Engineering thermodynamics, steam plant & heat transfer

Thermodynamics & Heat Transfer

0 of 185 stars · 0 of 37 lessons done · your report card →

Properties of State

  • L1
    Lesson 1
    Reading the state
    pressure, temperature, heat — and which zero each one counts from

    Thermodynamics is bookkeeping on a substance's state: the handful of numbers that say what condition it is in right now.

  • L2
    Lesson 2
    Gauge versus absolute
    one pressure, two zeros — and the gas laws accept only one of them

    Every pressure gauge in the plant is lying to you, politely and by design. It has the atmosphere on both sides of its element, so the atmosphere cancels and the needle reads the EXCESS over ambient.

    The formula in this lesson
    Pabs=Pgauge+PatmP_{abs} = P_{gauge} + P_{atm}
  • L3
    Lesson 3
    Heating a mass
    The price of a degree, four ways round

    Warming something costs energy, and every material charges its own rate.

    The formula in this lesson
    Q=mcΔTQ = m c \Delta T
  • L4
    Lesson 4
    Changing phase
    Where the thermometer stops and the bill begins

    Heat a pot of ice and watch the thermometer. It climbs to 0 °C, then STOPS while the ice melts, then climbs again to 100 °C, then stops again while the water boils.

    The formula in this lesson
    Q=mLQ = m L
  • L5
    Lesson 5
    The gas laws
    Boyle, Charles, Gay-Lussac — and the one law they are pieces of

    Take a fixed amount of gas and move it from one state to another.

    The formulas in this lesson
    P1V1=P2V2P_1 V_1 = P_2 V_2,V1T1=V2T2\dfrac{V_1}{T_1} = \dfrac{V_2}{T_2},P1T1=P2T2\dfrac{P_1}{T_1} = \dfrac{P_2}{T_2},P1V1T1=P2V2T2\dfrac{P_1 V_1}{T_1} = \dfrac{P_2 V_2}{T_2}
  • L6
    Lesson 6
    The ideal gas
    PV = nRT for any unknown, and a density from a molar mass

    The gas laws compare two states of the same gas. The equation of state describes ONE state completely, and needs nothing to compare it to: PV = nRT, read aloud P V equals n R T.

  • L7
    Lesson 7
    Real gas corrections
    Z as the honest multiplier, and van der Waals as the reason for it

    PV = nRT assumes two things that are not true: that molecules take up no room, and that they do not pull on one another.

    The formulas in this lesson
    Z=PVnRTZ = \dfrac{PV}{nRT},(P+an2V2)(V−nb)=nRT\left(P + \dfrac{a n^{2}}{V^{2}}\right)\left(V - nb\right) = nRT
  • L8
    Lesson 8
    Vapour pressure curves
    Antoine and Clausius–Clapeyron — why a vacuum boils water cold

    Above every liquid sits its own vapour, pressing down with a pressure that depends on one thing only: temperature. When that vapour pressure reaches the pressure of the surroundings, the liquid boils.

  • ★
    Boss lesson
    The State Final
    the boss · no calculator · one receiver heated, one deaerator duty

    No calculator — the barometer reads a round 100 kPa, water costs a round 4 kJ/(kg·K), and steam a round 2250 kJ/kg.

    The formula in this lesson
    Pabs=Pgauge+PatmP_{abs} = P_{gauge} + P_{atm}

Steam, Turbines & Power Cycles

  • L10
    Lesson 10
    Reading the steam table
    saturation pressure and temperature, both directions

    Everything in this chapter hangs off one curve: the saturation line, where water and steam sit together at the same temperature and pressure.

  • L11
    Lesson 11
    Wet steam and quality
    The h_g-for-h_fg mixup

    Steam on the saturation line is rarely all vapour. Its quality x is the fraction of each kilogram that has actually boiled: x = 0 is saturated water, x = 1 is dry saturated steam, and a working header lives somewhere near 0.95.

    The formulas in this lesson
    x=h−hfhfgx = \dfrac{h - h_f}{h_{fg}},h=(1−x) hf+x hgh = (1-x)\,h_f + x\,h_g
  • L12
    Lesson 12
    Degrees of superheat
    how far above the line the steam is sitting

    Keep heating dry saturated steam and it leaves the saturation line altogether.

    The formula in this lesson
    ΔTsh=T−Tsat\Delta T_{sh} = T - T_{sat}
  • L13
    Lesson 13
    Superheated enthalpy
    h(p, T) · two coordinates to find the entry, one subtraction to use it

    On the saturation line, pressure alone fixes everything: name the pressure and the table hands you the temperature and every enthalpy.

    The formulas in this lesson
    h=h(p, T)h = h(p,\,T),q=h2−h1q = h_2 - h_1,Q˙=m˙ (h2−h1)\dot Q = \dot m\,(h_2 - h_1)
  • L14
    Lesson 14
    Flash steam
    what boils off when condensate is let down

    Hot condensate under pressure is holding more sensible heat than it can hold at a lower pressure. Open a trap into a flash vessel and the surplus goes somewhere: part of the water instantly boils.

  • L15
    Lesson 15
    Turbine work
    w = h₁ − h₂, and kJ/kg × kg/s = kW

    Strip the steady-flow energy equation down to a turbine and almost everything cancels: no heat crosses the casing worth counting, and the velocity terms are small.

    The formulas in this lesson
    P=m˙ wP = \dot m\,w,w=h1−h2w = h_1 - h_2
  • L16
    Lesson 16
    Isentropic efficiency
    the real drop against the drop the chart allows

    A frictionless turbine would expand the steam at constant entropy and land at a specific point on the chart. A real one generates entropy, so it lands to the RIGHT of that point — higher enthalpy, less work extracted.

    The formula in this lesson
    ηisen=h1−h2h1−h2s\eta_{isen} = \dfrac{h_1 - h_2}{h_1 - h_{2s}}
  • L17
    Lesson 17
    Steam losses and loads
    leaks, spray water and condensate — the plant audit

    Away from the turbine hall, steam engineering is bookkeeping. Three relations cover most of a plant walk-down, and all three are mass balances in disguise.

    The formulas in this lesson
    m˙=A P70\dot m = \dfrac{A\,P}{70},m˙w=m˙1 h1−h2h2−hw\dot m_w = \dot m_1\,\dfrac{h_1 - h_2}{h_2 - h_w},m˙=Q˙hfg\dot m = \dfrac{\dot Q}{h_{fg}}
  • L18
    Lesson 18
    Cycle efficiencies
    thermal, Carnot, Rankine, Otto, Brayton

    Every efficiency on this page answers the same sentence — what you got, over what you paid for — and they differ only in what the question hands you.

    The formulas in this lesson
    η=WQh\eta = \dfrac{W}{Q_h},η=1−TcTh\eta = 1 - \dfrac{T_c}{T_h},η=(h1−h2)−(h4−h3)h1−h4\eta = \dfrac{(h_1 - h_2) - (h_4 - h_3)}{h_1 - h_4},η=1−1rγ−1\eta = 1 - \dfrac{1}{r^{\gamma - 1}}
  • ★
    Boss lesson
    The Turbine Hall
    the boss · no calculator · throttle to megawatts

    Enthalpies are rounded to the nearest ten and the latent heat to a flat 2,400 kJ/kg — the kind of rounding an engineer does out loud on the machine floor, and the numbers are chosen to fit in your head.

    The formula in this lesson
    x=h−hfhfgx = \dfrac{h - h_f}{h_{fg}}

Conduction & the Building Envelope

  • L20
    Lesson 20
    Fourier's law
    Thickness is the only thing fighting you

    Heat does one thing in a solid: it walks from hot to cold, and it walks faster through some materials than others.

    The formula in this lesson
    P=kAΔTdP = \dfrac{k A \Delta T}{d}
  • L21
    Lesson 21
    R-value of a layer
    The number printed on the bag

    Fourier's law is exact and inconvenient: nobody wants to carry a conductivity and a thickness around a job site.

    The formulas in this lesson
    R=LkR = \dfrac{L}{k},R=LkAR = \dfrac{L}{k A}
  • L22
    Lesson 22
    Stacking the wall
    R-values in series · the air films count

    A real wall is a sandwich: cladding, sheathing, insulation, a vapour control layer, gypsum, paint. Every watt that leaves the room crosses all of them, one after another, in a queue.

    The formula in this lesson
    Rtot=R1+R2+R3R_{tot} = R_1 + R_2 + R_3
  • L23
    Lesson 23
    From R to U
    one clean reciprocal · and why U-factors never add

    Insulation is sold in R-values; energy codes are written in U-factors.

  • L24
    Lesson 24
    Whole-wall heat loss
    design ΔT, real areas, and an estimate first

    The two primes are the trade's way of writing “per unit area”. Flux is what a thermographer measures and what a designer compares between assemblies, because it does not care how big the wall is.

  • L25
    Lesson 25
    The framing penalty
    parallel paths · weight the U-factors, never the R-values

    Every wall you have stacked so far pretended the insulation covered all of it.

    The formula in this lesson
    1Reff=ffrRfr+1−ffrRcav\dfrac{1}{R_{eff}} = \dfrac{f_{fr}}{R_{fr}} + \dfrac{1 - f_{fr}}{R_{cav}}
  • L26
    Lesson 26
    Pipes and the critical radius
    the log-mean geometry, and when lagging backfires

    Everything so far assumed a flat wall: the same area at the hot face and the cold face. Wrap a pipe and that stops being true — the outside of the lagging has far more surface than the inside, and the heat spreads out as it crosses.

    The formulas in this lesson
    Q˙=2πkLΔTln⁡(r2/r1)\dot{Q} = \dfrac{2\pi k L \Delta T}{\ln(r_2/r_1)},rcr=khr_{cr} = \dfrac{k}{h}
  • ★
    Boss lesson
    The Envelope Audit
    the boss · no calculator · films to flux, one wall

    No calculator — every R-value in it sums to a clean number and every reciprocal is one you already know: RSI 2 is U-0.5, RSI 2.5 is U-0.4, RSI 4 is U-0.25, RSI 5 is U-0.2.

    The formula in this lesson
    Rtot=R1+R2+R3R_{tot} = R_1 + R_2 + R_3

Convection, Radiation & Heat Exchangers

  • L28
    Lesson 28
    Newton's law of cooling
    The film coefficient, and the film as a resistance

    Conduction happens inside solids. Convection happens where a solid meets a moving fluid, and almost all of the resistance lives in a thin, sluggish layer of fluid clinging to the surface — the boundary-layer film.

    The formulas in this lesson
    Q˙=hA ΔT\dot{Q} = h A \, \Delta T,R=1hAR = \dfrac{1}{hA}
  • L29
    Lesson 29
    The dimensionless crew
    Re · Pr · Nu · Gr · Ra — which ratio is which

    Nobody measures a film coefficient in the field. They correlate it — and every correlation is written in dimensionless groups, because a group that carries no units carries across scales, fluids and unit systems without being re-fitted.

  • L30
    Lesson 30
    Dittus–Boelter
    Nu from Re and Pr in turbulent tubes · then h

    Read aloud: Nusselt equals nought-point-nought-two-three, Reynolds to the nought-point-eight, Prandtl to the n.

  • L31
    Lesson 31
    Radiation exchange
    εσAT⁴ · the fourth power demands kelvin

    Every surface above absolute zero radiates.

    The formulas in this lesson
    P=εσAT4P = \varepsilon \sigma A T^{4},Q˙=εσA(T14−T24)\dot{Q} = \varepsilon \sigma A (T_1^{4} - T_2^{4}),ht=hc+hrh_t = h_c + h_r
  • L32
    Lesson 32
    Building the U
    films plus wall in series · then foul it

    An exchanger wall has fluid on both sides, so heat crosses three resistances in series: the inside film, the metal, the outside film.

    The formulas in this lesson
    1U=1hi+Lk+1ho\dfrac{1}{U} = \dfrac{1}{h_i} + \dfrac{L}{k} + \dfrac{1}{h_o},1Uf=1Uc+Rf\dfrac{1}{U_f} = \dfrac{1}{U_c} + R_f
  • L33
    Lesson 33
    Log mean temperature difference
    pairing the ends · counterflow always wins

    Along an exchanger, the gap between the two streams changes from one end to the other.

  • L34
    Lesson 34
    Rating the exchanger
    U·A·F·ΔT_lm against the stream balance

    There are exactly two ways to say how much heat an exchanger moves, and a rating is honest only when both agree.

    The formula in this lesson
    Q˙=m˙ cp ΔT\dot{Q} = \dot{m} \, c_p \, \Delta T
  • L35
    Lesson 35
    Effectiveness–NTU
    NTU · Cr · ε — rating without the outlets

    The LMTD method needs all four terminal temperatures. Very often you know only the two inlets and the hardware — and then the effectiveness–NTU method is the one that works.

    The formulas in this lesson
    NTU=UACmin\mathrm{NTU} = \dfrac{UA}{C_{min}},Q˙max=Cmin (Th,in−Tc,in)\dot{Q}_{max} = C_{min}\,(T_{h,in} - T_{c,in}),ε=1−e−NTU(1−Cr)1−Cr e−NTU(1−Cr)\varepsilon = \dfrac{1 - e^{-\mathrm{NTU}(1 - C_r)}}{1 - C_r \, e^{-\mathrm{NTU}(1 - C_r)}}
  • L36
    Lesson 36
    Transient cooling
    check Biot, then ride the lumped curve

    A hot body dropped into cooler fluid has two resistances in series: conduction out through its own inside, and convection off its surface.

  • ★
    Boss lesson
    The Exchanger Final
    the boss · no calculator · one unit, rated end to end

    That last choice is a gift with a lesson inside it: with equal capacity rates in counterflow, the two streams' temperature profiles run parallel down the shell, both terminal differences come out identical, and the log mean quietly equals…

    The formula in this lesson
    Q˙=m˙ cp ΔT\dot{Q} = \dot{m} \, c_p \, \Delta T

Nothing here is locked — the path recommends an order, and you study what you need. Progress lives in this browser (it survives cache clears, not “clear site data”); sign-in with permanent tracking is coming.

On paper: the study guide — formulas, worked examples, practice problems with the key — or the formula sheet alone. All downloads live in the study guide library.