Intuition What this page is for
The parent note gave you the law ρ 1 A 1 v 1 = ρ 2 A 2 v 2 . Knowing a formula and knowing every situation it can be thrown at are different skills. Here we build a matrix of every case class the continuity equation can hide behind — narrowing, widening, splitting, gases, degenerate blockages, real bucket-filling — and then work an example for each cell so no exam or lab surprises you.
Before anything else, one reminder so every symbol is earned:
Definition The quantities in play
ρ (rho) = density = mass packed into each cubic metre, units kg/m 3 .
A = cross-sectional area = the size of the "window" the fluid flows through, units m 2 . For a round pipe of radius r , A = π r 2 .
v = flow speed = how fast the fluid front advances, units m/s .
V = volume = the amount of space a body of fluid fills (e.g. how much a bucket holds), units m 3 . Note: 1 L = 1 0 − 3 m 3 .
ρ A v = mass flow rate m ˙ , units kg/s — the mass passing a section each second.
Q = A v = volume flow rate (see Volume flow rate and discharge ), units m 3 / s — conserved only when ρ is constant.
Continuity problems all obey one master line — mass in per second = mass out per second — but they look different depending on what changes and what is held fixed. Here is every class:
Cell
What changes
Held fixed
Conserved quantity
Watch out for
A Narrowing
A shrinks
ρ
A v
speed goes up
B Widening
A grows
ρ
A v
speed goes down
C Radius given
r (not A )
ρ
A v , with A ∝ r 2
square the ratio
D Splitting / merging
one pipe → many
ρ
total A v
sum the branches
E Compressible gas
ρ changes
A (here)
ρ A v only
do not cancel ρ
F Word problem (fill/drain)
time from rate
ρ
Q
t = V / Q
G Degenerate: A → 0
window closes
ρ
m ˙ = ρ A v
v → ∞ limit
H Exam twist: solve for area
A 2 unknown
ρ , mixed units
A v
convert cm↔m first
I Compressible split
one gas pipe → many, ρ changes
(nothing)
total ρ A v
sum mass flows
The 9 examples below hit cells A–I in order. Forecast each answer before reading the steps — guessing first is how the intuition sticks.
Worked example A: water squeezed
Water (ρ constant) flows through area A 1 = 6 × 1 0 − 4 m 2 at v 1 = 3 m/s . The pipe narrows to A 2 = 2 × 1 0 − 4 m 2 . Find v 2 .
Forecast: area cut to one-third → speed should triple . Guess ≈ 9 m/s .
Since ρ is fixed, use the incompressible form A 1 v 1 = A 2 v 2 .
Why this step? Water barely compresses, so ρ cancels — only A v survives.
Solve for the exit speed:
v 2 = v 1 A 2 A 1 = 3 × 2 × 1 0 − 4 6 × 1 0 − 4 = 3 × 3 = 9 m/s .
Why this step? Smaller window, same litres/sec → each parcel must hurry through.
Verify: A 1 v 1 = 6 × 1 0 − 4 × 3 = 1.8 × 1 0 − 3 ; A 2 v 2 = 2 × 1 0 − 4 × 9 = 1.8 × 1 0 − 3 . Equal ✓. Units: m 2 ⋅ m/s = m 3 / s both sides ✓.
Figure s01 below draws exactly this pipe — compare the thin blue arrow (v 1 ) in the wide section with the fat orange arrow (v 2 ) in the throat: same flow, faster where narrow.
Figure s01 — Cell A: a wide pipe (blue, area A 1 , slow v 1 ) narrowing into a throat (orange, area A 2 , fast v 2 ). The two arrows show the speed jump that A 1 v 1 = A 2 v 2 forces.
Worked example B: water into a reservoir mouth
The same 1.8 × 1 0 − 3 m 3 / s of water now flows from area A 1 = 2 × 1 0 − 4 m 2 at 9 m/s into a wide section A 2 = 9 × 1 0 − 4 m 2 . Find v 2 .
Forecast: area grows by factor 4.5 → speed should drop by 4.5 . Guess ≈ 2 m/s .
Incompressible again: A 1 v 1 = A 2 v 2 .
Why this step? Same fluid, ρ unchanged.
v 2 = v 1 A 2 A 1 = 9 × 9 × 1 0 − 4 2 × 1 0 − 4 = 9 × 9 2 = 2 m/s .
Why this step? Bigger window spreads the same flow rate thin — fluid crawls. This is the "wide ⇒ slow" half of the story.
Verify: A 2 v 2 = 9 × 1 0 − 4 × 2 = 1.8 × 1 0 − 3 m 3 / s , matching the input ✓.
Worked example C: halving the radius
Blood (ρ const) flows in a vessel of radius r 1 = 4 mm at v 1 = 0.5 m/s . A constriction narrows it to r 2 = 2 mm . Find v 2 .
Forecast: radius halved → area quartered → speed × 4 . Guess 2 m/s .
Write area in terms of radius: A = π r 2 , so A 2 A 1 = π r 2 2 π r 1 2 = ( r 2 r 1 ) 2 .
Why this step? The π cancels; the danger is using r 1 / r 2 (=2) instead of its square (=4).
v 2 = v 1 ( r 2 r 1 ) 2 = 0.5 × ( 2 4 ) 2 = 0.5 × 4 = 2 m/s .
Why this step? Area lives in two dimensions , so it responds to the square of the size.
Verify: ratio A 1 / A 2 = ( 4/2 ) 2 = 4 ; v 2 / v 1 = 2/0.5 = 4 . Match ✓. (Units mm cancel in the ratio, so no conversion needed.)
Figure s02 contrasts the wrong straight line (r ) with the true parabola (r 2 ); the red dot marks where the radius halves and the area falls to a quarter.
Figure s02 — Cell C: area ratio vs radius ratio. The dashed gray line is the naive (wrong) r ; the blue curve is the true A ∝ r 2 . At the red dot, radius halved ⇒ area 1/4 ⇒ speed × 4 .
Worked example D: one pipe feeds two
A main pipe carries water at Q in = 1.2 × 1 0 − 2 m 3 / s . It splits into two identical branches, each of area A = 3 × 1 0 − 3 m 2 . If both branches run at the same speed, find that speed.
Forecast: each branch handles half the flow. Guess speed = 0.003 0.006 = 2 m/s .
Mass (here volume, since ρ const) can't pile up at the junction: Q in = Q 1 + Q 2 .
Why this step? Conservation of mass at a junction just means whatever arrives leaves , now shared across outlets (see Streamlines and stream tubes ).
Equal branches → each carries Q 1 = Q 2 = 2 Q in = 6 × 1 0 − 3 m 3 / s .
v = A Q 1 = 3 × 1 0 − 3 6 × 1 0 − 3 = 2 m/s .
Why this step? Q = A v ⇒ v = Q / A per branch.
Verify: total out = 2 × ( A v ) = 2 × ( 3 × 1 0 − 3 × 2 ) = 1.2 × 1 0 − 2 m 3 / s = Q in ✓.
Worked example E: air compressed in a duct
Air enters a duct at ρ 1 = 1.0 kg/m 3 , A 1 = 0.4 m 2 , v 1 = 20 m/s . Downstream it is compressed to ρ 2 = 2.5 kg/m 3 in a wider section A 2 = 0.8 m 2 . Find v 2 .
Forecast: area doubled and density × 2.5 — both slow it. Guess well below 20 .
Because ρ changes, only mass flow is conserved (see Incompressible vs compressible flow ): ρ 1 A 1 v 1 = ρ 2 A 2 v 2 .
Why this step? Cancelling ρ here would be the classic error — A v is not constant for gases.
v 2 = ρ 2 A 2 ρ 1 A 1 v 1 = 2.5 × 0.8 1.0 × 0.4 × 20 = 2 8 = 4 m/s .
Why this step? Denser + wider both shrink the required speed to move the same mass.
Verify: m ˙ in = 1.0 × 0.4 × 20 = 8 kg/s ; m ˙ out = 2.5 × 0.8 × 4 = 8 kg/s ✓. Note A 1 v 1 = 8 = A 2 v 2 = 3.2 — volume flow is not conserved, exactly as warned.
Worked example F: filling a drum
A hose of area 2 × 1 0 − 4 m 2 delivers water at 2.5 m/s . How long to fill a 200 L = 0.2 m 3 drum? (Here V = 0.2 m 3 is the drum's volume , defined above.)
Forecast: flow Q = A v = 5 × 1 0 − 4 m 3 / s ; time = 0.2/0.0005 — order of hundreds of seconds.
Volume flow rate: Q = A v = ( 2 × 1 0 − 4 ) ( 2.5 ) = 5 × 1 0 − 4 m 3 / s .
Why this step? Q is litres-per-second delivered; that's what fills the drum.
t = Q V = 5 × 1 0 − 4 0.2 = 400 s .
Why this step? total volume ÷ (volume per second) = seconds.
Verify: Q ⋅ t = 5 × 1 0 − 4 × 400 = 0.2 m 3 ✓ = 200 L. Units: m 3 / s m 3 = s ✓.
Worked example G: thumb on the hose
Water flows in at A 1 = 1 × 1 0 − 4 m 2 , v 1 = 4 m/s . You press your thumb so the exit shrinks to A 2 . (a) Find v 2 when A 2 = 1 × 1 0 − 5 m 2 . (b) What happens to v 2 as A 2 → 0 ?
Forecast: (a) area cut × 10 → speed × 10 = 40 m/s . (b) as the gap closes, speed blows up.
Incompressible: A 1 v 1 = A 2 v 2 ⇒ v 2 = A 2 A 1 v 1 .
Why this step? Same volume/sec through a tiny window.
(a) v 2 = 1 × 1 0 − 5 ( 1 × 1 0 − 4 ) ( 4 ) = 1 × 1 0 − 5 4 × 1 0 − 4 = 40 m/s .
(b) Take the limit: A 2 → 0 + lim v 2 = A 2 → 0 + lim A 2 A 1 v 1 = + ∞.
Why this step? Dividing a fixed positive flow by a shrinking area sends speed to infinity — the mathematical face of "squeeze harder, jet faster." In reality friction and the fluid's limits cap it, but the trend is real (this is your hose-jet).
Verify: A 2 v 2 = 1 × 1 0 − 5 × 40 = 4 × 1 0 − 4 = A 1 v 1 ✓. Limit sign: numerator > 0 , denominator → 0 + , so → + ∞ ✓.
Figure s03 plots v 2 against the shrinking exit area: the orange dot is part (a), and the curve rockets upward toward the vertical axis — the visual meaning of the limit in part (b).
Figure s03 — Cell G: exit speed v 2 vs exit area A 2 . As A 2 shrinks toward zero, v 2 = A 1 v 1 / A 2 climbs without bound; the orange dot marks the A 2 = 1 × 1 0 − 5 m² answer of 40 m/s.
Worked example H: what exit area gives a target speed?
Water enters at A 1 = 20 cm 2 , v 1 = 1.5 m/s . You want the exit speed to be exactly v 2 = 6 m/s . What exit area A 2 (in cm 2 ) is needed? This is the design idea behind a Venturi meter .
Forecast: speed must quadruple , so area must shrink to a quarter → 5 cm 2 .
Convert: A 1 = 20 cm 2 = 20 × 1 0 − 4 m 2 = 2 × 1 0 − 3 m 2 .
Why this step? 1 cm 2 = 1 0 − 4 m 2 ; mixing cm² with m/s silently corrupts the answer.
Rearrange A 1 v 1 = A 2 v 2 for the unknown area:
A 2 = v 2 A 1 v 1 = 6 ( 2 × 1 0 − 3 ) ( 1.5 ) = 6 3 × 1 0 − 3 = 5 × 1 0 − 4 m 2 .
Why this step? Continuity is one equation; solve for whichever symbol is unknown.
Convert back: 5 × 1 0 − 4 m 2 = 5 cm 2 .
Verify: A 1 v 1 = 2 × 1 0 − 3 × 1.5 = 3 × 1 0 − 3 ; A 2 v 2 = 5 × 1 0 − 4 × 6 = 3 × 1 0 − 3 ✓. Area ratio 20/5 = 4 = speed ratio 6/1.5 = 4 ✓.
Worked example I: hot gas manifold
A gas enters a single duct at ρ 1 = 1.2 kg/m 3 , A 1 = 0.5 m 2 , v 1 = 10 m/s . It splits into two outlet ducts. Outlet 1: ρ = 0.8 kg/m 3 , A = 0.5 m 2 , v = 6 m/s . Find the mass flow rate m ˙ 2 that must leave through outlet 2.
Forecast: whatever mass comes in must leave; outlet 1 can't carry it all, so outlet 2 takes the remainder.
Because density changes across the manifold, conserve mass flow, not volume, and sum the branches: ρ 1 A 1 v 1 = m ˙ out , 1 + m ˙ out , 2 .
Why this step? This fuses cell D (split → sum) with cell E (gas → keep ρ ). Volume flow A v is meaningless to sum here.
Mass in: m ˙ in = ρ 1 A 1 v 1 = 1.2 × 0.5 × 10 = 6 kg/s .
Mass out of outlet 1: m ˙ out , 1 = 0.8 × 0.5 × 6 = 2.4 kg/s .
Remainder through outlet 2: m ˙ out , 2 = 6 − 2.4 = 3.6 kg/s .
Why this step? The junction stores nothing; total mass out equals total mass in.
Verify: m ˙ out , 1 + m ˙ out , 2 = 2.4 + 3.6 = 6 kg/s = m ˙ in ✓. Units kg/m 3 ⋅ m 2 ⋅ m/s = kg/s ✓.
Common mistake The traps this matrix defends against
Cell C trap: using r 1 / r 2 instead of ( r 1 / r 2 ) 2 . Area is 2-D.
Cell E / I trap: cancelling ρ for a gas. Only ρ A v is conserved when density changes — and when a gas splits, you must sum mass flows, never volume flows.
Cell H trap: feeding cm 2 into a formula expecting m 2 . Convert first, always.
Mnemonic One line to hold it all
"Same mass per second, everywhere." Narrow ⇒ fast (A, C, G), wide ⇒ slow (B), split ⇒ share (D, I), gas ⇒ keep ρ (E, I), and the clock is just volume over rate (F).
Recall Which conserved quantity for a compressing gas?
Mass flow rate m ˙ = ρ A v — not A v , because ρ changes.
If radius halves (incompressible), speed does what? Becomes 4 × , since v ∝ 1/ r 2 .
One pipe splits into two branches — what is conserved at the junction? Total volume flow Q in = Q 1 + Q 2 (mass can't accumulate).
When a compressible gas splits, what do you sum across branches? The mass flows: ρ 1 A 1 v 1 = m ˙ out , 1 + m ˙ out , 2 .
As the exit area A 2 → 0 at fixed input, what does v 2 approach? + ∞ (speed = A 1 v 1 / A 2 blows up).
Convert 20 cm 2 to m 2 . 20 × 1 0 − 4 = 2 × 1 0 − 3 m 2 .
Time to fill volume V at volume flow rate Q ? t = V / Q .
2.2.12 Continuity equation — derivation (conservation of mass), ρAv = const (Hinglish) — parent derivation.
Bernoulli's equation — uses these speeds to get pressures.
Volume flow rate and discharge — the Q = A v used in cells B, D, F.
Incompressible vs compressible flow — why cells E and I keep ρ .
Venturi meter — the design in cell H.
Streamlines and stream tubes — the junction picture in cells D and I.
Conservation of mass — the law behind every cell.