Bernoulli's Equation — Venturi Tube

A pipe narrows in the middle. Conservation of mass says the fluid has to speed up; Bernoulli says the pressure has to fall. Watch both effects together.

Visualization
Input
cm\mathrm{cm}
cm\mathrm{cm}
L/s\mathrm{L/s}
kPa\mathrm{kPa}
m\mathrm{m}
kg/m3\mathrm{kg/m^{3}}
m/s2\mathrm{m/s^{2}}

Show the streamline + cross-section view

Two ideas talking to each other

A venturi tube — a pipe that gets narrower in the middle — is the cleanest way to see two of fluid mechanics' biggest ideas working together.

The first is conservation of mass (continuity). Whatever flow rate QQ enters the pipe has to come out the other side, so the velocity has to change as the cross-section changes. With area A1A_1 at the inlet and A2A_2 at the throat:

Q=A1v1=A2v2v2=A1A2v1Q = A_1 v_1 = A_2 v_2 \quad\Rightarrow\quad v_2 = \frac{A_1}{A_2}\,v_1

A throat half the diameter has a quarter the area, so the fluid moves four times as fast through it. Source: Wikipedia — Venturi effect.

The second is conservation of energy (Bernoulli's equation). Along a streamline of an inviscid, incompressible, steady flow, the sum of pressure, kinetic energy per volume, and gravitational potential energy per volume is constant:

p+12ρv2+ρgh=constp + \tfrac{1}{2}\rho v^{2} + \rho g h = \text{const}

Source: OpenStax University Physics §14.6; Wikipedia — Bernoulli's principle.

Velocity up, pressure down

Apply Bernoulli's equation between the inlet (subscript 1) and the throat (subscript 2):

p1+12ρv12+ρgh1=p2+12ρv22+ρgh2p_1 + \tfrac{1}{2}\rho v_1^{2} + \rho g h_1 = p_2 + \tfrac{1}{2}\rho v_2^{2} + \rho g h_2

Solving for the throat pressure:

p2=p112ρ(v22v12)ρgΔhp_2 = p_1 - \tfrac{1}{2}\rho\,(v_2^{2} - v_1^{2}) - \rho g\,\Delta h

The first correction term is the Venturi pressure drop: kinetic energy has to come from somewhere, and that "somewhere" is the static pressure. The second is the gravity term — when fluid climbs (Δh>0\Delta h > 0), it pays more pressure to gain potential energy. Try the elevation slider to see them trade off.

If p2p_2 goes below atmospheric, you'll get cavitation — vapour bubbles form in the low-pressure region. The diagram flags it.

The fire-hose example

OpenStax §14.6 Example 14.7 is a fire hose narrowing from 6.4 cm to a 3.0 cm nozzle, lifting water 10 m, with a 1.62 MPa source pressure pushing 40 L/s. The textbook reports v112.4v_1 \approx 12.4 m/s, v256.6v_2 \approx 56.6 m/s, and p20p_2 \approx 0 at the nozzle (atmospheric — exactly what you want at the open end). Load that preset and watch the model reproduce all three.

Show your work
Inlet cross-sectional area
A1  =  πD124  =  0.003217  m2A_1 \;=\; \dfrac{\pi D_1^{2}}{4} \;=\; 0.003217\;\mathrm{m^{2}}
Throat cross-sectional area
A2  =  πD224  =  7.069×104  m2A_2 \;=\; \dfrac{\pi D_2^{2}}{4} \;=\; 7.069 \times 10^{-4}\;\mathrm{m^{2}}
Inlet velocity (continuity)
v1  =  QA1  =  12.43  m/sv_1 \;=\; \dfrac{Q}{A_1} \;=\; 12.43\;\mathrm{m/s}
Throat velocity (continuity)
v2  =  QA2  =  56.59  m/sv_2 \;=\; \dfrac{Q}{A_2} \;=\; 56.59\;\mathrm{m/s}
Kinetic-energy pressure drop (½ρ Δv²)
Δpkin  =  12ρ(v22v12)  =  1.524×106  Pa\Delta p_{\text{kin}} \;=\; \tfrac{1}{2}\,\rho\,(v_2^{2} - v_1^{2}) \;=\; 1.524 \times 10^{6}\;\mathrm{Pa}
Gravity pressure drop (ρ g Δh)
Δpgrav  =  ρgΔh  =  ρ(9.8)Δh  =  98000  Pa\Delta p_{\text{grav}} \;=\; \rho\,g\,\Delta h \;=\; \rho\,\textcolor{#dc4124}{\left(9.8\right)}\,\Delta h \;=\; 98000\;\mathrm{Pa}
Outlet pressure (Bernoulli)
p2  =  p112ρ(v22v12)ρgΔh  =  p112ρ(v22v12)ρ(9.8)Δh  =  1823  Pap_2 \;=\; p_1 - \tfrac{1}{2}\rho(v_2^{2} - v_1^{2}) - \rho g\,\Delta h \;=\; p_1 - \tfrac{1}{2}\rho(v_2^{2} - v_1^{2}) - \rho \textcolor{#dc4124}{\left(9.8\right)}\,\Delta h \;=\; -1823\;\mathrm{Pa}
Worked Example

OpenStax University Physics §14.6 Example 14.7 (Fire Hose Nozzle): hose diameter 6.40 cm, nozzle diameter 3.00 cm, flow 40.0 L/s. Continuity gives v₁ ≈ 12.4 m/s and v₂ ≈ 56.6 m/s (the source's reported values).

QuantityExpectedComputedΔ
v112.4312.430.00398
v256.5956.590.001576
Worked Example

Same OpenStax Example 14.7: with p₁ = 1.62 MPa gauge and a 10.0 m height gain at the nozzle, Bernoulli predicts the nozzle exit pressure p₂ ≈ 0 (atmospheric). With unrounded velocities the model evaluates to p₂ ≈ −1.82 kPa — still essentially atmospheric; the small residual is the rounding propagating from OpenStax's 3-significant-figure intermediate velocities.

QuantityExpectedComputedΔ
p2_pa-1820-18232.949
Sources
  1. [1] OpenStax. University Physics Volume 1 — §14.6 Bernoulli's Equation, eq. p + ½ρv² + ρgh = constant; p₁ + ½ρv₁² + ρgh₁ = p₂ + ½ρv₂² + ρgh₂ (openstax.org)
  2. [2] Wikipedia — Bernoulli's principle, eq. ½ρv² + ρgz + p = constant; assumptions: steady, incompressible, inviscid, along a streamline (en.wikipedia.org)
  3. [3] Wikipedia — Venturi effect, eq. p₁ − p₂ = ρ/2·(v₂² − v₁²); Q = v₁A₁ = v₂A₂ (continuity) (en.wikipedia.org)
Assumptions
  • Steady flow — flow parameters at any point do not change with time (OpenStax §14.6).
  • Incompressible flow — fluid density ρ is constant (OpenStax §14.6).
  • Inviscid flow — viscous (frictional) forces are negligible (OpenStax §14.6; Wikipedia: Bernoulli's principle).
  • Bernoulli's equation applies along a streamline (Wikipedia: Bernoulli's principle).
  • The pipe contains a single fluid (no two-phase or compressible-gas effects).
  • Pressure is gauge pressure relative to atmospheric.