3.4.18 · D3 · Physics › Rocket Flight Mechanics › Fairing separation — altitude, dynamic pressure requirements
Intuition Yeh page kya hai
Parent note ne physics build ki thi: dynamic pressure q = 2 1 ρ v 2 , heat flux q ˙ = 2 1 ρ v 3 = q v , exponential density law ρ = ρ 0 e − h / H , aur Δ v trade. Yahan hum har case drill karte hain jo exam ya real mission throw kar sakta hai — ordinary numbers se lekar zero-density limits tak, trajectory twist tak. Compute karne se pehle guess karo; isi se intuition pakki hoti hai.
Theory ke liye parent dekho: 3.4.18 parent . Building blocks: Dynamic Pressure (Max-Q) , Atmospheric Density Model — Scale Height , Rocket Equation & Mass Ratios , Aerodynamic Heating & Free-Molecular Flow , Ascent Trajectory Optimization .
H
Scale height H woh altitude gain hai jitne mein atmospheric density ρ ek factor of e ≈ 2.718 se drop ho jaati hai. Yeh atmosphere ka natural "thickness ruler" hai: har H km upar jaane par density e se divide ho jaati hai. Earth ke lower thermosphere ke liye hum H ≈ 7.5 km lete hain. Yahi density law ρ = ρ 0 e − h / H ko chalata hai — dekho Atmospheric Density Model — Scale Height . Kyunki H neeche har formula mein aata hai, iska meaning ("har H km mein density ek e -fold") pehli line se yaad rakho.
Definition Jettison altitude
h jett
h jett woh altitude hai jahan fairing drop ki jaati hai — woh height jahan payload ka heat flux abhi safe limit tak gir gaya ho. Closed form mein (parent se):
h jett = H ln q ˙ limit 2 1 ρ 0 v 3 .
Yeh neeche lagbhag har example mein aata hai; jab bhi subscript "jett" dekho, matlab hai "woh height jahan hum jaane dete hain."
C D aur A (sirf q motivate karne ke liye use hote hain)
Drag-force formula F = C D q A mein: A frontal area hai (vehicle ki woh shadow jo hawa mein padti hai, m 2 mein) aur C D drag coefficient hai (ek dimensionless shape factor, nose cone ke liye roughly 0.5 –1 ). Hum yeh formula sirf isliye mention karte hain taaki dikhayein kyun q useful hai; kisi bhi example mein numeric C D ya A ki zaroorat nahi.
Definition Free-molecular flow (kyun
v 3 )
Kam altitude par, hawa dense hoti hai aur continuous fluid ki tarah behave karti hai (continuum flow ). Bahut upar hawa itni patli ho jaati hai ki ek molecule do collisions ke beech jo average distance travel karta hai (the mean free path ) vehicle se bada ho jaata hai — yahi free-molecular flow hai. Tab har molecule surface se independently takraata hai, apni kinetic energy 2 1 m v 2 dump karta hai. Mass arrival rate (∝ ρ v ) ko har molecule ki energy (∝ v 2 ) se multiply karne par heating ∝ ρ v 3 milti hai. v ki extra power (teen, do nahi) free-molecular signature hai — yahi heat flux ko ordinary drag force se alag karti hai.
Common mistake Unit consistency — yeh ek baar padho
Poore mein, altitude h aur scale height H kilometres mein hain , lekin velocity v metres/second mein hai aur density kg/m 3 mein. Yeh safe hai kyunki h aur H hamesha saath ratio h / H ke roop mein aate hain (kilometres cancel ho jaate hain), jabki v , ρ , q , q ˙ poori tarah SI (m, kg, s) mein rehte hain. Kabhi bhi ek km-altitude ko un formulas mein mat milaao jahan metres hain — pehle H se divide karo.
Definition Threshold par decision rule
Hum strict-safety convention adopt karte hain: fairing tab hi release ki ja sakti hai jab
q ˙ < q ˙ limit ( strictly below ) .
Exact equality q ˙ = q ˙ limit ko last unsafe instant maana jaata hai — boundary "abhi nahi" se belong karti hai. Toh "jettison at h jett " ka matlab hai pehla moment jab hum us height se thoda upar chadh gaye hon.
q ˙ = 2 1 ρ v 3 model valid hai
Free-molecular formula sirf free-molecular flow mein accurate hai — in speeds ke liye roughly 90–100 km se upar. Neeche, hawa continuum ya transitional flow mein hoti hai aur heating alag (kam) laws follow karti hai; v 3 formula wahan heating ko buri tarah over-estimate kar deta. Kyunki fairing jettison 110–140 km par hoti hai, hum safely free-molecular regime ke andar hain aur formula apply hota hai. Ise kam altitude tak mat kheencho.
Is topic ka har problem in cells mein se kisi ek mein aata hai. Neeche ke examples cell ke hisaab se label hain taaki dekh sako ki poora map cover hua hai.
Cell
Kya vary karta hai / trap
Example
A. Forward
Given h , v → find q aur q ˙ , decide jettison
Ex 1
B. Inverse (altitude)
Given flux limit → solve for h jett
Ex 2
C. Inverse (velocity)
Given h aur limit → kaunsa v limit trip karta hai
Ex 3
D. Zero / degenerate
v = 0 , ya h → ∞ (ρ → 0 ) — no heating
Ex 4
E. Limiting / scaling
Agar v double ho toh h jett kitna shift hoga? (log behaviour)
Ex 5
F. Trajectory twist
Steeper/faster ascent → higher jettison altitude
Ex 6
G. Δ v trade
Fairing carry karne vs drop karne ka mass penalty
Ex 7
H. Word / real-world
Mission engineer ka "is it safe yet?" call
Ex 8
Figure s01 ek single vertical logarithmic scale par dikhata hai ki jaise altitude badhti hai (fixed v = 4000 m/s ke liye) do quantities kaise girte hain:
cyan curve hai dynamic pressure q = 2 1 ρ v 2 (Pa mein),
amber curve hai heat flux q ˙ = 2 1 ρ v 3 (W/m 2 mein).
Horizontal axis altitude h km mein hai (60→160). Notice karo dono curves log scale par straight lines hain — yeh exponential density law ρ = ρ 0 e − h / H khud ko dikha rahi hai (ek exponential ka log straight line hota hai). Amber curve cyan wali se v = 4000 factor upar hai, exactly relation q ˙ = q v ki tarah. Dashed white horizontal line safe limit 1135 W/m 2 mark karti hai; dotted white vertical line jahan amber curve us se milti hai woh h jett ≈ 130 km hai — us intersection ko padho aur tumhare paas Example 2 ka jawab hai.
Definition Poore mein use hone wale constants
Jab tak problem kuch aur na kahe: sea-level density ρ 0 = 1.2 kg/m 3 , scale height H = 7.5 km , heat-flux limit q ˙ limit = 1135 W/m 2 . Standard gravity g 0 = 9.81 m/s 2 .
Worked example Example 1 — Kya 115 km par jettison karna safe hai?
Ek rocket h = 115 km par v = 4000 m/s se fly kar raha hai. q aur q ˙ find karo, phir decide karo.
Forecast: guess karo — kya q ˙ 1135 W/m 2 se upar hoga ya neeche? (Hint: v 3 enormous hai.)
Step 1 — altitude se density. ρ = ρ 0 e − h / H = 1.2 e − 115/7.5 = 1.2 e − 15.33 ≈ 2.6 × 1 0 − 7 kg/m 3 .
Yeh step kyun? Altitude physics mein sirf density ke through enter karti hai; is page par koi aur cheez directly h par depend nahi karti. (Yahan h / H = 115/7.5 — km cancel km, jaise promise kiya tha.)
Step 2 — dynamic pressure. q = 2 1 ρ v 2 = 0.5 × 2.6 × 1 0 − 7 × 400 0 2 ≈ 2.1 Pa .
Yeh step kyun? q aerodynamic "punch" hai; yeh drag force F = C D q A mein coefficient hai (upar C D aur A define hain), isliye yeh heat flux ka natural bridge hai.
Step 3 — heat flux. q ˙ = q v = 2.1 × 4000 ≈ 8.4 × 1 0 3 W/m 2 .
Yeh step kyun? Heat = energy/time = force-like flux × velocity, isliye hum q ko ek aur v se multiply karte hain (free-molecular v 3 signature).
Decision: 8.4 × 1 0 3 > 1135 → bahut jaldi hai. Aur upar ruko.
Verify: q ˙ ke units: [ Pa ] ⋅ [ m/s ] = m 2 N ⋅ s m = m 2 s N⋅m = m 2 s J = W/m 2 . ✓ Flux ke liye correct units.
Worked example Example 2 — Kis altitude par safe ho jaata hai?
Same v = 4000 m/s . h jett find karo jahan q ˙ = 1135 W/m 2 .
Forecast: Ex 1 ne kaha 115 km bahut hot hai. Guess karo: 130 km se upar hai ya neeche?
Step 1 — required density. q ˙ = 2 1 ρ v 3 se: ρ = v 3 2 q ˙ = 400 0 3 2 × 1135 = 6.4 × 1 0 10 2270 ≈ 3.5 × 1 0 − 8 kg/m 3 .
Yeh step kyun? Hum woh density chahte hain jis par heating exactly limit hit kare; flux formula ko ρ ke liye invert karo.
Step 2 — density law invert karo. h = H ln ρ ρ 0 = 7.5 ln 3.5 × 1 0 − 8 1.2 = 7.5 ln ( 3.4 × 1 0 7 ) ≈ 7.5 × 17.35 ≈ 130 km .
Yeh step kyun? Log ek gigantic density ratio (3.4 × 1 0 7 ) ko ek friendly number (≈ 17 ) mein badal deta hai; isi liye hum yahan logarithms use karte hain.
Answer: 130 km se thoda upar jettison karo (strict rule: 130 km par hum abhi limit par hain, isliye thoda aur chadho). Yeh parent note ke 110–140 km ke quoted band ke andar aata hai jo real launch programs ke liye hai, toh number physically reasonable hai.
Verify: 130 km plug back karo: ρ = 1.2 e − 130/7.5 = 1.2 e − 17.33 ≈ 3.6 × 1 0 − 8 , phir q ˙ = 2 1 ρ v 3 ≈ 1150 W/m 2 ≈ 1135 . ✓ (Thodi rounding.)
Worked example Example 3 — Fixed altitude, kaunsi speed limit trip karti hai?
h = 120 km par, kaunsi velocity q ˙ ko exactly 1135 W/m 2 banati hai?
Forecast: 120 km par density patli hai, toh kya rocket ko limit tak pahunchne ke liye slow ya fast hona chahiye?
Step 1 — 120 km par density. ρ = 1.2 e − 120/7.5 = 1.2 e − 16 ≈ 1.35 × 1 0 − 7 kg/m 3 .
Yeh step kyun? Altitude fix karo → density fix karo; ab sirf v unknown hai.
Step 2 — flux ko v ke liye solve karo. q ˙ = 2 1 ρ v 3 ⇒ v = ( ρ 2 q ˙ ) 1/3 = ( 1.35 × 1 0 − 7 2 × 1135 ) 1/3 .
Yeh step kyun? v ko isolate karo; kyunki q ˙ ∝ v 3 (upar define ki gayi free-molecular signature), hum cube root lete hain, square root nahi.
Step 3 — evaluate karo. 1.35 × 1 0 − 7 2270 ≈ 1.68 × 1 0 10 , aur ( 1.68 × 1 0 10 ) 1/3 ≈ 2560 m/s .
Answer: strict rule se, 120 km par v ≥ 2560 m/s abhi bhi unsafe hai; sirf v < 2560 m/s safe hai.
Verify: v = 2560 back-substitute karo: 2 1 ( 1.35 × 1 0 − 7 ) ( 2560 ) 3 ≈ 1132 W/m 2 ≈ 1135 . ✓
Worked example Example 4 — Edge cases:
v = 0 aur h → ∞
(a) Rocket momentarily hawa ke relative rest mein. (b) Rocket deep space mein, ρ → 0 .
Forecast: in mein se kaunsa payload ko abhi bhi cook kar sakta hai? (Koi nahi — kyun dekho.)
Step 1 — v = 0 . q ˙ = 2 1 ρ ⋅ 0 3 = 0.
Yeh step kyun? Koi motion nahi → koi molecule surface se nahi takraate → zero convective heating, chahe hawa kitni bhi thick ho.
Step 2 — h → ∞ . ρ = ρ 0 e − h / H → 0 , toh q ˙ = 2 1 ρ v 3 → 0 kisi bhi finite v ke liye.
Yeh step kyun? Yahi jettison ka poora point hai: itna upar jao ki density heating ko khatam kar de chahe speed kitni bhi ho.
Step 3 — khatarnak corner. Heating sirf tab badi hoti hai jab dono ρ aur v appreciable hoon. Product ρ v 3 asli master variable hai; koi bhi factor zero jaane par q ˙ → 0 .
Yeh step kyun? Yeh classic error rokta hai ki sirf altitude ya sirf speed dekho.
Verify: lim v → 0 2 1 ρ v 3 = 0 aur lim h → ∞ 2 1 ρ 0 e − h / H v 3 = 0 . ✓ Dono limits vanish ho jaate hain.
Worked example Example 5 — Agar rocket twice as fast ho, toh kitna aur upar chadna padega?
Threshold aur ρ 0 , H fixed. v aur 2 v ke liye h jett compare karo.
Forecast: double speed → double altitude? Guess karo, phir log check karo.
Step 1 — jettison altitude likho. h jett = H ln q ˙ limit 2 1 ρ 0 v 3 .
Yeh step kyun? Yeh parent se closed form hai; sirf log ke andar v 3 badalta hai.
Step 2 — 2 v vs v ka difference lo. Δ h = H [ ln ( 2 v ) 3 − ln v 3 ] = H ln v 3 ( 2 v ) 3 = H ln 8 = 3 H ln 2.
Yeh step kyun? Logs subtract karna change ko isolate karta hai; density aur threshold constants cancel ho jaate hain.
Step 3 — number. Δ h = 3 × 7.5 × ln 2 = 22.5 × 0.693 ≈ 15.6 km .
Yeh step kyun? Scaling law ko ek concrete "~16 km aur chadho" mein badle.
Answer: speed double karne par jettison altitude sirf ~15.6 km badhti hai, double NAHI hoti — kyunki altitude logarithm ke through enter karti hai. Ek badi speed change sirf ek modest height change maangti hai.
Verify: 3 H ln 2 = 3 ( 7.5 ) ( 0.6931 ) ≈ 15.6 km . ✓
Figure s02 jettison altitude h jett ko vertical axis par kilometres mein plot karta hai versus jettison par velocity v ko horizontal axis par metres per second mein (range 2500→6000), closed form h jett = H ln q ˙ limit 2 1 ρ 0 v 3 use karke. Cyan curve dheere badhti hai (yeh logarithm hai), aur do marked dots is example ki do trajectories hain: slower amber dot (A, v = 3500 m/s par) neeche hai, faster white dot (B, v = 5000 m/s par) upar hai. Dekho speed (m/s) mein bade jump ke liye height (km) kitni kam badhti hai — woh gentle slope hi is example ka poora lesson hai. Calculation follow karo, phir apne numbers un dono dots se check karo.
Worked example Example 6 — Steep-and-fast vs shallow-and-slow
Trajectory A jettison conditions v A = 3500 m/s par reach karti hai, trajectory B v B = 5000 m/s par (steeper, faster). Kaun upar jettison karta hai, aur kitne se?
Forecast: faster trajectory — zyada upar jettison karega ya kam? (v 3 yaad karo.)
Step 1 — har ek ke liye altitude. h = H ln q ˙ limit 2 1 ρ 0 v 3 with 2 1 ρ 0 = 0.6 .
Yeh step kyun? Same formula, do velocities; difference wahi hai jo chahiye. Yahi woh curve hai jo s02 mein draw ki gayi hai.
Step 2 — trajectory A. 1135 0.6 × 350 0 3 = 1135 0.6 × 4.29 × 1 0 10 ≈ 2.27 × 1 0 7 , toh h A = 7.5 ln ( 2.27 × 1 0 7 ) ≈ 7.5 × 16.94 ≈ 127 km . (Yeh s02 mein amber dot hai.)
Step 3 — trajectory B. 1135 0.6 × 500 0 3 = 1135 0.6 × 1.25 × 1 0 11 ≈ 6.61 × 1 0 7 , toh h B = 7.5 ln ( 6.61 × 1 0 7 ) ≈ 7.5 × 18.01 ≈ 135 km . (s02 mein white dot.)
Answer: faster trajectory B upar jettison karta hai (135 vs 127 km) — difference Δ h = 3 H ln ( 5000/3500 ) = 3 ( 7.5 ) ln ( 1.4286 ) ≈ 8 km hai. Yeh exactly parent ki warning hai: "steeper, faster → higher jettison altitude."
Verify: h B − h A = 3 H ln ( v B / v A ) = 22.5 ln ( 1.4286 ) ≈ 8.0 km , 135 − 127 se match karta hai. ✓
Worked example Example 7 — Fairing drop karne se kitna
Δ v bachta hai?
Upper stage: I s p = 450 s , m 0 = 20000 kg , m f = 6000 kg , fairing m f r = 1000 kg . Underlying equation ke liye dekho Rocket Equation & Mass Ratios .
Forecast: saving guess karo — tens, hundreds, ya thousands of m/s?
Step 1 — carry-through Δ v . Δ v = I s p g 0 ln m f m 0 = 450 × 9.81 × ln 6000 20000 = 4415 × 1.204 ≈ 5316 m/s .
Yeh step kyun? Rocket equation mass ratio ko velocity budget mein convert karta hai. Yahan hum fairing ko poore burn mein saath rakhte hain, toh yeh m 0 aur m f dono ko inflate karta hai.
Step 2 — drop-early Δ v . Dono masses m f r se girte hain: Δ v ′ = 4415 ln 5000 19000 = 4415 × 1.335 ≈ 5893 m/s .
Yeh step kyun? Dono ends se 1000 kg remove karna ratio 19000/5000 = 3.8 ko 20000/6000 = 3.33 se upar le jaata hai; zyada ratio zyada Δ v deta hai.
Step 3 — gain. Δ v saved = 5893 − 5316 ≈ 577 m/s .
Yeh step kyun? Yahi woh payoff hai jo engineers ko jitni jaldi heat limit allow kare utni jaldi jettison karne par push karta hai.
Answer: ~577 m/s free — orbit insertion change karne ke liye kaafi.
Verify: 4415 ( ln 3.8 − ln 3.333 ) = 4415 × 0.1307 ≈ 577 m/s . ✓
Worked example Example 8 — Flight director ka "go/no-go"
Telemetry: h = 112 km , v = 4200 m/s . Payload limit q ˙ limit = 1135 W/m 2 . Kya abhi fairing sep ke liye "GO" hai?
Forecast: 112 km manual ke hisaab se "kaafi upar" lagta hai — lekin altitude nahi, flux check karo.
Step 1 — density. ρ = 1.2 e − 112/7.5 = 1.2 e − 14.93 ≈ 3.9 × 1 0 − 7 kg/m 3 .
Yeh step kyun? Reported altitude ko us density mein convert karo jo actually heating drive karti hai.
Step 2 — heat flux. q ˙ = 2 1 ρ v 3 = 0.5 × 3.9 × 1 0 − 7 × 420 0 3 ≈ 0.5 × 3.9 × 1 0 − 7 × 7.41 × 1 0 10 ≈ 1.45 × 1 0 4 W/m 2 .
Yeh step kyun? Woh single number jo safety decide karta hai.
Step 3 — compare karo. 1.45 × 1 0 4 ≫ 1135 → NO-GO (strict rule: equality bhi no-go hoti, aur hum bahut upar hain). "112 km rule" sirf ek proxy hai; asli trajectory itni fast hai ki v 3 heating high rakhta hai.
Yeh step kyun? Parent ka mistake #3 demonstrate karta hai: akeli altitude decide nahi karti. Dekho bhi Ascent Trajectory Optimization .
Answer: Jettison mat karo. Flux girne tak ruko — is speed ke liye woh 133 km ke paas hai (Ex 2 ke method se v = 4200 ke saath).
Verify: 2 1 ( 3.9 × 1 0 − 7 ) ( 4200 ) 3 ≈ 1.45 × 1 0 4 W/m 2 > 1135 . ✓ NO-GO confirmed.
Recall Matrix ke paas quick self-test
Kaunsa cell? "Given h aur limit, woh speed find karo jo heating trip kare." ::: Cell C (velocity ke liye inverse, cube root).
v double karne par h jett kitna badhta hai? ::: 3 H ln 2 ≈ 15.6 km — sirf log-sized change.
Kyun ek 112 km "GO by altitude" abhi bhi NO-GO ho sakta hai? ::: Kyunki q ˙ ∝ ρ v 3 ; fast trajectory flux ko wahan bhi limit se upar rakhti hai.
Ex 7 mein 1000 kg fairing drop karne se kitna Δ v bacha? ::: Lagbhag 577 m/s.
Kya q ˙ = q ˙ limit safe hai? ::: Nahi — strict rule: equality last unsafe instant hai; sirf tab jettison karo jab strictly below ho.
"Speed ko cube karo, height ko log karo, flux check karo — map nahi." Heating hai ρ v 3 ; altitude logarithm ke through enter karti hai; aur manual ka altitude number asli flux condition ki sirf ek chhaya hai.