Physics · Book 3 · Bachelor Year 1

University Physics — Year 1

University Physics — Year 1 · Bachelor Year 1

22The First Law of Thermodynamics

Pump up a bicycle tire and the barrel of the pump gets too hot to hold. A diesel engine has no spark plug: it squeezes its air twenty times smaller, and the air becomes hot enough to light the fuel by itself. A cylinder of compressed gas frosts over as it empties. In each case energy changes form — work becomes heat, heat becomes work, both become internal energy — and the first law of thermodynamics is the bookkeeping that makes the accounts balance. This chapter defines work and heat for a thermodynamic system, states the first law, introduces internal energy and enthalpy as the quantities it conserves, and applies it to the transformations of a perfect gas and to calorimetry.

A bicycle pump: the work of the hand on the trapped air raises its internal energy, and the barrel gets warm — the first law in the palm.
A bicycle pump: the work of the hand on the trapped air raises its internal energy, and the barrel gets warm — the first law in the palm.

22.1 Transformations, work, and heat

Definition 22.1 (System, transformation)

A thermodynamic system is the matter inside a chosen boundary; everything else is the surroundings. A transformation takes it from an equilibrium state to another. It is quasi-static if the system passes through a succession of equilibrium states (slow enough for PP, TT to be defined throughout), and reversible if, in addition, reversing the external conditions reverses the path (no friction, no finite temperature or pressure gap with the surroundings). Names by what stays constant: isothermal (TT), isobaric (PP), isochoric (VV); adiabatic if no heat is exchanged; monobaric (monothermal) if the external pressure (temperature) is constant, whatever happens inside.

Proposition 22.2 (Work of pressure forces)

A system whose volume changes by  ⁣dV\dd V against an external pressure PextP_{\mathrm{ext}} receives the work

δW=Pext ⁣dV,W=V1V2Pext ⁣dV.\delta W = -P_{\mathrm{ext}}\,\dd V, \qquad W = -\int_{V_1}^{V_2}P_{\mathrm{ext}}\,\dd V .

For a quasi-static transformation Pext=PP_{\mathrm{ext}} = P (the system’s own pressure) and W=P ⁣dVW = -\int P\,\dd V is minus the area under the path in the Clapeyron diagram: positive when compressed, negative when expanding.

Proof. A piston of area SS pushed by the surroundings with the force PextSP_{\mathrm{ext}}S moves by  ⁣dx\dd x outward: the surroundings do the work PextS ⁣dx=Pext ⁣dV-P_{\mathrm{ext}}S\,\dd x = -P_{\mathrm{ext}}\,\dd V on the system. Any boundary is a collection of such pistons. Quasi-static: the piston is in equilibrium, Pext=PP_{\mathrm{ext}} = P up to a vanishing difference.

Definition 22.3 (Heat)

Heat QQ is energy transferred to the system other than by macroscopic work — by molecular collisions at a wall (conduction), by the circulation of a fluid (convection), by radiation. A thermostat is a body so large that its temperature does not change whatever heat it exchanges. Sign convention throughout: WW and QQ are received by the system, positive when they enter.

22.2 The first law

Theorem 22.4 (First law of thermodynamics)

A closed system possesses a state function, its internal energy UU (extensive), such that for any transformation

ΔU+ΔEk=W+Q,\Delta U + \Delta E_{k} = W + Q ,

EkE_k being the macroscopic kinetic energy (zero for a system at rest): the energy received as work and heat is stored as internal energy. WW and QQ each depend on the path; their sum does not.

Proof. Admitted at this level.

Remark 22.5 (What it says)

It is the conservation of energy, with heat recognized as a transfer of energy (Joule’s paddle-wheel experiment: a measured work always raises the temperature of water as much as a measured heat). “UU is a state function” means ΔU\Delta U is fixed by the initial and final states — so a cycle has ΔU=0\Delta U = 0 and W+Q=0W + Q = 0: an engine that delivers work must receive heat. The microscopic content of UU is that of Definition 20.10.

Definition 22.6 (Enthalpy; heat capacities)

The enthalpy H=U+PVH = U + PV is a state function adapted to transformations at constant pressure. The heat capacities at constant volume and pressure are

CV=(UT)V,CP=(HT)P,C_V = \left(\frac{\partial U}{\partial T}\right)_V, \qquad C_P = \left(\frac{\partial H}{\partial T}\right)_P ,

in J/K\mathrm{J}/\mathrm{K}; per mole CV,mC_{V,m}, CP,mC_{P,m}; per kilogram the specific heats cVc_V, cPc_P.

Proposition 22.7 (Heat at constant volume and at constant pressure)

For a system at rest exchanging work only through pressure forces:

  • isochoric transformation: W=0W = 0 and QV=ΔUQ_V = \Delta U;
  • monobaric transformation between two states at the external pressure P0P_0: QP=ΔHQ_P = \Delta H.

Proof. Isochoric:  ⁣dV=0\dd V = 0. Monobaric: W=P0(V2V1)W = -P_0(V_2 - V_1), so Q=ΔU+P0ΔV=Δ(U+PV)Q = \Delta U + P_0\Delta V = \Delta(U + PV) since P1=P2=P0P_1 = P_2 = P_0.

Proposition 22.8 (Perfect gas: UU, HH, Mayer’s relation)

For a perfect gas, UU and HH depend on TT alone (Joule’s laws):  ⁣dU=CV ⁣dT\dd U = C_V\,\dd T,  ⁣dH=CP ⁣dT\dd H = C_P\,\dd T, and

CP,mCV,m=R,γ=CPCV,CV,m=Rγ1,CP,m=γRγ1;C_{P,m} - C_{V,m} = R, \qquad \gamma = \frac{C_P}{C_V}, \qquad C_{V,m} = \frac{R}{\gamma - 1}, \quad C_{P,m} = \frac{\gamma R}{\gamma - 1} ;

γ=5/3\gamma = 5/3 for monatomic gases, 7/57/5 for diatomic ones at ordinary temperatures. For a condensed phase in the model of Proposition 20.13, CPCV=CC_P \approx C_V = C and  ⁣dU ⁣dH=C ⁣dT\dd U \approx \dd H = C\,\dd T.

Proof. H=U+nRTH = U + nRT; differentiate with respect to TT. CV,m=32RC_{V,m} = \tfrac32 R or 52R\tfrac52 R from Proposition 20.11.

22.3 Transformations of a perfect gas

Proposition 22.9 (The four standard transformations)

For nn moles of perfect gas:

  • isochoric: W=0W = 0, Q=ΔU=nCV,mΔTQ = \Delta U = nC_{V,m}\Delta T;
  • isobaric (quasi-static): W=PΔV=nRΔTW = -P\Delta V = -nR\Delta T, Q=ΔH=nCP,mΔTQ = \Delta H = nC_{P,m}\Delta T;
  • isothermal reversible: ΔU=0\Delta U = 0, W=Q=nRTln(V2/V1)=nRTln(P2/P1)W = -Q = -nRT\ln(V_2/V_1) = nRT\ln(P_2/P_1);
  • adiabatic reversible: Q=0Q = 0, W=ΔU=nCV,m(T2T1)W = \Delta U = nC_{V,m}(T_2 - T_1), and along the path (Laplace’s law)

    PVγ=const,TVγ1=const,TγP1γ=const.PV^\gamma = \text{const}, \qquad TV^{\gamma - 1} = \text{const}, \qquad T^\gamma P^{1 - \gamma} = \text{const} .

Proof. Isochoric and isobaric: the previous propositions. Isothermal: W=nRT ⁣dV/VW = -\int nRT\,\dd V/V. Adiabatic:  ⁣dU=δW\dd U = \delta W, i.e. nCV,m ⁣dT=P ⁣dV=nRT ⁣dV/VnC_{V,m}\dd T = -P\,\dd V = -nRT\,\dd V/V, so  ⁣dT/T=(γ1) ⁣dV/V\dd T/T = -(\gamma - 1)\dd V/V (using R/CV,m=γ1R/C_{V,m} = \gamma - 1); integrate: TVγ1TV^{\gamma - 1} constant; the other forms by PV=nRTPV = nRT.

Left: in the Clapeyron diagram the work received in a quasi-static compression is the area under the path; starting from the same point, an adiabat is steeper than an isotherm (> 1): a gas compressed without heat loss heats up and climbs to a higher isotherm. Right: the work of the surroundings on a piston. Left: in the Clapeyron diagram the work received in a quasi-static compression is the area under the path; starting from the same point, an adiabat is steeper than an isotherm (> 1): a gas compressed without heat loss heats up and climbs to a higher isotherm. Right: the work of the surroundings on a piston.
Left: in the Clapeyron diagram the work received in a quasi-static compression is the area under the path; starting from the same point, an adiabat is steeper than an isotherm (γ>1\gamma > 1): a gas compressed without heat loss heats up and climbs to a higher isotherm. Right: the work of the surroundings on a piston.

Example 22.10 (Pump and diesel)

Air (γ=1.4\gamma = 1.4) compressed adiabatically from 1bar1\,\mathrm{bar}, 300K300\,\mathrm{K} to 7bar7\,\mathrm{bar} (a bicycle pump): T2=300×70.286=523KT_2 = 300 \times 7^{0.286} = 523\,\mathrm{K}250C250{}^{\circ}\mathrm{C} for an instant, which the barrel feels. A diesel’s compression ratio of 2020: T2=300×200.4=994KT_2 = 300 \times 20^{0.4} = 994\,\mathrm{K}, P2=201.4=66barP_2 = 20^{1.4} = 66\,\mathrm{bar} — above the self-ignition temperature of the fuel: the engine needs no spark (the weekend problem runs the whole cycle).

Remark 22.11 (Irreversible transformations)

When the transformation is not quasi-static, Laplace’s law and W=P ⁣dVW = -\int P\,\dd V do not apply; only W=Pext ⁣dVW = -\int P_{\mathrm{ext}}\,\dd V and the first law do. Two classic cases: a gas expanding into vacuum (Joule expansion) receives no work and, in adiabatic walls, no heatΔU=0\Delta U = 0, and a perfect gas keeps its temperature; a gas suddenly compressed by an external pressure jumping to P2P_2 receives W=P2ΔVW = -P_2\Delta V, more than the reversible work to the same pressure, and ends hotter (Exercise 22.11).

22.4 Calorimetry

Method 22.12 (Calorimetric balance)

Bodies put in thermal contact inside an insulated vessel at constant (atmospheric) pressure exchange heat only among themselves: the total ΔH=QP=0\Delta H = \sum Q_P = 0. For each body ΔH=mcΔT\Delta H = mc\,\Delta T (no phase change) or ±mL\pm mL for a change of state at its transition temperature, with LL the latent heat (enthalpy of fusion or vaporization per unit mass: water, Lf=334kJ/kgL_f = 334\,\mathrm{kJ}/\mathrm{kg} at 0C0{}^{\circ}\mathrm{C}, Lv=2260kJ/kgL_v = 2260\,\mathrm{kJ}/\mathrm{kg} at 100C100{}^{\circ}\mathrm{C}). Write the balance, solve for the final temperature, and check that each body’s assumed phase is consistent with it.

Example 22.13 (Ice in water)

50g50\,\mathrm{g} of ice at 0C0{}^{\circ}\mathrm{C} into 200g200\,\mathrm{g} of water at 30C30{}^{\circ}\mathrm{C}: melting needs 16.7kJ16.7\,\mathrm{kJ}; the water can give 25.1kJ25.1\,\mathrm{kJ} in cooling to 0C0{}^{\circ}\mathrm{C}, so all the ice melts and the balance 0.250×4180×(Tf0)=25.116.70.250 \times 4180 \times (T_f - 0) = 25.1 - 16.7 kJ gives Tf=8CT_f = 8{}^{\circ}\mathrm{C}. Had there been 100g100\,\mathrm{g} of ice, 33.4kJ33.4\,\mathrm{kJ} would be needed: only part melts and Tf=0CT_f = 0{}^{\circ}\mathrm{C} — the check matters.

Heating one kilogram of water from ice at -20 C to steam: the temperature pauses during each change of state while the latent heat is supplied — 334\, kJ to melt, 2260\, kJ to boil, far more than the 418\, kJ that carries the liquid from 0\, to 100 C.
Heating one kilogram of water from ice at 20C-20{}^{\circ}\mathrm{C} to steam: the temperature pauses during each change of state while the latent heat is supplied — 334kJ334\,\mathrm{kJ} to melt, 2260kJ2260\,\mathrm{kJ} to boil, far more than the 418kJ418\,\mathrm{kJ} that carries the liquid from 00\, to 100C100{}^{\circ}\mathrm{C}.

22.5 Exercises

Exercise 22.1

One mole of air (CP,m=29.1J/(molK)C_{P,m} = 29.1\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K})) is heated from 300K300\,\mathrm{K} to 400K400\,\mathrm{K} at constant pressure. Heat received, work received, change of internal energy.

Solution

Solution of Exercise 22.1.

Q=CP,mΔT=29.1×100=2.91kJQ = C_{P,m}\Delta T = 29.1 \times 100 = 2.91\,\mathrm{kJ}; W=nRΔT=0.83kJW = -nR\Delta T = -0.83\,\mathrm{kJ}; ΔU=Q+W=2.08kJ=CV,mΔT\Delta U = Q + W = 2.08\,\mathrm{kJ} = C_{V,m}\Delta T.

Exercise 22.2

One mole of gas at 300K300\,\mathrm{K} is compressed isothermally and reversibly from 2.0L2.0\,\mathrm{L} to 0.50L0.50\,\mathrm{L}. Work received, heat exchanged, ΔU\Delta U.

Solution

Solution of Exercise 22.2.

W=nRTln(V2/V1)=2494ln(0.25)=+3.46kJW = -nRT\ln(V_2/V_1) = -2494\ln(0.25) = +3.46\,\mathrm{kJ}; ΔU=0\Delta U = 0 so Q=3.46kJQ = -3.46\,\mathrm{kJ} (given to the bath).

Exercise 22.3

Air at 300K300\,\mathrm{K}, 1bar1\,\mathrm{bar} is compressed adiabatically and reversibly to a tenth of its volume. Final temperature and pressure.

Solution

Solution of Exercise 22.3.

T2=T1×10γ1=300×100.4=754KT_2 = T_1 \times 10^{\gamma - 1} = 300 \times 10^{0.4} = 754\,\mathrm{K}; P2=101.4=25barP_2 = 10^{1.4} = 25\,\mathrm{bar}.

Exercise 22.4

Give CV,mC_{V,m}, CP,mC_{P,m} and γ\gamma for argon and for nitrogen. For liquid water (c=4180J/(kgK)c = 4180\,\mathrm{J}/(\mathrm{kg}\,\mathrm{K})), why is the distinction between cPc_P and cVc_V dropped?

Solution

Solution of Exercise 22.4.

Argon: CV,m=32R=12.5C_{V,m} = \tfrac32 R = 12.5, CP,m=52R=20.8C_{P,m} = \tfrac52 R = 20.8 J/(mol K), γ=1.67\gamma = 1.67; nitrogen: 20.820.8, 29.129.1, γ=1.40\gamma = 1.40. For water the expansion on heating is tiny, so the work P ⁣dVP\,\dd V at constant pressure is negligible against the heat: cPcV0c_P - c_V \approx 0.

Exercise 22.5 ★★

200g200\,\mathrm{g} of water at 80C80{}^{\circ}\mathrm{C} are mixed with 300g300\,\mathrm{g} at 20C20{}^{\circ}\mathrm{C} in an insulated cup. Final temperature; what changes if the cup itself has a heat capacity of 80J/K80\,\mathrm{J}/\mathrm{K} and starts at 20C20{}^{\circ}\mathrm{C}?

Solution

Solution of Exercise 22.5.

Tf=(200×80+300×20)/500=44CT_f = (200 \times 80 + 300 \times 20)/500 = 44{}^{\circ}\mathrm{C}. With the cup: (200×4.18×80+(300×4.18+80)×20)/(500×4.18+80)=43C(200 \times 4.18 \times 80 + (300 \times 4.18 + 80) \times 20)/(500 \times 4.18 + 80) = 43{}^{\circ}\mathrm{C}.

Exercise 22.6 ★★

50g50\,\mathrm{g} of ice at 10C-10{}^{\circ}\mathrm{C} (cice=2100J/(kgK)c_{\text{ice}} = 2100\,\mathrm{J}/(\mathrm{kg}\,\mathrm{K})) are dropped into 200g200\,\mathrm{g} of water at 30C30{}^{\circ}\mathrm{C}. Final state and temperature. Same question with 150g150\,\mathrm{g} of ice.

Solution

Solution of Exercise 22.6.

Ice: warm to 00: 0.050×2100×10=1.05kJ0.050 \times 2100 \times 10 = 1.05\,\mathrm{kJ}; melt: 16.7kJ16.7\,\mathrm{kJ}; total 17.8kJ17.8\,\mathrm{kJ}. Water can give 25.1kJ25.1\,\mathrm{kJ} down to 00: all melts; then 0.250×4180Tf=25.117.80.250 \times 4180\,T_f = 25.1 - 17.8 kJ: Tf=7CT_f = 7{}^{\circ}\mathrm{C}. With 150g150\,\mathrm{g}: needs 53.3kJ53.3\,\mathrm{kJ} >> 25.1kJ25.1\,\mathrm{kJ}: only (25.13.15)/334=66g(25.1 - 3.15)/334 = 66\,\mathrm{g} of ice melt, Tf=0CT_f = 0{}^{\circ}\mathrm{C}, 84g84\,\mathrm{g} of ice remain.

Exercise 22.7 ★★

A gas follows a rectangular cycle in the Clapeyron diagram: (V1,P1)(V2,P1)(V2,P2)(V1,P2)(V1,P1)(V_1, P_1) \to (V_2, P_1) \to (V_2, P_2) \to (V_1, P_2) \to (V_1, P_1) with V2>V1V_2 > V_1, P2>P1P_2 > P_1. Work received over the cycle, as a function of the area; sign, and meaning of the sign.

Solution

Solution of Exercise 22.7.

W=P1(V2V1)+0P2(V1V2)+0=(P2P1)(V2V1)>0W = -P_1(V_2 - V_1) + 0 - P_2(V_1 - V_2) + 0 = (P_2 - P_1)(V_2 - V_1) > 0: the cycle is traversed counterclockwise (expansion at low pressure, compression at high), so the gas receives net work, equal to the enclosed area; clockwise it would deliver it — an engine.

Exercise 22.8 ★★

A bicycle pump compresses air from 1bar1\,\mathrm{bar}, 300K300\,\mathrm{K} to 7bar7\,\mathrm{bar} quickly enough to be adiabatic. Temperature reached; why the pump warms up; and why the tire’s pressure drops a little after the pumping stops.

Solution

Solution of Exercise 22.8.

T2=300×70.286=523KT_2 = 300 \times 7^{0.286} = 523\,\mathrm{K}. The hot compressed air heats the barrel by conduction at each stroke. In the tire the air cools to ambient at fixed volume: PTP \propto T, the pressure falls by the ratio of temperatures — top it up.

Exercise 22.9 ★★

A perfect gas expands into an evacuated, insulated vessel (Joule expansion). Work, heat, ΔU\Delta U, ΔT\Delta T. Is the transformation reversible? What would a real gas do?

Solution

Solution of Exercise 22.9.

W=0W = 0 (no external pressure to push against), Q=0Q = 0: ΔU=0\Delta U = 0, hence ΔT=0\Delta T = 0 for a perfect gas. Irreversible: the gas never flows back by itself. A real gas, whose molecules attract, cools slightly (part of the kinetic energy becomes potential energy as they separate).

Exercise 22.10 ★★★

Boiling 1.0kg1.0\,\mathrm{kg} of water at 100C100{}^{\circ}\mathrm{C} and 1atm1\,\mathrm{atm} (steam volume 1.67m31.67\,\mathrm{m}^{3}). Heat supplied, work exchanged with the atmosphere, ΔU\Delta U. Where does most of the latent heat go?

Solution

Solution of Exercise 22.10.

Q=Lv=2.26MJQ = L_v = 2.26\,\mathrm{MJ}; W=P(VgVl)=1.013×105×1.67=0.17MJW = -P(V_g - V_l) = -1.013\times10^5 \times 1.67 = -0.17\,\mathrm{MJ}; ΔU=2.09MJ\Delta U = 2.09\,\mathrm{MJ}: 93%93\% of the heat goes into separating the molecules (internal energy), 7%7\% into pushing back the atmosphere.

Exercise 22.11 ★★★

One mole of diatomic gas at 300K300\,\mathrm{K}, 1bar1\,\mathrm{bar}, in an insulated cylinder, is compressed by suddenly setting the external pressure to 5bar5\,\mathrm{bar} and waiting for equilibrium. Final temperature and volume (first law with W=PextΔVW = -P_{\mathrm{ext}}\Delta V); compare with the reversible adiabatic compression to 5bar5\,\mathrm{bar}.

Solution

Solution of Exercise 22.11.

W=P2(V2V1)W = -P_2(V_2 - V_1), ΔU=nCV,m(T2T1)\Delta U = nC_{V,m}(T_2 - T_1), V2=nRT2/P2V_2 = nRT_2/P_2, V1=nRT1/P1V_1 = nRT_1/P_1: 52(T2300)=T2+300×5\tfrac52(T_2 - 300) = -T_2 + 300 \times 5, 3.5T2=22503.5T_2 = 2250, T2=643KT_2 = 643\,\mathrm{K}, V2=10.7LV_2 = 10.7\,\mathrm{L}. Reversible: T2=300×50.286=475KT_2 = 300 \times 5^{0.286} = 475\,\mathrm{K}, V2=7.9LV_2 = 7.9\,\mathrm{L}. The sudden compression does more work on the gas (the full 5bar5\,\mathrm{bar} acts from the start) and ends hotter and less compressed.

Exercise 22.12 ★★★

Sound is a fast compression, hence adiabatic: its speed is c=γP/ρc = \sqrt{\gamma P/\rho} (the isothermal value P/ρ\sqrt{P/\rho} was Newton’s mistake). Compute both for air at 20C20{}^{\circ}\mathrm{C} and compare with the measured 343m/s343\,\mathrm{m}/\mathrm{s}. Show that c=γRT/Mc = \sqrt{\gamma RT/M} and compare with the rms speed of Chapter 20.

Solution

Solution of Exercise 22.12.

ρ=PM/RT=1.20kg/m3\rho = PM/RT = 1.20\,\mathrm{kg}/\mathrm{m}^{3}: γP/ρ=1.4×1.013×105/1.20=343m/s\sqrt{\gamma P/\rho} = \sqrt{1.4 \times 1.013\times10^5/1.20} = 343\,\mathrm{m}/\mathrm{s}; P/ρ=290m/s\sqrt{P/\rho} = 290\,\mathrm{m}/\mathrm{s}, 15%15\% low. With P/ρ=RT/MP/\rho = RT/M: c=γRT/Mc = \sqrt{\gamma RT/M}; against u=3RT/Mu = \sqrt{3RT/M} = 502m/s502\,\mathrm{m}/\mathrm{s}: c/u=γ/3=0.68c/u = \sqrt{\gamma/3} = 0.68.

22.6 Problem: From the bicycle pump to the diesel engine

Problem 22.1

Weekend problem — a hand pump that burns the fingers, a cylinder that lights its own fuel, and a steel ball that bounces on a cushion of air: the first law in three compressions

Air: perfect diatomic gas, γ=1.40\gamma = 1.40, CV,m=52RC_{V,m} = \tfrac52 R, CP,m=72RC_{P,m} = \tfrac72 R, M=29g/molM = 29\,\mathrm{g}/\mathrm{mol}; R=8.314J/(molK)R = 8.314\,\mathrm{J}/(\mathrm{mol}\,\mathrm{K}). Initial state everywhere: P1=1.00barP_1 = 1.00\,\mathrm{bar}, T1=300KT_1 = 300\,\mathrm{K}.

Part I — The bicycle pump. The pump’s cylinder has a volume V1=212cm3V_1 = 212\,\mathrm{cm}^{3}; the air in it is compressed reversibly and adiabatically until it reaches the tire’s pressure, 7.0bar7.0\,\mathrm{bar}.

  1. Amount of air in the cylinder.
  2. Volume at the end of the compression.
  3. Temperature at the end of the compression.
  4. Work received by the air during one stroke.
  5. The tire (2.0L2.0\,\mathrm{L}) must be brought from 1bar1\,\mathrm{bar} to 7bar7\,\mathrm{bar} at 300K300\,\mathrm{K}: how many strokes, and how much work in all (take the work per stroke as constant)?
  6. The hot air then cools in the tire to 300K300\,\mathrm{K}: what happens to the tire’s pressure, and what does the cyclist do?
  7. Compare the adiabatic work per stroke with the work of an isothermal compression to the same 7bar7\,\mathrm{bar}. Why is the isothermal work larger although the gas ends cooler?

Part II — The diesel compression. A cylinder of V1=0.50LV_1 = 0.50\,\mathrm{L} compresses its air reversibly and adiabatically by a factor 2020.

  1. Amount of air, and temperature T2T_2 after compression.
  2. Pressure P2P_2.
  3. The fuel self-ignites above about 500K500\,\mathrm{K}: explain why a diesel needs no spark plug, and why a petrol engine (ratio 10\approx 10, see Exercise 22.3) must not self-ignite.
  4. Work received by the air during the compression.
  5. At 3000rpm3000\,\mathrm{rpm} one cylinder compresses 2525 times per second: power absorbed by the compression (it is returned later in the cycle).
  6. Real compressions are fast (irreversibility) and lose heat to the walls: in which direction does each effect move T2T_2?

Part III — Combustion and expansion. At the top of the stroke 20mg20\,\mathrm{mg} of fuel (heating value 43MJ/kg43\,\mathrm{MJ}/\mathrm{kg}) burn while the piston starts down, at constant pressure P2P_2; then the gas expands reversibly and adiabatically back to V1V_1. Treat the gas as air throughout.

  1. Heat released by the fuel.
  2. Temperature T3T_3 and volume V3V_3 at the end of the isobaric combustion.
  3. Work exchanged during the isobaric phase (sign!).
  4. Temperature T4T_4 at the end of the adiabatic expansion, and the work exchanged during it.
  5. Net work delivered by the gas over the four strokes, and the ratio to the heat released (the ideal efficiency).
  6. Compare that efficiency with 1T1/T31 - T_1/T_3, the bound that Chapter 24 will establish for any engine working between these extreme temperatures.
  7. Heat rejected with the exhaust, by the first law over the cycle; check the balance.

Part IV — Measuring γ\gamma with a bouncing ball. A steel ball of mass m=16.5gm = 16.5\,\mathrm{g} fits a vertical glass tube of cross-section S=2.0cm2S = 2.0\,\mathrm{cm}^{2} closed at the bottom by a flask of volume V=10LV = 10\,\mathrm{L} of air at P=1.0barP = 1.0\,\mathrm{bar}; displaced by xx from its equilibrium position, it oscillates.

  1. Why can the compressions and expansions of the air be taken as adiabatic? Write the relation between a small displacement xx and the pressure change  ⁣dP\dd P (Laplace’s law, linearized).
  2. Deduce the restoring force on the ball and show that its motion is harmonic, with ω02=γPS2/mV\omega_0^2 = \gamma PS^2/mV.
  3. Compute the period, and the value of γ\gamma one would deduce from a measured period of 1.10s1.10\,\mathrm{s}.
  4. Why does friction between ball and tube, and leakage of air, bias the result, and in which direction?
  5. Summarize the three compressions: which quantity the first law conserved in each, and what the adiabatic exponent γ\gamma governed.
Solution

Solution of Problem 22.1.

1. n=P1V1/RT1=105×2.12×104/2494=8.5×103moln = P_1V_1/RT_1 = 10^5 \times 2.12\times10^{-4}/2494 = 8.5 \times 10^{-3}\,\mathrm{mol}.

2. PVγPV^\gamma constant: V2=V1(P1/P2)1/γ=212×70.714=53cm3V_2 = V_1(P_1/P_2)^{1/\gamma} = 212 \times 7^{-0.714} = 53\,\mathrm{cm}^{3}.

3. T2=T1(P2/P1)(γ1)/γ=300×70.286=523KT_2 = T_1(P_2/P_1)^{(\gamma - 1)/\gamma} = 300 \times 7^{0.286} = 523\,\mathrm{K}.

4. W=nCV,m(T2T1)=8.5×103×20.8×223=39JW = nC_{V,m}(T_2 - T_1) = 8.5\times10^{-3} \times 20.8 \times 223 = 39\,\mathrm{J}.

5. Air to add: Δn=ΔPV/RT=6×105×2×103/2494=0.48mol\Delta n = \Delta P\,V/RT = 6\times10^5 \times 2\times10^{-3}/ 2494 = 0.48\,\mathrm{mol}: 0.48/8.5×103=570.48/8.5\times10^{-3} = 57 strokes, about 2.2kJ2.2\,\mathrm{kJ} — a minute of honest effort.

6. At constant volume PTP \propto T: the pressure falls as the air cools (by up to 300/523300/523 for the last stroke’s air); the cyclist adds a few strokes after a pause.

7. Wiso=nRTln(P2/P1)=8.5×103×2494×1.95=41J>39JW_{\text{iso}} = nRT\ln(P_2/P_1) = 8.5\times10^{-3} \times 2494 \times 1.95 = 41\,\mathrm{J} > 39\,\mathrm{J}: the isothermal path compresses the gas further (to 30cm330\,\mathrm{cm}^{3} instead of 53cm353\,\mathrm{cm}^{3}) to reach 7bar7\,\mathrm{bar}, because it stays cool — more volume swept, more work.

8. n=105×5×104/2494=0.020moln = 10^5 \times 5\times10^{-4}/2494 = 0.020\,\mathrm{mol}; T2=300×200.4=994KT_2 = 300 \times 20^{0.4} = 994\,\mathrm{K}.

9. P2=201.4=66barP_2 = 20^{1.4} = 66\,\mathrm{bar}.

10. 994K994\,\mathrm{K} is well above the fuel’s self-ignition point: the injected fuel lights on contact. A petrol engine compresses its air–fuel mixture only to about 750K750\,\mathrm{K} so that it does not ignite before the spark; too high a ratio gives “knock”.

11. W=nCV,m(T2T1)=0.020×20.8×694=289JW = nC_{V,m}(T_2 - T_1) = 0.020 \times 20.8 \times 694 = 289\,\mathrm{J}.

12. 25×289=7.2kW25 \times 289 = 7.2\,\mathrm{kW} per cylinder, stored in the hot gas and given back in the expansion.

13. Irreversibility (the gas does not follow the quasi-static path; extra work is dissipated) raises T2T_2; heat lost to the walls lowers it. In a real engine the second usually wins: T2T_2 is a little below the ideal value.

14. Q=20×106×43×106=860JQ = 20\times10^{-6} \times 43\times10^6 = 860\,\mathrm{J}.

15. Isobaric: Q=nCP,m(T3T2)Q = nC_{P,m}(T_3 - T_2): T3T2=860/(0.020×29.1)=1480KT_3 - T_2 = 860/(0.020 \times 29.1) = 1480\,\mathrm{K}, T3=2470KT_3 = 2470\,\mathrm{K}; V3=V2T3/T2=25×2.48=62cm3V_3 = V_2T_3/T_2 = 25 \times 2.48 = 62\,\mathrm{cm}^{3}.

16. W=P2(V3V2)=66×105×37×106=244JW = -P_2(V_3 - V_2) = -66\times10^5 \times 37\times10^{-6} = -244\,\mathrm{J}: work delivered by the gas.

17. T4=T3(V3/V1)γ1=2470×(0.124)0.4=1070KT_4 = T_3(V_3/V_1)^{\gamma - 1} = 2470 \times (0.124)^{0.4} = 1070\,\mathrm{K}; W=nCV,m(T4T3)=0.020×20.8×(1400)=582JW = nC_{V,m}(T_4 - T_3) = 0.020 \times 20.8 \times (-1400) = -582\,\mathrm{J}.

18. Net work delivered =244+582289=537J= 244 + 582 - 289 = 537\,\mathrm{J}; ratio 537/860=62%537/860 = 62\% (the ideal Diesel efficiency at these settings; real engines reach about 40%40\%).

19. 1300/2470=88%1 - 300/2470 = 88\%: the ideal Diesel cycle stays well below the Carnot bound, because its heat is received over a range of temperatures rather than at the highest one.

20. Over a cycle ΔU=0\Delta U = 0: Qout=(860537)=323JQ_{\text{out}} = -(860 - 537) = -323\,\mathrm{J}, i.e. 323J323\,\mathrm{J} leave with the exhaust; check: nCV,m(T4T1)=0.020×20.8×770=320JnC_{V,m}(T_4 - T_1) = 0.020 \times 20.8 \times 770 = 320\,\mathrm{J}.

21. The oscillation is fast (a second) compared with heat conduction through 10L10\,\mathrm{L} of air: adiabatic. Linearizing PVγPV^\gamma:  ⁣dP/P=γ ⁣dV/V=γSx/V\dd P/P = -\gamma\,\dd V/V = -\gamma Sx/V.

22. Force on the ball S ⁣dP=γPS2x/VS\,\dd P = -\gamma PS^2x/V: mx¨=(γPS2/V)xm\ddot x = -(\gamma PS^2/V)x, harmonic, ω02=γPS2/mV\omega_0^2 = \gamma PS^2/mV.

23. ω02=1.4×105×4×108/(0.0165×0.010)=33.9s2\omega_0^2 = 1.4 \times 10^5 \times 4\times10^{-8}/(0.0165 \times 0.010) = 33.9\,\mathrm{s}^{-2}: T=2π/5.83=1.08sT = 2\pi/5.83 = 1.08\,\mathrm{s}. From T=1.10sT = 1.10\,\mathrm{s}: γ=4π2mV/(T2PS2)=4π2×0.0165×0.010/(1.21×105×4×108)=1.35\gamma = 4\pi^2mV/(T^2PS^2) = 4\pi^2 \times 0.0165 \times 0.010/(1.21 \times 10^5 \times 4\times10^{-8}) = 1.35.

24. Friction damps the motion and, if it is dry, shifts the equilibrium; leakage past the ball lets air escape during a compression, lowering the restoring force: both lengthen the period and bias γ\gamma low — as the 1.351.35 above.

25. Pump and diesel: Q=0Q = 0, so ΔU=W\Delta U = W — work became internal energy and temperature, by Laplace’s law with exponent γ\gamma. Ball: a fast compression is adiabatic, and γ\gamma sets the stiffness of an air spring.

Terms defined in this chapter

See all 393 terms in the glossary