko samjhao
Imagine karo tumhare paas sugar cubes ka ek dher hai aur paani ka ek glass. Agar ek sugar cube daalo, kuch dissolve ho jaata hai. Agar das sugar cubes daalo, total zyada sugar dissolve hota hai, lekin paani itna hi hold kar sakta hai—aakhirkar woh "saturated" ho jaata hai aur aur dissolve nahi kar sakta.
Us saturated paani mein, dissolved sugar ki concentration same hoti hai chahe neeche 1 extra cube baitha ho ya 100 extra cubes. Paani har case mein "full" hai.
Chemical reactions ke liye, pure solids aur liquids un extra undissolved cubes ki tarah hain. Woh wahin hain, reaction ka hissa hain, lekin aur add karne se solution mein dissolved ya gas ke roop mein floating jo hai woh nahi badalta. Equilibrium "balance" sirf un cheezein ki care karta hai jo freely move kar sakti hain—gases aur dissolved stuff—nahi un bade solid chunks ki jo neeche baithe hain.
Isliye jab hum equilibrium math formula (jise kehte hain) likhte hain, hum sirf un cheezein ko include karte hain jinki amounts actually change hoti hain aur matter karti hain: gases aur dissolved chemicals. Solids aur pure liquids hamesha "full strength" par hain, isliye hum unhe formula mein nahi likhte, taaki yeh simple aur accurate rahe.
Connections and Extensions
Prerequisites:
- Chemical Equilibrium Fundamentals
- Equilibrium Constant Expressions
- Le Chatelier's Principle
- Activity vs Concentration
Related Concepts:
- Solubility Product (Ksp)
- Precipitation Reactions
- Phase Diagrams
- Gibbs Free Energy and Equilibrium
Applications:
- Metallurgy: Ore Reduction
- Cement Production
- Limestone Caves and Stalactites
- Buffer Solutions (when water matters)
Advanced:
- Ellingham Diagrams for Metal Oxides
- Activity Coefficients in Concentrated Solutions
- Multi-phase Equilibria
#flashcards/chemistry
Pure solids aur liquids ko equilibrium expressions se kyun exclude kiya jaata hai? :: Unki activity constant (≈1) rehti hai chahe kitni bhi amount present ho, kyunki pure substance ke liye concentration = density/molar mass nahi badlta. K mein ek constant ko include karna redundant hai—use equilibrium constant ki value mein absorb kar lete hain.
Is equilibrium ke liye expression likho: CaCO₃(s) ⇌ CaO(s) + CO₂(g) :: (solids excluded; sirf gas partial pressure include hoti hai)
AgCl(s) ⇌ Ag⁺(aq) + Cl⁻(aq) ke liye Ksp kya hai?
Agar tum equilibrium CaCO₃(s) ⇌ CaO(s) + CO₂(g) mein aur CaCO₃(s) add karo, toh kya equilibrium par CO₂ ki amount change hoti hai?
Paani ko equilibrium expression mein kab include kiya jaata hai?
K kis par depend karta hai?
C(s) + H₂O(g) ⇌ CO(g) + H₂(g) ke liye Kp likho :: (solid carbon excluded; paani yahan gas hai, isliye included)
N₂ + 3H₂ ⇌ 2NH₃ mein solid catalyst K mein kyun nahi aata?
Agar equilibrium reach hone se pehle saara CaCO₃ decompose ho jaaye, toh kya system abhi bhi heterogeneous hai?
Heterogeneous equilibrium ke liye Kp aur Kc relate karo :: jahan = (gas products ke moles) − (gas reactants ke moles). R = 0.0821 L·atm/(mol·K) ya 8.314 J/(mol·K).