Fluid Mechanics: Fluid Properties, Pressure, Density, and Viscosity

Fundamental Concepts and Fluid Definitions

  • Definition of a Fluid:

    • A fluid is defined as matter that deforms continuously to take the shape of its container.

    • A fluid is defined as matter that cannot sustain a shear stress while remaining at rest.

  • States of Matter and Phase Transitions:

    • Solid to Liquid: Melting / Fusion

    • Liquid to Solid: Freezing / Solidification

    • Liquid to Gas: Evaporation

    • Gas to Liquid: Condensation

    • Solid to Gas: Sublimation

    • Gas to Solid: Deposition

Phase Transitions Between Solid, Liquid, and Gas States
  • Scope and Branches of Fluid Mechanics:

    • Fluid Mechanics is a fundamental branch of general Continuum Mechanics with extensive engineering applications.

    • Fluid Statics: The study of fluids at rest.

    • Fluid Dynamics: The study of fluids in motion.

    • Core Engineering Goals:

      • Accurate flow measurement.

      • Predicting forces acting on bodies submerged in fluids or containing moving fluid masses.

      • Predicting flow regimes, sizing pipes, and designing pumps.

      • Calculating total energy consumption and system losses.

Units and Dimensional Analysis in Fluid Mechanics

  • Fundamental SI Units:

    • Fundamental units cannot be subdivided into other units and form the basis of the SI system:

      • Mass: kilogram (kg\text{kg}), dimension [M][\text{M}]

      • Length: metre (m\text{m}), dimension [L][\text{L}]

      • Time: second (s\text{s}), dimension [T][\text{T}]

      • Temperature: kelvin (K\text{K}), dimension [Θ][\Theta]

      • Amount of Substance: mole (mol\text{mol}), dimension [N][\text{N}]

      • Electric Current: ampere (A\text{A}), dimension [I][\text{I}]

      • Luminous Intensity: candela (cd\text{cd}), dimension [J][\text{J}]

  • Derived SI Units Named After Scientists:

    • Derived units represent products or quotients of fundamental units raised to powers:

      • Force: newton (N\text{N}), fundamental unit equivalent: kg⋅m/s2\text{kg}\cdot\text{m/s}^2

      • Pressure: pascal (Pa\text{Pa} or N/m2\text{N/m}^2), fundamental unit equivalent: kg/(m⋅s2)\text{kg}/(\text{m}\cdot\text{s}^2)

      • Energy: joule (J\text{J} or N⋅m\text{N}\cdot\text{m}), fundamental unit equivalent: kg⋅m2/s2\text{kg}\cdot\text{m}^2/\text{s}^2

      • Power: watt (W\text{W} or J/s\text{J/s}), fundamental unit equivalent: kg⋅m2/s3\text{kg}\cdot\text{m}^2/\text{s}^3

      • Frequency: hertz (Hz\text{Hz}), fundamental unit equivalent: s−1\text{s}^{-1}

      • Angle: radian (rad\text{rad}), dimensionless

  • Key Fluid Mechanics Quantities and Symbols:

    • Area (AA): m2\text{m}^2

    • Volume (VV): m3\text{m}^3

    • Density (ρ\rho): kg/m3\text{kg/m}^3

    • Specific Volume (vv): m3/kg\text{m}^3/\text{kg}

    • Average Velocity (uu): m/s\text{m/s}

    • Point Velocity (vv): m/s\text{m/s}

    • Mass Flow Rate (m˙\dot{m}): kg/s\text{kg/s}

    • Volumetric Flow Rate (QQ): m3/s\text{m}^3/\text{s}

    • Pressure / Normal Stress (PP or σ\sigma): Pa\text{Pa}

    • Shear Stress (τ\tau): Pa\text{Pa}

    • Shear Rate (γ˙\dot{\gamma}): s−1\text{s}^{-1}

    • Dynamic Viscosity (μ\mu): Pa⋅s\text{Pa}\cdot\text{s}

    • Surface Tension (σ\sigma): N/m\text{N/m}

    • Compressibility (cc): Pa−1\text{Pa}^{-1}

Density, Specific Properties, and Equations of State

  • Behavioral Distinction Between Liquids and Gases:

    • Liquids: Occupy an enclosing container only to the extent of their own volume and are treated as incompressible.

    • Gases: Expand completely to occupy the total enclosure volume and are treated as compressible.

  • Specific Fluid Properties:

    • Specific properties are intensive properties, meaning they are independent of the total size or mass of the system.

    • Density (ρ\rho): Mass per unit volume:         ρ=mV[kg/m3]\rho = \frac{m}{V} \quad [\text{kg/m}^3]

    • Specific Volume (vv): Volume per unit mass, defined as the reciprocal of density:         v=1ρ[m3/kg]v = \frac{1}{\rho} \quad [\text{m}^3/\text{kg}]

    • Specific Weight (ww): Weight per unit volume:         w=ρg[N/m3]w = \rho g \quad [\text{N/m}^3]

    • Specific Gravity (γ\gamma): Ratio of the density of a given fluid to the density of standard water:         γ=ρfρw\gamma = \frac{\rho_f}{\rho_w}

  • Density Variations in Liquids vs. Gases:

    • Liquids: Density depends primarily on temperature and varies minimally with pressure. For example, water density varies with temperature from ∼1000 kg/m3\sim 1000\,\text{kg/m}^3 at 20 ∘C20\,^{\circ}\text{C} to ∼958 kg/m3\sim 958\,\text{kg/m}^3 at 100 ∘C100\,^{\circ}\text{C}. Empirical density variations can be expressed as:         1ρ=A+BT\frac{1}{\rho} = A + B T

    • Gases: Density depends strongly on both temperature and pressure, governed by an Equation of State (EoS).

  • The Ideal Gas Law:

    • An Equation of State relates the state variables of pressure, temperature, and density.

    • Molar Form:         PV=nR0TP V = n R_0 T

    • Mass Form:         PV=mRspecTP V = m R_{\text{spec}} T

    • Density Form:         ρ=PRspecT\rho = \frac{P}{R_{\text{spec}} T}

    • Universal Gas Constant (R0R_0):         R0=8.314 J/(mol⋅K)R_0 = 8.314\,\text{J}/(\text{mol}\cdot\text{K})

    • Specific Gas Constant (RspecR_{\text{spec}}):         Rspec=1000×R0M[J/(kg⋅K)]R_{\text{spec}} = 1000 \times \frac{R_0}{M} \quad [\text{J}/(\text{kg}\cdot\text{K})]         where MM is the molar mass in g/mol\text{g/mol}.

    • Specific Gas Constant Values:

      • Air: 287 J/(kg⋅K)287\,\text{J}/(\text{kg}\cdot\text{K})

      • Hydrogen (H2\text{H}_2): 4160 J/(kg⋅K)4160\,\text{J}/(\text{kg}\cdot\text{K})

      • Carbon Dioxide (CO2\text{CO}_2): 190 J/(kg⋅K)190\,\text{J}/(\text{kg}\cdot\text{K}) (or 189 J/(kg⋅K)189\,\text{J}/(\text{kg}\cdot\text{K}) derived from M=44 g/molM = 44\,\text{g/mol})

    • Temperature Units: Temperature TT must always be converted to absolute temperature in kelvin (K\text{K}) where T=t[∘C]+273.15T = t [^{\circ}\text{C}] + 273.15.

Stress, Tensor Representation, and Hydrostatic Pressure

  • Distinction Between Force and Stress:

    • Stress represents force applied over a specific area (Stress=ForceArea\text{Stress} = \frac{\text{Force}}{\text{Area}}).

    • Normal Stress (σ\sigma): Applied perpendicular to a surface, producing compression or tension.

    • Shear Stress (τ\tau): Applied parallel to a surface, causing relative sliding or flow.

    • The surface areas over which normal stress and shear stress act are physically distinct.

  • The Stress Tensor:

    • The complete state of stress at any point within a fluid element is described by a second-order Stress Tensor (σ\boldsymbol{\sigma}):         σ=(σxxτxyτxzτyxσyyτyzτzxτzyσzz)\boldsymbol{\sigma} = \begin{pmatrix} \sigma_{xx} & \tau_{xy} & \tau_{xz} \\ \tau_{yx} & \sigma_{yy} & \tau_{yz} \\ \tau_{zx} & \tau_{zy} & \sigma_{zz} \end{pmatrix}

    • Each component σij\sigma_{ij} or τij\tau_{ij} is a vector operating on a face perpendicular to axis ii in the direction of axis jj.

Normal Stress Components on a 3D Fluid ElementShear Stress Components on a 3D Fluid Element
  • Hydrostatic Pressure:

    • Hydrostatic pressure (PP) is an overall scalar measure of uniform, isotropic compression.

    • Mathematically, hydrostatic pressure is defined as one-third of the trace of the stress tensor:         P=13tr(σ)=σxx+σyy+σzz3P = \frac{1}{3}\text{tr}(\boldsymbol{\sigma}) = \frac{\sigma_{xx} + \sigma_{yy} + \sigma_{zz}}{3}

  • Physical Origin and Units of Pressure:

    • Pressure is a physical consequence of continuous molecular activity and collisions against a bounding surface.

    • SI Unit: Pascal (1 Pa=1 N/m21\,\text{Pa} = 1\,\text{N/m}^2).

    • Standard Unit Conversions:

      • 1 bar=105 N/m2=105 Pa1\,\text{bar} = 10^5\,\text{N/m}^2 = 10^5\,\text{Pa}

      • 1 atm=101325 N/m2=101325 Pa1\,\text{atm} = 101325\,\text{N/m}^2 = 101325\,\text{Pa}

Absolute Pressure vs Gauge Pressure

  • Reference Baselines:

    • Absolute Zero Reference: Perfect vacuum (P=0 PaP = 0\,\text{Pa}).

    • Atmospheric Pressure Reference (PatmP_{\text{atm}}): Standard atmospheric pressure (Patm=1 atm=101325 PaP_{\text{atm}} = 1\,\text{atm} = 101325\,\text{Pa}), as measured by a barometer.

  • Pressure Definitions and Mathematical Relationships:

    • Absolute Pressure (PabsP_{\text{abs}}): Total pressure measured relative to a perfect vacuum (P=0 PaP = 0\,\text{Pa}).

    • Gauge Pressure (PgaugeP_{\text{gauge}}): Pressure measured relative to local atmospheric pressure (PatmP_{\text{atm}}).         Pgauge=Pabs−PatmP_{\text{gauge}} = P_{\text{abs}} - P_{\text{atm}}

  • Operating Regimes:

    • Positive Gauge Pressure (Pgauge>0 PaP_{\text{gauge}} > 0\,\text{Pa}): Absolute pressure exceeds atmospheric pressure (Pabs>PatmP_{\text{abs}} > P_{\text{atm}}).

    • Negative Gauge Pressure / Vacuum (Pgauge<0 PaP_{\text{gauge}} < 0\,\text{Pa}): Absolute pressure is below atmospheric pressure (Pabs<PatmP_{\text{abs}} < P_{\text{atm}}).

Shear Stress, Viscosity, and Newton's Law

  • Response to Shear Stress: Solids vs. Fluids:

    • Elastic Solid:

      • Resists an applied shear stress τ=FA\tau = \frac{F}{A}.

      • Deforms in a reversible way (or breaks permanently).

      • The deformation or shear strain (γ\gamma) is directly proportional to the applied force.

      • Solids remain deformed for as long as the force is applied. Solids do NOT flow, they DEFORM.

Deformation of an Elastic Solid under Shear Stress
*   **Fluid**:
    *   Cannot resist a shear stress while at rest.
    *   Upon application of τ\tau, the top layer slides over adjacent lower layers, dragging them along via fluid friction.
    *   Continuous slipping occurs between layers as long as τ\tau is applied. Fluids FLOW, and do NOT deform statically.
Layer Sliding and Flow of a Fluid under Shear Stress
  • Definition and Geometric Derivation of Shear Rate:

    • Consider a fluid element deforming between time t=t0t = t_0 and t=t0+Δtt = t_0 + \Delta t.

    • The top face moves at velocity u+Δuu + \Delta u while the bottom face moves at velocity uu.

    • The angular deformation (shear strain Δγ\Delta\gamma) is given by:         tan⁡(Δγ)=[x+(u+Δu)Δt]−[x+uΔt](y+Δy)−y=ΔuΔtΔy\tan(\Delta\gamma) = \frac{[x + (u + \Delta u)\Delta t] - [x + u\Delta t]}{(y + \Delta y) - y} = \frac{\Delta u \Delta t}{\Delta y}

    • Taking the differential limit yields the shear rate (γ˙\dot{\gamma}):         γ˙=dudy\dot{\gamma} = \frac{du}{dy}

    • Shear rate represents the velocity gradient perpendicular to the direction of flow/force application.

Geometric Derivation of Shear Strain and Velocity Profile
  • Newton's Law of Viscosity:

    • States that the shear rate generated in a fluid is directly proportional to the applied shear stress:         τ=μγ˙=μdudy\tau = \mu \dot{\gamma} = \mu \frac{du}{dy}

    • Fluids that obey this linear relation are known as Newtonian Fluids.

    • Crucial Rule: In fluids, shear stress τ\tau is proportional to the shear rate γ˙\dot{\gamma}, NOT the shear strain γ\gamma

  • Viscosity Definitions and Units:

    • Dynamic Viscosity (μ\mu): Fluid shear viscosity representing resistance to sliding friction between fluid layers.

    • SI Units of Dynamic Viscosity:         kg/(m⋅s)=N⋅s/m2=Pa⋅s\text{kg}/(\text{m}\cdot\text{s}) = \text{N}\cdot\text{s}/\text{m}^2 = \text{Pa}\cdot\text{s}

    • Traditional Units (Poise / Centipoise):         1 P=100 cP=0.1 Pa⋅s1\,\text{P} = 100\,\text{cP} = 0.1\,\text{Pa}\cdot\text{s}

    • Kinematic Viscosity (ν\nu): Ratio of viscous forces to inertial forces:         ν=μρ[m2/s]\nu = \frac{\mu}{\rho} \quad [\text{m}^2/\text{s}]

Worked Examples and Engineering Calculations

  • Problem 1: Force Calculation for Sled Sliding on Thin Water Layer over Ice:

    • Problem Statement: A skier pushes a sled over ice. Friction melts a thin layer of water of thickness t=1 μm=10−6 mt = 1\,\mu\text{m} = 10^{-6}\,\text{m}. Contact area is a rectangle of length 1 m1\,\text{m} and width 20 cm=0.2 m20\,\text{cm} = 0.2\,\text{m}. Water viscosity μ=10−3 Pa⋅s\mu = 10^{-3}\,\text{Pa}\cdot\text{s}. Find the required force when moving at u=60 cm/s=0.60 m/su = 60\,\text{cm/s} = 0.60\,\text{m/s}.

Sled Moving on Thin Water Layer over Ice
*   **Contact Area**:

        A=1×0.2=0.2 m2A = 1 \times 0.2 = 0.2\,\text{m}^2 * Shear Rate:         γ˙=dudy=ΔuΔy=0.60−010−6=6×105 s−1\dot{\gamma} = \frac{du}{dy} = \frac{\Delta u}{\Delta y} = \frac{0.60 - 0}{10^{-6}} = 6 \times 10^5\,\text{s}^{-1} * Shear Stress:         τ=μγ˙=0.001×(6×105)=600 Pa\tau = \mu \dot{\gamma} = 0.001 \times (6 \times 10^5) = 600\,\text{Pa} * Required Force:         F=τA=600×0.2=120 NF = \tau A = 600 \times 0.2 = 120\,\text{N}

  • Problem 2: Force Calculation for Shaft Pulled Linearly Through Bearing:

    • Problem Statement: A shaft of diameter D=25 mm=0.025 mD = 25\,\text{mm} = 0.025\,\text{m} and length L=50 mm=0.05 mL = 50\,\text{mm} = 0.05\,\text{m} passes through a bearing with uniform radial clearance Δy=0.1 mm=0.1×10−3 m\Delta y = 0.1\,\text{mm} = 0.1 \times 10^{-3}\,\text{m} filled with oil (μ=0.25 Pa⋅s\mu = 0.25\,\text{Pa}\cdot\text{s}). Calculate force required to pull shaft at u=10 m/su = 10\,\text{m/s}.

    • Shear Rate:         γ˙=dudy=ΔuΔy=10−00.1×10−3=105 s−1\dot{\gamma} = \frac{du}{dy} = \frac{\Delta u}{\Delta y} = \frac{10 - 0}{0.1 \times 10^{-3}} = 10^5\,\text{s}^{-1}

    • Shear Stress:         τ=μγ˙=0.25×105=2.5×104 Pa\tau = \mu \dot{\gamma} = 0.25 \times 10^5 = 2.5 \times 10^4\,\text{Pa}

    • Surface Area:         A=πDL=π×0.025×0.05=3.927×10−3 m2A = \pi D L = \pi \times 0.025 \times 0.05 = 3.927 \times 10^{-3}\,\text{m}^2

    • Pulling Force:         F=τA=(2.5×104)×(π×0.025×0.05)=98.2 NF = \tau A = (2.5 \times 10^4) \times (\pi \times 0.025 \times 0.05) = 98.2\,\text{N}

  • Problem 3: Torque Calculation for Shaft Rotated in Bearing:

    • Problem Statement: For the same shaft system (D=25 mmD = 25\,\text{mm}, L=50 mmL = 50\,\text{mm}, clearance Δy=0.1 mm\Delta y = 0.1\,\text{mm}, μ=0.25 Pa⋅s\mu = 0.25\,\text{Pa}\cdot\text{s}), calculate the torque needed to rotate the shaft at 1000 rev/min1000\,\text{rev/min}.

    • Surface Velocity:         ux=rω=(D2)(1000×2π60)=0.0252×104.72=1.31 m/su_x = r \omega = \left(\frac{D}{2}\right) \left(\frac{1000 \times 2\pi}{60}\right) = \frac{0.025}{2} \times 104.72 = 1.31\,\text{m/s}

    • Shear Rate:         γ˙=ΔuΔy=1.31−00.1×10−3=1.31×104 s−1\dot{\gamma} = \frac{\Delta u}{\Delta y} = \frac{1.31 - 0}{0.1 \times 10^{-3}} = 1.31 \times 10^4\,\text{s}^{-1}

    • Shear Stress:         τ=μγ˙=0.25×(1.31×104)=3.27×103 Pa\tau = \mu \dot{\gamma} = 0.25 \times (1.31 \times 10^4) = 3.27 \times 10^3\,\text{Pa}

    • Tangential Force:         F=τA=(3.27×103)×(π×0.025×0.05)=12.9 NF = \tau A = (3.27 \times 10^3) \times (\pi \times 0.025 \times 0.05) = 12.9\,\text{N}

    • Required Torque:         T=rF=(12.5×10−3)×12.9=0.161 N⋅mT = r F = (12.5 \times 10^{-3}) \times 12.9 = 0.161\,\text{N}\cdot\text{m}

  • Problem 4: Air Mass Calculation in Elevated Spherical Balloon:

    • Problem Statement: Calculate mass of air contained in a spherical balloon of diameter D=10 mD = 10\,\text{m} (r=5 mr = 5\,\text{m}) at altitude 2000 m2000\,\text{m} where T=−10 ∘CT = -10\,^{\circ}\text{C} and P=80000 PaP = 80000\,\text{Pa}. Given Rspec,air=287 J/(kg⋅K)R_{\text{spec,air}} = 287\,\text{J}/(\text{kg}\cdot\text{K}).

    • Absolute Temperature:         T=273.15−10=263.15 KT = 273.15 - 10 = 263.15\,\text{K}

    • Sphere Volume:         V=43πr3=43π(5)3=523.6 m3V = \frac{4}{3} \pi r^3 = \frac{4}{3} \pi (5)^3 = 523.6\,\text{m}^3

    • Mass Evaluation:         m=PVRspecT=80000×523.6287×263.15=554.6 kgm = \frac{P V}{R_{\text{spec}} T} = \frac{80000 \times 523.6}{287 \times 263.15} = 554.6\,\text{kg}

  • Problem 5: CO2 Production Rate from Thermal Plant:

    • Problem Statement: A thermal plant produces 100 tons/h=100000 kg/h100\,\text{tons/h} = 100000\,\text{kg/h} of CO2\text{CO}_2 exiting at T=600 KT = 600\,\text{K} and P=1 atm=101325 PaP = 1\,\text{atm} = 101325\,\text{Pa}. Calculate volumetric flow rate in m3/h\text{m}^3/\text{h}.

    • Specific Gas Constant for CO2:         Rspec,CO2=8314 J/(kmol⋅K)44 kg/kmol=189 J/(kg⋅K)R_{\text{spec,CO2}} = \frac{8314\,\text{J}/(\text{kmol}\cdot\text{K})}{44\,\text{kg/kmol}} = 189\,\text{J}/(\text{kg}\cdot\text{K})

    • Gas Density:         ρCO2=PRspecT=101325189×600=0.89 kg/m3\rho_{\text{CO2}} = \frac{P}{R_{\text{spec}} T} = \frac{101325}{189 \times 600} = 0.89\,\text{kg/m}^3

    • Volumetric Flow Rate:         Qflow=mflowρ=100000 kg/h0.89 kg/m3=112360 m3/hQ_{\text{flow}} = \frac{m_{\text{flow}}}{\rho} = \frac{100000\,\text{kg/h}}{0.89\,\text{kg/m}^3} = 112360\,\text{m}^3/\text{h}

  • Problem 6: Cryogenic Hydrogen Storage Temperature:

    • Problem Statement: Calculate temperature of 2 kg2\,\text{kg} of hydrogen (H2\text{H}_2) stored in a cubic deposit of side length l=0.6 ml = 0.6\,\text{m} at P=80 bar=80×105 PaP = 80\,\text{bar} = 80 \times 10^5\,\text{Pa}. Given MH2=2 g/molM_{\text{H2}} = 2\,\text{g/mol}.

    • Deposit Volume:         V=l3=(0.6)3=0.216 m3V = l^3 = (0.6)^3 = 0.216\,\text{m}^3

    • Specific Gas Constant for H2:         Rspec,H2=8.314 J/(mol⋅K)2 g/mol=4.16 J/(g⋅K)R_{\text{spec,H2}} = \frac{8.314\,\text{J}/(\text{mol}\cdot\text{K})}{2\,\text{g/mol}} = 4.16\,\text{J}/(\text{g}\cdot\text{K})         Rspec,H2=4.16×1000=4160 J/(kg⋅K)R_{\text{spec,H2}} = 4.16 \times 1000 = 4160\,\text{J}/(\text{kg}\cdot\text{K})

    • Temperature Evaluation:         T=PVmRspec=8000000×0.2162×4160=207.7 KT = \frac{P V}{m R_{\text{spec}}} = \frac{8000000 \times 0.216}{2 \times 4160} = 207.7\,\text{K}