3.2.30 · D1 · Physics › Orbital Mechanics & Astrodynamics › Lagrange points L1–L5 — derivation, stability
Do bhari bodies apne shared balance point ke around ghoomti hain; agar tum ek spinning merry-go-round par kood jao jo unke saath ghoomta hai, toh woh freeze ho jaate hain aur tumhe ek naya outward "centrifugal" push mehsoos hota hai. Exactly paanch jagahein hain jahan dono bodies ki gravity aur woh outward push perfectly cancel ho jaate hain — Lagrange points — aur parent note mein jo bhi hai woh inhi cancel hote arrows ki careful bookkeeping hai.
Yeh page assume karta hai ki tumne kuch bhi nahi dekha. Hum har letter, symbol aur picture ko build karte hain jo parent note use karta hai, us order mein jis order mein tumhe chahiye. Jab tum neeche di gayi checklist answer kar sako, tab parent derivation padhne jao.
M
M ek number hai jo batata hai ki ek body mein kitna matter hai. Zyada mass → gravity ka pull zyada strong. Hum M 1 likhte hain badi body ke liye (Sun), M 2 chhoti ke liye (Earth), aur hamesha M 1 > M 2 .
Chhota number ek subscript hai — sirf ek naam ka tag, multiplication nahi. M 2 padho "mass number two", "M times 2 " nahi.
Hum m (small letter) bhi use karte hain test mass ke liye — woh satellite ya dust grain jo itna tiny hai ki woh kisi ko pull nahi karta. Bade letters pull karte hain; small letter bas saath chalta hai.
( x , y )
Ek flat sheet par location dene wala numbers ka pair. x = kitna right (negative = left); y = kitna upar (negative = neeche). ( 0 , 0 ) par dot origin hai.
Hum do badi bodies ko horizontal line y = 0 (x-axis ) ke saath line up karte hain. Sab kuch isi ek flat plane mein hota hai, isliye do numbers kaafi hain.
Figure s01 kaise padhein: baayein taraf bada lavender dot M 1 hai; daayein taraf chhota coral dot M 2 hai; upar aur daayein taraf chhota mint dot hamara test mass m hai kisi ( x , y ) par. Dashed lines ke crossing par butter dot origin ( 0 , 0 ) hai. Notice karo ki mint dot axis se off hai (uska y = 0 ) — yahi off-axis position hai jo hume baad mein L4/L5 ke liye chahiye. Neeche ke do double-headed arrows dikhate hain ki M 1 origin se sirf ek chhoti distance μ par hai, jabki M 2 ek badi distance ( 1 − μ ) par hai.
Do bodies ek doosre ke around orbit nahi karte jaise ek nailed down ho . Dono ek shared pivot ke around circle karte hain — barycenter (centre of mass). Do bachche see-saw par imagine karo: bhaari wala middle ke paas baithta hai, halka wala door, taaki balance ho.
Pehle humein names chahiye ki har body kahan hai . x 1 ko body M 1 ka x -coordinate hone do aur x 2 ko body M 2 ka x -coordinate (dono axis par hain, isliye unka y = 0 ).
Do masses ka balance point . Barycenter ko origin maankar positions measure karne par, yeh satisfy karta hai:
M 1 x 1 + M 2 x 2 = 0 ,
jahan x 1 , x 2 dono bodies ke coordinates hain. Yeh kehta hai bhaari body origin ke paas baithti hai aur halki body door, mass ke inverse proportion mein — see-saw rule.
Pair kitna "lopsided" hai yeh ONE number se describe karne ke liye, mass ratio define karo:
Ratio kyun aur do masses kyun nahi?
Lagrange points ki geometry sirf iss par depend karti hai ki pair kitna lopsided hai, actual kilograms par nahi. μ use karne ka matlab hai ek solved problem Sun–Earth, Earth–Moon, Pluto–Charon — sab ek saath cover karta hai.
Parent M 1 ko x 1 = − μ par aur M 2 ko x 2 = + ( 1 − μ ) par rakhta hai. Scaled masses M 1 = 1 − μ , M 2 = μ ke saath balance rule check karo: ( 1 − μ ) ( − μ ) + μ ( 1 − μ ) = 0 ✓. Figure s01 mein bhaari body origin se chhoti distance μ baayein baithti hai, halki body badi distance ( 1 − μ ) daayein — exactly see-saw rule.
Hume baar baar chahiye hoga "test mass har badi body se kitni door hai?" Pehle un do distances ke naam rakh lo:
r 1 aur r 2
r 1 ko ==test mass m se body M 1 tak straight-line distance== hone do, aur r 2 ko m se body M 2 tak distance. Subscript sirf batata hai ki hum kis body tak measure kar rahe hain.
Ab hum coordinates se straight-line distance kaise compute karein? Pehle coordinate differences define karo:
Definition Coordinate differences
Δ x , Δ y
Agar ek point ke coordinates ( x , y ) hain aur doosre ke ( x ′ , y ′ ) , toh Δ x = x − x ′ (horizontally kitne apart) aur Δ y = y − y ′ (vertically kitne apart). Symbol Δ ("delta") ka matlab hai "difference of".
Intuition Square root kyun? — yeh Pythagorean theorem hai
Right-triangle: horizontal leg Δ x , vertical leg Δ y , aur straight distance slanted hypotenuse hai. Pythagoras kehta hai r 2 = Δ x 2 + Δ y 2 , isliye r = Δ x 2 + Δ y 2 . Square root simply undo karta hai square ko taaki "r 2 " wapas length ban sake.
Figure s02 kaise padhein: lavender dot M 1 hai, mint dot test mass m hai. Coral horizontal leg Δ x = x + μ hai (test mass ka x minus M 1 ka x = − μ ), butter vertical leg Δ y = y hai, aur slate slanted line distance r 1 khud hai — hypotenuse. Corner par chhota square right angle mark karta hai jo Pythagoras apply hone deta hai.
Toh do distances jo parent likhta hai woh sirf m se har body tak Pythagoras hain:
r 1 = ( x + μ ) 2 + y 2 ( to M 1 ) , r 2 = ( x − ( 1 − μ ) ) 2 + y 2 ( to M 2 ) .
( x + μ ) hai "kitna right m hai M 1 se", kyunki M 1 x 1 = − μ par baitha hai aur negative subtract karne se add ho jaata hai.
Definition Newtonian gravity
Har mass har doosre ko pull karta hai. Masses M aur m ke beech, r distance par, force hai:
F = r 2 GM m ,
unhe jodne wali line ke saath point karta hua. G gravitational constant hai — ek fixed number jo gravity ki strength set karta hai har jagah.
1/ r 2 (inverse-square) kyun?
Socho pull balloon ki surface par evenly sprayed paint ki tarah bahar faila raha hai. Radius double karo → balloon ki surface area 4 × grow kati hai (area ∝ r 2 ) → wahi paint chaar guna thin ho jaati hai. Isliye influence 1/ r 2 se dilute hota hai. Exponent mein yeh "2 " exactly wahan se aata hai jahan parent ke Hill-radius estimate mein tidal factors aate hain.
Parent force ki jagah potential energy use karta hai. Energy "stored pull" hai:
Definition Gravitational potential (energy per unit mass)
ϕ = − r GM .
Yeh woh energy hai jo lagti hai ek unit mass ko distance r se infinity tak kheenchne mein. Minus sign kyun: gravity attractive hai, isliye bound positions "ek hole mein" hain — lower (zyada negative) matlab zyada deep well mein.
Intuition Force = potential ka downhill slope
Potential ko ek landscape ki tarah picture karo. Ball hamesha downhill roll karta hai; slope jitna steep, push utna strong. Mathematically "landscape ki steepness" gradient hai — neeche mile. Note karo ϕ ∝ 1/ r jabki force ∝ 1/ r 2 : 1/ r ka slope 1/ r 2 hai, consistent.
Definition Angular velocity
ω (Greek "omega")
Koi cheez kitni fast spin karti hai, radians per second mein. Ek full turn = 2 π radians. Bada ω = fast spin.
Hum spinning pair ke saath ride karna choose karte hain — ek rotating reference frame . Is frame mein do badi bodies move karna band kar deti hain (frozen ho jaati hain), yahi poora trick hai jo "parking spots" possible banata hai.
v (rotating frame mein)
v hai ==kitna fast, aur kis direction mein, test mass m move kar raha hai jaise frame ke saath spin karne wale kisi ko dikhta hai ==. Agar m ek Lagrange point par perfectly still baitha hai, toh v = 0 . Agar drift karta hai, v = 0 . Hume yahi v neeche do baar chahiye hoga: Coriolis force aur Jacobi constant ke liye.
Intuition Centrifugal force — merry-go-round ka outward shove
Spinning roundabout par tum outward flung feel karte ho. Woh apparent outward push, sirf isliye feel hota hai kyunki tum spin kar rahe ho, woh centrifugal force hai. Spin axis se distance ρ (Greek "rho") par unit mass par iska size ω 2 ρ hai, seedha bahar point karta hua.
Figure s03 kaise padhein: centre par slate "×" spin axis hai; lavender aur coral dots M 1 aur M 2 hain, frozen kyunki hum unke saath spin kar rahe hain. Mint arrows sab axis se seedhe outward point karte hain, aur woh lambe hote jaate hain jitna door se start hon — yeh ω 2 ρ ka ρ ke saath grow karna picture karta hai. Faint grey curl tumhe remind karta hai ki poora frame rate ω se turn kar raha hai. Yeh outward push teesri force hai jo, dono gravities ke saath milkar, ek Lagrange point par cancel honi chahiye.
potential − 2 1 ω 2 ρ 2 kyun hai (aur 2 1 kahan se aata hai)
Force apne potential ka downhill slope hota hai. Hum chahte hain ek potential U ( ρ ) jiska outward slope outward force ω 2 ρ reproduce kare. "Slope" ka matlab ρ ke respect mein derivative hai, aur force = − d ρ d U . Toh hume chahiye:
− d ρ d U = ω 2 ρ ⟹ d ρ d U = − ω 2 ρ .
Kis function ka slope − ω 2 ρ hai? Kyunki ρ 2 ka derivative 2 ρ hai, 2 1 ρ 2 ka derivative exactly ρ hai. Isliye U = − 2 1 ω 2 ρ 2 ka slope − ω 2 ρ hai. Woh 2 1 ρ 2 differentiate karne ka leftover hai — wahi 2 1 jo tab aata hai jab tum ek linear force integrate karo (bilkul jaise spring ke liye 2 1 k x 2 ). ρ 2 = x 2 + y 2 aur ω = 1 ke saath yeh parent ke effective potential mein woh − 2 1 ( x 2 + y 2 ) term hai.
Definition Coriolis force — sideways deflector
Rotating frame mein ek doosri apparent force, sirf unhi chezon ko feel hoti hai jo move kar rahi hain : − 2 ω × v , us v ko use karke jo humne abhi define ki. Yeh ek moving path ko sideways bend karta hai. Frame mein still baithne wale particle ke liye, v = 0 , isliye Coriolis = 0 .
Common mistake "Coriolis Lagrange points locate karne mein help karta hai."
Kyun sahi lagta hai: yeh genuine rotating-frame physics hai. Fix: Lagrange point par test mass frame mein at rest hota hai, isliye v = 0 aur Coriolis vanish ho jaata hai. Yeh baad mein sirf stability ke liye matter karta hai, jahan mass drift karta hai aur move karta hai. Dekho Coriolis and Centrifugal Forces (Rotating Frames) .
Ye dono forces properly build hain Coriolis and Centrifugal Forces (Rotating Frames) mein; poora spinning-frame setup Restricted Three-Body Problem hai.
Parent units choose karta hai jahan D = 1 aur G ( M 1 + M 2 ) = 1 , toh ω 2 = 1 , yani ω = 1 . Yeh sirf rulers aur clocks ki ek smart choice hai taaki equations se clutter hat sake — koi physics change nahi hoti. Dekho Kepler's Third Law .
∇ ("del" symbol)
∇Ω woh arrow hai jo us direction mein point karta hai jahan landscape Ω sabse fast rise karta hai, us steepness ke barabar length ke saath. Iske components har direction mein slopes hain: ∇Ω = ( ∂ x ∂ Ω , ∂ y ∂ Ω ) .
Definition Partial derivative
∂ x ∂ Ω
Landscape ka slope jab tum sirf x -direction mein step karte ho, y ko fixed rakh ke . "∂ " ek curly-d hai jiska matlab hai "change in, while freezing the other variables."
Intuition Sab kuch ek landscape
Ω mein bundle kyun karein?
Teen force arrows juggle karne ki jagah, hum unke saare potentials ek single surface Ω mein stack karte hain. Tab force = − ∇Ω (downhill roll karo), aur special "no net force" spots simply flat spots hain, jahan ∇Ω = 0 . Flat ka matlab har slope zero hai — ek hilltop, valley bottom, ya saddle. Woh single condition paanch sab points find karta hai.
Intuition Dimensional gravity se scaled form tak (kyun
− G M 1 / r 1 becomes − ( 1 − μ ) / r 1 )
Shuru karo unit mass per honest gravitational potentials se, − r 1 G M 1 − r 2 G M 2 . Har mass ko total ka fraction likho: M 1 = ( 1 − μ ) ( M 1 + M 2 ) aur M 2 = μ ( M 1 + M 2 ) . Tab:
− r 1 G M 1 − r 2 G M 2 = − G ( M 1 + M 2 ) ( r 1 1 − μ + r 2 μ ) .
Ab unit choice impose karo G ( M 1 + M 2 ) = 1 (part 7). Poora prefactor 1 ban jaata hai aur simply disappear ho jaata hai, chhod jaata hai − r 1 1 − μ − r 2 μ . Yahi poora scaling step hai — koi physics lost nahi, sirf cleaner bookkeeping.
Definition Jacobi constant
C J
Rotating frame mein ek conserved "energy", C J = − 2Ω − v 2 , jahan v rotating frame mein test mass ki speed hai (part 6). Iske level curves mark karti hain ki given energy ka spacecraft kahan travel kar sakta hai: kyunki v 2 ≥ 0 , − 2Ω < C J wale regions ko v 2 < 0 ki zaroorat hogi aur woh forbidden hain. Detail Effective Potential & Jacobi Constant mein.
Ek polynomial equation jiska highest power 5 hai (jaise x 5 + ⋯ = 0 ). Iska generally koi neat formula nahi hota — tum roots numerical searching se dhundho. Teen collinear points L1, L2, L3 aise hi ek equation se aate hain.
Definition Saddle vs maximum (flat spot ki shapes)
Maximum hilltop hai: har direction mein downhill. Saddle mountain pass hai: ek taraf downhill, crossing direction mein uphill. L1/L2/L3 saddles par baithte hain; L4/L5 hilltops par (maxima).
Definition Equilateral triangle
Ek triangle jiske teeno sides equal hain. L4 aur L5 wahan baithte hain jahan r 1 = r 2 = D , isliye m , M 1 , M 2 ek perfect equilateral triangle banate hain — L4 6 0 ∘ ahead, L5 6 0 ∘ behind. Trojan Asteroids ka ghar.
Intuition L4/L5 stable kyun ho sakte hain even though woh hilltops hain (aur mass-ratio condition)
Ω ke hilltop par baithna unstable lagta hai — ek nudge m ko roll off kar dena chahiye. Lekin jab m drift karna start karta hai toh woh moving hai, isliye Coriolis force (− 2 ω × v ) kick in karta hai aur uska path ek tiny loop mein curl kar deta hai, use point ke paas trap kar ke. Yeh whirlpool rescue tabhi kaam karta hai jab spin dominant enough ho, jo tab hota hai jab do bodies kaafi lopsided hon. Classical result hai:
L4/L5 stable ⟺ μ < μ crit ≈ 0.0385 ( equivalently M 2 M 1 > 24.96 ) .
Sun–Jupiter (M 1 / M 2 ≈ 1047 ) aur Earth–Moon (≈ 81 ) easily pass karte hain, isliye real Trojan Asteroids billions of years tak survive karte hain. Full linear-stability algebra parent note mein hai.
L1/L2 ke liye use ki gayi near-body scale r ≈ D ( μ /3 ) 1/3 Hill Sphere radius hai — ek body ka gravitational control ka zone.
Intuition Neeche ka map kaise padhein
Ise upar se neeche padho, arrows follow karte hue: har box is page ka ek idea hai, aur ek arrow "A → B " ka matlab hai "B samajhne se pehle A chahiye". Sabse neeche wala box, Lagrange points L1–L5 , destination hai; har path jo usme aata hai prerequisites ki ek chain hai jo tumne ab build kar li hai. Agar koi bhi box shaky lage, uske section par upar wapas jaao.
Coordinates x y and origin
Distance r from Pythagoras
Gravity and potential phi
Spinning frame omega and velocity v
Effective potential Omega
Gradient del and partial slopes
Right side cover karo aur khud test karo. Agar tum sab answer kar sako, tum parent note ke liye ready ho.
M 2 mein subscript ka matlab kya hai?Ek naam ka tag ("mass number two"), kabhi multiplication nahi.
Mass ratio μ words mein kya hai? Total mass ka woh fraction jo chhoti body mein hai, M 2 / ( M 1 + M 2 ) .
Barycenter equation mein x 1 aur x 2 kya represent karte hain? Axis par bodies M 1 aur M 2 ke x -coordinates.
Barycenter do masses ke relative kahan hota hai? Bhaari wale ke paas, halke wale se door (see-saw balance).
Δ x aur Δ y kya hain?Do points ke beech horizontal aur vertical coordinate differences, x − x ′ aur y − y ′ .
r 1 aur r 2 kya measure karte hain?Test mass m se M 1 aur M 2 tak ki distances respectively.
r = Δ x 2 + Δ y 2 kyun?Pythagoras: yeh right triangle ka hypotenuse hai jiske legs Δ x aur Δ y hain.
Gravity 1/ r 2 se kyun fade hoti hai? Pull ek sphere ki surface par spread hota hai jiska area r 2 se grow karta hai, isliye yeh 1/ r 2 se thin hota hai.
Potential energy negative kyun hoti hai? Gravity attractive hai; bound positions ek well mein baithte hain, deeper = zyada negative.
Rotating frame mein v kya hai, aur yeh zero kab hota hai? Frame ke saath spin karne wale kisi ko dikhti m ki velocity; zero jab m Lagrange point par still baitha ho.
Centrifugal force kya hai aur kitna bada hota hai? Spinning frame mein feel hone wala outward shove, axis se ρ distance par size ω 2 ρ .
Centrifugal potential − 2 1 ω 2 ρ 2 mein 2 1 kahan se aata hai? Linear force ω 2 ρ integrate karne se — ρ 2 ka derivative 2 ρ hai, isliye potential 2 1 carry karta hai.
Coriolis force zero kab hota hai? Jab particle rotating frame mein at rest ho (v = 0 ).
− G M 1 / r 1 kyun − ( 1 − μ ) / r 1 ban jaata hai?M 1 = ( 1 − μ ) ( M 1 + M 2 ) likho aur unit choice G ( M 1 + M 2 ) = 1 use karo, toh prefactor 1 ban jaata hai.
∇Ω = 0 ka physically kya matlab hai?Wahan landscape flat hai — koi net force nahi — ek Lagrange point.
Saddle aur maximum mein kya fark hai? Saddle = ek taraf downhill, doosri taraf uphill (L1,L2,L3); maximum = har taraf downhill (L4,L5).
L4/L5 par m , M 1 , M 2 kaisi shape banate hain? Ek equilateral triangle (r 1 = r 2 = D ).
L4/L5 stable hone ki kya condition hai? Jab μ < μ crit ≈ 0.0385 , yani M 1 / M 2 > 24.96 .
Kepler's Third Law ω = 1 kaise deta hai? ω 2 = G ( M 1 + M 2 ) / D 3 , aur G ( M 1 + M 2 ) = 1 , D = 1 units choose karne par ω = 1 milta hai.