WHY autonomous matters: because t is absent, the velocity vector (x˙,y˙) depends only on where you are, not when. So through each point there is a unique direction → trajectories never cross (except at critical points).
HOW to find them: solve the simultaneous algebraic equations f=0,g=0. These are the only points where the direction (x˙,y˙) is undefined as a "where to go" arrow, hence the only places trajectories may meet.
Derivation from scratch. Shift origin: let u=x−x0,v=y−y0. Taylor expand:
u˙=fxu+fyv+(higher order),v˙=gxu+gyv+⋯
all partials evaluated at the critical point. Drop higher-order terms:
(u˙v˙)=J(uv),J=(fxgxfygy).J is the Jacobian at the critical point.
WHY eλt: try u=veλt. Then λveλt=Jveλt⇒Jv=λv. So λ must be an eigenvalue. The sign of Reλ says grow (unstable) or decay (stable); imaginary part says rotate.
System: x˙=x+y,y˙=−2x+4y? Let's instead use clean one:
x˙=−x+3y,y˙=−3x−y?
Let me do a transparent saddle:
x˙=x+2y,y˙=2x+y.
Step 1 — critical point. Set x+2y=0,2x+y=0. Why? equilibrium needs both rates zero. Subtract: 3x+3y=0⇒... solve: only solution (0,0).
Step 2 — Jacobian. Here f,g are already linear so J=(1221). Why?fx=1,fy=2,gx=2,gy=1.
Step 3 — eigenvalues.τ=2,Δ=1⋅1−2⋅2=−3.
λ2−2λ−3=0⇒(λ−3)(λ+1)=0⇒λ=3,−1.Step 4 — classify. Real, opposite signs ⇒ saddle, unstable. Why this step? opposite signs mean one direction grows, one shrinks — the hallmark of a saddle.
Step 1 — critical point. At origin the cubic terms vanish: x˙=−y,y˙=x, both zero only at (0,0). Why drop cubics? near origin x2+y2 is tiny.
Step 2 — Jacobian at origin. Linear part is x˙=−y+x,y˙=x+y (since 1−x2−y2→1). So
J=(11−11).Why this step? differentiate including the x⋅1 term from x(1−…).
Step 3 — eigenvalues.τ=2,Δ=1+1=2, discriminant τ2−4Δ=4−8=−4<0.
λ=1±i.Step 4 — classify. Complex with Reλ=1>0⇒ unstable spiral outward. (In fact trajectories spiral out toward a circular limit cycle r=1 — that's the full nonlinear truth.)
Imagine a windy field where a leaf is blown by wind that's the same at the same spot every day. Drop the leaf anywhere and it follows a path — that's a trajectory. Some spots have no wind at all; a leaf there just sits — those are critical points. Some no-wind spots suck leaves in (sinks), some blow them away (sources), some swirl them (spirals), and some are passes between hills where leaves come close then get flung off (saddles). By only studying the no-wind spots and the wind right around them, you can guess where every leaf ends up — without watching each leaf the whole day.
Dekho, kabhi-kabhi do ODE aapas mein itne coupled hote hain ki x(t) aur y(t) ka exact formula nikalna namumkin ho jata hai. Tab hum phase plane ka trick use karte hain: t ko bhool jao, sirf xy-plane mein curve ka shape dekho. Har solution ek trajectory banata hai, jaise hawa mein patta udta hai. Important baat: autonomous system mein har point pe direction fix hai, isliye do trajectory kabhi cross nahi karte (sirf critical point pe milte hain).
Critical point wo jagah hai jahan f=0 aur g=0 — yaani system ekdum rest pe, kuch move nahi karta. Yeh points pure flow ko organize karte hain, jaise floor pe drain aur fountain paani ka pattern decide karte hain. Inhe dhoondhne ke liye bas f=0,g=0 algebraically solve karo.
Ab in points ke around behaviour janne ke liye hum linearize karte hain — Taylor expand karke Jacobian J banate hain. J ke eigenvalues sab kuch bata dete hain: real opposite signs = saddle (unstable), dono negative = stable node, complex with negative real part = stable spiral, pure imaginary = center. Shortcut: detJ<0 hamesha saddle; agar detJ>0 to trace ka sign stability decide karta hai (negative = stable). Bas itna yaad rakho aur 80% questions ho jayenge — baaki sirf discriminant τ2−4Δ se node vs spiral confirm kar lo.