8.1 Fluid Dynamics: Continuity and Energy Equations

Key Takeaways

  • Fluid flow regimes are classified by temporal constancy (steady vs unsteady), spatial constancy along streamlines (uniform vs non-uniform), viscous shear stability (laminar vs turbulent), and vorticity (rotational vs irrotational).

  • The Continuity Equation enforces conservation of mass: for steady one-dimensional flow of an incompressible fluid (ρ=constant\rho = \text{constant}), volumetric flow rate remains constant across all cross-sections: Q=A1v1=A2v2Q = A_1 v_1 = A_2 v_2.

  • Total energy head along a streamline is the sum of elevation head (zz), pressure head (P/γP/\gamma), and velocity head (αv2/(2g)\alpha v^2 / (2g)), where the Coriolis kinetic energy correction factor α\alpha is 2.0 for fully developed laminar flow and approximately 1.01 to 1.05 for turbulent flow.

  • The Extended Energy Equation balances mechanical energy across flow stations: z1+P1/γ+v12/(2g)+Hp−Ht−hL=z2+P2/γ+v22/(2g)z_1 + P_1/\gamma + v_1^2/(2g) + H_p - H_t - h_L = z_2 + P_2/\gamma + v_2^2/(2g), where pump head HpH_p adds energy (Powerin=QγHp/η\text{Power}_{\text{in}} = Q\gamma H_p / \eta), turbine head HtH_t extracts energy (Powerout=QγHtη\text{Power}_{\text{out}} = Q\gamma H_t \eta), and hLh_L accounts for total frictional and minor head loss.

  • The Hydraulic Grade Line (HGL: z+P/γz + P/\gamma) runs parallel below the Energy Grade Line (EGL) by the velocity head v2/(2g)v^2/(2g); whenever the conduit profile rises above the HGL, sub-atmospheric (vacuum) gauge pressure occurs, creating a severe cavitation hazard if absolute pressure drops to water vapor pressure (Pv≈2.34 kPa absP_v \approx 2.34\text{ kPa abs} at 20°C, corresponding to -10.1 m of water gauge).

Last updated: October 2026

8.1 Fluid Dynamics: Continuity and Energy Equations

In fluid mechanics, fluid dynamics investigates fluids in motion under the action of unbalanced body and surface forces. In the Philippine Civil Engineering Licensure Examination (CELE), fluid dynamics, closed conduit flow, and open channel hydraulics represent major quantitative components of the Hydraulics and Principles of Geotechnical Engineering (HGE) syllabus. Mastery of these topics requires a firm grasp of the fundamental conservation laws: conservation of mass (Continuity Equation), conservation of energy (First Law of Thermodynamics / Extended Bernoulli Equation), and conservation of linear momentum.


1. Flow Classifications and Streamline Kinematics

To analyze a moving fluid, engineers classify the velocity vector field v⃗(x,y,z,t)\vec{v}(x, y, z, t) according to its variation across time and space:

ClassificationMathematical CriterionPhysical Meaning / Practical Example
Steady Flow∂v⃗∂t=0,  ∂P∂t=0,  ∂ρ∂t=0\frac{\partial \vec{v}}{\partial t} = 0, \; \frac{\partial P}{\partial t} = 0, \; \frac{\partial \rho}{\partial t} = 0Velocity, pressure, and density at any fixed point remain invariant over time (e.g., constant outflow from a regulated reservoir).
Unsteady Flow∂v⃗∂t≠0\frac{\partial \vec{v}}{\partial t} \ne 0Fluid properties at a fixed spatial point change over time (e.g., water hammer pressure surges, draining a tank under falling head).
Uniform Flow∂v⃗∂s=0\frac{\partial \vec{v}}{\partial s} = 0Velocity vector (magnitude and direction) remains constant along a streamline at any instant (e.g., flow in a straight prismatic canal of constant cross-section).
Non-Uniform Flow∂v⃗∂s≠0\frac{\partial \vec{v}}{\partial s} \ne 0Velocity changes along the path of flow due to changing cross-sectional area or alignment (e.g., flow through a pipe reducer or over a spillway).
Laminar FlowLow Reynolds number (Re<2000Re < 2000 in pipes)Fluid moves in smooth, parallel laminas or layers without macroscopic mixing; viscous shear stresses dominate.
Turbulent FlowHigh Reynolds number (Re>4000Re > 4000 in pipes)Fluid particles move in chaotic, erratic three-dimensional eddy trajectories; momentum exchange dominates.
Rotational Flowcurl v⃗=∇×v⃗≠0\text{curl } \vec{v} = \nabla \times \vec{v} \ne 0Fluid elements rotate about their own mass centers while translating (vorticity ω⃗≠0\vec{\omega} \ne 0).
Irrotational Flowcurl v⃗=∇×v⃗=0\text{curl } \vec{v} = \nabla \times \vec{v} = 0Fluid elements undergo deformation and translation without angular rotation (potential flow).

Streamlines, Pathlines, and Streaklines

  • Streamline: An imaginary continuous curve drawn through a flowing fluid such that the velocity vector of fluid particles at every point along the curve is tangent to it at that instant (dx/u=dy/v=dz/wdx/u = dy/v = dz/w). Because velocity is tangent, no fluid can cross a streamline.
  • Pathline: The actual trajectory traced by an individual fluid particle over a period of time (Lagrangian description).
  • Streakline: The instantaneous locus of all fluid particles that have previously passed through a specific common injection point (e.g., dye injected continuously from a fixed needle).
  • Under steady flow conditions, streamlines, pathlines, and streaklines are completely identical.

2. Conservation of Mass: The Continuity Equation

For a control volume bounded by a control surface, conservation of mass dictates that the net mass flux exiting through the control surface equals the time rate of mass decrease within the control volume.

Volumetric and Mass Flow Rate

For a cross-section of area AA with a local velocity profile vnv_n perpendicular to dAdA: Volumetric Flow Rate: Q=∫Avn dA=Av\text{Volumetric Flow Rate: } Q = \int_A v_n \, dA = A v Mass Flow Rate: m˙=∫Aρvn dA=ρAv=ρQ\text{Mass Flow Rate: } \dot{m} = \int_A \rho v_n \, dA = \rho A v = \rho Q where v=vavgv = v_{\text{avg}} is the area-weighted mean velocity (m/s\text{m/s}), AA is the flow area (m2\text{m}^2), ρ\rho is mass density (kg/m3\text{kg/m}^3), and QQ is discharge (m3/s\text{m}^3/\text{s} or L/s\text{L/s}, where 1 m3/s=1,000 L/s1\text{ m}^3/\text{s} = 1,000\text{ L/s}). The weight flow rate is Wf=γQ=ρgQW_f = \gamma Q = \rho g Q (N/s\text{N/s} or kN/s\text{kN/s}).

One-Dimensional Continuity for Incompressible Flow

For steady flow of an incompressible fluid (ρ1=ρ2=constant\rho_1 = \rho_2 = \text{constant}): ρ1A1v1=ρ2A2v2  ⟹  A1v1=A2v2=Q=constant\rho_1 A_1 v_1 = \rho_2 A_2 v_2 \implies A_1 v_1 = A_2 v_2 = Q = \text{constant} For circular pipes of internal diameter D1D_1 and D2D_2: πD124v1=πD224v2  ⟹  v2=v1(D1D2)2\frac{\pi D_1^2}{4} v_1 = \frac{\pi D_2^2}{4} v_2 \implies v_2 = v_1 \left(\frac{D_1}{D_2}\right)^2 For a branching pipe junction with mm incoming conduits and nn outgoing conduits: ∑i=1mQin,i=∑j=1nQout,j\sum_{i=1}^m Q_{\text{in}, i} = \sum_{j=1}^n Q_{\text{out}, j}


3. Total Energy Head and Bernoulli's Theorem

Consider an elemental fluid prism moving along a streamline in steady, frictionless (inviscid) flow. Integrating Euler's equation of motion along the streamline yields Bernoulli's Theorem.

Components of Fluid Energy Head

Every unit weight of a flowing fluid possesses three distinct mechanical energy components, each expressed in linear dimensions of length (meters of fluid):

  1. Elevation (Potential) Head (zz): Energy of position above an arbitrary horizontal datum plane (meters, m\text{m}).
  2. Pressure Head (Pγ\frac{P}{\gamma}): Energy stored in the fluid due to static hydrostatic pressure PP relative to specific weight γ=ρg\gamma = \rho g (meters, m\text{m}).
  3. Velocity (Kinetic) Head (αv22g\alpha \frac{v^2}{2g}): Kinetic energy per unit weight of fluid moving at average velocity vv (meters, m\text{m}).

The Coriolis Kinetic Energy Correction Factor (α\alpha)

Because the true velocity profile across a conduit is non-uniform (zero at the pipe wall, maximum at centerline), the actual integrated kinetic energy exceeds vavg22g\frac{v_{\text{avg}}^2}{2g}. The kinetic energy correction factor α\alpha is defined as: α=1Av3∫Au3 dA\alpha = \frac{1}{A v^3} \int_A u^3 \, dA

  • Laminar pipe flow (parabolic profile): α=2.0\alpha = 2.0.
  • Turbulent pipe flow (logarithmic profile): α≈1.01 to 1.05\alpha \approx 1.01\text{ to }1.05. In civil engineering licensure calculations, α\alpha is taken as 1.01.0 for turbulent flow unless explicitly instructed otherwise.

Classical Bernoulli Equation (Ideal / Frictionless Flow)

Between any two sections 1 and 2 along a streamline in steady, incompressible, frictionless flow: z1+P1γ+v122g=z2+P2γ+v222g=H=constantz_1 + \frac{P_1}{\gamma} + \frac{v_1^2}{2g} = z_2 + \frac{P_2}{\gamma} + \frac{v_2^2}{2g} = H = \text{constant} where HH is the total mechanical energy head.


4. The Extended Energy Equation: Pumps, Turbines, and Head Losses

Real engineering hydraulic systems experience energy inputs from mechanical pumps, energy extractions from turbines, and irreversibilities due to boundary shear friction and turbulence.

z1+P1γ+α1v122g+Hp−Ht−hL=z2+P2γ+α2v222g\boxed{z_1 + \frac{P_1}{\gamma} + \alpha_1 \frac{v_1^2}{2g} + H_p - H_t - h_L = z_2 + \frac{P_2}{\gamma} + \alpha_2 \frac{v_2^2}{2g}}

Mechanical Energy Devices and Power Formulations

  1. Pumps (HpH_p): A pump adds mechanical energy head HpH_p (m\text{m}) to the fluid, raising its pressure and/or elevation.

    • Water (Fluid) Power Output: The rate of useful energy transferred to the liquid: Pwater=QγHp=ρgQHp(Watts or kW)P_{\text{water}} = Q \gamma H_p = \rho g Q H_p \quad (\text{Watts or kW})
    • Brake (Input) Shaft Power: The mechanical power required to drive the pump shaft, considering pump efficiency ηp<1.0\eta_p < 1.0: Pinput=QγHpηpP_{\text{input}} = \frac{Q \gamma H_p}{\eta_p} (For QQ in m3/s\text{m}^3/\text{s}, γ\gamma in kN/m3\text{kN/m}^3, and HpH_p in m\text{m}, PinputP_{\text{input}} is in kW\text{kW}. In Imperial units: HP=QγHp550η\text{HP} = \frac{Q \gamma H_p}{550 \eta}, with QQ in ft3/s\text{ft}^3/\text{s} and γ=62.4 lb/ft3\gamma = 62.4\text{ lb/ft}^3).
  2. Turbines (HtH_t): A hydraulic turbine extracts energy head HtH_t (m\text{m}) from the fluid to generate electrical power.

    • Power Extracted from Fluid: Pfluid=QγHtP_{\text{fluid}} = Q \gamma H_t.
    • Delivered Output Power: The electrical/mechanical power produced, considering turbine efficiency ηt<1.0\eta_t < 1.0: Poutput=QγHtηtP_{\text{output}} = Q \gamma H_t \eta_t
  3. Total Head Loss (hLh_L): Head lost between sections 1 and 2, consisting of pipe wall friction loss (hfh_f) and minor fitting losses (hmh_m): hL=hf+∑hmh_L = h_f + \sum h_m


5. Hydraulic Grade Line (HGL) and Energy Grade Line (EGL)

The graphical representation of energy along a hydraulic conduit provides vital diagnostic insight into operational pressures and vacuum zones.

LineMathematical FormulationPhysical Significance
Energy Grade Line (EGL)EGL=z+Pγ+v22g\text{EGL} = z + \frac{P}{\gamma} + \frac{v^2}{2g}Represents total mechanical head available to the fluid at each station relative to datum.
Hydraulic Grade Line (HGL)HGL=z+Pγ\text{HGL} = z + \frac{P}{\gamma}Represents the piezometric head—the height to which liquid would rise in a vertical piezometer tube.

Fundamental Geometric Rules for EGL and HGL

  1. Vertical Separation: The EGL always lies vertically above the HGL by exactly the velocity head v22g\frac{v^2}{2g}. Where the velocity is zero (such as in large storage reservoirs), the EGL and HGL coincide at the free liquid surface.
  2. Frictional Slope: In passive conduits (no pumps), the EGL must always slope downward in the direction of flow at a hydraulic slope Sf=dhfdLS_f = \frac{dh_f}{dL}.
  3. Pump Discontinuity: A pump introduces an instantaneous vertical upward jump in both the EGL and HGL equal to the pump head HpH_p.
  4. Turbine Discontinuity: A turbine introduces an instantaneous vertical downward drop in both lines equal to HtH_t.
  5. Conduit Contraction: When pipe diameter decreases, velocity vv increases, expanding the velocity head v22g\frac{v^2}{2g}. Consequently, the HGL drops sharply below the EGL.
  6. Conduit Expansion: When pipe diameter increases, velocity vv drops. If the reduction in velocity head exceeds the localized expansion head loss, the HGL experiences a localized rise, termed pressure recovery.
  7. Sub-Atmospheric (Vacuum) Zones: If the physical pipe profile rises above the HGL, the gauge pressure head Pγ=HGL−zpipe\frac{P}{\gamma} = \text{HGL} - z_{\text{pipe}} becomes negative (gauge vacuum).

6. Siphon Hydraulics and Cavitation Phenomena

A siphon is a closed conduit configured to convey liquid from an elevated reservoir over an intermediate topographic summit to a discharge point at lower elevation without mechanical pumping, relying on atmospheric pressure and gravity.

Loading diagram...

The Mechanism of Cavitation

At the summit of a functioning siphon, the physical elevation of the pipe invert (zsz_s) exceeds the Hydraulic Grade Line elevation (HGLs\text{HGL}_s), producing sub-atmospheric pressure: Ps,gaugeγ=HGLs−zs=zres−zs−vs22g−hL,1→s<0\frac{P_{s, \text{gauge}}}{\gamma} = \text{HGL}_s - z_s = z_{\text{res}} - z_s - \frac{v_s^2}{2g} - h_{L, 1\to s} < 0 If this absolute pressure falls to the saturation vapor pressure of the liquid (PvP_v): Ps,abs≤Pv  ⟹  Ps,gaugeγ≤Pv−PatmγP_{s, \text{abs}} \le P_v \implies \frac{P_{s, \text{gauge}}}{\gamma} \le \frac{P_v - P_{\text{atm}}}{\gamma} For water at standard ambient temperature (20∘C20^\circ\text{C}), Pv≈2.34 kPa absP_v \approx 2.34\text{ kPa abs} and Patm=101.325 kPaP_{\text{atm}} = 101.325\text{ kPa}. The maximum permissible negative gauge pressure head before vapor formation is: (Pgaugeγ)limit=2.34−101.3259.81=−10.09 m of water\left(\frac{P_{\text{gauge}}}{\gamma}\right)_{\text{limit}} = \frac{2.34 - 101.325}{9.81} = -10.09\text{ m of water} When absolute pressure reaches PvP_v, the liquid boils at ambient temperature, generating vapor-filled bubbles (vapor cavities). As these vapor cavities travel into downstream zones of higher pressure, they collapse violently within microseconds, generating localized microjets and shockwave pressures exceeding 500 MPa500\text{ MPa}. This causes severe pitting erosion, pipe wall fatigue failure, intense vibration, and immediate de-priming (air locking) of the siphon.


7. Worked Example: High-Lift Pumping Conduit Analysis

Problem Statement: A municipal water supply pumping station lifts water (γ=9.81 kN/m3\gamma = 9.81\text{ kN/m}^3) from a suction well with water surface at Elev 18.00 m\text{Elev } 18.00\text{ m} to a distribution reservoir with water surface at Elev 68.00 m\text{Elev } 68.00\text{ m}. The system features:

  • Discharge rate: Q=0.120 m3/sQ = 0.120\text{ m}^3/\text{s} (120 L/s120\text{ L/s}).
  • Total pipe length: L=550 mL = 550\text{ m} of 300 mm300\text{ mm} internal diameter ductile iron pipe (D=0.300 mD = 0.300\text{ m}).
  • Darcy-Weisbach friction factor: f=0.020f = 0.020.
  • Minor losses: square-edged entrance (Ke=0.50K_e = 0.50), four 90∘90^\circ flanged bends (Kb=4×0.35=1.40K_b = 4 \times 0.35 = 1.40), one swing check valve (Kv=2.50K_v = 2.50), and submerged pipe exit into the reservoir (Kexit=1.00K_{\text{exit}} = 1.00).
  • Combined pump-motor efficiency: η=76%\eta = 76\%.

Determine (a) the velocity head in the pipe, (b) the total head loss, (c) the total dynamic head developed by the pump (HpH_p), and (d) the electrical input power required in kilowatts.

Step-by-Step Solution:

  1. Calculate flow velocity and velocity head: A=πD24=π(0.300 m)24=0.070686 m2A = \frac{\pi D^2}{4} = \frac{\pi (0.300\text{ m})^2}{4} = 0.070686\text{ m}^2 v=QA=0.120 m3/s0.070686 m2=1.6976 m/sv = \frac{Q}{A} = \frac{0.120\text{ m}^3/\text{s}}{0.070686\text{ m}^2} = 1.6976\text{ m/s} v22g=(1.6976 m/s)22(9.81 m/s2)=2.881919.62=0.1469 m\frac{v^2}{2g} = \frac{(1.6976\text{ m/s})^2}{2(9.81\text{ m/s}^2)} = \frac{2.8819}{19.62} = 0.1469\text{ m}

  2. Compute major friction head loss (hfh_f): hf=fLDv22g=(0.020)(550 m0.300 m)(0.1469 m)=36.667×0.1469 m=5.386 mh_f = f \frac{L}{D} \frac{v^2}{2g} = (0.020) \left(\frac{550\text{ m}}{0.300\text{ m}}\right) (0.1469\text{ m}) = 36.667 \times 0.1469\text{ m} = 5.386\text{ m}

  3. Compute minor head losses (hmh_m): ∑K=Ke+Kb+Kv+Kexit=0.50+1.40+2.50+1.00=5.40\sum K = K_e + K_b + K_v + K_{\text{exit}} = 0.50 + 1.40 + 2.50 + 1.00 = 5.40 hm=∑Kv22g=5.40×0.1469 m=0.793 mh_m = \sum K \frac{v^2}{2g} = 5.40 \times 0.1469\text{ m} = 0.793\text{ m} Total Head Loss: hL=hf+hm=5.386+0.793=6.179 m\text{Total Head Loss: } h_L = h_f + h_m = 5.386 + 0.793 = 6.179\text{ m}

  4. Apply Energy Equation between suction well surface (1) and upper reservoir surface (2): z1+P1γ+v122g+Hp−hL=z2+P2γ+v222gz_1 + \frac{P_1}{\gamma} + \frac{v_1^2}{2g} + H_p - h_L = z_2 + \frac{P_2}{\gamma} + \frac{v_2^2}{2g} Because both reservoirs are open to atmosphere, P1=P2=0 kPa gaugeP_1 = P_2 = 0\text{ kPa gauge}. For large reservoirs, v1≈0v_1 \approx 0 and v2≈0v_2 \approx 0. 18.00+0+0+Hp−6.179=68.00+0+018.00 + 0 + 0 + H_p - 6.179 = 68.00 + 0 + 0 Hp=(68.00−18.00)+6.179=50.00+6.179=56.18 mH_p = (68.00 - 18.00) + 6.179 = 50.00 + 6.179 = 56.18\text{ m}

  5. Compute Water Power and Electrical Input Power: Pwater=QγHp=(0.120 m3/s)(9.81 kN/m3)(56.179 m)=66.134 kWP_{\text{water}} = Q \gamma H_p = (0.120\text{ m}^3/\text{s})(9.81\text{ kN/m}^3)(56.179\text{ m}) = 66.134\text{ kW} Pinput=Pwaterη=66.134 kW0.76=87.02 kWP_{\text{input}} = \frac{P_{\text{water}}}{\eta} = \frac{66.134\text{ kW}}{0.76} = 87.02\text{ kW}


8. The Momentum Equation: Forces on Bends, Nozzles, Jets and Vanes

Energy equations give pressures and heads. The impulse-momentum principle gives the forces that moving water exerts on pipes, nozzles and blades. For steady flow through a control volume:

∑F⃗=ρQ(v⃗2−v⃗1)\sum \vec{F} = \rho Q (\vec{v}_2 - \vec{v}_1)

The left side includes pressure forces on the inlet and outlet areas, weight if relevant, and the force exerted by the solid boundary on the fluid. The fluid's force on the boundary is equal and opposite.

Free jet striking a fixed flat plate normal to the jet

The jet loses all its velocity in the original direction, so:

F=ρQv=ρAv2F = \rho Q v = \rho A v^2

Example. A 50 mm50\text{ mm} jet moves at 20 m/s20\text{ m/s}. A=0.0019635 m2A = 0.0019635\text{ m}^2 and Q=0.03927 m3/sQ = 0.03927\text{ m}^3/\text{s}, so F=1000(0.03927)(20)=785 NF = 1000(0.03927)(20) = 785\text{ N}.

Moving vane

For a single vane moving at speed uu in the jet's direction, the relative velocity is (v−u)(v - u). The mass actually deflected per second is ρA(v−u)\rho A (v - u). For a flat plate normal to the jet:

F=ρA(v−u)2F = \rho A (v - u)^2

For a series of vanes on a wheel, as in an impulse turbine, all the jet's mass is used, so F=ρQ(v−u)(1−cos⁡θ)F = \rho Q (v - u)(1 - \cos\theta) for a deflection angle θ\theta. Power is FuF u, which is maximized near u=v/2u = v/2.

Pipe bend in a horizontal plane

For a bend that turns the flow through angle θ\theta, with pressures p1,p2p_1, p_2 and areas A1,A2A_1, A_2:

Fx=p1A1−p2A2cos⁡θ−ρQ(v2cos⁡θ−v1)F_x = p_1 A_1 - p_2 A_2 \cos\theta - \rho Q (v_2 \cos\theta - v_1) Fy=−p2A2sin⁡θ−ρQv2sin⁡θF_y = - p_2 A_2 \sin\theta - \rho Q v_2 \sin\theta

Here FxF_x and FyF_y are the components the fluid exerts on the bend; the anchor block must resist R=Fx2+Fy2R = \sqrt{F_x^2 + F_y^2}.

Example. A 300 mm300\text{ mm} horizontal 90∘90^\circ bend carries 0.15 m3/s0.15\text{ m}^3/\text{s} at 200 kPa200\text{ kPa}, assuming negligible head loss. A=0.070686 m2A = 0.070686\text{ m}^2, so v=2.122 m/sv = 2.122\text{ m/s} and ρQv=1000(0.15)(2.122)=318 N\rho Q v = 1000(0.15)(2.122) = 318\text{ N}. The pressure force is pA=200,000(0.070686)=14,137 NpA = 200{,}000(0.070686) = 14{,}137\text{ N}. Each component is 14,137+318=14,455 N14{,}137 + 318 = 14{,}455\text{ N}. The resultant is 2(14,455)=20,443 N≈20.4 kN\sqrt{2}(14{,}455) = 20{,}443\text{ N} \approx 20.4\text{ kN}, acting at 45∘45^\circ toward the outside of the bend.

9. CELE Exam Traps & Common Computational Errors

Warning

Trap 1: Pump Efficiency Inversion: Never multiply pump head or fluid power by η\eta when calculating input electrical power. A pump consumes more energy than it delivers to the liquid: Pinput=PwaterηP_{\text{input}} = \frac{P_{\text{water}}}{\eta}. Conversely, for a turbine, electrical output is less than extracted fluid energy: Poutput=Pfluid×ηP_{\text{output}} = P_{\text{fluid}} \times \eta.

Warning

Trap 2: Ignoring Velocity Head in Siphon Vacuum Calculations: When finding the absolute pressure at a siphon summit, candidates frequently set Ps/γ=zres−zs−hLP_s/\gamma = z_{\text{res}} - z_s - h_L, forgetting to subtract the kinetic velocity head vs22g\frac{v_s^2}{2g}. In high-velocity siphons, omission of velocity head overestimates the summit pressure and fails to predict impending cavitation.

Warning

Trap 3: Piezometer Readings and HGL vs. EGL: An open piezometer tube measures static pressure head plus elevation (z+P/γz + P/\gamma), which corresponds strictly to the HGL. A Pitot tube with its opening facing into the flow measures total energy head (z+P/γ+v2/(2g)z + P/\gamma + v^2/(2g)), which corresponds to the EGL.

Loading diagram...
Energy Grade Line (EGL) and Hydraulic Grade Line (HGL) Profile for a Reservoir-Pump-Piping System
Test Your Knowledge

A centrifugal pump lifts freshwater (γ = 9.81 kN/m³) from a lower storage sump (surface elevation 15.0 m) to an elevated tank (surface elevation 75.0 m) at a constant rate of 0.150 m³/s. The suction and discharge piping system has a cumulative head loss of 12.0 m. If the overall efficiency of the pump-motor assembly is 78.0%, what is the required electrical input power to the motor?

A

82.6 kW

B

113.2 kW

C

105.9 kW

D

135.8 kW

Test Your Knowledge

A siphon of uniform 150-mm diameter discharges water from an open reservoir (water level at Elev 24.0 m) to the atmosphere at Elev 14.0 m. The summit of the siphon is located at Elev 28.5 m. The total head loss from the reservoir intake to the summit is 1.20 m, and the discharge velocity through the siphon is 3.00 m/s. Assuming an atmospheric pressure of 101.30 kPa and γ = 9.81 kN/m³, what is the absolute pressure at the siphon summit?

A

60.4 kPa abs

B

31.5 kPa abs

C

52.7 kPa abs

D

40.9 kPa abs

Test Your Knowledge

In fluid conduit analysis, what is the Coriolis kinetic energy correction factor (α), and what are its standard values for fully developed laminar and turbulent pipe flows?

A

α = 1.0 for laminar flow and α = 2.0 for turbulent flow, because turbulent flow possesses turbulent eddy kinetic energy.

B

α is identically 1.0 for all real fluid flows because mass conservation automatically enforces kinetic energy uniformity.

C

α = 2.0 for laminar flow and α ≈ 1.01 to 1.05 for turbulent flow, because the parabolic laminar profile exhibits a significantly greater peak-to-average velocity ratio.

D

α = 0.50 for laminar flow and α = 1.33 for turbulent flow, derived directly from the momentum correction factor β.

Sections you finish are checked off in the contents.