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Hydraulics, open channels and fluid power

Equivalent resistance of two parallel quadratic branches

Single resistance that replaces two branches joined at the same two nodes, each obeying h = Ri Qi² with positive flow.

Ref
HYD-14
Rev
v1
Field
Hydraulics, open channels and fluid power
Result
Rp [s²/m⁵]

Parallel branches joined at the same two nodes share the same head loss h, and each carries Qᵢ = √(h/Rᵢ). The flows add, so Q = √h Σ Rᵢ^(−1/2), and the equivalent resistance is Rp = [Σ Rᵢ^(−1/2)]⁻². It is smaller than either branch resistance. This calculator takes two branches; flow must be positive and no branch has a pump or a static lift.

Single resistance that replaces two branches joined at the same two nodes, each obeying h = Ri Qi² with positive flow. The branch flows add at a common head, so the resistances combine through their inverse square roots.

Calculator

Solve for
s²/m⁵
s²/m⁵
11e8
s²/m⁵
11e8
  • Share of the flow in branch 1, √(Rp/R₁)0.6
  • Equivalent resistance as a share of the smaller branch0.36
  • Head loss at 0.1 m³/s1.44 m

What drives the result

Each variable is moved across its typical range while the others stay at the values above. The longest bar is the key driver.

Equivalent resistance (s²/m⁵) current value 144 s²/m⁵
R1Resistance of branch 1Key driver
0.937895
R2Resistance of branch 2
0.907398
  • Two branches of 400 and 900 s²/m⁵ act as one of 144; the lower-resistance branch carries 60 % of the flow.
  • Two identical branches give a quarter of one branch’s resistance, not half, because the flow in each is half and the loss varies with the square.
Chart data as tables

Ranked variables

VariableTypical rangeLowest resultHighest resultSwing (s²/m⁵)Local stepChange in result
R1 Resistance of branch 11 to 1e8 s²/m⁵0.9365894.6893.7+10%+5.83 %
R2 Resistance of branch 21 to 1e8 s²/m⁵0.907398.4397.5+10%+3.83 %

Sweep of Resistance of branch 1

Resistance of branch 1 (s²/m⁵)Equivalent resistance (s²/m⁵)
10.9365
108.184
10056.25
1,000237
10,000532.5
100,000750.8
1,000,000848.3
1e7883.2
1e8894.6

Sweep one variable

Equivalent resistance (s²/m⁵)Hover, touch, or use the arrow keys on the chart
0200400600800 110010k1M100M Resistance of branch 1 (s²/m⁵), log scale now 144

Variables and how each one contributes

Rp

Equivalent resistance

Result · s²/m⁵

What the equation gives you. Everything else feeds it.

R1

Resistance of branch 1

s²/m⁵ · typical 1 to 1e8

The resistance of branch 1, in s²/m⁵. Raises the equivalent resistance, with less than direct proportion since the other branch shares the flow. Raising it by 10 % (to 440) moves the result by +5.83 %, from 144 to 152.4 s²/m⁵.

R2

Resistance of branch 2

s²/m⁵ · typical 1 to 1e8

The resistance of branch 2, in s²/m⁵. Raises the equivalent resistance, with less than direct proportion since the other branch shares the flow. Raising it by 10 % (to 990) moves the result by +3.83 %, from 144 to 149.5 s²/m⁵.

Worked example with the values above

  1. Inverse square roots: 1/√400 + 1/√900 = 0.05 + 0.033333 = 0.083333.
  2. Square it: 0.0069444.
  3. Rp = 1 / that = 144 s²/m⁵.

Assumptions and limits

  • Steady incompressible flow, with the friction factor and loss coefficients held at their duty-point values.
  • Head losses proportional to the square of the flow, with positive flow in each pipe.

Common mistakes

  • Using a loss coefficient that is referred to a different velocity from the one in the formula.
  • Mixing the Darcy friction factor with the Fanning factor, which is a quarter of it.
  • Adding resistances in parallel as if they were in series.

Statistics and uncertainty

Loss coefficients and friction factors are empirical and are usually known to within 10 % to 20 %, so network results carry that uncertainty. The quadratic forms assume the friction factor stays fixed as the flow changes.

Where it is used

  • Building system curves for pumps and checking the effect of fittings.
  • Balancing flows in looped water networks, and simplifying branches into one resistance.

Maths you need

  • Head loss: energy lost per unit weight, in metres
  • Darcy friction factor: f, as in hL = f (L/D) V²/2g
  • Continuity: flow into a node equals flow out

Related formulas

Practise this formula