What JEE Adds to This Chapter

Sections 1 to 12 built this chapter properly. Expansion, specific heat, calorimetry, latent heat, conduction, convection, radiation and cooling are all in place, and for the Board paper that build is complete.

What JEE adds is not new physics. It is still ΔL=αLΔT\Delta L = \alpha L \Delta T, still Q=msΔTQ = ms\Delta T, still H=KAΔTLH = \frac{KA\Delta T}{L}, still σAeT4\sigma A e T^4. What changes is that the quantity you want stops being uniform.

The rod is no longer the same thickness at both ends. The conductivity is no longer the same at both ends. The heat no longer flows through a fixed area, because the area is a shell that grows as you move outward. The ice sheet that is conducting the heat is itself getting thicker while you watch. The mixture's final state is not given to you — you have to work out whether the ice all melted before you can even write the balance.

Every one of those is answered the same way: stop assuming the thing is constant, take a slice, and add the slices up. And before you write a single temperature into a fourth power, say out loud whether it is in kelvin.

Some of what follows sits outside the rationalised syllabus body text — thermal resistance and series-parallel networks, bimetallic strips, Kirchhoff's law — but JEE Main and JEE Advanced ask this material every year, so it is developed here from first principles.

The eleven things this section teaches

# Skill Why it earns marks
1 A composite rod's effective α\alpha, and the condition for the difference of two lengths to stay constant One line of algebra, asked as a full question
2 The pendulum clock — the temperature for correct time, and the seconds gained or lost per day The only place a 12\frac{1}{2} from a binomial expansion earns four marks
3 Apparent versus real expansion, and the weight thermometer Two coefficients that differ by the vessel's, and a mass that gets expelled
4 The bimetallic strip's radius of curvature Pure geometry once you see that both mid-lines turn through the same angle
5 Conduction through a rod of varying cross-section, by integration The answer is a geometric mean, and the guess is always wrong
6 Conduction with KK varying along the length Resistances in series, taken to the continuum limit
7 Radial conduction through pipe lagging and through a spherical shell Needs drr\int \frac{dr}{r}; a slab formula is not merely inaccurate, it is meaningless
8 Growth of ice on a pond and the time to thicken from one depth to another The famous ty2t \propto y^2
9 Networks with junction temperatures, series, parallel and star Equal heat current at every node is the whole method
10 Multi-phase calorimetry where the final state must be determined Assume it and you will be wrong roughly half the time
11 Radiation exchange, equilibrium in sunlight, and Newton's law in exponential form Fourth powers, kelvin, and knowing where the linear law dies

Conventions, fixed now

This section uses the chapter's symbol table without exception. Restating the five that matter here:

  • TT is an absolute temperature in kelvin. tt or tCt_C is Celsius. Every fourth power, every ratio, every gas-law step needs kelvin.
  • LL bare is a length; LfL_f and LvL_v are the latent heats of fusion and vaporisation.
  • α\alpha is linear expansion, β\beta areal, γ\gamma volume. Absorptive power is aa, never α\alpha.
  • KK is thermal conductivity; lowercase kk is the cooling constant in Newton's law.
  • ss is specific heat capacity, CC molar specific heat, SS the heat capacity of a whole body. RR is thermal resistance LKA\frac{L}{KA}, in K/W. The one exception is the solar constant, also written SS, in W/m2^2 — the units separate them wherever both appear.

Constants used throughout, unless a problem states otherwise:

Quantity Value
αsteel\alpha_{\text{steel}} 1.2×1051.2 \times 10^{-5} K1^{-1}
αbrass\alpha_{\text{brass}} 1.8×1051.8 \times 10^{-5} K1^{-1}
αcopper\alpha_{\text{copper}} 1.7×1051.7 \times 10^{-5} K1^{-1}
γmercury\gamma_{\text{mercury}} 1.82×1041.82 \times 10^{-4} K1^{-1}
swaters_{\text{water}} 4186 J/(kg K)
sices_{\text{ice}} 2100 J/(kg K)
LfL_f (ice) 3.33×1053.33 \times 10^{5} J/kg
LvL_v (water) 22.6×10522.6 \times 10^{5} J/kg
KcopperK_{\text{copper}} 385 W/(m K)
KsteelK_{\text{steel}} 50.2 W/(m K)
KiceK_{\text{ice}} 1.6 W/(m K)
σ\sigma 5.67×1085.67 \times 10^{-8} W/(m2^2 K4^4)
Density of ice 900 kg/m3^3

Every solution restates the constants it uses. No problem here mixes two values of the same constant.

Key Point — the master move of this whole section: Rth=dxK(x)A(x)andH=ΔTRthR_{th} = \int \frac{dx}{K(x)\,A(x)} \qquad\text{and}\qquad H = \frac{\Delta T}{R_{th}} Thermal resistance is what adds. Take a slab so thin that KK and AA are constant across it, write its resistance, and integrate along the path the heat takes. Every non-uniform conduction problem in this section is that one integral with a different A(x)A(x). For a slab AA is constant; for a taper A=πr(x)2A = \pi r(x)^2; for a pipe A=2πrLA = 2\pi r L; for a sphere A=4πr2A = 4\pi r^2.

[Exam Tip] Three questions, asked before any algebra, choose the method for almost every problem below. Is the cross-section the same everywhere? Is the conductivity the same everywhere? Is anything changing while the heat flows? A "no" to the first two means integrate. A "no" to the third means write a differential equation in time. Answer all three and you have chosen your method before writing a symbol.

Composite Rods, the Frozen Gap, and the Pendulum Clock

A rod made of two metals

Join a rod of length L1L_1 and coefficient α1\alpha_1 end to end with a rod of length L2L_2 and coefficient α2\alpha_2. Heat the pair through ΔT\Delta T. Each piece expands on its own account, so the total elongation is

ΔL=L1α1ΔT+L2α2ΔT\Delta L = L_1\alpha_1\Delta T + L_2\alpha_2\Delta T

Define the effective coefficient of the composite by insisting it behaves like a single rod of length L1+L2L_1 + L_2:

Key Point — effective linear expansion coefficient: αeff=L1α1+L2α2L1+L2\alpha_{\text{eff}} = \frac{L_1\alpha_1 + L_2\alpha_2}{L_1 + L_2} It is the length-weighted average of the two coefficients, not the plain average. The longer piece gets more of a say.

Note carefully what this is not. It is not α1+α22\frac{\alpha_1+\alpha_2}{2} unless the two lengths happen to be equal. And it is not the parallel-resistor-looking 2α1α2α1+α2\frac{2\alpha_1\alpha_2}{\alpha_1+\alpha_2} — that formula belongs to a different problem (two rods side by side with a common expansion), and mixing them up is a standard way to lose four marks.

The difference that refuses to change

Two rods keeping a fixed gap, and a bimetallic strip radius of curvature

Here is the classic. Two rods of different metals are laid side by side, not joined. We want the difference in their lengths to be the same at every temperature. What does that demand?

At temperature tt the two lengths are L1(1+α1ΔT)L_1(1+\alpha_1\Delta T) and L2(1+α2ΔT)L_2(1+\alpha_2\Delta T), so the difference is

L1L2+(L1α1L2α2)ΔTL_1 - L_2 + \left(L_1\alpha_1 - L_2\alpha_2\right)\Delta T

For that to be independent of ΔT\Delta T, the bracket must vanish.

Key Point — the frozen-gap condition: L1α1=L2α2L1L2=α2α1L_1\alpha_1 = L_2\alpha_2 \qquad\Longleftrightarrow\qquad \frac{L_1}{L_2} = \frac{\alpha_2}{\alpha_1} Read it physically: the two rods must grow by the same absolute amount. Then whatever gap there was between their ends stays exactly that gap. The rod with the smaller α\alpha has to be the longer one, which is the part students get backwards.

That is the whole trick behind a gridiron pendulum and behind the invar-and-brass compensating strips inside a good clock: not to stop things expanding, but to arrange that two expansions cancel out where it matters.

The pendulum clock

A pendulum clock counts time by counting swings. Its period is

Tp=2πLgT_p = 2\pi\sqrt{\frac{L}{g}}

Heat the pendulum and LL grows, so TpT_p grows, so each swing takes longer and the clock runs slow. Cool it and the clock runs fast.

Put in L=L(1+αΔT)L^{\,\prime} = L(1+\alpha\Delta T):

TpTp=1+αΔT1+12αΔT\frac{T_p^{\,\prime}}{T_p} = \sqrt{1+\alpha\Delta T} \approx 1 + \frac{1}{2}\alpha\Delta T

using the binomial expansion, which is superb here because αΔT\alpha\Delta T is of order 10410^{-4}.

Key Point — the clock formula: ΔTpTp=12αΔT\frac{\Delta T_p}{T_p} = \frac{1}{2}\alpha\,\Delta T and the time gained or lost in one day of 86400 seconds is Δt=12αΔT×86400 s\left\lvert \Delta t \right\rvert = \frac{1}{2}\alpha\,\Delta T \times 86400 \ \text{s} Slow if the pendulum is warmer than the calibration temperature, fast if it is cooler. The 12\frac{1}{2} is the entire question; forget it and your answer is exactly double.

Three shapes this comes in:

  1. Given the calibration temperature and the room temperature, find the daily error. Straight substitution.
  2. Given the daily error, find the temperature at which the clock is correct. Solve for ΔT\Delta T, then add or subtract from the stated temperature — and check the sign by asking whether the clock is gaining or losing.
  3. Given errors at two temperatures, find α\alpha or the correct temperature. The error is linear in temperature, so two points fix the line. Where the line crosses zero is where the clock is right.

[Exam Tip] The daily error per kelvin is 12α×86400=43200α\frac{1}{2}\alpha \times 86400 = 43200\,\alpha seconds. For steel, α=1.2×105\alpha = 1.2\times10^{-5} K1^{-1}, that is 0.518 s per day per kelvin. Memorise that one number and most clock questions become mental arithmetic: 20 K of warming costs about 10.4 s a day.

Liquids, the Weight Thermometer, and the Bimetallic Radius

Apparent expansion: you cannot see the vessel move

Heat a flask of mercury and the mercury level rises. But the flask expanded too, so the rise you actually observe is short of the true expansion of the liquid.

Let the flask hold volume V0V_0 of liquid at 00°C. Heat both through ΔT\Delta T:

  • the liquid wants to occupy V0(1+γrΔT)V_0(1+\gamma_r\Delta T), where γr\gamma_r is its real coefficient of volume expansion;
  • the flask now holds V0(1+γgΔT)V_0(1+\gamma_g\Delta T);
  • the overflow, or the visible rise, corresponds to the difference.

Key Point — apparent expansion: γapp=γrealγvessel\gamma_{\text{app}} = \gamma_{\text{real}} - \gamma_{\text{vessel}} and since the vessel is a solid, γvessel=3αvessel\gamma_{\text{vessel}} = 3\alpha_{\text{vessel}}. What you measure in a flask is always γapp\gamma_{\text{app}}. The real coefficient is only reachable if you know the vessel's material — or if you use a method that eliminates the vessel entirely.

Because γ\gamma for a liquid is typically ten times γ\gamma for glass, the correction is real but not enormous. For mercury in glass, γr=1.82×104\gamma_r = 1.82\times10^{-4} K1^{-1} and γg=2.7×105\gamma_g = 2.7\times10^{-5} K1^{-1}, so γapp=1.55×104\gamma_{\text{app}} = 1.55\times10^{-4} K1^{-1} — about 15% below the real value. Quote the wrong one and you are 15% out.

The weight thermometer

Now the beautiful version. Fill a bulb completely with liquid at t1t_1, seal nothing, heat it to t2t_2 and catch what spills out. Weigh the spilt liquid. That is a weight thermometer, and it is how γapp\gamma_{\text{app}} is actually measured.

Take t1=0t_1 = 0°C so that the mass in the bulb is mm and the liquid's density there is ρ0\rho_0. At temperature tt:

  • the volume that overflows is V0γapptV_0\,\gamma_{\text{app}}\,t, measured at the hot temperature;
  • the density of the hot liquid is ρt=ρ01+γrt\rho_t = \dfrac{\rho_0}{1+\gamma_r t}.

Multiply:

Key Point — mass expelled by a weight thermometer: m=mγappt1+γrtm^{\,\prime} = \frac{m\,\gamma_{\text{app}}\,t}{1+\gamma_r\,t} The denominator is there because the expelled liquid is hot, therefore less dense, so the same volume weighs less. It is often dropped, giving m=mγapptm^{\,\prime} = m\gamma_{\text{app}}t; that is a fine first estimate but it runs about γrt\gamma_r t high — for mercury over 100 K, about 1.8% high.

Rearranged for the experimenter:

γappm(mm)t\gamma_{\text{app}} \approx \frac{m^{\,\prime}}{\left(m - m^{\,\prime}\right)t}

which is the form to use when the question gives you the mass remaining rather than the mass expelled. But notice the \approx: only the first form is exact. Put m=mγappt1+γrtm^{\,\prime} = \frac{m\gamma_{\text{app}}t}{1+\gamma_r t} into it, so that the mass left behind is mm=m(1+γgt)1+γrtm - m^{\,\prime} = \frac{m\left(1+\gamma_g t\right)}{1+\gamma_r t}, and the γr\gamma_r cancels to leave

m(mm)t=γapp1+γgt\frac{m^{\,\prime}}{\left(m - m^{\,\prime}\right)t} = \frac{\gamma_{\text{app}}}{1+\gamma_g\,t}

So the remaining-mass form returns γapp\gamma_{\text{app}} low by the factor 1+γgt1+\gamma_g t — the vessel's own expansion, which this rearrangement cannot see. For mercury in glass over 100 K that factor is γgt=2.7×103\gamma_g t = 2.7\times10^{-3}, so the answer comes out about 0.3% low: harmless in an exam, but it is an approximation and not an identity. Multiply by (1+γgt)\left(1+\gamma_g t\right) if you ever need it exact.

The bimetallic strip, and its radius of curvature

Bond a strip of brass to a strip of iron, both of the same length at room temperature. Heat them. Brass wants to be longer than iron does, they are stuck together, so the only way both can be satisfied is for the pair to bend, with the brass on the outside where the arc is longer.

Take each strip to have thickness tt, so the pair has total thickness 2t2t. After heating through ΔT\Delta T the strip becomes an arc of radius RR, measured to the bonded interface, subtending an angle θ\theta at the centre.

The key observation: both mid-lines turn through the same angle θ\theta. They are stuck together, so they must. The mid-line of the inner strip sits at radius Rt2R - \frac{t}{2} and the mid-line of the outer at R+t2R + \frac{t}{2}, and each has the length free expansion would have given it:

L(1+α1ΔT)=(Rt2)θ,L(1+α2ΔT)=(R+t2)θL\left(1+\alpha_1\Delta T\right) = \left(R - \tfrac{t}{2}\right)\theta, \qquad L\left(1+\alpha_2\Delta T\right) = \left(R + \tfrac{t}{2}\right)\theta

Divide one by the other and the unknowns LL and θ\theta both disappear:

1+α2ΔT1+α1ΔT=R+t2Rt2\frac{1+\alpha_2\Delta T}{1+\alpha_1\Delta T} = \frac{R+\frac{t}{2}}{R-\frac{t}{2}}

Apply componendo and dividendo — subtract the two sides' numerators and denominators, then add them:

(α2α1)ΔT2+(α1+α2)ΔT=t2R\frac{\left(\alpha_2-\alpha_1\right)\Delta T}{2+\left(\alpha_1+\alpha_2\right)\Delta T} = \frac{t}{2R}

Key Point — radius of curvature of a bimetallic strip: R=t[2+(α1+α2)ΔT]2(α2α1)ΔT    t(α2α1)ΔTR = \frac{t\left[\,2+\left(\alpha_1+\alpha_2\right)\Delta T\,\right]}{2\left(\alpha_2-\alpha_1\right)\Delta T} \;\approx\; \frac{t}{\left(\alpha_2-\alpha_1\right)\Delta T} with tt the thickness of EACH strip, so 2t2t is the thickness of the pair. The same result is often written using the total thickness d=2td = 2t, giving Rd2(α2α1)ΔTR \approx \frac{d}{2(\alpha_2-\alpha_1)\Delta T} — identical physics, so read which thickness a formula means before you use it. The dropped term is of order (α1+α2)ΔT103\left(\alpha_1+\alpha_2\right)\Delta T \sim 10^{-3}, so the approximation is good to about a tenth of a percent.

Three things to read off that result, because each is a question in its own right:

  • R1ΔTR \propto \frac{1}{\Delta T}. Double the heating, halve the radius, so the strip curls twice as tightly. That is exactly what makes it a usable thermostat: the deflection is proportional to temperature.
  • RtR \propto t. A thinner pair curls more. Thermostat strips are thin for that reason, not to save metal.
  • RR depends only on the difference of the coefficients. Two metals with α\alpha values of 1.2×1051.2\times10^{-5} and 1.8×1051.8\times10^{-5} behave exactly like a pair with 2.2×1052.2\times10^{-5} and 2.8×1052.8\times10^{-5}.

For a strip of length LL clamped at one end, the free tip swings sideways through

δ=R(1cosLR)    L22R\delta = R\left(1 - \cos\frac{L}{R}\right) \;\approx\; \frac{L^{2}}{2R}

[Exam Tip] Which way does it bend? Say it in words rather than trusting a formula: on heating it bends towards the metal that expands less; on cooling it bends towards the metal that expands more. Iron-brass heated curls with brass outside; the same strip cooled below its flat temperature curls the other way, with iron outside.

Conduction When the Rod Is Not Uniform

Everything in Section 8 assumed a bar of constant cross-section made of one material, and gave H=KAΔTLH = \frac{KA\Delta T}{L}. Take away either assumption and that formula is not merely inaccurate — it does not have a well-defined AA or KK to put into it.

The fix is the same one every time. Resistances in series add, so slice the rod into slabs so thin that KK and AA are constant across each, and integrate.

Rth=0LdxK(x)A(x),H=ΔTRthR_{th} = \int_0^{L}\frac{dx}{K(x)\,A(x)}, \qquad H = \frac{\Delta T}{R_{th}}

Tapered rod sliced for integration and temperature profiles that are not straight

Two facts make this workable, and both are worth saying out loud before you start:

  1. In the steady state, HH is the same through every slice. Nothing is accumulating anywhere, so whatever enters a slice must leave it. This is what lets you treat HH as a constant and pull it out of the integral.
  2. The temperature gradient is therefore steepest where KAKA is smallest. The heat has to squeeze through, and it needs a bigger push to do it. That single sentence predicts the shape of every profile below before you integrate anything.

A rod of varying cross-section: the truncated cone

A solid rod tapers uniformly from radius r1r_1 at the hot end to r2r_2 at the cold end over a length LL, and its conductivity KK is uniform. At distance xx,

r(x)=r1+(r2r1)xL,A(x)=πr(x)2r(x) = r_1 + \frac{\left(r_2-r_1\right)x}{L}, \qquad A(x) = \pi r(x)^2

Rth=0LdxKπr(x)2=LKπ(r2r1)[1r11r2]=LKπr1r2R_{th} = \int_0^{L}\frac{dx}{K\pi r(x)^2} = \frac{L}{K\pi\left(r_2-r_1\right)}\left[\frac{1}{r_1}-\frac{1}{r_2}\right] = \frac{L}{K\pi r_1 r_2}

Key Point — the tapered rod: H=Kπr1r2ΔTLH = \frac{K\pi r_1 r_2\,\Delta T}{L} The effective area is πr1r2\pi r_1 r_2 — the geometric mean of the two end areas, A1A2\sqrt{A_1A_2}. It is not the arithmetic mean A1+A22\frac{A_1+A_2}{2}, and it is not the area at the mid-point. Put r1=r2=rr_1 = r_2 = r and it collapses correctly to Kπr2ΔTL\frac{K\pi r^2\Delta T}{L}, which is your check that the algebra is right.

And the temperature at a point is not what you would guess. The profile follows from integrating only as far as xx:

T(x)=T1HKπLr2r1[1r11r(x)]T(x) = T_1 - \frac{H}{K\pi}\cdot\frac{L}{r_2-r_1}\left[\frac{1}{r_1}-\frac{1}{r(x)}\right]

For a rod running from 100°C to 0°C with r2=2r1r_2 = 2r_1, the mid-point sits at 33.3°C, not 50°C. It is bunched toward the cold end because the thin half has most of the resistance, so most of the temperature drop happens there. Draw the profile once and you will never guess 50 again.

A rod whose conductivity varies along its length

Now keep the area constant and let the material change, say K(x)=K0(1+xL)K(x) = K_0\left(1+\frac{x}{L}\right): conductivity K0K_0 at the hot end rising to 2K02K_0 at the cold end.

Rth=0LdxK0(1+xL)A=LK0Aln2R_{th} = \int_0^{L}\frac{dx}{K_0\left(1+\frac{x}{L}\right)A} = \frac{L}{K_0A}\ln 2

H=K0AΔTLln2=K0AΔT0.693LH = \frac{K_0A\,\Delta T}{L\ln 2} = \frac{K_0 A \Delta T}{0.693\,L}

so the equivalent conductivity of the whole rod is

Keq=K0ln2=1.443K0K_{\text{eq}} = \frac{K_0}{\ln 2} = 1.443\,K_0

Key Point: The rod behaves as though its conductivity were 1.443K01.443\,K_0, not the arithmetic mean 1.5K01.5\,K_0 of its end values. The equivalent conductivity of a series arrangement is always dragged below the arithmetic mean, because the poor conductor is the bottleneck and bottlenecks dominate series resistance.

The temperature profile is logarithmic here: T(x)=T1ΔTln(1+xL)ln2T(x) = T_1 - \frac{\Delta T\,\ln\left(1+\frac{x}{L}\right)}{\ln 2}, which for 100°C to 0°C puts the mid-point at 41.5°C. Again below 50, and for the same reason — the resistive half is nearer the hot end.

The two profiles side by side

Rod HH Mid-point temperature for 100°C to 0°C
uniform, area AA, conductivity KK KAΔTL\dfrac{KA\Delta T}{L} 50.0°C
tapered, r2=2r1r_2 = 2r_1 Kπr1r2ΔTL\dfrac{K\pi r_1r_2\Delta T}{L} 33.3°C
K=K0(1+xL)K = K_0\left(1+\frac{x}{L}\right) K0AΔTLln2\dfrac{K_0A\Delta T}{L\ln 2} 41.5°C

[Exam Tip] Two checks worth five seconds each. First, set the varying quantity constant and see whether your formula collapses to KAΔTL\frac{KA\Delta T}{L}. If it does not, the integration is wrong. Second, ask which half has the greater resistance and check that most of the temperature drop happened there. A profile that drops more across the fat, well-conducting half is telling you the integral was set up backwards.

Radial Conduction: Pipes and Shells

Lag a steam pipe. Heat leaves the pipe and travels outward through the lagging. What area is it crossing?

There is no single answer — that is the whole point. Just outside the pipe the heat crosses a small cylinder; at the outer surface of the lagging it crosses a much larger one. A slab formula needs one fixed area, and this geometry does not have one. So we slice again, this time into shells.

Cylindrical pipe lagging and a spherical shell each needing a radial integral

Cylindrical lagging

Take a shell of radius rr and thickness drdr, on a pipe of length LL. Its area is 2πrL2\pi r L and its resistance is

dR=drK(2πrL)dR = \frac{dr}{K\left(2\pi r L\right)}

In the steady state the same HH crosses every shell, so the resistances are in series and simply add:

Rth=r1r2dr2πrLK=12πLKlnr2r1R_{th} = \int_{r_1}^{r_2}\frac{dr}{2\pi r L K} = \frac{1}{2\pi L K}\ln\frac{r_2}{r_1}

Key Point — radial conduction through a cylindrical shell: H=2πLK(T1T2)ln(r2r1)H = \frac{2\pi L K\left(T_1 - T_2\right)}{\ln\left(\frac{r_2}{r_1}\right)} The logarithm is the signature of cylindrical geometry, and it comes from drr\int\frac{dr}{r} and nowhere else. The temperature at any intermediate radius is T(r)=T1(T1T2)ln(rr1)ln(r2r1)T(r) = T_1 - \left(T_1-T_2\right)\frac{\ln\left(\frac{r}{r_1}\right)}{\ln\left(\frac{r_2}{r_1}\right)}

Read that profile carefully, because it contains a trap. Halfway in radius is not halfway in temperature. For lagging running from 5.0 cm to 10.0 cm with faces at 120°C and 30°C, the radius 7.5 cm sits at 67.4°C, not 75°C. Most of the temperature drop happens in the inner shells, where the area is small and the resistance per unit thickness is large.

The doubling trap. Because the answer depends on lnr2r1\ln\frac{r_2}{r_1}, doubling the thickness of the lagging does not halve the loss. Going from r2=2r1r_2 = 2r_1 to r2=3r1r_2 = 3r_1 changes the heat loss by a factor ln2ln3=0.631\frac{\ln 2}{\ln 3} = 0.631 — a 37% saving for a doubling of the lagging material. Insulation has diminishing returns, and the logarithm is why.

The spherical shell

Same method, different area law. A shell at radius rr has area 4πr24\pi r^2:

Rth=r1r2dr4πr2K=14πK[1r11r2]=r2r14πKr1r2R_{th} = \int_{r_1}^{r_2}\frac{dr}{4\pi r^{2}K} = \frac{1}{4\pi K}\left[\frac{1}{r_1}-\frac{1}{r_2}\right] = \frac{r_2-r_1}{4\pi K r_1 r_2}

Key Point — radial conduction through a spherical shell: H=4πKr1r2(T1T2)r2r1H = \frac{4\pi K r_1 r_2\left(T_1-T_2\right)}{r_2-r_1} Here the effective area is 4πr1r24\pi r_1 r_2 — the geometric mean of the inner and outer surface areas, exactly as it was for the tapered rod, and for exactly the same reason: the integrand went as 1r2\frac{1}{r^2}. The profile is T(r)=T1(T1T2)1r11r1r11r2T(r) = T_1 - \left(T_1-T_2\right)\dfrac{\frac{1}{r_1}-\frac{1}{r}}{\frac{1}{r_1}-\frac{1}{r_2}}.

The family, in one table

Geometry Area crossed Resistance Effective area
slab, thickness LL AA, constant LKA\dfrac{L}{KA} AA
tapered rod, radii r1r_1, r2r_2 πr(x)2\pi r(x)^2 LKπr1r2\dfrac{L}{K\pi r_1r_2} πr1r2\pi r_1 r_2
cylindrical shell, length LL 2πrL2\pi rL ln(r2r1)2πLK\dfrac{\ln\left(\frac{r_2}{r_1}\right)}{2\pi LK} logarithmic mean
spherical shell 4πr24\pi r^2 r2r14πKr1r2\dfrac{r_2-r_1}{4\pi Kr_1r_2} 4πr1r24\pi r_1 r_2

Every row is the same integral drKA(r)\int \frac{dr}{KA(r)} with a different A(r)A(r).

[Exam Tip] How to tell instantly which one you are in. If the two faces are flat and parallel, it is a slab. If they are two circles of different radii about a common axis, it is cylindrical and you will get a logarithm. If they are two spheres about a common centre, you will get 1r11r2\frac{1}{r_1}-\frac{1}{r_2}. Getting a logarithm out of a spherical problem, or a 1r\frac{1}{r} difference out of a cylindrical one, is a sign you integrated the wrong area law — check before you substitute numbers.

Networks, Junction Temperatures, and the Growing Ice Sheet

The whole method for a network, in one sentence

In the steady state the heat current into every junction equals the heat current out of it. That is it. Write that equation at each junction and you have as many equations as unknown junction temperatures.

It is worth naming what this is: an exact analogue of Kirchhoff's current law, with ΔT\Delta T playing the part of voltage, HH the part of current, and R=LKAR = \frac{L}{KA} the part of resistance. Series resistances add; parallel ones combine as reciprocals. In a JEE question you will almost always be faster writing thermal resistances than quoting an equivalent-conductivity formula, because the resistance route never asks you to remember whether the rods were in series or in parallel — the circuit tells you.

Two rods in series, and where the junction sits

Two rods of the same cross-section AA and length LL, conductivities K1K_1 and K2K_2, joined end to end, free ends held at T1T_1 and T2T_2. Equal current through both:

T1TjR1=TjT2R2Tj=T1R1+T2R21R1+1R2=K1T1+K2T2K1+K2\frac{T_1 - T_j}{R_1} = \frac{T_j - T_2}{R_2} \qquad\Longrightarrow\qquad T_j = \frac{\frac{T_1}{R_1} + \frac{T_2}{R_2}}{\frac{1}{R_1}+\frac{1}{R_2}} = \frac{K_1T_1 + K_2T_2}{K_1+K_2}

(the last step only when the two rods share LL and AA).

Key Point: The junction temperature is a conductance-weighted average of the two end temperatures. The better conductor pulls the junction toward its own end. Copper against steel is 385 against 50.2, so the junction ends up within a dozen degrees of the copper end — which is exactly why a copper handle on a hot pan is a bad idea and a steel one is survivable.

And the equivalent conductivity of the pair, for equal lengths:

Kseries=2K1K2K1+K2,Kparallel=K1+K22K_{\text{series}} = \frac{2K_1K_2}{K_1+K_2}, \qquad K_{\text{parallel}} = \frac{K_1+K_2}{2}

The first is a harmonic mean and always sits closer to the smaller conductivity; the second is an arithmetic mean and always sits in the middle. If you cannot remember which is which, rebuild them from resistances in ten seconds rather than guessing.

A star of three rods

Three rods meet at a common junction, their other ends held at T1T_1, T2T_2 and T3T_3. There is one unknown, the junction temperature TT^{\,\star}, and one equation:

T1TR1+T2TR2+T3TR3=0T=TiRi1Ri\frac{T_1-T^{\,\star}}{R_1} + \frac{T_2-T^{\,\star}}{R_2} + \frac{T_3-T^{\,\star}}{R_3} = 0 \qquad\Longrightarrow\qquad T^{\,\star} = \frac{\sum \frac{T_i}{R_i}}{\sum \frac{1}{R_i}}

Write the currents all flowing in and set the sum to zero. Then a negative answer for one of them simply means that rod is carrying heat away, and no sign has to be guessed in advance. This one habit removes most of the sign errors in network questions.

The growth of ice on a pond

Now the famous one, and the only conduction problem in this section where something is changing with time.

Ice thickening on a pond with thickness against time curving as root t

A pond has frozen to depth yy. The air above is at θ-\theta (with θ\theta a positive number of degrees below zero), the water below is at 0°C, and the ice in between conducts. For a new layer of thickness dydy to freeze onto the underside, its latent heat must be carried up through the ice already there.

Heat released by freezing a layer dydy over an area AA: dQ=(ρAdy)LfdQ = \left(\rho A\,dy\right)L_f

Heat conducted up through the sheet in time dtdt, treating the sheet as a slab of thickness yy: dQ=KAθydtdQ = \frac{KA\theta}{y}\,dt

Two things deserve a moment. First, the temperature difference across the sheet is θ\theta, not θ\theta plus anything — the underside is pinned at 0°C because that is where ice and water coexist. Second, we are treating the conduction as quasi-steady: the sheet thickens so slowly compared with how fast it reaches its steady gradient that using the steady-state formula at each instant is an excellent approximation.

Equate and separate:

ρLfydy=Kθdty1y2ydy=KθρLf0tdt\rho L_f\,y\,dy = K\theta\,dt \qquad\Longrightarrow\qquad \int_{y_1}^{y_2} y\,dy = \frac{K\theta}{\rho L_f}\int_0^{t}dt

Key Point — time for ice to thicken: t=ρLf2Kθ(y22y12)t = \frac{\rho L_f}{2K\theta}\left(y_2^{2}-y_1^{2}\right) and starting from bare water, y1=0y_1 = 0, this is t=ρLfy22Kθt = \dfrac{\rho L_f\,y^{2}}{2K\theta}, so the thickness grows as the square root of time.

Three consequences, each of which has been an exam question:

  • Going from 5 cm to 10 cm takes three times as long as going from 0 to 5 cm, because 10252=7510^2 - 5^2 = 75 against 520=255^2 - 0 = 25. The ice sheet is its own insulator, and the thicker it gets the more slowly it grows. This is why deep lakes never freeze solid.
  • Doubling the thickness costs four times the total time, so a pond that froze to 10 cm in a day needs four days to reach 20 cm at the same air temperature.
  • The rate at any instant is dydt=KθρLfy\frac{dy}{dt} = \frac{K\theta}{\rho L_f y}, so if a question asks how fast the ice is thickening right now, differentiate rather than dividing the total thickness by the total time.

[Exam Tip] Use the ice density, about 900 kg/m3^3, not the water density. Some questions hand you 917 and some hand you 1000; use whatever the question states and say so in your solution. The answer scales directly with it, so a silently assumed 1000 against a stated 900 is an 11% error.

Multi-Phase Calorimetry, Radiation Exchange, and Newton's Law Honestly

When you do not know the final state

The calorimetry of Section 6 was straightforward because you were told what happened. At JEE level you are not. Mix steam with ice and any of these can be the answer:

  • everything ends as water between 0°C and 100°C;
  • everything pins at 0°C with ice and water coexisting;
  • everything pins at 100°C with water and steam coexisting;
  • rarely, it all ends as ice below 0°C.

Guessing wrong does not cost you a mark or two. It costs the whole question, because the equation you wrote was the wrong equation.

Key Point — the method that never fails: 1. Pick a reference state — 0°C water is convenient. 2. Compute the heat available from the hot side down to that reference, as a single number. 3. Compute the heat required by the cold side up to that reference, as a single number. 4. Compare them, and only then write the balance for the branch you are actually in. Do steps 2 and 3 as separate numbers on separate lines. The comparison is the physics; the arithmetic afterwards is bookkeeping.

The three tests, written out:

Compare Conclusion
available heat << heat needed to warm the ice to 0°C final state is ice below 0°C; not all the steam condenses
heat needed to warm the ice to 0°C << available << that plus miceLfm_{\text{ice}}L_f pins at 0°C, ice and water together; find how much ice melts
available >> that plus miceLfm_{\text{ice}}L_f all the ice melts; solve for a final temperature above 0°C, then check it came out below 100

And check the answer against its own branch. A final temperature of 115°C from a case you assumed ended as water means the assumption was wrong, not that water reached 115°C. A final temperature outside the branch you assumed is the equation telling you to go back to step 4.

Radiation exchange and the equilibrium temperature

A body of area AA, emissivity ee and absolute temperature TT in surroundings at TsT_s loses net power

Pnet=σAe(T4Ts4)P_{\text{net}} = \sigma A e\left(T^{4} - T_s^{4}\right)

Key Point — the kelvin rule, in the place it matters most: TT and TsT_s in that expression are absolute temperatures in kelvin, always. A body at 727°C radiates (1000500)4=16\left(\frac{1000}{500}\right)^4 = 16 times as much as one at 227°C. Feed the Celsius numbers in and you get (727227)4=105\left(\frac{727}{227}\right)^4 = 105, which is wrong by a factor of nearly seven. Write "K" next to every temperature you substitute into a fourth power.

Equilibrium in sunlight. A body absorbing sunlight settles at the temperature where absorption balances emission. For a sphere of radius rr in space, sunlight of flux SS falls on the cross-section πr2\pi r^2 but the body radiates from its whole surface 4πr24\pi r^2:

aSπr2=eσ(4πr2)T4T=(aS4eσ)1/4a\,S\,\pi r^{2} = e\,\sigma\left(4\pi r^{2}\right)T^{4} \qquad\Longrightarrow\qquad T = \left(\frac{a\,S}{4e\,\sigma}\right)^{1/4}

The radius cancels — a small satellite and a large one reach the same temperature. For a black body (a=ea = e) with S=1400S = 1400 W/m2^2 that gives T=280T = 280 K, a little above the freezing point of water, which is roughly why Earth's neighbourhood is habitable at all.

Key Point — why white paint works: the ratio ae\frac{a}{e} decides everything, and aa is the absorptivity for sunlight while ee is the emissivity in the infrared the body itself radiates. Kirchhoff's law says a good absorber is a good emitter at the same wavelength, so these need not be equal — sunlight peaks near 0.5 μ\mum and a 300 K body emits near 10 μ\mum. A surface with a=0.6a = 0.6 and e=0.9e = 0.9 runs at (0.60.9)1/4=0.904\left(\frac{0.6}{0.9}\right)^{1/4} = 0.904 times the black-body temperature, so 253 K instead of 280 K. That is a selective surface, and it is how spacecraft and solar water heaters are engineered.

Newton's law of cooling, and where it dies

Expand the Stefan-Boltzmann net loss for a body only slightly hotter than its surroundings. Put T=Ts+ΔT = T_s + \Delta:

T4Ts4=Ts4[(1+ΔTs)41]4Ts3Δwhen ΔTsT^4 - T_s^4 = T_s^4\left[\left(1+\frac{\Delta}{T_s}\right)^4 - 1\right] \approx 4T_s^{3}\Delta \qquad\text{when } \Delta \ll T_s

The fourth power has been linearised. With P=msdTdtP = ms\frac{dT}{dt} that gives

dTdt=k(TTs),k=4σAeTs3ms-\frac{dT}{dt} = k\left(T - T_s\right), \qquad k = \frac{4\sigma A e T_s^{3}}{ms}

and integrating,

Key Point — the exponential form: T=Ts+(T0Ts)ektT = T_s + \left(T_0 - T_s\right)e^{-kt} The excess temperature decays exponentially, so a graph of ln(TTs)\ln\left(T-T_s\right) against tt is a straight line of slope k-k. The excess takes the same time to halve whatever it starts from, exactly like radioactive decay.

Now the honesty. The linearisation dropped terms of order (ΔTs)2\left(\frac{\Delta}{T_s}\right)^2, so:

Body at Surroundings at 20°C Newton's prediction as a fraction of the true net loss
25°C 293 K 0.975
40°C 293 K 0.903
200°C 293 K 0.424

At a 180 K excess Newton's law under-predicts the loss by well over half. Any question that quotes a body at a few hundred degrees and asks you to "use Newton's law" is asking for an approximation, and saying so in one line is worth a mark.

There is a second, quieter limitation, and examiners like it: the derivation above assumed radiation only. Real cooling in air also involves convection, and forced convection follows a genuinely linear law of its own. Newton's law is therefore often a better description of a real object in a draught than the derivation would suggest — for the wrong reason.

The average-temperature shortcut, measured

The familiar school form T1T2t=k(T1+T22Ts)\frac{T_1-T_2}{t} = k\left(\frac{T_1+T_2}{2} - T_s\right) is a trapezoidal approximation to the exponential. How good is it? Take a body cooling from 80°C to 64°C in 5 minutes in surroundings at 24°C.

  • The exact fit gives k=0.0673k = 0.0673 min1^{-1}; the average form gives k=0.0667k = 0.0667 min1^{-1}, 0.93% low.
  • Stepping forward in 5-minute intervals, the same size as the interval it was fitted on, the average form reproduces the exponential to the last decimal place. That is not luck: fitting on one interval forces the ratio of successive excesses to be right, and that ratio is all the exponential is.
  • Taking one 15-minute step instead gives 42.7°C where the exponential gives 44.4°C — 1.7°C out, because the shortcut assumes the cooling rate is constant across the whole step.

Key Point: The average-temperature form is safe when the interval is short and the excess changes by only a modest fraction across it. Never use it across an interval over which the excess more than halves, and never mix a kk obtained from the average form into the exponential formula.

The three traps, collected

Trap 1 — Celsius in a fourth power. Already stated, and worth stating again because it is the single commonest wrong answer in this chapter. T4T^4, λmT=b\lambda_m T = b, T2T1\frac{T_2}{T_1} and PV=nRTPV = nRT all demand kelvin. Only ΔT\Delta T may be quoted in either.

Trap 2 — forgetting that a hole expands. Heat a plate with a hole in it and the hole gets bigger, at exactly the same fractional rate as everything else. The material does not creep inward. A disc that fits its hole exactly at 20°C still fits it exactly at 220°C, because both scale by the same factor (1+αΔT)\left(1+\alpha\Delta T\right). Every cavity, bore, ring and gap in this chapter obeys the same rule.

Trap 3 — treating Newton's law as exact. It is a linearisation with a stated range of validity. Use it for a body a few tens of degrees above its surroundings; flag it when the excess is large. Writing "valid because the excess is small compared with TsT_s" costs one line and earns the mark that separates a correct solution from a lucky one.

Solved Examples, Part 1: Expansion at JEE Level

Values used throughout, unless a problem says otherwise: αsteel=1.2×105\alpha_{\text{steel}} = 1.2\times10^{-5} K1^{-1}, αbrass=1.8×105\alpha_{\text{brass}} = 1.8\times10^{-5} K1^{-1}, γmercury=1.82×104\gamma_{\text{mercury}} = 1.82\times10^{-4} K1^{-1}. Every constant is restated inside the solution that uses it.

Example 1: The gap that will not close

A steel rod and a brass rod are laid side by side with their left ends level. The difference in their lengths is to be 10.0 cm at every temperature. Find the length of each rod, and then find the effective coefficient of linear expansion of the composite rod formed by joining those same two pieces end to end. Take αsteel=1.2×105\alpha_{\text{steel}} = 1.2\times10^{-5} K1^{-1} and αbrass=1.8×105\alpha_{\text{brass}} = 1.8\times10^{-5} K1^{-1}.

Solution:

  1. Write the difference at a general temperature. With L1L_1 steel and L2L_2 brass, Δ=L1(1+α1ΔT)L2(1+α2ΔT)=(L1L2)+(L1α1L2α2)ΔT\Delta = L_1\left(1+\alpha_1\Delta T\right) - L_2\left(1+\alpha_2\Delta T\right) = \left(L_1-L_2\right) + \left(L_1\alpha_1 - L_2\alpha_2\right)\Delta T

  2. Kill the temperature-dependent term. For Δ\Delta to be the same at every temperature the bracket must vanish: L1α1=L2α2L1L2=α2α1=1.8×1051.2×105=1.5L_1\alpha_1 = L_2\alpha_2 \qquad\Longrightarrow\qquad \frac{L_1}{L_2} = \frac{\alpha_2}{\alpha_1} = \frac{1.8\times10^{-5}}{1.2\times10^{-5}} = 1.5 So the steel rod, with the smaller α\alpha, is the longer one.

  3. Use the given difference. With L1=1.5L2L_1 = 1.5L_2 and L1L2=0.100L_1 - L_2 = 0.100 m: 0.5L2=0.100L2=0.200 m,L1=0.300 m0.5\,L_2 = 0.100 \qquad\Longrightarrow\qquad L_2 = 0.200\ \text{m}, \quad L_1 = 0.300\ \text{m}

  4. Check the physical meaning. Over a 200 K rise the steel grows by (0.300)(1.2×105)(200)=7.2×104\left(0.300\right)\left(1.2\times10^{-5}\right)\left(200\right) = 7.2\times10^{-4} m and the brass by (0.200)(1.8×105)(200)=7.2×104\left(0.200\right)\left(1.8\times10^{-5}\right)\left(200\right) = 7.2\times10^{-4} m. Identical. The gap is frozen because both ends advance by the same amount.

  5. Now join them end to end into a rod of total length 0.500 m. Over ΔT\Delta T the total elongation is the sum of the two: αeff=L1α1+L2α2L1+L2=(0.300)(1.2×105)+(0.200)(1.8×105)0.500\alpha_{\text{eff}} = \frac{L_1\alpha_1 + L_2\alpha_2}{L_1+L_2} = \frac{\left(0.300\right)\left(1.2\times10^{-5}\right)+\left(0.200\right)\left(1.8\times10^{-5}\right)}{0.500} αeff=3.6×106+3.6×1060.500=1.44×105 K1\alpha_{\text{eff}} = \frac{3.6\times10^{-6}+3.6\times10^{-6}}{0.500} = 1.44\times10^{-5}\ \text{K}^{-1}

Final Answer: Steel 0.300 m, brass 0.200 m; the composite rod has αeff=1.44×105\alpha_{\text{eff}} = 1.44\times10^{-5} K1^{-1}, and over a 100 K rise it lengthens by 0.72 mm.

Takeaway: The plain average of the two coefficients is 1.5×1051.5\times10^{-5} K1^{-1}, which is not the answer — the steel piece is longer, so its smaller α\alpha carries more weight. And note the sanity check in step 4: whenever the frozen-gap condition holds, the two absolute elongations are equal. If yours are not, you have the ratio upside down.

Example 2: A clock that runs slow in summer

A pendulum clock with a steel pendulum keeps correct time at 20°C. Take αsteel=1.2×105\alpha_{\text{steel}} = 1.2\times10^{-5} K1^{-1}. (a) How many seconds does it lose per day at 40°C? (b) How many does it gain per day at 0°C? (c) A second, identical clock is found to lose 12.0 s per day when the room is at 40°C. At what temperature does it keep correct time?

Solution:

  1. Set up the fractional change. The period is Tp=2πLgT_p = 2\pi\sqrt{\frac{L}{g}}, so TpTp=LL=1+αΔT1+12αΔT\frac{T_p^{\,\prime}}{T_p} = \sqrt{\frac{L^{\,\prime}}{L}} = \sqrt{1+\alpha\Delta T} \approx 1+\frac{1}{2}\alpha\Delta T The binomial step is safe here because αΔT104\alpha\Delta T \sim 10^{-4}.

  2. Turn it into seconds per day. A longer period means fewer swings counted, so the clock loses Δt=12αΔT×86400 s=43200αΔT\left\lvert \Delta t \right\rvert = \frac{1}{2}\alpha\,\Delta T \times 86400\ \text{s} = 43200\,\alpha\,\Delta T

  3. (a) At 40°C, ΔT=+20\Delta T = +20 K: Δt=(43200)(1.2×105)(20)=10.4 s per day, LOST\left\lvert \Delta t \right\rvert = \left(43200\right)\left(1.2\times10^{-5}\right)\left(20\right) = 10.4\ \text{s per day, LOST}

  4. (b) At 0°C, ΔT=20\Delta T = -20 K. The magnitude is the same, 10.4 s, but the pendulum is now shorter, the period smaller, and the clock GAINS 10.4 s per day.

  5. (c) Invert the formula. The clock loses 12.0 s, so it is above its correct-time temperature by ΔT=12.0(43200)(1.2×105)=12.00.5184=23.1 K\Delta T = \frac{12.0}{\left(43200\right)\left(1.2\times10^{-5}\right)} = \frac{12.0}{0.5184} = 23.1\ \text{K} tcorrect=40.023.1=16.9 °Ct_{\text{correct}} = 40.0 - 23.1 = 16.9\ \text{°C}

Final Answer: (a) loses 10.4 s per day; (b) gains 10.4 s per day; (c) the second clock keeps correct time at about 16.9°C.

Takeaway: The rate is 43200α43200\,\alpha seconds per day per kelvin, which for steel is 0.518 s per day per kelvin. Carry that number and part (a) is one multiplication. And notice that (b) has the same magnitude as (a) — the daily error is linear in ΔT\Delta T, so equal departures either side of the calibration temperature give equal and opposite errors. That linearity is what makes part (c) solvable from a single reading.

Example 3: The weight thermometer

A glass bulb is completely filled with 100.0 g of mercury at 0°C. It is heated to 100.0°C and the mercury that spills out is collected and weighed. Take γmercury=1.82×104\gamma_{\text{mercury}} = 1.82\times10^{-4} K1^{-1} and αglass=9.0×106\alpha_{\text{glass}} = 9.0\times10^{-6} K1^{-1}. Find the coefficient of apparent expansion and the mass of mercury expelled.

Solution:

  1. The vessel's volume coefficient. For an isotropic solid γ=3α\gamma = 3\alpha: γglass=3(9.0×106)=2.7×105 K1\gamma_{\text{glass}} = 3\left(9.0\times10^{-6}\right) = 2.7\times10^{-5}\ \text{K}^{-1}

  2. Apparent coefficient. γapp=γrealγvessel=1.82×1042.7×105=1.55×104 K1\gamma_{\text{app}} = \gamma_{\text{real}} - \gamma_{\text{vessel}} = 1.82\times10^{-4} - 2.7\times10^{-5} = 1.55\times10^{-4}\ \text{K}^{-1}

  3. Volume expelled. Let the bulb hold V0V_0 at 0°C. The mercury wants V0(1+γrt)V_0\left(1+\gamma_r t\right), the bulb offers V0(1+γgt)V_0\left(1+\gamma_g t\right), so the overflow, measured hot, is ΔV=V0(γrγg)t=V0γappt\Delta V = V_0\left(\gamma_r - \gamma_g\right)t = V_0\,\gamma_{\text{app}}\,t

  4. Convert volume to mass — and this is where the marks are. That overflow is hot mercury, whose density has fallen to ρt=ρ01+γrt\rho_t = \frac{\rho_0}{1+\gamma_r t}. So m=ρtΔV=ρ01+γrtV0γappt=mγappt1+γrtm^{\,\prime} = \rho_t\,\Delta V = \frac{\rho_0}{1+\gamma_r t}\cdot V_0\gamma_{\text{app}}t = \frac{m\,\gamma_{\text{app}}\,t}{1+\gamma_r t}

  5. Substitute m=100.0m = 100.0 g, t=100.0t = 100.0°C: m=(100.0)(1.55×104)(100.0)1+(1.82×104)(100.0)=1.5501.0182=1.522 gm^{\,\prime} = \frac{\left(100.0\right)\left(1.55\times10^{-4}\right)\left(100.0\right)}{1+\left(1.82\times10^{-4}\right)\left(100.0\right)} = \frac{1.550}{1.0182} = 1.522\ \text{g}

  6. Cross-check by going backwards. With 1.522 g gone, 98.478 g remain, and m(mm)t=1.522(98.478)(100.0)=1.546×104 K1\frac{m^{\,\prime}}{\left(m-m^{\,\prime}\right)t} = \frac{1.522}{\left(98.478\right)\left(100.0\right)} = 1.546\times10^{-4}\ \text{K}^{-1} That is step 2's 1.55×1041.55\times10^{-4} divided by 1+γgt=1.00271+\gamma_g t = 1.0027, so the remaining-mass form is short by 0.27% — precisely the glass expansion it has no way of seeing. Multiply back by 1.0027 and step 2 returns.

Final Answer: γapp=1.55×104\gamma_{\text{app}} = 1.55\times10^{-4} K1^{-1}, and 1.52 g of mercury is expelled.

Takeaway: The naive answer mγappt=1.55m\gamma_{\text{app}}t = 1.55 g is 1.8% high, and the missing 1.8%1.8\% is exactly γrt\gamma_r t — the density drop of the hot mercury. Whenever a question converts an expanded volume into a mass, ask at what temperature that mass is being weighed. And read step 6 carefully: the mass-remaining form is not an identity, it is short by the vessel's own 1+γgt1+\gamma_g t — only 0.27% here, but it is there.

Example 4: How tightly does a bimetallic strip curl?

A bimetallic strip is made of an iron strip and a brass strip bonded face to face, each 0.20 mm thick, the pair being 10.0 cm long and straight at 20°C. It is heated to 120°C. Take αiron=1.2×105\alpha_{\text{iron}} = 1.2\times10^{-5} K1^{-1} and αbrass=1.8×105\alpha_{\text{brass}} = 1.8\times10^{-5} K1^{-1}. Find the radius of curvature of the strip and, if it is clamped at one end, the sideways deflection of its free tip.

Solution:

  1. Which way does it bend? Brass has the larger α\alpha, so brass must occupy the longer arc: brass on the outside, iron on the inside.

  2. Both mid-lines turn through the same angle. With t=0.20t = 0.20 mm =2.0×104= 2.0\times10^{-4} m the thickness of each strip, the mid-lines sit at R±t2R \pm \frac{t}{2}, and their lengths are the free-expansion lengths: L(1+α1ΔT)=(Rt2)θ,L(1+α2ΔT)=(R+t2)θL\left(1+\alpha_1\Delta T\right) = \left(R-\tfrac{t}{2}\right)\theta, \qquad L\left(1+\alpha_2\Delta T\right) = \left(R+\tfrac{t}{2}\right)\theta

  3. Divide, then use componendo and dividendo: (α2α1)ΔT2+(α1+α2)ΔT=t2R\frac{\left(\alpha_2-\alpha_1\right)\Delta T}{2+\left(\alpha_1+\alpha_2\right)\Delta T} = \frac{t}{2R}

  4. Substitute ΔT=100\Delta T = 100 K, α2α1=6.0×106\alpha_2-\alpha_1 = 6.0\times10^{-6} K1^{-1}, α1+α2=3.0×105\alpha_1+\alpha_2 = 3.0\times10^{-5} K1^{-1}: R=t[2+(3.0×105)(100)]2(6.0×106)(100)=(2.0×104)(2.003)1.2×103=0.334 mR = \frac{t\left[2 + \left(3.0\times10^{-5}\right)\left(100\right)\right]}{2\left(6.0\times10^{-6}\right)\left(100\right)} = \frac{\left(2.0\times10^{-4}\right)\left(2.003\right)}{1.2\times10^{-3}} = 0.334\ \text{m}

  5. Compare with the standard approximation. Rt(α2α1)ΔT=2.0×104(6.0×106)(100)=0.333 mR \approx \frac{t}{\left(\alpha_2-\alpha_1\right)\Delta T} = \frac{2.0\times10^{-4}}{\left(6.0\times10^{-6}\right)\left(100\right)} = 0.333\ \text{m} The approximation is 0.15% low — the dropped term was (α1+α2)ΔT=3×103\left(\alpha_1+\alpha_2\right)\Delta T = 3\times10^{-3}, and half of that is exactly the discrepancy.

  6. The tip deflection. The strip is an arc of length L=0.100L = 0.100 m on a circle of radius 0.334 m, so it turns through θ=LR=0.2996\theta = \frac{L}{R} = 0.2996 rad, and the tip moves sideways by δ=R(1cosθ)=(0.334)(10.9555)=1.49×102 m=1.49 cm\delta = R\left(1-\cos\theta\right) = \left(0.334\right)\left(1-0.9555\right) = 1.49\times10^{-2}\ \text{m} = 1.49\ \text{cm} The small-angle form L22R=0.01000.668=1.50\frac{L^2}{2R} = \frac{0.0100}{0.668} = 1.50 cm agrees to within a percent.

Final Answer: R=0.334R = 0.334 m, and the free tip deflects about 1.49 cm.

Takeaway: A 100 K rise turns a 10 cm strip 0.2 mm thick into an arc of radius one third of a metre and swings its tip a centimetre and a half. That is a huge, easily detected mechanical movement from a temperature change, which is why bimetallic strips run thermostats, circuit breakers and old-fashioned car indicators. Halve the thickness of each strip and you halve RR and double the deflection.

Example 5: A rod that gets fatter as it goes

A copper rod 0.50 m long tapers uniformly from a radius of 2.0 cm at one end to 4.0 cm at the other. Its curved surface is perfectly lagged. The narrow end is held at 100°C and the wide end at 0°C. Take Kcopper=385K_{\text{copper}} = 385 W/(m K). Find the rate of heat flow and the temperature at the mid-point of the rod.

Solution:

  1. Why the slab formula is unusable. There is no single area AA: the cross-section runs from π(0.020)2\pi\left(0.020\right)^2 to π(0.040)2\pi\left(0.040\right)^2, a factor of four. Slice and integrate instead.

  2. Set up the radius profile. With xx measured from the narrow end, r(x)=r1+(r2r1)xL=0.020+(0.020)x0.50r(x) = r_1 + \frac{\left(r_2-r_1\right)x}{L} = 0.020 + \frac{\left(0.020\right)x}{0.50}

  3. Resistance of a slice, then the total: dR=dxKπr(x)2Rth=0LdxKπr(x)2=LKπ(r2r1)[1r11r2]=LKπr1r2dR = \frac{dx}{K\pi r(x)^2} \quad\Longrightarrow\quad R_{th} = \int_0^{L}\frac{dx}{K\pi r(x)^2} = \frac{L}{K\pi\left(r_2-r_1\right)}\left[\frac{1}{r_1}-\frac{1}{r_2}\right] = \frac{L}{K\pi r_1r_2}

  4. Substitute: Rth=0.50(385)π(0.020)(0.040)=0.500.9676=0.5168 K/WR_{th} = \frac{0.50}{\left(385\right)\pi\left(0.020\right)\left(0.040\right)} = \frac{0.50}{0.9676} = 0.5168\ \text{K/W} H=ΔTRth=1000.5168=194 WH = \frac{\Delta T}{R_{th}} = \frac{100}{0.5168} = 194\ \text{W}

  5. The mid-point temperature. At x=0.25x = 0.25 m the radius is 0.030 m. Integrate the resistance only that far: R0L/2=1Kπ(r2r1L)[1r11r(L/2)]=0.50(385)π(0.020)[50.033.33]R_{0\to L/2} = \frac{1}{K\pi\left(\frac{r_2-r_1}{L}\right)}\left[\frac{1}{r_1}-\frac{1}{r(L/2)}\right] = \frac{0.50}{\left(385\right)\pi\left(0.020\right)}\left[50.0-33.33\right] R0L/2=(0.02067)(16.67)=0.3446 K/WR_{0\to L/2} = \left(0.02067\right)\left(16.67\right) = 0.3446\ \text{K/W} Tmid=100HR0L/2=100(193.5)(0.3446)=33.3 °CT_{\text{mid}} = 100 - H\,R_{0\to L/2} = 100 - \left(193.5\right)\left(0.3446\right) = 33.3\ \text{°C}

Final Answer: H=194H = 194 W, and the mid-point of the rod is at 33.3°C.

Takeaway: Two results worth carrying. The effective area is πr1r2\pi r_1r_2, the geometric mean A1A2\sqrt{A_1A_2} — the arithmetic mean would have given π(0.0316)2\pi\left(0.0316\right)^2 and a heat current of 242 W, 25% too high. And the mid-point is at 33.3°C, not 50°C: two thirds of the temperature drop happens in the narrow half, because that is where two thirds of the resistance lives.

Example 6: A rod whose material changes as you walk along it

A rod of uniform cross-section 1.0 cm2^2 and length 1.0 m is made so that its thermal conductivity varies linearly along it, K(x)=K0(1+xL)K(x) = K_0\left(1+\frac{x}{L}\right) with K0=100K_0 = 100 W/(m K). The sides are lagged, the x=0x=0 end is at 100°C and the x=Lx=L end at 0°C. Find the rate of heat flow, the equivalent conductivity of the rod, and the temperature at its mid-point.

Solution:

  1. Slice and add resistances. The area is constant at A=1.0×104A = 1.0\times10^{-4} m2^2, so only KK varies: Rth=0LdxK0(1+xL)A=LK0A[ln(1+xL)]0L=Lln2K0AR_{th} = \int_0^{L}\frac{dx}{K_0\left(1+\frac{x}{L}\right)A} = \frac{L}{K_0A}\Big[\ln\left(1+\tfrac{x}{L}\right)\Big]_0^{L} = \frac{L\ln 2}{K_0A}

  2. Substitute: Rth=(1.0)(0.6931)(100)(1.0×104)=0.69311.0×102=69.31 K/WR_{th} = \frac{\left(1.0\right)\left(0.6931\right)}{\left(100\right)\left(1.0\times10^{-4}\right)} = \frac{0.6931}{1.0\times10^{-2}} = 69.31\ \text{K/W} H=10069.31=1.44 WH = \frac{100}{69.31} = 1.44\ \text{W}

  3. Equivalent conductivity. Define it by H=KeqAΔTLH = \frac{K_{\text{eq}}A\Delta T}{L}: Keq=HLAΔT=(1.443)(1.0)(1.0×104)(100)=144 W/(m K)K_{\text{eq}} = \frac{HL}{A\,\Delta T} = \frac{\left(1.443\right)\left(1.0\right)}{\left(1.0\times10^{-4}\right)\left(100\right)} = 144\ \text{W/(m K)} which is exactly K0ln2=1000.6931\frac{K_0}{\ln 2} = \frac{100}{0.6931}.

  4. Mid-point temperature. Integrate only to x=0.5x = 0.5 m: R0L/2=Lln(1.5)K0A=(1.0)(0.4055)1.0×102=40.55 K/WR_{0\to L/2} = \frac{L\ln\left(1.5\right)}{K_0A} = \frac{\left(1.0\right)\left(0.4055\right)}{1.0\times10^{-2}} = 40.55\ \text{K/W} Tmid=100(1.4427)(40.55)=10058.5=41.5 °CT_{\text{mid}} = 100 - \left(1.4427\right)\left(40.55\right) = 100 - 58.5 = 41.5\ \text{°C}

Final Answer: H=1.44H = 1.44 W, Keq=144K_{\text{eq}} = 144 W/(m K), and the mid-point is at 41.5°C.

Takeaway: The conductivity runs from 100 to 200 W/(m K), so the tempting answer for KeqK_{\text{eq}} is the average, 150. The truth is K0ln2=144\frac{K_0}{\ln 2} = 144, and it is below the average because this is a series arrangement and series resistance is dominated by the worst conductor. In series, always expect an answer nearer the smaller conductivity; in parallel, nearer the larger.

Solved Examples, Part 2: Radial Flow, Networks, Mixtures and Radiation

Values used throughout, unless a problem says otherwise: Lf=3.33×105L_f = 3.33\times10^{5} J/kg, Lv=22.6×105L_v = 22.6\times10^{5} J/kg, swater=4186s_{\text{water}} = 4186 J/(kg K), sice=2100s_{\text{ice}} = 2100 J/(kg K), σ=5.67×108\sigma = 5.67\times10^{-8} W/(m2^2 K4^4), Kice=1.6K_{\text{ice}} = 1.6 W/(m K), density of ice 900 kg/m3^3.

Example 7: Lagging a steam pipe, and a shell of ice

(a) A steam pipe of outer radius 5.0 cm carries steam at 120°C. It is lagged to an outer radius of 10.0 cm with material of conductivity 0.050 W/(m K), and the outside of the lagging is at 30°C. Find the heat lost per metre of pipe, and the temperature midway through the lagging at a radius of 7.5 cm. (b) A spherical container has inner radius 10.0 cm and outer radius 12.0 cm, walls of conductivity 0.080 W/(m K), and holds an ice-water mixture at 0°C. Its outer surface is at 25°C. Find the rate at which heat enters and the mass of ice melted per hour. Take Lf=3.33×105L_f = 3.33\times10^{5} J/kg.

Solution to (a):

  1. Take a shell of radius rr and thickness drdr on a length LL of pipe. Its area is 2πrL2\pi rL, so dR=dr2πrLKRth=12πLKlnr2r1dR = \frac{dr}{2\pi r L K} \quad\Longrightarrow\quad R_{th} = \frac{1}{2\pi LK}\ln\frac{r_2}{r_1}

  2. Per metre, put L=1.0L = 1.0 m: Rth=ln(0.1000.050)2π(1.0)(0.050)=0.69310.3142=2.206 K/W per metreR_{th} = \frac{\ln\left(\frac{0.100}{0.050}\right)}{2\pi\left(1.0\right)\left(0.050\right)} = \frac{0.6931}{0.3142} = 2.206\ \text{K/W per metre} H=120302.206=40.8 W per metreH = \frac{120-30}{2.206} = 40.8\ \text{W per metre}

  3. The temperature at 7.5 cm. Resistance from r1r_1 out to 0.075 m: Rr1r=ln(1.5)0.3142=0.40550.3142=1.291 K/WR_{r_1\to r} = \frac{\ln\left(1.5\right)}{0.3142} = \frac{0.4055}{0.3142} = 1.291\ \text{K/W} T=120(40.79)(1.291)=12052.7=67.3 °CT = 120 - \left(40.79\right)\left(1.291\right) = 120 - 52.7 = 67.3\ \text{°C}

Solution to (b):

  1. Same method, spherical area. A shell at radius rr has area 4πr24\pi r^2: Rth=r1r2dr4πr2K=r2r14πKr1r2=0.0204π(0.080)(0.100)(0.120)=0.0200.012064=1.658 K/WR_{th} = \int_{r_1}^{r_2}\frac{dr}{4\pi r^2K} = \frac{r_2-r_1}{4\pi Kr_1r_2} = \frac{0.020}{4\pi\left(0.080\right)\left(0.100\right)\left(0.120\right)} = \frac{0.020}{0.012064} = 1.658\ \text{K/W}

  2. Heat current inward: H=2501.658=15.1 WH = \frac{25-0}{1.658} = 15.1\ \text{W}

  3. Ice melted per hour. In 3600 s the heat delivered is (15.08)(3600)=5.43×104\left(15.08\right)\left(3600\right) = 5.43\times10^{4} J, so m=5.43×1043.33×105=0.163 kg=163 g per hourm = \frac{5.43\times10^{4}}{3.33\times10^{5}} = 0.163\ \text{kg} = 163\ \text{g per hour}

Final Answer: (a) 40.8 W per metre, with the mid-radius at 67.3°C. (b) 15.1 W inward, melting 163 g of ice per hour.

Takeaway: Two traps in one example. In (a), 7.5 cm is halfway in radius but the temperature there is 67.3°C, not 75°C — the inner shells are small and resistive, so they take most of the drop. And if you had treated the lagging as a slab of thickness 5.0 cm with the mean area 2π(0.075)(1.0)2\pi\left(0.075\right)\left(1.0\right), you would have found 42.4 W per metre, about 4% high. That error is small here only because the radius ratio is 2. The slab-with-mean-area estimate exceeds the true radial answer by the factor (r1+r2)ln(r2r1)2(r2r1)\frac{\left(r_1+r_2\right)\ln\left(\frac{r_2}{r_1}\right)}{2\left(r_2-r_1\right)}, which is 1.040 at a ratio of 2 but 1.207 at a ratio of 5: at a radius ratio of 5 the slab answer is about 21% higher than the correct radial one.

Example 8: How long does the pond take to freeze deeper?

A pond is covered with ice 5.0 cm thick. The air above stays at 10-10°C and the water below at 0°C. Take Kice=1.6K_{\text{ice}} = 1.6 W/(m K), the density of ice as 900 kg/m3^3 and Lf=3.33×105L_f = 3.33\times10^{5} J/kg. How long does the ice take to thicken to 10.0 cm? How does that compare with the time it took to form the first 5.0 cm?

Solution:

  1. What has to happen for the sheet to thicken by dydy. A layer of thickness dydy and area AA must freeze on the underside, releasing dQ=(ρAdy)LfdQ = \left(\rho A\,dy\right)L_f

  2. Where that heat goes. It is conducted up through the ice already present, of thickness yy, across a temperature difference of 10 K (the underside is pinned at 0°C, the top is at 10-10°C): dQ=KAθydtwith θ=10 KdQ = \frac{KA\theta}{y}\,dt \qquad\text{with }\theta = 10\ \text{K}

  3. Equate and separate the variables: ρLfydy=Kθdtt=ρLf2Kθ(y22y12)\rho L_f\,y\,dy = K\theta\,dt \qquad\Longrightarrow\qquad t = \frac{\rho L_f}{2K\theta}\left(y_2^{2}-y_1^{2}\right)

  4. Substitute y1=0.050y_1 = 0.050 m, y2=0.100y_2 = 0.100 m: t=(900)(3.33×105)2(1.6)(10)(0.01000.0025)=2.997×10832(7.5×103)t = \frac{\left(900\right)\left(3.33\times10^{5}\right)}{2\left(1.6\right)\left(10\right)}\left(0.0100-0.0025\right) = \frac{2.997\times10^{8}}{32}\left(7.5\times10^{-3}\right) t=7.02×104 s=19.5 hourst = 7.02\times10^{4}\ \text{s} = 19.5\ \text{hours}

  5. And the first 5.0 cm, from y1=0y_1 = 0: t1=(2.997×108)(2.5×103)32=2.34×104 s=6.50 hourst_1 = \frac{\left(2.997\times10^{8}\right)\left(2.5\times10^{-3}\right)}{32} = 2.34\times10^{4}\ \text{s} = 6.50\ \text{hours}

  6. The ratio. 19.56.50=3.00\frac{19.5}{6.50} = 3.00, which is just 1025252=7525\frac{10^2-5^2}{5^2} = \frac{75}{25}.

Final Answer: 19.5 hours to go from 5.0 cm to 10.0 cm, three times the 6.50 hours the first 5.0 cm took.

Takeaway: ty2t \propto y^2, so the second centimetre always takes longer than the first. The ice sheet is its own insulator: as it thickens, the temperature gradient driving the heat away falls, and the freezing slows. That is why a deep lake never freezes solid however long the winter — and it is also why the answer to "how long to double the thickness?" is always "four times the time so far", regardless of the numbers.

Example 9: Three ways to build a network

Rods of cross-section 2.0 cm2^2 and length 0.20 m are available in copper, K=385K = 385 W/(m K), and steel, K=50.2K = 50.2 W/(m K). All rods are lagged along their sides. (a) One copper rod and one steel rod are joined end to end, the free copper end held at 100°C and the free steel end at 0°C. Find the heat current and the junction temperature. (b) A second identical steel rod is now added in parallel with the first. Find the new junction temperature. (c) Separately, three rods of the same length 0.50 m and cross-section 1.0 cm2^2, with conductivities KK, 2K2K and 3K3K where K=50K = 50 W/(m K), are joined at a common point, their far ends held at 100°C, 50°C and 0°C. Find the junction temperature and the heat current in each rod.

Solution to (a):

  1. Write the two resistances, R=LKAR = \frac{L}{KA} with A=2.0×104A = 2.0\times10^{-4} m2^2: RCu=0.20(385)(2.0×104)=2.60 K/W,RSt=0.20(50.2)(2.0×104)=19.92 K/WR_{\text{Cu}} = \frac{0.20}{\left(385\right)\left(2.0\times10^{-4}\right)} = 2.60\ \text{K/W}, \qquad R_{\text{St}} = \frac{0.20}{\left(50.2\right)\left(2.0\times10^{-4}\right)} = 19.92\ \text{K/W}

  2. They are in series, so H=10002.60+19.92=10022.52=4.44 WH = \frac{100-0}{2.60+19.92} = \frac{100}{22.52} = 4.44\ \text{W}

  3. Junction temperature, from the drop across the copper alone: Tj=100HRCu=100(4.441)(2.597)=88.5 °CT_j = 100 - H\,R_{\text{Cu}} = 100 - \left(4.441\right)\left(2.597\right) = 88.5\ \text{°C}

Solution to (b):

  1. Two identical steel rods in parallel halve that branch's resistance: RSt,par=19.922=9.96 K/WR_{\text{St,par}} = \frac{19.92}{2} = 9.96\ \text{K/W} H=1002.60+9.96=7.96 W,Tj=100(7.963)(2.597)=79.3 °CH = \frac{100}{2.60+9.96} = 7.96\ \text{W}, \qquad T_j = 100 - \left(7.963\right)\left(2.597\right) = 79.3\ \text{°C}

Solution to (c):

  1. One unknown, one node equation. Take every current as flowing into the junction and set the sum to zero: T1TR1+T2TR2+T3TR3=0\frac{T_1-T^{\,\star}}{R_1}+\frac{T_2-T^{\,\star}}{R_2}+\frac{T_3-T^{\,\star}}{R_3} = 0 With equal LL and AA, 1RiKi\frac{1}{R_i} \propto K_i, so this collapses to K(100T)+2K(50T)+3K(0T)=0K\left(100-T^{\,\star}\right)+2K\left(50-T^{\,\star}\right)+3K\left(0-T^{\,\star}\right)=0 100+100=6TT=33.3 °C100+100 = 6\,T^{\,\star} \qquad\Longrightarrow\qquad T^{\,\star} = 33.3\ \text{°C}

  2. The individual currents, with R1=0.50(50)(1.0×104)=100R_1 = \frac{0.50}{\left(50\right)\left(1.0\times10^{-4}\right)} = 100 K/W, R2=50R_2 = 50 K/W, R3=33.3R_3 = 33.3 K/W: H1=10033.33100=+0.667 W,H2=5033.3350=+0.333 W,H3=033.3333.33=1.00 WH_1 = \frac{100-33.33}{100} = +0.667\ \text{W}, \quad H_2 = \frac{50-33.33}{50} = +0.333\ \text{W}, \quad H_3 = \frac{0-33.33}{33.33} = -1.00\ \text{W}

  3. Check the node. 0.667+0.3331.000=00.667+0.333-1.000 = 0. Heat enters along the two hotter rods and leaves entirely along the third.

Final Answer: (a) 4.44 W with the junction at 88.5°C; (b) the junction falls to 79.3°C and the current rises to 7.96 W; (c) the star junction sits at 33.3°C, with 0.667 W and 0.333 W flowing in and 1.00 W flowing out.

Takeaway: In (a) the junction sits at 88.5°C, only 11.5 K below the hot end, because copper's resistance is one eighth of steel's and the temperature drop divides in proportion to resistance. In (b), adding a parallel steel rod lowered the junction — more of the total resistance now lies in the copper, so more of the drop does too. And in (c), writing every current inward meant no sign had to be guessed: the negative answer identified the outgoing rod for us.

Example 10: Steam into very cold ice

10.0 g of steam at 100°C is passed into 100.0 g of ice at 10.0-10.0°C in a container of negligible heat capacity. Take Lv=22.6×105L_v = 22.6\times10^{5} J/kg, Lf=3.33×105L_f = 3.33\times10^{5} J/kg, swater=4186s_{\text{water}} = 4186 J/(kg K) and sice=2100s_{\text{ice}} = 2100 J/(kg K). Find the final temperature and the composition of the final mixture.

Solution:

  1. Do not assume the answer. Compute the heat available and the heat required separately, as two numbers.

  2. Heat available, taking all the steam down to water at 0°C: Qavail=msLv+mssw(1000)=(0.0100)(22.6×105)+(0.0100)(4186)(100)Q_{\text{avail}} = m_sL_v + m_ss_w\left(100-0\right) = \left(0.0100\right)\left(22.6\times10^{5}\right) + \left(0.0100\right)\left(4186\right)\left(100\right) Qavail=22600+4186=2.679×104 JQ_{\text{avail}} = 22600 + 4186 = 2.679\times10^{4}\ \text{J}

  3. Heat required by the ice, in two stages: Qwarm=misi(10.0)=(0.100)(2100)(10.0)=2100 JQ_{\text{warm}} = m_is_i\left(10.0\right) = \left(0.100\right)\left(2100\right)\left(10.0\right) = 2100\ \text{J} Qmelt,all=miLf=(0.100)(3.33×105)=3.330×104 JQ_{\text{melt,all}} = m_iL_f = \left(0.100\right)\left(3.33\times10^{5}\right) = 3.330\times10^{4}\ \text{J} Qwarm+Qmelt,all=3.540×104 JQ_{\text{warm}}+Q_{\text{melt,all}} = 3.540\times10^{4}\ \text{J}

  4. Branch. Qavail=26786Q_{\text{avail}} = 26786 J is more than the 2100 J needed to bring the ice to 0°C, but less than the 35400 J needed to melt it all. So the mixture pins at 0°C with ice and water together, and only part of the ice melts.

  5. How much melts? mmelt=QavailQwarmLf=2678621003.33×105=246863.33×105=0.0741 kg=74.1 gm_{\text{melt}} = \frac{Q_{\text{avail}}-Q_{\text{warm}}}{L_f} = \frac{26786-2100}{3.33\times10^{5}} = \frac{24686}{3.33\times10^{5}} = 0.0741\ \text{kg} = 74.1\ \text{g}

  6. Compose the final mixture. All 10.0 g of the steam has condensed and cooled to 0°C, and 74.1 g of ice has melted: mwater=10.0+74.1=84.1 g,mice=100.074.1=25.9 gm_{\text{water}} = 10.0+74.1 = 84.1\ \text{g}, \qquad m_{\text{ice}} = 100.0-74.1 = 25.9\ \text{g}

  7. Audit. Total enthalpy before, relative to water at 0°C, is (0.010)(4186×100+22.6×105)+(0.100)(3.33×1052100×10)=2678635400=8614\left(0.010\right)\left(4186\times100+22.6\times10^{5}\right) + \left(0.100\right)\left(-3.33\times10^{5} - 2100\times10\right) = 26786 - 35400 = -8614 J. After: (0.0259)(3.33×105)=8614\left(0.0259\right)\left(-3.33\times10^{5}\right) = -8614 J. It balances.

Final Answer: The mixture settles at 0°C, containing about 84.1 g of water and 25.9 g of ice.

Takeaway: Anyone who assumed "all the ice melts, then solve for a final temperature" would have written a linear equation and got a negative final temperature — the equation's way of shouting that the branch was wrong. The comparison in step 4 IS the physics; steps 5 and 6 are bookkeeping. Note also how much punch the steam carries: 10 g of it melted 74 g of ice, because LvL_v is nearly seven times LfL_f.

Example 11: How hot does a satellite get?

A small spherical satellite is painted matt black and orbits at a distance from the Sun where the solar flux is 1400 W/m2^2. Take σ=5.67×108\sigma = 5.67\times10^{-8} W/(m2^2 K4^4). (a) Find its steady temperature, treating the surrounding space as being at effectively 0 K. (b) It is repainted with a selective coating whose absorptivity for sunlight is 0.60 and whose emissivity in the infrared is 0.90. Find the new steady temperature. (c) Instead, the same black sphere is placed inside a large chamber whose walls are at 27°C while still receiving the 1400 W/m2^2. Find its steady temperature now.

Solution:

  1. Set up the balance for (a). Sunlight is intercepted by the cross-section πr2\pi r^2; radiation leaves from the whole surface 4πr24\pi r^2. For a black body a=e=1a = e = 1: Sπr2=σ(4πr2)T4T=(S4σ)1/4S\,\pi r^{2} = \sigma\left(4\pi r^{2}\right)T^{4} \qquad\Longrightarrow\qquad T = \left(\frac{S}{4\sigma}\right)^{1/4} The radius cancels, so the answer is the same for a marble and for a bus.

  2. Substitute — in kelvin, because this is a fourth power: T4=14004(5.67×108)=14002.268×107=6.173×109 K4T^{4} = \frac{1400}{4\left(5.67\times10^{-8}\right)} = \frac{1400}{2.268\times10^{-7}} = 6.173\times10^{9}\ \text{K}^4 T=280 K=7.1 °CT = 280\ \text{K} = 7.1\ \text{°C}

  3. (b) A selective surface. Absorption uses aa, emission uses ee: aSπr2=eσ(4πr2)T4T=(ae)1/4(S4σ)1/4a\,S\,\pi r^{2} = e\,\sigma\left(4\pi r^{2}\right)T^{4} \qquad\Longrightarrow\qquad T = \left(\frac{a}{e}\right)^{1/4}\left(\frac{S}{4\sigma}\right)^{1/4} T=(0.600.90)1/4(280.3)=(0.9036)(280.3)=253 K=20 °CT = \left(\frac{0.60}{0.90}\right)^{1/4}\left(280.3\right) = \left(0.9036\right)\left(280.3\right) = 253\ \text{K} = -20\ \text{°C}

  4. (c) Warm surroundings. Now the sphere also absorbs from the walls, so the balance uses the net exchange: Sπr2=σ(4πr2)(T4Ts4),Ts=27+273.15=300.15 KS\,\pi r^{2} = \sigma\left(4\pi r^{2}\right)\left(T^{4}-T_s^{4}\right), \qquad T_s = 27 + 273.15 = 300.15\ \text{K} T4=Ts4+S4σ=8.116×109+6.173×109=1.429×1010 K4T^{4} = T_s^{4} + \frac{S}{4\sigma} = 8.116\times10^{9} + 6.173\times10^{9} = 1.429\times10^{10}\ \text{K}^4 T=346 K=72.6 °CT = 346\ \text{K} = 72.6\ \text{°C}

Final Answer: (a) 280 K, about 7°C; (b) 253 K, about 20-20°C; (c) 346 K, about 73°C.

Takeaway: Part (b) is the whole of thermal control engineering in one line. Kirchhoff's law says a good absorber is a good emitter at the same wavelength, and sunlight arrives near 0.5 μ\mum while a 280 K body radiates near 10 μ\mum — so aa and ee are free to differ, and a coating with ae<1\frac{a}{e} < 1 runs cold. Part (c) is the kelvin trap in disguise: had you written Ts=27T_s = 27 instead of 300.15 K, Ts4T_s^4 would have been 5.3×1055.3\times10^5 instead of 8.1×1098.1\times10^9, four orders of magnitude out.

Example 12: Newton's law, and how far you can trust it

A body cools from 80.0°C to 64.0°C in 5.00 minutes in surroundings held at 24.0°C. (a) Find the cooling constant kk and the temperature after a further 10.0 minutes, using the exponential form. (b) Repeat the estimate using the average-temperature form and say how far it is off. (c) A different body sits at 200°C in a room at 20°C. By what fraction does the linear Newton form under-predict its true net radiative loss?

Solution to (a):

  1. The exponential form follows from dTdt=k(TTs)-\frac{dT}{dt} = k\left(T-T_s\right): T=Ts+(T0Ts)ektT = T_s + \left(T_0-T_s\right)e^{-kt}

  2. Fit kk to the given interval. The excess falls from 56.0 K to 40.0 K in 5.00 min: k=1tlnT0TsTTs=15.00ln56.040.0=0.33655.00=0.0673 min1k = \frac{1}{t}\ln\frac{T_0-T_s}{T-T_s} = \frac{1}{5.00}\ln\frac{56.0}{40.0} = \frac{0.3365}{5.00} = 0.0673\ \text{min}^{-1}

  3. Predict at t=15.0t = 15.0 min from the start: T=24.0+(56.0)e(0.06729)(15.0)=24.0+(56.0)(0.3644)=44.4 °CT = 24.0 + \left(56.0\right)e^{-\left(0.06729\right)\left(15.0\right)} = 24.0 + \left(56.0\right)\left(0.3644\right) = 44.4\ \text{°C}

Solution to (b):

  1. Fit the average form on the same first interval: 80.064.05.00=k(80.0+64.0224.0)k=16.0(5.00)(48.0)=0.0667 min1\frac{80.0-64.0}{5.00} = k\left(\frac{80.0+64.0}{2}-24.0\right) \quad\Longrightarrow\quad k = \frac{16.0}{\left(5.00\right)\left(48.0\right)} = 0.0667\ \text{min}^{-1} That is 0.93% below the exact value.

  2. Step forward in 5-minute intervals with that kk. Doing so twice more lands on 44.41°C — indistinguishable from the exponential. That is not luck: fitting on a 5-minute interval forces the ratio of successive excesses to be exactly right, and a fixed ratio per interval is an exponential.

  3. Now take one 15-minute step instead: 80.0T15.0=(0.06667)(80.0+T224.0)T=42.7 °C\frac{80.0-T}{15.0} = \left(0.06667\right)\left(\frac{80.0+T}{2}-24.0\right) \quad\Longrightarrow\quad T = 42.7\ \text{°C} 1.7°C below the true 44.4°C, because the shortcut assumed the cooling rate stayed at its 15-minute average across an interval over which the excess more than halved.

Solution to (c):

  1. Compare the two laws, in kelvin. With Ts=293.15T_s = 293.15 K and T=473.15T = 473.15 K: trueT4Ts4=(473.15)4(293.15)4=5.011×10107.386×109=4.272×1010\text{true} \propto T^{4}-T_s^{4} = \left(473.15\right)^4-\left(293.15\right)^4 = 5.011\times10^{10}-7.386\times10^{9} = 4.272\times10^{10} Newton4Ts3(TTs)=4(2.520×107)(180)=1.814×1010\text{Newton} \propto 4T_s^{3}\left(T-T_s\right) = 4\left(2.520\times10^{7}\right)\left(180\right) = 1.814\times10^{10} Newtontrue=0.424\frac{\text{Newton}}{\text{true}} = 0.424

Final Answer: (a) k=0.0673k = 0.0673 min1^{-1} and T=44.4T = 44.4°C; (b) the average form gives the same answer stepped at 5 minutes but 42.7°C in one 15-minute step, 1.7°C low; (c) Newton's law predicts only 42% of the true loss, under-predicting it by 58%.

Takeaway: Three separate lessons. The average form is a stepping method, not a formula — it is accurate over the interval size it was calibrated on and degrades over longer ones. A kk from the average form is not the kk of the exponential; substituting the 0.0667 into ekte^{-kt} gives 44.6°C rather than 44.4°C. And Newton's law is a linearisation with a range: fine at 5 K of excess (97.5% accurate), acceptable at 20 K (90%), badly wrong at 180 K (42%). Say which regime you are in and the examiner has nothing to take marks for.