Step 1 — One particle (the source). Let the particle at x=0 do SHM:
y(0,t)=Asin(ωt)Why this step? We choose the source's motion; everything else follows by delay.
Step 2 — Delay the rest. A disturbance moving at speed v reaches position x a time tdelay=x/v later. So the particle at x does now what the source did a time x/vago:
y(x,t)=Asin(ω(t−vx))Why this step? This is the heart of a travelling wave: position x just lags in time.
Step 3 — Tidy with wave number. Define ==k=ω/v== (the angular wave number). Then:
Step 4 — Get the wave speed relation. The phase(ωt−kx) must stay constant to "ride a crest." Differentiate:
ωdt−kdx=0⇒v=dtdx=kω=2π/λ2πf=fλ
Derivation sketch (string), why each factor: a small element of length dx has mass μdx (inertia) and is pulled back by the net vertical component of tension T acting on its curved ends (restoring). Newton's law F=ma applied to the element gives T∂x2∂2y=μ∂t2∂2y, i.e. the wave equation ∂t2∂2y=μT∂x2∂2y. Matching to v2∂x2∂2y gives v=T/μ.
A neat link (slope of the snapshot):
∂t∂y=−v∂x∂y⇒vp=−v×(slope)Why: both come from differentiating y=Asin(ωt−kx); ∂y/∂t=Aωcos(⋅) and ∂y/∂x=−Akcos(⋅), and ω/k=v.
Why can't transverse waves travel through the bulk of a gas? → No shear rigidity.
What stays put and what travels in a wave? → Matter stays (oscillates); energy/pattern travels.
In v=fλ, which is set by the source and which by the medium? → f by source, v by medium, so λ adjusts.
Max particle speed? → Aω.
Recall Feynman: explain to a 12-year-old
Imagine a long line of friends holding hands. The first kid wiggles. Because they're holding hands, the next kid feels the tug and wiggles a tiny moment later, then the next, and the next. The wiggle travels down the line even though every kid stays in their own spot. If kids wiggle side-to-side, that's a transverse wave (like a snake). If they push-and-pull forward-and-back, squishing together then spreading out, that's a longitudinal wave (like sound). The kids never go anywhere — only the wiggle does.
Dekho, ek mechanical wave ka matlab hai ek disturbance jo travel karti hai, par medium ke particles khud travel nahi karte. Har particle bas apni jagah pe oscillate karta hai (SHM jaisa), aur ye hilna-dulna ka pattern aage badhta hai. Energy aur momentum transfer hoti hai, lekin matter ka net transport zero hota hai — jaise stadium mein "Mexican wave": log baithe rehte hain, sirf wave ghoomti hai.
Do types hain. Transverse wave mein particles propagation ke perpendicular hilte hain — isme crests aur troughs dikhte hain (string ki wave). Longitudinal mein particles propagation ke parallel hilte hain — isme compressions aur rarefactions banti hain (sound). Important baat: gases aur liquids mein shear rigidity nahi hoti, isliye unke bulk mein transverse mechanical wave nahi chal sakti — sirf longitudinal (sound) chalti hai. Solids dono carry kar sakte hain.
Sabse zaroori formula hai v=fλ. Yaad rakho: speed medium decide karta hai, frequency source decide karta hai. To agar frequency badhao, to λ chhoti ho jaati hai, par v same rehta hai. Aur speed ka general rule: v=restoring/inertia — string ke liye T/μ, sound ke liye B/ρ. Stiff medium fast, heavy medium slow.
Ek common galti: particle velocity (Aω) ko wave velocity (fλ) samajh lena. Dono alag hain — particle velocity har instant change hoti hai, wave velocity constant rehti hai. Aur sound ko transverse mat samajhna; book mein jo sine curve dikhta hai wo pressure-vs-position ka graph hai, actual particle motion aage-peeche (longitudinal) hai. Ye basics clear ho gaye to waves ka pura chapter aasaan ho jaata hai.