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8.3 Thermal-Fluid Engineering — Thermodynamics & Fluid Mechanics

Key Takeaways

  • The First Law of Thermodynamics (ΔU=Q−W\Delta U = Q - W for closed systems, q−w=Δh+Δke+Δpeq - w = \Delta h + \Delta ke + \Delta pe for steady flow) establishes strict energy conservation across thermodynamic processes.

  • Ideal gas processes (isobaric, isochoric, isothermal, isentropic PVγ=CP V^\gamma = C, polytropic PVn=CP V^n = C) are governed by PV=mRTP V = m R T and specific heat relations (cp−cv=Rc_p - c_v = R, γ=cp/cv\gamma = c_p/c_v).

  • Thermodynamic cycles (Carnot, Rankine, Otto, Diesel) dictate heat engine thermal efficiency, bounded by Carnot limit ηth,Carnot=1−TLTH\eta_{th, Carnot} = 1 - \frac{T_L}{T_H}.

  • Fluid statics evaluates hydrostatic pressure (P=P0+ρghP = P_0 + \rho g h), manometric differential head, and buoyant forces via Archimedes' Principle (FB=ρfluidgVdisplacedF_B = \rho_{fluid} g V_{displaced}).

  • Fluid dynamics integrates the Continuity Equation (m˙=ρAv=C\dot{m} = \rho A v = C) and Bernoulli's Energy Equation with Darcy-Weisbach friction head loss (hf=fLDv22gh_f = f \frac{L}{D} \frac{v^2}{2g}) and pump power calculations.

Last updated: August 2026

8.3 Thermal-Fluid Engineering — Thermodynamics & Fluid Mechanics

Thermal-Fluid Engineering integrates thermodynamics, heat transfer, and fluid mechanics. For electrical engineers, these principles are indispensable when analyzing thermal power generation systems (steam, gas turbine, geothermal, diesel), transformer cooling, electrical enclosure heat dissipation, hydraulic power generation, and pump/fan fluid dynamics.


1. First & Second Laws of Thermodynamics & Ideal Gas Processes

The First Law of Thermodynamics (Conservation of Energy)

  • Closed System (Non-Flow Process): Q−W=ΔUQ - W = \Delta U where QQ is heat added to system, WW is boundary work done by system, and ΔU=mcv(T2−T1)\Delta U = m c_v (T_2 - T_1) is change in internal energy.
  • Open System (Steady-Flow Energy Equation - SFEE): q−w=(h2−h1)+v22−v122+g(z2−z1)q - w = (h_2 - h_1) + \frac{v_2^2 - v_1^2}{2} + g (z_2 - z_1) where h=u+Pvh = u + P v is specific enthalpy (Δh=cpΔT\Delta h = c_p \Delta T).

Ideal Gas Equation & Specific Heat Relations

PV=mRTorPv=RTP V = m R T \quad \text{or} \quad P v = R T

where R=RˉMR = \frac{\bar{R}}{M} is the specific gas constant (Rair=287 J/(kg⋅K)R_{\text{air}} = 287\ \text{J/(kg}\cdot\text{K)}).

  • Specific Heat Capacity Identity: cp−cv=R,γ=cpcvc_p - c_v = R, \quad \gamma = \frac{c_p}{c_v} cv=Rγ−1,cp=γRγ−1c_v = \frac{R}{\gamma - 1}, \quad c_p = \frac{\gamma R}{\gamma - 1} (For air: cp=1.005 kJ/(kg⋅K)c_p = 1.005\ \text{kJ/(kg}\cdot\text{K)}, cv=0.718 kJ/(kg⋅K)c_v = 0.718\ \text{kJ/(kg}\cdot\text{K)}, γ=1.4\gamma = 1.4).

Summary of Ideal Gas Non-Flow Processes

Process TypeGoverning RelationBoundary Work (W1−2W_{1-2})Heat Transfer (Q1−2Q_{1-2})
Isochoric (Constant Vol)V=C  ⟹  P1T1=P2T2V = C \implies \frac{P_1}{T_1} = \frac{P_2}{T_2}W=0W = 0Q=mcv(T2−T1)Q = m c_v (T_2 - T_1)
Isobaric (Constant Press)P=C  ⟹  V1T1=V2T2P = C \implies \frac{V_1}{T_1} = \frac{V_2}{T_2}W=P(V2−V1)W = P(V_2 - V_1)Q=mcp(T2−T1)Q = m c_p (T_2 - T_1)
Isothermal (Constant Temp)T=C  ⟹  P1V1=P2V2T = C \implies P_1 V_1 = P_2 V_2W=P1V1ln⁡(V2V1)W = P_1 V_1 \ln\left(\frac{V_2}{V_1}\right)Q=WQ = W
Isentropic (Reversible Adiabatic)PVγ=C  ⟹  T2T1=(P2P1)γ−1γP V^\gamma = C \implies \frac{T_2}{T_1} = \left(\frac{P_2}{P_1}\right)^{\frac{\gamma-1}{\gamma}}W=P1V1−P2V2γ−1W = \frac{P_1 V_1 - P_2 V_2}{\gamma - 1}Q=0Q = 0
PolytropicPVn=C  ⟹  T2T1=(P2P1)n−1nP V^n = C \implies \frac{T_2}{T_1} = \left(\frac{P_2}{P_1}\right)^{\frac{n-1}{n}}W=P1V1−P2V2n−1W = \frac{P_1 V_1 - P_2 V_2}{n - 1}Q=W+mcv(T2−T1)Q = W + m c_v (T_2 - T_1)

Second Law of Thermodynamics & Entropy

  • Kelvin-Planck Statement: No heat engine operating in a cycle can convert all absorbed heat into useful work (100% thermal efficiency is impossible).
  • Clausius Statement: Heat cannot spontaneously flow from a colder body to a hotter body without external work input.
  • Thermal Efficiency of Heat Engine: ηth=WnetQH=1−QLQH\eta_{\text{th}} = \frac{W_{\text{net}}}{Q_H} = 1 - \frac{Q_L}{Q_H}
  • Carnot Cycle Efficiency Limit: Operating between absolute temperatures THT_H and TLT_L (in Kelvin): ηCarnot=1−TLTH\eta_{\text{Carnot}} = 1 - \frac{T_L}{T_H}
  • Entropy Change (Isentropic / Reversible): dS=δQrevTdS = \frac{\delta Q_{\text{rev}}}{T}.

2. Power Cycles & Heat Transfer Fundamentals

Standard Thermodynamic Power Cycles

  1. Rankine Cycle: Standard ideal cycle for steam power plants (boilers, steam turbines, condensers, feed pumps).
  2. Otto Cycle: Ideal air-standard cycle for spark-ignition engines: ηOtto=1−1rvγ−1\eta_{\text{Otto}} = 1 - \frac{1}{r_v^{\gamma - 1}} where rv=V1/V2r_v = V_1 / V_2 is the volumetric compression ratio.
  3. Diesel Cycle: Ideal cycle for compression-ignition engines: ηDiesel=1−1rvγ−1[rcγ−1γ(rc−1)]\eta_{\text{Diesel}} = 1 - \frac{1}{r_v^{\gamma - 1}} \left[ \frac{r_c^\gamma - 1}{\gamma (r_c - 1)} \right] where rc=V3/V2r_c = V_3 / V_2 is the fuel cut-off ratio.

Modes of Heat Transfer

  • Conduction (Fourier's Law): Heat diffusion through solid media: q=−kAdTdx  ⟹  Q=kA(T1−T2)Lq = -k A \frac{dT}{dx} \implies Q = \frac{k A (T_1 - T_2)}{L} where kk is thermal conductivity (W/m·K).
  • Convection (Newton's Law of Cooling): Heat transfer between solid surface and moving fluid: Q=hA(Ts−T∞)Q = h A (T_s - T_\infty) where hh is convection heat transfer coefficient (W/m²·K).
  • Radiation (Stefan-Boltzmann Law): Electromagnetic wave thermal emission: Q=ϵσA(Ts4−Tsurr4)Q = \epsilon \sigma A (T_s^4 - T_{\text{surr}}^4) where σ=5.67×10−8 W/(m2⋅K4)\sigma = 5.67 \times 10^{-8}\ \text{W/(m}^2\cdot\text{K}^4) and ϵ\epsilon is surface emissivity.

3. Fluid Statics, Hydrostatic Pressure & Buoyancy

Fluid Properties

  • Density (ρ\rho): Mass per unit volume (Water ρw=1000 kg/m3\rho_w = 1000\ \text{kg/m}^3).
  • Specific Weight (γ\gamma): Weight per unit volume: γ=ρg(Water γw=9810 N/m3=9.81 kN/m3)\gamma = \rho g \quad (\text{Water } \gamma_w = 9810\ \text{N/m}^3 = 9.81\ \text{kN/m}^3)
  • Specific Gravity (SGSG): Ratio of fluid density to standard water density: SG=ρfluidρw=γfluidγw(Mercury SGHg=13.6)SG = \frac{\rho_{\text{fluid}}}{\rho_w} = \frac{\gamma_{\text{fluid}}}{\gamma_w} \quad (\text{Mercury } SG_{\text{Hg}} = 13.6)

Hydrostatic Pressure Equation

P=P0+ρgh=P0+γhP = P_0 + \rho g h = P_0 + \gamma h
  • Absolute vs. Gage Pressure: Pabs=Pgage+PatmP_{\text{abs}} = P_{\text{gage}} + P_{\text{atm}} (Standard Atmospheric Pressure Patm=101.325 kPa=1.01325 bar=14.7 psi=760 mmHgP_{\text{atm}} = 101.325\ \text{kPa} = 1.01325\ \text{bar} = 14.7\ \text{psi} = 760\ \text{mmHg}).

Archimedes' Buoyancy Principle

Any body submerged partially or fully in a fluid experiences an upward buoyant force equal to the weight of the fluid displaced:

FB=ρfluidgVdisplaced=γfluidVdisplacedF_B = \rho_{\text{fluid}} g V_{\text{displaced}} = \gamma_{\text{fluid}} V_{\text{displaced}}

4. Fluid Dynamics, Bernoulli's Equation & Pipe Flow Head Loss

Mass Continuity Equation (Incompressible Flow)

m˙=ρA1v1=ρA2v2  ⟹  Q=A1v1=A2v2\dot{m} = \rho A_1 v_1 = \rho A_2 v_2 \implies Q = A_1 v_1 = A_2 v_2

where QQ is volumetric flow rate (m³/s) and vv is mean flow velocity (m/s).

Bernoulli's Energy Equation (Inviscid, Incompressible Flow)

Along a streamline in steady friction-free flow, total energy head remains constant:

P1γ+v122g+z1=P2γ+v222g+z2\frac{P_1}{\gamma} + \frac{v_1^2}{2g} + z_1 = \frac{P_2}{\gamma} + \frac{v_2^2}{2g} + z_2

where Pγ\frac{P}{\gamma} is pressure head, v22g\frac{v^2}{2g} is velocity head, and zz is elevation head.

Extended Energy Equation with Pipe Friction Head Loss (hfh_f) & Pump Head (HpH_p)

P1γ+v122g+z1+Hp=P2γ+v222g+z2+hf\frac{P_1}{\gamma} + \frac{v_1^2}{2g} + z_1 + H_p = \frac{P_2}{\gamma} + \frac{v_2^2}{2g} + z_2 + h_f

Darcy-Weisbach Equation for Pipe Head Loss

hf=f(LD)(v22g)h_f = f \left(\frac{L}{D}\right) \left(\frac{v^2}{2g}\right)

where ff is the Darcy friction factor, LL is pipe length, DD is pipe inside diameter, and vv is fluid velocity.

  • Reynolds Number (ReRe): Characterizes flow regime: Re=ρvDμ=vDνRe = \frac{\rho v D}{\mu} = \frac{v D}{\nu}
    • Laminar Flow (Re<2300Re < 2300): Friction factor f=64Ref = \frac{64}{Re}.
    • Turbulent Flow (Re>4000Re > 4000): ff depends on relative roughness ϵ/D\epsilon/D and ReRe (Moody Chart or Colebrook equation).

Hydraulic & Electrical Pump Power

  • Hydraulic Power Output (PhydP_{\text{hyd}}): Phyd=γQHp=ρgQHpP_{\text{hyd}} = \gamma Q H_p = \rho g Q H_p
  • Electrical Motor Input Power (PelecP_{\text{elec}}): Pelec=Phydηpump⋅ηmotor=γQHpηoverallP_{\text{elec}} = \frac{P_{\text{hyd}}}{\eta_{\text{pump}} \cdot \eta_{\text{motor}}} = \frac{\gamma Q H_p}{\eta_{\text{overall}}}

Solved Board Exam Examples

Example 1: Polytropic Gas Compression Work Calculation

Problem: Air (R=287 J/(kg⋅K)R = 287\ \text{J/(kg}\cdot\text{K)}, γ=1.4\gamma = 1.4) with mass m=2.0 kgm = 2.0\ \text{kg} is compressed polytropically with exponent n=1.30n = 1.30 from initial conditions P1=100 kPaP_1 = 100\ \text{kPa} and T1=300 KT_1 = 300\ \text{K} to a final pressure P2=800 kPaP_2 = 800\ \text{kPa}. Calculate the final temperature T2T_2, final volume V2V_2, and boundary work W1−2W_{1-2}.

Solution:

  1. Calculate initial volume V1V_1 using Ideal Gas Law: V1=mRT1P1=2.0×287×300100,000=172,200100,000=1.722 m3V_1 = \frac{m R T_1}{P_1} = \frac{2.0 \times 287 \times 300}{100,000} = \frac{172,200}{100,000} = 1.722\ \text{m}^3
  2. Determine final temperature T2T_2 using polytropic relation: T2=T1(P2P1)n−1n=300(800100)1.3−11.3=300(8)0.230769T_2 = T_1 \left(\frac{P_2}{P_1}\right)^{\frac{n-1}{n}} = 300 \left(\frac{800}{100}\right)^{\frac{1.3 - 1}{1.3}} = 300 \left(8\right)^{0.230769} T2=300×1.6146=484.39 K(211.24∘C)T_2 = 300 \times 1.6146 = 484.39\ \text{K} \quad (211.24^\circ\text{C})
  3. Calculate final volume V2V_2: V2=mRT2P2=2.0×287×484.39800,000=278,039.86800,000=0.34755 m3V_2 = \frac{m R T_2}{P_2} = \frac{2.0 \times 287 \times 484.39}{800,000} = \frac{278,039.86}{800,000} = 0.34755\ \text{m}^3
  4. Calculate polytropic boundary work W1−2W_{1-2}: W1−2=mR(T1−T2)n−1=2.0×287×(300−484.39)1.3−1=574×(−184.39)0.3W_{1-2} = \frac{m R (T_1 - T_2)}{n - 1} = \frac{2.0 \times 287 \times (300 - 484.39)}{1.3 - 1} = \frac{574 \times (-184.39)}{0.3} W1−2=−105,839.860.3=−352,799.5 J=−352.80 kJW_{1-2} = \frac{-105,839.86}{0.3} = -352,799.5\ \text{J} = -352.80\ \text{kJ} (Negative sign indicates work is done ON the air during compression).

Example 2: Bernoulli Pipeline Flow, Friction Head Loss & Pump Power

Problem: Water (γ=9810 N/m3\gamma = 9810\ \text{N/m}^3) is pumped from an open intake reservoir (surface elevation z1=10 mz_1 = 10\ \text{m}) to an elevated storage tank (surface elevation z2=45 mz_2 = 45\ \text{m}) at a rate of Q=0.05 m3/sQ = 0.05\ \text{m}^3/\text{s} through a pipeline of diameter D=0.15 mD = 0.15\ \text{m} and length L=200 mL = 200\ \text{m}. Total pipe friction head loss is calculated to be hf=8.5 mh_f = 8.5\ \text{m}. If the combined pump-motor overall efficiency is ηoverall=75%\eta_{\text{overall}} = 75\%, calculate the total pump dynamic head HpH_p required and the electrical power input PelecP_{\text{elec}}.

Solution:

  1. Apply extended Bernoulli equation between free water surfaces (where P1=P2=PatmP_1 = P_2 = P_{\text{atm}} and v1=v2≈0v_1 = v_2 \approx 0): z1+Hp=z2+hf  ⟹  Hp=(z2−z1)+hfz_1 + H_p = z_2 + h_f \implies H_p = (z_2 - z_1) + h_f Hp=(45−10)+8.5=35+8.5=43.5 mH_p = (45 - 10) + 8.5 = 35 + 8.5 = 43.5\ \text{m}
  2. Calculate hydraulic power delivered to water (PhydP_{\text{hyd}}): Phyd=γQHp=9810×0.05×43.5=21,336.75 W=21.34 kWP_{\text{hyd}} = \gamma Q H_p = 9810 \times 0.05 \times 43.5 = 21,336.75\ \text{W} = 21.34\ \text{kW}
  3. Calculate electrical power input required (PelecP_{\text{elec}}): Pelec=Phydηoverall=21.34 kW0.75=28.45 kWP_{\text{elec}} = \frac{P_{\text{hyd}}}{\eta_{\text{overall}}} = \frac{21.34\ \text{kW}}{0.75} = 28.45\ \text{kW}
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Extended Bernoulli Energy Balance in a Pumped Hydraulic Pipeline
Test Your Knowledge

A thermal electric power generation plant operates between a high-temperature heat source at TH = 550°C and a cooling water heat sink at TL = 30°C. What is the maximum theoretical (Carnot) thermal efficiency of this power plant?

A

94.55%

B

36.83%

C

63.17%

D

48.20%

Test Your Knowledge

A U-tube differential manometer containing mercury (specific gravity SG_Hg = 13.6) measures the pressure difference between two taps in a water pipeline (density ρ = 1000 kg/m³). If the differential mercury column reading is h = 0.25 m, what is the pressure difference (Pa - Pb) between the two taps? Take g = 9.81 m/s².

A

33.35 kPa

B

24.53 kPa

C

3.34 kPa

D

30.90 kPa

Test Your Knowledge

Water flows through a long horizontal commercial steel pipe of inside diameter D = 0.20 m and length L = 500 m at a average velocity v = 3.0 m/s. Given a Darcy friction factor f = 0.020 and g = 9.81 m/s², what is the head loss due to pipe friction (hf)?

A

45.87 m

B

22.94 m

C

11.47 m

D

15.29 m

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