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 = ρfluid/ρwater
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
| Shape | Area | Ic |
|---|---|---|
| Rectangle (b × h) | bh | bh³/12 |
| Triangle (base b, height h) | bh/2 | bh³/36 |
| Circle (diameter d) | πd²/4 | πd⁴/64 |
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
| Fitting | K Value |
|---|---|
| Sharp-edged entrance | 0.5 |
| Rounded entrance | 0.04 |
| Exit loss | 1.0 |
| 90° elbow (regular) | 0.3 |
| 90° elbow (long radius) | 0.2 |
| Gate valve (fully open) | 0.2 |
| Globe valve (fully open) | 10 |
| Check valve | 2.5 |
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 Type | n Value |
|---|---|
| Glass, PVC | 0.010 |
| Smooth concrete | 0.012 |
| Finished concrete | 0.015 |
| 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
| Classification | lpcd (liters/capita/day) |
|---|---|
| Rural communities | 60-100 |
| Small towns | 100-150 |
| Cities (residential) | 150-200 |
| Metro areas | 200-300 |
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/η
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/γ
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