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Study Notes/Civil Engineering/Hydraulics & Water Resources

Hydraulics & Water Resources

Fluid mechanics, pipe flow, and open channel hydraulics

1. Fluid Properties

Fundamental Properties

Properties that define fluid behavior and response to applied forces.

Mass Density (ρ)

ρ = m/V

Water: ρ = 1000 kg/m³

Specific Weight (γ)

γ = ρg = W/V

Water: γ = 9.81 kN/m³

Specific Gravity (SG)

SG = ρfluidwater

Dimensionless ratio

Specific Volume

vs = 1/ρ = V/m

Volume per unit mass

Viscosity

Dynamic Viscosity (μ)

τ = μ(dv/dy)

Newton's Law of Viscosity

Units: Pa·s or N·s/m²

Kinematic Viscosity (ν)

ν = μ/ρ

Ratio of dynamic to density

Units: m²/s

Surface Tension & Capillarity

Surface Tension (σ)

Force per unit length at liquid surface

Water at 20°C: σ ≈ 0.073 N/m

Capillary Rise

h = 4σ cos θ / (γd)

θ = contact angle, d = tube diameter

Compressibility

Ev = -Δp / (ΔV/V) = -Δp / (Δρ/ρ)

Bulk Modulus of Elasticity

Water: Ev ≈ 2.2 GPa (relatively incompressible)

2. Hydrostatics (Fluid at Rest)

Pressure Variation with Depth

In a static fluid, pressure increases linearly with depth due to fluid weight.

p = γh = ρgh

Pressure at depth h below free surface

pabs = patm + pgauge

Pressure Measurement

Manometer

p₁ + γ₁h₁ = p₂ + γ₂h₂

Pressure balance at same elevation

Pressure Head

h = p/γ

Height of fluid column equivalent to pressure

Hydrostatic Force on Plane Surfaces

Inclined Plane Surface

F = γh̄A = γȳ sin θ A

h̄ = vertical depth to centroid, ȳ = inclined distance to centroid

Center of Pressure (yp)

yp = ȳ + Ic/(ȳA)

Ic = moment of inertia about centroidal axis

Common Moments of Inertia

ShapeAreaIc
Rectangle (b × h)bhbh³/12
Triangle (base b, height h)bh/2bh³/36
Circle (diameter d)πd²/4πd⁴/64

Buoyancy

Archimedes' Principle

FB = γVdisplaced

Buoyant force equals weight of fluid displaced

Acts through centroid of displaced volume (center of buoyancy)

Stability of Floating Bodies

MB = I/Vdisplaced - GB

  • • M = metacenter, B = center of buoyancy, G = center of gravity
  • • Stable if M is above G (positive MB)
  • • Unstable if M is below G (negative MB)

3. Fluid Dynamics Fundamentals

Types of Flow

Based on Time

  • Steady: Properties don't change with time
  • Unsteady: Properties vary with time

Based on Space

  • Uniform: Same velocity at all points
  • Non-uniform: Velocity varies spatially

Reynolds Number

Re = ρVD/μ = VD/ν

Ratio of inertial to viscous forces

Pipe Flow:

• Laminar: Re < 2000

• Transition: 2000 < Re < 4000

• Turbulent: Re > 4000

Open Channel:

• Laminar: Re < 500

• Transition: 500 < Re < 2000

• Turbulent: Re > 2000

Continuity Equation

Q = A₁V₁ = A₂V₂

For incompressible, steady flow

Q = AV

Discharge = Area × Velocity

Bernoulli's Equation

p₁/γ + V₁²/2g + z₁ = p₂/γ + V₂²/2g + z₂

For ideal fluid: steady, incompressible, frictionless flow along streamline

Head Components:

  • Pressure Head: p/γ (energy due to pressure)
  • Velocity Head: V²/2g (kinetic energy)
  • Elevation Head: z (potential energy)
  • Total Head: H = p/γ + V²/2g + z

Energy Equation (with losses)

p₁/γ + V₁²/2g + z₁ = p₂/γ + V₂²/2g + z₂ + hL

hL = head loss due to friction and minor losses

Momentum Equation

ΣF = ρQ(V₂ - V₁)

Force = Rate of change of momentum

Used for calculating forces on pipe bends, jets, etc.

4. Pipe Flow

Darcy-Weisbach Equation

hf = fLV²/(2gD)

f = friction factor, L = pipe length, D = diameter

Friction Factor (f)

Laminar Flow (Re < 2000)

f = 64/Re

Hagen-Poiseuille equation

Turbulent Flow

Use Moody diagram or:

• Colebrook equation (implicit)

• Swamee-Jain (explicit approximation)

Hazen-Williams Formula

V = 0.8492CHWR0.63S0.54

Commonly used for water distribution (SI units)

CHW: New cast iron = 130, Old cast iron = 100, PVC = 150

Minor Losses

hm = KV²/2g

K = loss coefficient

FittingK Value
Sharp-edged entrance0.5
Rounded entrance0.04
Exit loss1.0
90° elbow (regular)0.3
90° elbow (long radius)0.2
Gate valve (fully open)0.2
Globe valve (fully open)10
Check valve2.5

Pipes in Series and Parallel

Series

Q = Q₁ = Q₂ = Q₃

hL = hL1 + hL2 + hL3

Same flow, head losses add

Parallel

Q = Q₁ + Q₂ + Q₃

hL = hL1 = hL2 = hL3

Flows add, same head loss

5. Open Channel Flow

Open Channel vs Pipe Flow

Open channel has free surface exposed to atmosphere. Driving force is gravity (slope), not pressure difference.

Geometric Properties

  • Wetted Perimeter (P): Length of channel boundary in contact with water
  • Hydraulic Radius (R): R = A/P (flow efficiency)
  • Hydraulic Depth (Dh): Dh = A/T (T = top width)
  • Slope (S): S = hf/L = sin θ ≈ tan θ (for small angles)

Manning's Equation

V = (1/n)R2/3S1/2

Q = (1/n)AR2/3S1/2

n = Manning's roughness coefficient (SI units)

Channel Typen Value
Glass, PVC0.010
Smooth concrete0.012
Finished concrete0.015
Earth channel (clean)0.022
Natural stream (clean)0.030
Natural stream (weeds)0.050

Froude Number

Fr = V/√(gDh)

Ratio of inertial to gravitational forces

Fr < 1: Subcritical (tranquil) - Deep, slow flow

Fr = 1: Critical flow

Fr > 1: Supercritical (rapid) - Shallow, fast flow

Specific Energy

E = y + V²/2g = y + Q²/(2gA²)

Energy per unit weight relative to channel bottom

Critical Depth (rectangular channel):

yc = (Q²/gb²)1/3 = (q²/g)1/3

q = Q/b = unit discharge

Hydraulic Jump

Sequent Depth Relationship (rectangular channel)

y₂/y₁ = ½(√(1 + 8Fr₁²) - 1)

Energy loss: ΔE = (y₂ - y₁)³/(4y₁y₂)

6. Weirs and Orifices

Orifice Flow

Q = CdA√(2gH)

Cd = discharge coefficient (typically 0.60-0.65)

H = head above center of orifice

Orifice Coefficients:

  • Cc: Contraction coefficient = Ajet/Aorifice
  • Cv: Velocity coefficient = Vactual/Vtheoretical
  • Cd: Discharge coefficient = Cc × Cv

Rectangular Weirs

Suppressed (Full Width)

Q = Cd(2/3)b√(2g)H3/2

Francis formula:

Q = 1.84bH3/2 (SI)

Contracted

Q = 1.84(b - 0.2H)H3/2

Account for end contractions

Two contractions: subtract 0.1H each side

V-Notch (Triangular) Weir

Q = Cd(8/15)√(2g)tan(θ/2)H5/2

θ = notch angle

For 90° V-notch:

Q = 1.38H5/2 (SI, with Cd = 0.58)

Cipolletti Weir

Trapezoidal weir with 4:1 side slopes (compensates for contractions)

Q = 1.86bH3/2 (SI)

Broad-Crested Weir

Q = Cdb√g(2/3H)3/2

Critical flow occurs at crest

Q ≈ 1.7bH3/2 (SI, approximate)

7. Water Supply Systems

Water Demand

Design Periods (Typical):

  • • Source of supply: 25-50 years
  • • Transmission mains: 25-30 years
  • • Distribution system: 25 years
  • • Treatment plant: 15-25 years
  • • Pumps & equipment: 10-15 years

Per Capita Consumption

Classificationlpcd (liters/capita/day)
Rural communities60-100
Small towns100-150
Cities (residential)150-200
Metro areas200-300

Demand Variations

  • Average Daily Demand: Qavg = Population × per capita consumption
  • Maximum Daily Demand: Qmax,day = 1.5 to 2.0 × Qavg
  • Maximum Hourly Demand: Qmax,hr = 2.0 to 3.0 × Qavg
  • Fire Demand: Qfire = 100√P (P = population in thousands, Q in liters/min)

Storage Requirements

Components of Storage:

  • Equalizing storage: 25-30% of max daily demand
  • Fire reserve: Fire flow × duration (typically 4-6 hours)
  • Emergency storage: 25% of average daily demand

Distribution System

Grid/Loop System

  • • Multiple supply paths
  • • More reliable (redundancy)
  • • Lower head loss
  • • Higher cost

Tree/Dead-End System

  • • Single supply path
  • • Less reliable
  • • Lower cost
  • • Used for small communities

8. Pumps and Pumping Systems

Total Dynamic Head (TDH)

TDH = Hs + Hd + hf + V²d/2g

Hs = static suction lift, Hd = static discharge head

hf = friction losses, V²d/2g = velocity head at discharge

Pump Power

Water Power (Output)

Pw = γQH = ρgQH

Theoretical power delivered to water

Brake Power (Input)

Pb = Pw

Power required at pump shaft

Pump Efficiency

η = Pw/Pb = γQH/Pb

Typical centrifugal pump: η = 60-85%

Specific Speed

Ns = NQ1/2/H3/4

N = rpm, Q = flow rate, H = head

Low Ns (500-1500): Radial flow - high head, low flow

Medium Ns (1500-4000): Mixed flow

High Ns (4000-15000): Axial flow - low head, high flow

Net Positive Suction Head (NPSH)

NPSHa = patm/γ - Hs - hf,s - pv

NPSHa = Available, pv = vapor pressure

NPSHa > NPSHr (to avoid cavitation)

Affinity Laws

For same pump, variable speed:

Q₂/Q₁ = N₂/N₁

Flow ∝ Speed

H₂/H₁ = (N₂/N₁)²

Head ∝ Speed²

P₂/P₁ = (N₂/N₁)³

Power ∝ Speed³

Pumps in Series and Parallel

Series

Same Q, heads add

Htotal = H₁ + H₂

Used for high head applications

Parallel

Same H, flows add

Qtotal = Q₁ + Q₂

Used for high flow applications

Key Takeaways for CE Board Exam

Must-Know Formulas

  • ✓ Pressure: p = γh
  • ✓ Bernoulli: p/γ + V²/2g + z = constant
  • ✓ Continuity: Q = AV
  • ✓ Darcy: hf = fLV²/2gD
  • ✓ Manning: V = (1/n)R2/3S1/2
  • ✓ Weir: Q ∝ H3/2 (rectangular)
  • ✓ Pump power: P = γQH

Critical Concepts

  • ✓ Reynolds number: Re = VD/ν
  • ✓ Froude number: Fr = V/√(gD)
  • ✓ Critical depth and specific energy
  • ✓ Pipe series vs parallel
  • ✓ Minor loss coefficients (K values)
  • ✓ NPSH and cavitation prevention
  • ✓ Affinity laws for pumps