3.1.3 · D3 · Physics › Compressible Flow & Aerodynamics › Speed of sound — a = √(γRT) — derivation
Yeh page speed-of-sound formula ke liye "koi surprise nahi" wali drill hai. Hum
a = γ R T
ko har tarah ke case mein push karte hain jo exam ya real wing pe aa sakta hai: normal air, thandi air, dusri gases, degenerate inputs (T → 0 pe kya hoga?), classic Newton ki galti, ratios, aur ek word problem. Har example se pehle tum ek Forecast banate ho — pehle answer ka ballpark guess karo, phir khud ko check karo.
a = γ R T ke baare mein har problem inhi cells mein se kisi ek mein aata hai. Neeche ke worked examples mein har ek pe ek tag hai jo batata hai ki woh kaun si cell nail karta hai.
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Case class
Kya badalta hai
Example
A
Baseline — standard sea-level air
kuch nahi (reference case)
Ex 1
B
Cold input — T kam
T ↓⇒ a ↓
Ex 2
C
Different gas — naya γ , R , M
teeno constants swap karo
Ex 3
D
Ratio / relative — do states compare karo
constants cancel, sirf T ratio bachta hai
Ex 4
E
Degenerate / limiting — T → 0 , T → ∞
boundary behaviour
Ex 5
F
Wrong process trap — isothermal vs adiabatic
γ / Newton error
Ex 6
G
Unit trap — Celsius, ya universal R
classic slip pakdo
Ex 7
H
Real-world word problem — Mach + altitude
a ko M mein chain karo
Ex 8
I
Exam twist — ulta solve karo T ke liye
formula invert karo
Ex 9
Worked example Example 1 — Baseline: sea-level air
(cell A)
Dry air mein T = 288 K pe a nikalo, jahan γ = 1.4 , R = 287 J k g − 1 K − 1 .
Forecast: tumne shayad "lagbhag 340 m/s" suna hoga — wohi guess karo.
Root ke andar teeno numbers multiply karo: 1.4 × 287 × 288 = 115 , 718 .
Yeh step kyun? Formula a 2 = γ R T kehta hai ki answer ka square yahi product hai; hum pehle a 2 banate hain.
Square root lo: a = 115 , 718 ≈ 340 m/s .
Yeh step kyun? a 2 nahi, a chahiye; root square ko undo karta hai.
Verify: units hain 1 ⋅ kg K J ⋅ K = kg J = kg kg m 2 / s 2 = m 2 / s 2 = m/s . ✓ Yeh ek speed hai, aur ≈ 340 roz ke experience se match karta hai.
Worked example Example 2 — Cold input at cruise altitude
(cell B)
11 km pe air T = 217 K hai. Same air constants. a nikalo.
Forecast: thandi gas → dhimi sound. Toh 340 se kam . ~290–300 guess karo.
Product: 1.4 × 287 × 217 = 87 , 176 .
Yeh step kyun? Sirf T badla; constants wahi rahe, toh hum bas naye T ke saath a 2 rebuild karte hain.
Root: a = 87 , 176 ≈ 295 m/s .
Yeh step kyun? Wahi reason — square undo karo.
Verify: 295 < 340 ✓ (thanda → dhima, jaise forecast tha). Yeh bhi: 340 295 = 217/288 = 0.753 = 0.868 ✓ — neeche cell D ke ratio rule se consistent.
Worked example Example 3 — Different gas: helium
(cell C)
Helium at T = 288 K : γ ≈ 1.667 , molar mass M = 4 g/mol toh R = R u / M = 8314/4 = 2078 J k g − 1 K − 1 .
Forecast: helium air se bahut halka hai (M = 4 vs 29), toh R bahut bada hai — sound 340 se kaafi tez honi chahiye. ~1000 guess karo.
Specific R compute karo: 8314/4 = 2078 .
Yeh step kyun? a specific constant use karta hai (per kg), aur halke molecules ise bada banate hain — yahi pura reason hai ki helium fast hai.
Product: 1.667 × 2078 × 288 = 997 , 700 (approx).
Yeh step kyun? Helium ke apne teeno constants ke saath a 2 rebuild karo.
Root: a = 997 , 700 ≈ 999 m/s .
Verify: 999 ≫ 340 ✓. Isliye helium pe tumhari awaaz squeaky hoti hai — yeh medium pressure pulses ~3× tez carry karta hai. Dekho Ideal gas law and specific gas constant .
Worked example Example 4 — Ratio of two states (constants cancel)
(cell D)
Same gas, do temperatures T 1 = 288 K aur T 2 = 320 K . a 2 / a 1 nikalo bina koi bhi speed compute kiye.
Forecast: garam → tez, toh ratio > 1 , aur thoda hi (kyunki yeh T-ratio ka square root hai, changes gentle hote hain).
Likho a 1 a 2 = γ R T 1 γ R T 2 = T 1 T 2 .
Yeh step kyun? γ aur R dono mein identical hain, toh cancel ho jaate hain — ratio problem mein sirf T ki zaroorat hoti hai.
Plug in: 320/288 = 1.111 = 1.054 .
Yeh step kyun? Ab sirf ek square root hai, koi gas constants nahi chahiye.
Verify: a ∝ T , toh + 11% temperature rise se sirf + 5.4% speed rise hoti hai — square roots changes ko soften karte hain, "gentle" forecast se match karta hai. ✓
Worked example Example 5 — Degenerate & limiting inputs
(cell E)
T → 0 K pe a kya hai? Aur T → ∞ kya imply karta hai? Jahan numbers help karein wahan air constants use karo.
Forecast: absolute zero pe molecules chalna band kar dete hain, toh kuch bhi push carry nahi karta — guess a → 0 . Bahut bade T pe a bina bound ke badhta hai (lekin dheere, T ki tarah).
Limit T → 0 : a = γ R ⋅ 0 = 0 .
Yeh step kyun? Root ke neeche product vanish ho jaata hai; zero factor ise khatam kar deta hai. Physically: koi thermal molecular motion nahi → wave ke liye koi carrier nahi.
Limit T → ∞ : a = γ R T → ∞ , lekin yeh T ki tarah badhta hai, toh dheere — T double karne se a sirf 2 ≈ 1.41 se multiply hota hai.
Yeh step kyun? Exponent 2 1 control karta hai ki limit kitni tez blow up hoti hai; yeh sub-linear hai, toh koi runaway nahi.
Sanity numbers: T = 1152 K (=4 × 288 ) pe, a = 1.4 ⋅ 287 ⋅ 1152 = 462 , 872 ≈ 680 m/s — exactly 2 × 340 , kyunki 4 = 2 .
Verify: T = 0 answer 0 hai ✓ (koi negative ya complex speed nahi — hamesha physical kyunki kelvin mein T ≥ 0 ). 4 × T se 2 × a milna T scaling confirm karta hai. ✓
Worked example Example 6 — Wrong-process trap: Newton vs Laplace
(cell F)
T = 288 K pe isothermal (Newton) speed a iso = R T aur sahi adiabatic (Laplace) speed a = γ R T compute karo. Newton kitne percent galat hai?
Forecast: Newton ne γ drop kar diya, toh uska number γ = 1.4 ≈ 1.18 factor se chhota hai. Expect karo ~15% too low.
Newton: a iso = 287 × 288 = 82 , 656 ≈ 287.5 m/s .
Yeh step kyun? Isothermal p = ρR T se d p / d ρ = R T milta hai, koi γ nahi — yeh exactly woh tempting error hai jo parent note mein hai.
Laplace (sahi): a = 1.4 × a iso = 1.183 × 287.5 ≈ 340 m/s .
Yeh step kyun? Real wave adiabatic hai, a 2 ko γ se multiply karti hai, matlab a ko γ se.
Error: 340 340 − 287.5 = 0.154 = 15.4% too low.
Verify: do speeds exactly 1.4 = 1.183 se differ karti hain ✓, aur 287.5 m/s Newton ka famous ~15% miss hai. ✓
Worked example Example 7 — Unit traps: Celsius & universal
R (cell G)
Ek student likhta hai a = 1.4 × 8.314 × 15 "air at 1 5 ∘ C" ke liye. Kya do galtiyan hain, aur sahi value kya hai?
Forecast: R u = 8.314 use karna 287 ki jagah number ko ~287/8.314 ≈ 5.9 × chhota bana deta hai, aur 288 K ki jagah 15 bhi bahut galat hai. Unka answer nonsense hoga (tens of m/s).
Unki (galat) value: 1.4 × 8.314 × 15 = 174.6 ≈ 13.2 m/s .
Yeh step kyun? Dikhao ki double error kitna far off land karti hai — real sound speed ke paas kahin nahi.
Temperature fix karo: 1 5 ∘ C = 15 + 273 = 288 K .
Yeh step kyun? Formula ko absolute temperature chahiye; Celsius ka zero false hai.
Constant fix karo: R = 287 use karo (specific), R u = 8.314 (universal) nahi.
Yeh step kyun? a per-kilogram physics hai; R u per-mole hai. Pehle molar mass se divide karo: 8314/29 ≈ 287 .
Sahi value: 1.4 × 287 × 288 ≈ 340 m/s .
Verify: galat answer (13.2 ) absurd hai (ek bicycle tez hai) ✓; corrected wala 340 hai ✓.
Worked example Example 8 — Real-world word problem: Mach at altitude
(cell H)
Ek jet 11 km pe true airspeed V = 250 m/s pe cruise karta hai jahan T = 217 K hai. Kya yeh compressible regime mein hai? Dekho Compressibility and why M > 0.3 matters .
Forecast: altitude pe sound slow hai (~295 Ex 2 se), toh M = 250/295 comfortably 0.3 se upar hai — haan, compressible; shayad high-subsonic ~0.85.
Local sound speed: a = 1.4 × 287 × 217 ≈ 295 m/s (Ex 2 se).
Yeh step kyun? Mach local a use karta hai, jo local temperature se set hota hai — sea-level value nahi.
Mach number: M = a V = 295 250 ≈ 0.847 .
Yeh step kyun? M = V / a plane ki speed ko compare karta hai ki pressure signals kitni tez travel karte hain; yeh decide karta hai ki density changes matter karti hain ya nahi.
Thresholds se compare karo: 0.847 > 0.3 → compressible, aur < 1 → abhi bhi subsonic .
Verify: M ≈ 0.85 ✓ — ek realistic airliner cruise Mach. Note karo ki wahi 250 m/s sea level pe (a = 340 ) M = 0.74 deta hai: altitude pe same speed "zyada transonic" hai kyunki a drop ho gaya. ✓
Worked example Example 9 — Exam twist: ulta solve karo
T ke liye (cell I)
Ek microphone air mein a = 350 m/s measure karta hai. Air temperature kya thi?
Forecast: 350 baseline 340 -at-288 -K se thoda upar hai, toh T 288 K se thoda upar hona chahiye, shayad ~305 K.
a 2 = γ R T se shuru karo aur T isolate karo: T = γ R a 2 .
Yeh step kyun? Hume output diya gaya hai; algebra formula ko invert karta hai input recover karne ke liye.
Plug in: T = 1.4 × 287 35 0 2 = 401.8 122 , 500 ≈ 305 K .
Yeh step kyun? Fixed constants se measured a 2 divide karo temperature tak wapas pahunchne ke liye.
Verify: 305 K = 3 2 ∘ C , ek garam din — reasonable ✓. Re-forward-check: 1.4 × 287 × 305 = 122 , 549 ≈ 350 ✓, loop band ho gaya.
Recall Answers cover karo — kya tumne har cell hit ki?
Agar sirf T gire toh a kaise change hota hai? ::: Yeh girta hai, kyunki a ∝ T (cell B/D).
T 2 aur T 1 pe sound speeds ka ratio? ::: T 2 / T 1 — constants cancel ho jaate hain (cell D).
T → 0 K pe a kya hai? ::: 0 — wave carry karne ke liye koi thermal motion nahi (cell E).
Newton ki isothermal error kitni badi hai? ::: ~15% too low; usne γ factor drop kar diya (cell F).
Do classic unit slips? ::: Kelvin ki jagah Celsius; specific R ki jagah universal R u (cell G).
Measured a se T nikalne ke liye? ::: T = a 2 / ( γ R ) (cell I).
"Root the T, halve the wobble" — kyunki a ∝ T , temperature changes a mein apni percentage se aadhi ho jaati hain.