ARCHETYPE: Method-of-Mixtures Problems

Drop an ice cube into a warm drink and something quietly outrageous happens: the drink cools, the ice melts — and while it melts, the thermometer flatly refuses to move. Heat is pouring in and the temperature will not budge. That single stubborn fact is why calorimetry questions cost students so many marks. They set up one tidy equation, solve for a final temperature, and confidently write −8 ∘C-8\ ^\circ\mathrm{C} for a mixture that contains liquid water. The physics did not fail. The bookkeeping did. An isolated calorimeter is an accounting problem wearing a lab coat. Energy cannot leave the vessel, so every joule that a hot body loses must show up in a cold body: ∑Qlost=∑Qgained\sum Q_{\text{lost}} = \sum Q_{\text{gained}}. There are only ever two kinds of entry in the ledger — sensible heat mc ΔTmc\,\Delta T, which changes the temperature, and latent heat mLmL, which changes the state at a fixed temperature. Melt one gram of ice and you have spent as much heat as cooling one gram of water by about 80 ∘C80\ ^\circ\mathrm{C}; condense one gram of steam and you release the equivalent of 540 ∘C540\ ^\circ\mathrm{C} of cooling. Those two monsters are what pin the answer to a plateau and wreck a careless linear equation. So this article treats the calorimeter itself as the archetype. One master equation, four standard variants — two-liquid mix, unknown specific heat, how-much-ice-melts, steam condensing — and one habit that separates a full-marks script from a plausible-looking wreck: before you assume a final temperature, test whether a phase change starts, and whether it finishes. Learn the ledger, and an entire family of CBSE, JEE and NEET problems becomes fill-in-the-blanks.

Key takeaways
  • An isolated calorimeter conserves energy, so the whole subject is one line: ∑Qlost=∑Qgained\sum Q_{\text{lost}} = \sum Q_{\text{gained}}.
  • Every term is one of exactly two species — sensible Q=mc ΔTQ = mc\,\Delta T (temperature moves) or latent Q=mLQ = mL (state changes, temperature frozen).
  • Two-liquid mix: Tf=m1c1T1+m2c2T2m1c1+m2c2T_f = \dfrac{m_1c_1T_1 + m_2c_2T_2}{m_1c_1 + m_2c_2} — a heat-capacity-weighted average that always lands strictly between the two starting temperatures.
  • The vessel drinks heat too. Fold it in with its water equivalent w=mcalccal/cww = m_{\text{cal}}c_{\text{cal}}/c_w: a 100100 g copper calorimeter behaves like 9.239.23 g of extra water.
  • The archetype skill: run the budget test before writing one linear equation. Compare the heat available with the heat a complete phase change would cost. If the heat runs out mid-melt, the answer is pinned at the plateau — 0 ∘C0\ ^\circ\mathrm{C} — and only part of the ice melts.
  • Anchors: 100100 g at 80 ∘C80\ ^\circ\mathrm{C} plus 200200 g at 20 ∘C20\ ^\circ\mathrm{C} gives 40 ∘C40\ ^\circ\mathrm{C}; 300300 g of water at 25 ∘C25\ ^\circ\mathrm{C} melts only 93.993.9 g of a 100100 g ice block; 1010 g of steam into 200200 g of water at 20 ∘C20\ ^\circ\mathrm{C} gives 49.6 ∘C49.6\ ^\circ\mathrm{C}.
  • Key idea: calorimetry is double-entry bookkeeping for joules — put every term on the correct side, and always ask whether a phase change interrupts the sum before you solve it.
The core insight

In an isolated calorimeter the heat lost by the hot bodies equals the heat gained by the cold ones, where each entry is either sensible heat mc ΔTmc\,\Delta T or latent heat mLmL; the whole art is deciding which terms exist — that is, whether a phase change begins and whether it completes — before solving for the final temperature.

Where this lives today

The instrument never left. Bomb calorimeters burn a food sample in oxygen inside a steel vessel immersed in a stirred water bath, and the calorie count on a cereal packet is the temperature rise of that bath run backwards through ∑Qlost=∑Qgained\sum Q_{\text{lost}} = \sum Q_{\text{gained}}. Differential scanning calorimetry does the same trick with microwatts, tracking the tiny latent heats absorbed as a polymer melts or a protein unfolds — a plateau on a graph, exactly like the one that pins the ice water at zero. The ledger also designs anything built to move heat on purpose. Phase-change materials exploit the latent term deliberately: a wax sealed into a ceiling panel, chosen to melt at room temperature, absorbs a huge slug of heat at almost constant temperature and flattens an office's afternoon peak with no air conditioning at all — the physics of the 6.16.1 g of surviving ice, aimed at a building. A laptop's heat pipe runs on LvL_v, the same monster term that made 1010 g of steam worth nearly 3030 K. Every one of them is keeping Laplace's account: joules out on one side, joules in on the other, and the books must balance.

The setup

Picture the apparatus, because in an archetype the setup is the physics. A calorimeter is a metal cup — copper, usually — sitting inside an insulating jacket, with a stirrer and a thermometer through the lid. Inside it: some water at a known temperature. Into it: a hot body, or an ice cube, or a jet of steam. The lid goes on, the stirrer turns, and after a short while every part of the contents reads the same temperature. That common end-point is thermal equilibrium, and reaching it is the only thing the apparatus is for. The insulation is the whole reason the problem is solvable. "Isolated" means no heat leaks in from the room and none escapes to it, so the energy inside is a closed account. Whatever the hot contents lose, the cold contents must have received — there is nowhere else for it to go:

∑Qlost  =  ∑Qgained(1)\sum Q_{\text{lost}} \;=\; \sum Q_{\text{gained}} \qquad (1)

where: ∑Qlost\sum Q_{\text{lost}} — the total heat given out by everything that ends up colder than it started; ∑Qgained\sum Q_{\text{gained}} — the total heat taken in by everything that ends up warmer (or that melts, or boils). This is the principle of calorimetry, and it is nothing more than conservation of energy with the leaks sealed. Read it as a balance sheet: the left column is money out, the right column is money in, and the books must close to the last joule.

Figure
The calorimeter ledger — heat lost by the hot side must equal heat gained by the cold side
insulating jacket: no heat in, no heat out water, m c T cup hot thermometer THE LEDGER LOST hot body cools: m c ΔT steam condenses: m L GAINED water warms: m c ΔT ice melts: m L cup warms: m c ΔT Σ LOST = Σ GAINED every joule leaving the hot body arrives somewhere on the cold side — the sealed jacket leaves nowhere else to go Two species of entry only: sensible m c ΔT, and latent m L

Three idealizations turn this cartoon into an exam problem, and a good board answer states them:

The system is isolated. No conduction through the jacket, no convection out of the lid, no radiation to the lab. Real calorimeters leak a little, which is why careful experimenters apply a cooling correction — but for the problem in front of you, the account is closed.

Stirring makes the temperature common. Without it, water near the hot body would be hotter than water at the wall, and "the final temperature" would not be a single number. The stirrer buys us the right to write one symbol, TfT_f.

Everything ends at the same temperature. That is what equilibrium means, and it is what lets you connect two bodies you were handed separately. It is also the assumption that breaks when a phase change is involved: if ice is left over at the end, the final temperature is not free at all — it is nailed to 0 ∘C0\ ^\circ\mathrm{C}.

The two species of heat term

Every entry in the ledger is one of exactly two kinds. Nothing else exists at this level, and half of all lost marks come from writing the wrong species.

Sensible heat changes the temperature of a body that stays in the same state:

Q=m c ΔT(2)Q = m\,c\,\Delta T \qquad (2)

where: mm — mass in kg; cc — specific heat capacity in J/kg·K (water 41804180, ice 21002100, steam 20102010, copper 386386, iron 450450); ΔT\Delta T — the temperature change, taken as a positive magnitude once the term sits on the correct side of the ledger. "Sensible" is the old word for sensed: this is the heat the thermometer feels. Note the scale of cw=4180c_w = 4180 — water needs about ten times as much heat per kilogram per kelvin as a typical metal, which is why a metal spoon in soup burns your fingers and the soup does not.

Latent heat changes the state of a body at constant temperature:

Q=m L(3)Q = m\,L \qquad (3)

where: LL — the specific latent heat in J/kg: for fusion (melting or freezing) of ice Lf=3.34×105L_f = 3.34\times10^{5}; for vaporization (boiling or condensing) of water Lv=2.26×106L_v = 2.26\times10^{6}. There is no ΔT\Delta T here, and there must not be — the temperature is not changing. "Latent" means hidden: the joules go into breaking the bonds that hold the solid together, not into speeding molecules up, so the thermometer sees nothing. Feel the sizes, because the sizes are what make calorimetry surprising. Divide each latent heat by cwc_w to get the water-cooling that would buy the same energy: Lf/cw=79.9 KL_f/c_w = 79.9\ \mathrm{K} and Lv/cw=540.7 KL_v/c_w = 540.7\ \mathrm{K}. In words: melting one gram of ice costs as much heat as cooling one gram of water by 80 ∘C80\ ^\circ\mathrm{C}, and condensing one gram of steam releases as much as cooling one gram of water by 540 ∘C540\ ^\circ\mathrm{C}. The latent terms are giants — they routinely dominate the sum, and they are exactly the terms students forget.

The master equation

Now assemble the archetype. Take a hot body (mass m1m_1, specific heat c1c_1, temperature T1T_1) and a cold body (mass m2m_2, specific heat c2c_2, temperature T2<T1T_2 < T_1), with no phase change anywhere. Let them come to a common final temperature TfT_f. Heat lost by the hot body equals heat gained by the cold one:

m1c1(T1−Tf)  =  m2c2(Tf−T2)(4)m_1 c_1 (T_1 - T_f) \;=\; m_2 c_2 (T_f - T_2) \qquad (4)

where: each bracket is a positive temperature drop or rise — the hot body falls from T1T_1 to TfT_f, the cold body climbs from T2T_2 to TfT_f. Writing the brackets this way is the sign discipline that saves you: no minus signs to babysit, and every quantity in sight is positive. Solve (4) for TfT_f:

Tf  =  m1c1T1+m2c2T2m1c1+m2c2(5)T_f \;=\; \frac{m_1 c_1 T_1 + m_2 c_2 T_2}{m_1 c_1 + m_2 c_2} \qquad (5)

where: the products mcm c are heat capacities (J/K) — the "thermal inertia" of each body. Read equation (5) physically: the final temperature is the average of the starting temperatures, weighted by heat capacity. The body with the bigger mcmc drags the answer toward itself, exactly as the bigger mass dominates a centre-of-mass calculation. Two consequences double as instant sanity checks. The final temperature always lies strictly between T1T_1 and T2T_2, because a weighted average of two numbers cannot escape them. An answer of 95 ∘C95\ ^\circ\mathrm{C} for a mix of water at 8080 and 20 ∘C20\ ^\circ\mathrm{C} is an algebra slip — stop and find it. And if the two bodies are the same substance (c1=c2c_1 = c_2), the cc cancels and (5) collapses to a plain mass-weighted average. Equal masses of water at 8080 and 20 ∘C20\ ^\circ\mathrm{C} therefore meet at exactly 50 ∘C50\ ^\circ\mathrm{C}, while 100100 g at 80 ∘C80\ ^\circ\mathrm{C} poured into 200200 g at 20 ∘C20\ ^\circ\mathrm{C} lands at 40 ∘C40\ ^\circ\mathrm{C} — two-thirds of the way toward the cold side, because the cold side carries twice the heat capacity.

The vessel drinks heat too — water equivalent

Real calorimeters are made of metal, and metal warms up. The copper cup, the stirrer and (strictly) the thermometer bulb all sit at the water's temperature and all absorb a share of the heat. Ignore them and your answer is systematically wrong — in the same direction, every time. The tidy fix is to give the calorimeter an alias. Its heat capacity is mcalccalm_{\text{cal}}c_{\text{cal}} J/K. Ask: what mass of water would have that same heat capacity? Call it the water equivalent ww:

w cw=mcal ccal⟹w=mcal ccalcw(6)w \,c_w = m_{\text{cal}}\,c_{\text{cal}} \quad\Longrightarrow\quad w = \frac{m_{\text{cal}}\,c_{\text{cal}}}{c_w} \qquad (6)

where: ww — the water equivalent in kg, a fictitious extra slug of water that soaks up heat exactly as the cup does. Once you have ww, the cup disappears from the problem: just pretend the calorimeter contains (mwater+w)(m_{\text{water}} + w) of water and use the master equation unchanged. A 100100 g copper calorimeter has mcalccal=0.100×386=38.6 J/Km_{\text{cal}}c_{\text{cal}} = 0.100 \times 386 = 38.6\ \mathrm{J/K}, so w=38.6/4180=9.23 gw = 38.6/4180 = 9.23\ \mathrm{g}. A whole 100100 g cup of copper is thermally worth barely nine grams of water — copper's specific heat is roughly a tenth of water's. Small, but not zero. Run the 40 ∘C40\ ^\circ\mathrm{C} mixture of Example 1 inside that cup — the cold side becomes 200+9.23=209.23200 + 9.23 = 209.23 g of water — and the answer drops to 12 184.6/309.23=39.4 ∘C12\,184.6/309.23 = 39.4\ ^\circ\mathrm{C}. A shift of 0.60.6 K is the difference between a right answer and a "close" one, and when a question hands you mcalm_{\text{cal}} and ccalc_{\text{cal}} it is because the examiner intends to charge you for ignoring them.

Derivation AThe master mix — heat lost equals heat gained

We derive the final temperature of a two-body mixture with no phase change, equation (5), by the route every marking scheme rewards: name the hot side and the cold side, write each body's heat as a positive quantity, set the totals equal, and solve. The strategy is to keep every bracket positive by construction — hot bodies get (T1−Tf)(T_1 - T_f), cold bodies get (Tf−T2)(T_f - T_2) — so that not one minus sign is left to lose you a mark. It also shows why the answer is a heat-capacity-weighted average that can never escape the two starting temperatures.

Step 1. Seal the account. The calorimeter is isolated, so no heat crosses the jacket: every joule the hot body releases is absorbed by the cold one, and nothing changes state. Why: without isolation the two bodies are not connected by any equation at all, and the problem has no answer.

Step 2. The hot body (m1m_1, c1c_1) falls from T1T_1 to the common TfT_f; the cold body (m2m_2, c2c_2) climbs from T2T_2 to TfT_f:

Qlost=m1c1(T1−Tf),Qgained=m2c2(Tf−T2)Q_{\text{lost}} = m_1 c_1 (T_1 - T_f), \qquad Q_{\text{gained}} = m_2 c_2 (T_f - T_2)

Why: both brackets are positive because T2<Tf<T1T_2 < T_f < T_1 — we assert in advance that the answer lies between the starts, and the algebra confirms it. This is the sign discipline that kills the topic's commonest error.

Step 3. Close the books, Qlost=QgainedQ_{\text{lost}} = Q_{\text{gained}}, and expand:

m1c1T1−m1c1Tf=m2c2Tf−m2c2T2m_1 c_1 T_1 - m_1 c_1 T_f = m_2 c_2 T_f - m_2 c_2 T_2

Step 4. Collect the TfT_f terms and divide by the total heat capacity:

Tf=m1c1T1+m2c2T2m1c1+m2c2T_f = \frac{m_1 c_1 T_1 + m_2 c_2 T_2}{m_1 c_1 + m_2 c_2}

Step 5. Read it. The numerator sums (heat capacity × temperature), the denominator is the total heat capacity, so TfT_f is the weighted mean of T1T_1 and T2T_2 — and a weighted mean of two numbers always lies between them, which proves the sanity check. Equal heat capacities give the plain average; m2c2→∞m_2c_2 \to \infty gives Tf→T2T_f \to T_2, a huge cold bath swallowing the hot body without warming. Verified: 100100 g at 80 ∘C80\ ^\circ\mathrm{C} into 200200 g at 20 ∘C20\ ^\circ\mathrm{C} gives Tf=40 ∘CT_f = 40\ ^\circ\mathrm{C} with Qlost=Qgained=16 720Q_{\text{lost}} = Q_{\text{gained}} = 16\,720 J; equal masses at 8080 and 2020 give 50 ∘C50\ ^\circ\mathrm{C}; 11 g at 80 ∘C80\ ^\circ\mathrm{C} into 100100 kg at 20 ∘C20\ ^\circ\mathrm{C} gives 20.0 ∘C20.0\ ^\circ\mathrm{C} — recomputed in verify_hs2-calorimetry-mixing-problems.py

Go deeper · Derivation B · 2 minThe phase-change interrupt — does all the ice actually melt?
Derivation BThe phase-change interrupt — does all the ice actually melt?

We now derive the archetype's signature move, and the reason a naive linear equation blows up. When ice at 0 ∘C0\ ^\circ\mathrm{C} meets warm water, the mixture may end above 0 ∘C0\ ^\circ\mathrm{C} with all the ice gone, or it may end pinned at 0 ∘C0\ ^\circ\mathrm{C} with ice still floating — and which of the two happens is not something you may assume. It is something you must test, by comparing two energy budgets before writing any equation for TfT_f. The test costs ten seconds and is worth the whole question.

Step 1. Compute the heat available: the most the warm water can possibly give up before it, too, arrives at the plateau temperature 0 ∘C0\ ^\circ\mathrm{C}. For water of mass mwm_w at TwT_w, and for ice of mass mim_i, the heat demanded by a complete melt:

Qavail=mwcw(Tw−0),Qdemand=miLfQ_{\text{avail}} = m_w c_w (T_w - 0), \qquad Q_{\text{demand}} = m_i L_f

Why: while any ice is present the mixture sits at the melting point, so the warm water cannot cool below 0 ∘C0\ ^\circ\mathrm{C}. That makes QavailQ_{\text{avail}} a hard ceiling on the energy the ice can ever receive.

Step 2. Compare the two numbers. That comparison is the whole test, and everything else follows from which way it goes.

Step 3. If Qavail>QdemandQ_{\text{avail}} > Q_{\text{demand}}, the ice all melts with energy to spare. The problem is now an ordinary mix: the surplus warms the combined water — original plus melt water — above 0 ∘C0\ ^\circ\mathrm{C}, and the ledger reads

mwcw(Tw−Tf)=miLf+micw(Tf−0)m_w c_w (T_w - T_f) = m_i L_f + m_i c_w (T_f - 0)

with the melt water appearing twice on the right: once for melting, once for warming.

Step 4. If Qavail<QdemandQ_{\text{avail}} < Q_{\text{demand}}, the heat runs out mid-melt. The mixture cannot get past the plateau, so

Tf=0 ∘C,mmelted=QavailLf(7)T_f = 0\ ^\circ\mathrm{C}, \qquad m_{\text{melted}} = \frac{Q_{\text{avail}}}{L_f} \qquad (7)

and mi−mmeltedm_i - m_{\text{melted}} of ice survives, still solid, sharing the vessel with water at exactly 0 ∘C0\ ^\circ\mathrm{C}. Why: this is the case a single linear equation gets catastrophically wrong. Force mwcw(Tw−Tf)=miLf+micwTfm_w c_w(T_w - T_f) = m_i L_f + m_i c_w T_f when the budget fails and it obediently returns a negative TfT_f — liquid water below freezing, next to ice. The equation is not lying; it is answering a question you should not have asked, because the assumption "all the ice melts" was false before you started.

Step 5. The threshold. All the ice just barely melts when the budgets exactly balance, mwcwTw=miLfm_w c_w T_w = m_i L_f. For 300300 g of water and 100100 g of ice that means Tw=33 400/(0.300×4180)=26.6 ∘CT_w = 33\,400/(0.300 \times 4180) = 26.6\ ^\circ\mathrm{C}: water any cooler leaves ice behind, water any warmer melts the block and rises above zero. Verified: 300300 g of water at 25 ∘C25\ ^\circ\mathrm{C} onto 100100 g of ice offers 31 35031\,350 J against a demand of 33 40033\,400 J, so only 93.993.9 g melts, 6.16.1 g of ice survives, and Tf=0 ∘CT_f = 0\ ^\circ\mathrm{C}; with 5050 g of ice the budget passes and Tf=10.0 ∘CT_f = 10.0\ ^\circ\mathrm{C}; the threshold is 26.6 ∘C26.6\ ^\circ\mathrm{C} — recomputed in verify_hs2-calorimetry-mixing-problems.py

Figure
The budget test — heat available versus heat demanded decides the entire answer
300 g water at 25 °C + 100 g ice at 0 °C 0 J 31 350 J AVAILABLE water cooling 25 °C down to 0 °C 0.3 × 4180 × 25 33 400 J DEMANDED to melt ALL the ice 0.1 × 3.34e5 short by 2050 J VERDICT available is less than demanded Melt is INCOMPLETE → T pinned at 0 °C, only 93.9 g melts, 6.1 g of ice survives

The variants examiners actually pose

Four dressings of the same ledger cover essentially every calorimetry question a board has ever set. The equation never changes; only the list of terms does.

Variant 1 — the two-liquid mix. Two masses of liquid at different temperatures; find TfT_f. Straight application of equation (5), and if both are water the specific heat cancels.

Variant 2 — the unknown specific heat. Drop a hot metal block into cool water, measure the final temperature, and solve the ledger for cmetalc_{\text{metal}} instead of TfT_f. This is the classic school experiment — Black's original method of mixtures — so the rearranged form is worth memorising:

cmetal  =  mwcw (Tf−Tw)mmetal (Tmetal−Tf)(8)c_{\text{metal}} \;=\; \frac{m_w c_w\,(T_f - T_w)}{m_{\text{metal}}\,(T_{\text{metal}} - T_f)} \qquad (8)

where: the numerator is the heat the water gained; the denominator is (mass × temperature drop) of the metal. Count the calorimeter and mwcwm_w c_w becomes (mw+w)cw(m_w + w)c_w — a correction worth about 3%3\%, as Example 5 shows.

Variant 3 — the ice interrupt. Ice meets warm water. Run the budget test of equation (7) first. If the melt is incomplete, the answer is Tf=0 ∘CT_f = 0\ ^\circ\mathrm{C} plus a mass of melted ice; if it completes, carry the leftover heat into an ordinary mix. Ice starting below 0 ∘C0\ ^\circ\mathrm{C} needs a sensible term micice ΔTm_i c_{\text{ice}}\,\Delta T first (with cice=2100c_{\text{ice}} = 2100, not 41804180) to reach the melting point before any melting can begin.

Variant 4 — steam condensing. Steam at 100 ∘C100\ ^\circ\mathrm{C} blown into cool water gives up two things in order: its latent heat msLvm_s L_v as it condenses to water at 100 ∘C100\ ^\circ\mathrm{C}, then sensible heat mscw(100−Tf)m_s c_w (100 - T_f) as that condensate cools. The ledger reads

msLv+mscw(100−Tf)  =  mwcw(Tf−Tw)(9)m_s L_v + m_s c_w (100 - T_f) \;=\; m_w c_w (T_f - T_w) \qquad (9)

where: the LvL_v term is enormous — 2.26×1062.26\times10^{6} J/kg — which is why a few grams of steam heat a whole beaker startlingly far. The mirror-image test applies here too: if the steam offers more than the water needs to reach 100 ∘C100\ ^\circ\mathrm{C}, not all of it condenses and the mixture is pinned at 100 ∘C100\ ^\circ\mathrm{C} with steam left over. Same interrupt logic, other end of the thermometer.

Limiting cases

Every one of these can be read straight off equation (5) or the budget test, and each is a five-second check on an answer you are unsure of. Note where the final temperature is allowed to land: a pure mix lands strictly between the two starts, and only an unfinished phase change can pin it to a plateau — 0 ∘C0\ ^\circ\mathrm{C} with ice left over, 100 ∘C100\ ^\circ\mathrm{C} with steam left over.

caseresultmeaning
m1c1=m2c2m_1c_1 = m_2c_2Tf=12(T1+T2)T_f = \tfrac{1}{2}(T_1 + T_2)equal heat capacities meet exactly in the middle: water at 8080 and 2020 gives 50 ∘C50\ ^\circ\mathrm{C}
m2c2≫m1c1m_2c_2 \gg m_1c_1Tf→T2T_f \to T_2a huge cold bath swallows the hot body: 11 g at 80 ∘C80\ ^\circ\mathrm{C} into 100100 kg at 20 ∘C20\ ^\circ\mathrm{C} ends at 20.0 ∘C20.0\ ^\circ\mathrm{C}
T1=T2T_1 = T_2Tf=T1T_f = T_1already in equilibrium — no heat flows, whatever the masses
c→0c \to 0 or m→0m \to 0that body is invisiblea body with no heat capacity cannot shift the mixture at all
ice left overTf=0 ∘CT_f = 0\ ^\circ\mathrm{C} exactlythe melt ran out of energy; temperature is pinned, not solved for
steam left overTf=100 ∘CT_f = 100\ ^\circ\mathrm{C} exactlythe condensation ran out of cold; same trap, other plateau
any pure mixT2<Tf<T1T_2 < T_f < T_1a weighted average can never escape its inputs

Worked examples

1 · Board level — the two-liquid mix (CBSE/ICSE pattern, 3 marks)

100100 g of water at 80 ∘C80\ ^\circ\mathrm{C} is poured into 200200 g of water at 20 ∘C20\ ^\circ\mathrm{C} in a vessel of negligible heat capacity. Find the final temperature of the mixture. Take cw=4180c_w = 4180 J/kg·K.

Step 1. Check for phase changes. Both bodies are liquid water and any TfT_f between 2020 and 80 ∘C80\ ^\circ\mathrm{C} keeps them liquid — no melting, no boiling, so the ledger carries sensible terms only. Saying this in one line is what earns the method mark.

Step 2. Name the sides — hot water falling from 8080 to TfT_f, cold water rising from 2020 to TfT_f:

0.100×4180×(80−Tf)  =  0.200×4180×(Tf−20)0.100 \times 4180 \times (80 - T_f) \;=\; 0.200 \times 4180 \times (T_f - 20)

Step 3. The specific heat is common to both sides, so cancel it:

100(80−Tf)=200(Tf−20)  ⇒  8000−100Tf=200Tf−4000100(80 - T_f) = 200(T_f - 20) \;\Rightarrow\; 8000 - 100T_f = 200T_f - 4000

Step 4. Collect and solve: 12 000=300 Tf12\,000 = 300\,T_f, so Tf=40 ∘CT_f = \boxed{40\ ^\circ\mathrm{C}}.

Step 5. Check the books. Lost =0.100×4180×40=16 720= 0.100 \times 4180 \times 40 = 16\,720 J; gained =0.200×4180×20=16 720= 0.200 \times 4180 \times 20 = 16\,720 J ✓. And 40 ∘C40\ ^\circ\mathrm{C} lies between 2020 and 8080 ✓, nearer the cold side because the cold side has twice the heat capacity — the hot water fell 4040 K while the cold water rose only 2020 K.

2 · Board level — the unknown specific heat of a metal (the method of mixtures)

A 200200 g block of metal is heated to 100 ∘C100\ ^\circ\mathrm{C} and dropped into 300300 g of water at 20 ∘C20\ ^\circ\mathrm{C}. The mixture settles at 25 ∘C25\ ^\circ\mathrm{C}. Neglecting the calorimeter, find the specific heat capacity of the metal.

Step 1. Direction of flow: the metal is hot, so it loses; the water is cold, so it gains. Nothing melts or boils, so there are no latent terms.

Step 2. Heat gained by the water, which rises by 25−20=525 - 20 = 5 K:

Qgained=0.300×4180×5=6270 JQ_{\text{gained}} = 0.300 \times 4180 \times 5 = 6270\ \mathrm{J}

Step 3. Heat lost by the metal, which falls by 100−25=75100 - 25 = 75 K. That drop is the number students most often get wrong — it runs to the final temperature, not to the water's starting temperature.

Qlost=0.200×c×75=15 cQ_{\text{lost}} = 0.200 \times c \times 75 = 15\,c

Step 4. Close the books and solve:

15 c=6270  ⇒  c=418 J/kg⋅K15\,c = 6270 \;\Rightarrow\; c = \boxed{418\ \mathrm{J/kg\cdot K}}

Step 5. Sanity: one tenth of water's 41804180, squarely in the metal range (copper 386386, iron 450450). A value larger than water's would mean you divided by the wrong temperature drop. The experiment's design says the same thing — a big fall on the metal side (7575 K) against a small rise on the water side (55 K) is exactly what a small cc looks like.

3 · Competitive level — the ice interrupt (JEE-Main/NEET pattern, ~3 minutes)

300300 g of water at 25 ∘C25\ ^\circ\mathrm{C} is poured onto 100100 g of ice at 0 ∘C0\ ^\circ\mathrm{C} in an insulated flask. Find the final temperature and the mass of ice that melts. Take Lf=3.34×105L_f = 3.34\times10^{5} J/kg, cw=4180c_w = 4180 J/kg·K.

Step 1. Do not write a linear equation yet. Run the budget test. Heat available from the water, cooling all the way to the plateau at 0 ∘C0\ ^\circ\mathrm{C}:

Qavail=0.300×4180×25=31 350 JQ_{\text{avail}} = 0.300 \times 4180 \times 25 = 31\,350\ \mathrm{J}

Step 2. Heat demanded to melt the whole block:

Qdemand=0.100×3.34×105=33 400 JQ_{\text{demand}} = 0.100 \times 3.34\times10^{5} = 33\,400\ \mathrm{J}

Step 3. Compare: 31 350<33 40031\,350 < 33\,400. The water runs out of energy 20502050 J short of a complete melt. So the melt is incomplete — ice survives, and while ice survives, the mixture cannot leave the melting point:

Tf=0 ∘CT_f = \boxed{0\ ^\circ\mathrm{C}}

Step 4. Mass melted, from equation (7): the 31 35031\,350 J that were available bought

mmelted=31 3503.34×105=0.0939 kg=93.9 gm_{\text{melted}} = \frac{31\,350}{3.34\times10^{5}} = 0.0939\ \mathrm{kg} = \boxed{93.9\ \mathrm{g}}

leaving 100−93.9=6.1 g100 - 93.9 = \boxed{6.1\ \mathrm{g}} of ice floating in 393.9393.9 g of water, the whole flask sitting at exactly 0 ∘C0\ ^\circ\mathrm{C}.

Step 5. The counterfactual, so the boundary is unforgettable. Had the ice been only 5050 g, the demand would have been 0.050×3.34×105=16 7000.050 \times 3.34\times10^{5} = 16\,700 J — comfortably inside the budget. All of it melts, 31 350−16 700=14 65031\,350 - 16\,700 = 14\,650 J is left over, and that surplus warms the combined 350350 g of water: Tf=14 650/(0.350×4180)=10.0 ∘CT_f = 14\,650/(0.350 \times 4180) = 10.0\ ^\circ\mathrm{C}. Same water, half the ice, and a completely different kind of answer. Timing note: the budget test is two multiplications — under thirty seconds — and it decides whether the rest of the question takes one line or five. In an MCQ, "0 ∘C0\ ^\circ\mathrm{C} with ice left over" is usually one of the options precisely because most candidates never test for it. Threshold worth memorising: with 300300 g of water you would need a start of 26.6 ∘C26.6\ ^\circ\mathrm{C} to melt all 100100 g of the ice.

4 · Competitive level — steam condensing (JEE/NEET pattern, ~3 minutes)

1010 g of steam at 100 ∘C100\ ^\circ\mathrm{C} is passed into 200200 g of water at 20 ∘C20\ ^\circ\mathrm{C} in an insulated container of negligible heat capacity. Find the final temperature. Take Lv=2.26×106L_v = 2.26\times10^{6} J/kg, cw=4180c_w = 4180 J/kg·K.

Step 1. Completion test first, at the upper plateau this time. The most the steam can ever deliver is its latent heat plus the cooling of its condensate all the way down to 20 ∘C20\ ^\circ\mathrm{C}:

Qsteam,max=0.010×2.26×106+0.010×4180×80=22 600+3344=25 944 JQ_{\text{steam,max}} = 0.010 \times 2.26\times10^{6} + 0.010 \times 4180 \times 80 = 22\,600 + 3344 = 25\,944\ \mathrm{J}

The heat needed to take the water all the way up to 100 ∘C100\ ^\circ\mathrm{C} is 0.200×4180×80=66 8800.200 \times 4180 \times 80 = 66\,880 J. Since 25 944<66 88025\,944 < 66\,880, the water never reaches 100 ∘C100\ ^\circ\mathrm{C}: all the steam condenses, and TfT_f lands strictly between 2020 and 100 ∘C100\ ^\circ\mathrm{C}.

Step 2. Now write the ledger, equation (9). Steam side loses twice — condensing, then cooling:

0.010×2.26×106⏟condense  +  0.010×4180×(100−Tf)⏟condensate cools  =  0.200×4180×(Tf−20)⏟water warms\underbrace{0.010 \times 2.26\times10^{6}}_{\text{condense}} \;+\; \underbrace{0.010 \times 4180 \times (100 - T_f)}_{\text{condensate cools}} \;=\; \underbrace{0.200 \times 4180 \times (T_f - 20)}_{\text{water warms}}

Step 3. Expand: 22 600+41.8(100−Tf)=836(Tf−20)22\,600 + 41.8(100 - T_f) = 836(T_f - 20), i.e. 22 600+4180−41.8 Tf=836 Tf−16 72022\,600 + 4180 - 41.8\,T_f = 836\,T_f - 16\,720.

Step 4. Collect: 43 500=877.8 Tf43\,500 = 877.8\,T_f, so

Tf=43 500877.8=49.6 ∘CT_f = \frac{43\,500}{877.8} = \boxed{49.6\ ^\circ\mathrm{C}}

Step 5. Feel the size of the latent term. Ten grams — one twentieth of the water's mass — dragged the mixture up by nearly 3030 K. Replace the steam with 1010 g of liquid water at 100 ∘C100\ ^\circ\mathrm{C} and equation (5) gives only 23.8 ∘C23.8\ ^\circ\mathrm{C}: the phase change alone is worth an extra 25.725.7 K. That is why steam burns are so much worse than boiling-water burns — a gram of steam landing on 37 ∘C37\ ^\circ\mathrm{C} skin dumps 25232523 J, against 263263 J for a gram of boiling water: a factor of 9.69.6. Timing note: candidates lose this question by dropping the mscw(100−Tf)m_s c_w(100 - T_f) term — forgetting that the condensate is still at 100 ∘C100\ ^\circ\mathrm{C} and has more heat to give. Budget ninety seconds: completion test, ledger, solve. If the numbers ever give Tf>100 ∘CT_f > 100\ ^\circ\mathrm{C}, do not "round down" — it means some steam never condensed and the true answer is exactly 100 ∘C100\ ^\circ\mathrm{C}.

5 · Competitive level — JEE-Advanced stretch: cold ice, and the calorimeter correction (~5 minutes)

Part (a): repeat Example 3 with the ice starting at −10 ∘C-10\ ^\circ\mathrm{C} instead of 0 ∘C0\ ^\circ\mathrm{C} (cice=2100c_{\text{ice}} = 2100 J/kg·K). Part (b): repeat Example 2, but now the 300300 g of water sits in a 100100 g copper calorimeter (cCu=386c_{\text{Cu}} = 386 J/kg·K) that starts at 20 ∘C20\ ^\circ\mathrm{C} with it. By what percentage was the metal's specific heat underestimated?

Step 1. Part (a): the ice cannot melt until it reaches its melting point, so a sensible term now comes first. Warming 100100 g of ice from −10-10 to 0 ∘C0\ ^\circ\mathrm{C} costs

Qwarm ice=0.100×2100×10=2100 JQ_{\text{warm ice}} = 0.100 \times 2100 \times 10 = 2100\ \mathrm{J}

Use cice=2100c_{\text{ice}} = 2100, not cwc_w — ice is not water, and this is a favourite one-mark theft.

Step 2. Re-run the budget. The water still offers 31 35031\,350 J, but 21002100 J of it is eaten before any melting begins, leaving 29 25029\,250 J for the melt. Demand is still 33 40033\,400 J, so the melt is still incomplete:

mmelted=29 2503.34×105=87.6 g,Tf=0 ∘Cm_{\text{melted}} = \frac{29\,250}{3.34\times10^{5}} = \boxed{87.6\ \mathrm{g}}, \qquad T_f = \boxed{0\ ^\circ\mathrm{C}}

with 12.412.4 g of ice left — about 6.36.3 g more ice saved than in Example 3, bought by the ice's 1010 K head start.

Step 3. Part (b): the calorimeter joins the cold side, because it starts at 20 ∘C20\ ^\circ\mathrm{C} with the water and warms with it. The gaining heat capacity is now

mwcw+mcalccal=0.300×4180+0.100×386=1254+38.6=1292.6 J/Km_wc_w + m_{\text{cal}}c_{\text{cal}} = 0.300 \times 4180 + 0.100 \times 386 = 1254 + 38.6 = 1292.6\ \mathrm{J/K}

Step 4. Redo equation (8) with that corrected capacity:

cmetal=1292.6×50.200×75=646315=430.9 J/kg⋅Kc_{\text{metal}} = \frac{1292.6 \times 5}{0.200 \times 75} = \frac{6463}{15} = \boxed{430.9\ \mathrm{J/kg\cdot K}}

The water-equivalent route must agree, and does: (0.300+0.00923)×4180×5/(0.200×75)(0.300 + 0.00923) \times 4180 \times 5 / (0.200 \times 75) returns the same 430.9430.9.

Step 5. The verdict. Ignoring the cup gave 418418 instead of 430.9430.9 — an underestimate of 3%3\%, and always an underestimate, because the heat the cup absorbed was silently credited to nobody. A systematic error, not a random one: repeating the experiment a hundred times would never fix it. Timing note: part (a) is Example 3 with one extra line at the front — recognise it and it costs ninety seconds. The trap is arithmetic drift: students subtract the 21002100 J from the wrong budget, or add it to the demand side. Keep the sides honest — the ice warming is heat GAINED, so it comes out of the available pot before the melt begins.

Exam traps

Skipping the budget test — the number-one mark killer. Any question containing ice or steam must begin with the completion test, before a single equation for TfT_f is written. Compare the heat available with the heat a complete phase change demands. Get this wrong and everything downstream is wasted ink, however neat the algebra. (CBSE and ICSE reward the test explicitly; JEE and NEET simply put "0 ∘C0\ ^\circ\mathrm{C}" in the options and wait.)

Sign discipline on the ledger. Write each term as a positive quantity and put it on the side it belongs to: bodies that cool go on the LOST side with (Tstart−Tf)(T_{\text{start}} - T_f); bodies that warm, melt or boil go on the GAINED side with (Tf−Tstart)(T_f - T_{\text{start}}) or mLmL. Mixing ΔT=Tf−Tstart\Delta T = T_f - T_{\text{start}} into a "lost" term flips a sign and silently corrupts the answer. If you prefer the ∑Q=0\sum Q = 0 convention, use it consistently — but never blend the two.

Latent heat is mLmL, never mL ΔTmL\,\Delta T — and the wrong cc is just as fatal. There is no temperature change during a phase transition, so there is no ΔT\Delta T to multiply by; conversely, a solid that merely sits at 0 ∘C0\ ^\circ\mathrm{C} without melting gets no latent term at all. Ask of every term: is this body changing temperature, or changing state? It cannot do both at once. And use the right specific heat when it is changing temperature — ice 21002100, water 41804180, steam 20102010 J/kg·K. Writing 41804180 for ice roughly doubles that term and quietly poisons the melt budget. (For ΔT\Delta T itself, Celsius and kelvin are interchangeable: a change of 1 ∘C1\ ^\circ\mathrm{C} is a change of 11 K.)

Forgetting the calorimeter. If the question gives you the cup's mass and specific heat, it wants them used — via (mw+w)cw(m_w + w)c_w with w=mcalccal/cww = m_{\text{cal}}c_{\text{cal}}/c_w, or by adding mcalccalm_{\text{cal}}c_{\text{cal}} straight to the gaining heat capacity. Both routes give the same number. Ignoring the cup is wrong by a few percent in a predictable direction: measured specific heats come out too low, as Example 5 shows (418418 instead of 430.9430.9). CBSE and ISC practicals mark this explicitly.

The metal's temperature drop is to the FINAL temperature. In "hot block into cool water", the drop is (Tmetal−Tf)(T_{\text{metal}} - T_f), not (Tmetal−Twater)(T_{\text{metal}} - T_{\text{water}}). Both bodies end at TfT_f; that is what equilibrium means. This single slip accounts for more wrong specific heats than any other.

An answer outside the starting temperatures is a bug report. A pure mix must land strictly between the two starts. A negative TfT_f, or one above 100 ∘C100\ ^\circ\mathrm{C}, is the algebra telling you that a phase change interrupted the sum and pinned the answer to a plateau. Do not round it away. Go back and re-test.

Origins · 1 minPierre-Simon Laplace and how this was discovered
PL
Pierre-Simon Laplace
1749–1827 · France

Laplace is remembered for the mechanics of the heavens — five volumes proving the Solar System stable — but in the bitter Paris winter of 1782 he built something small and very earthbound. Working with the chemist Antoine Lavoisier, he packed a body inside a shell of crushed ice inside a second shell of ice, and caught the meltwater in a pan. The idea was ruthlessly direct: the heat given out by the body is measured by the mass of ice it melts. Their Mémoire sur la chaleur, presented in 1783, put numbers on the heats of combustion and even on the breathing of a guinea pig, whose warmth melted ice at the rate a slow fire would — evidence that respiration is a kind of combustion. Laplace also fixed Newton's speed of sound by treating the compressions as adiabatic. The word calorimeter is theirs.

History
1760
s — Black develops the method of mixtures, separating the ideas of heat and temperature and putting the first reliable numbers on specific heats.
1761
— Joseph Black, at Glasgow, measures the latent heat of fusion of ice: heat pours in while the thermometer stubbornly reads the melting point.
1765
— James Watt, Black's associate at Glasgow, exploits the latent heat of steam in his separate-condenser engine.
1782
— Lavoisier and Laplace run their ice-calorimeter experiments in Paris, measuring heat by the mass of ice melted.
1783
— Their Mémoire sur la chaleur is presented to the Académie royale des sciences, and quantitative calorimetry begins.
1840
s — Joule's mechanical-equivalent experiments tie the calorimeter's heat to energy in joules, retiring the caloric fluid for good.

Going further

Texts. NCERT Physics Class 11, Ch. 11 (Thermal Properties of Matter) · HC Verma, Concepts of Physics Vol. 2, Ch. 25 (Calorimetry) · Halliday, Resnick and Walker, Fundamentals of Physics, Ch. 18 · Zemansky and Dittman, Heat and Thermodynamics, for the experimental technique.

Provenance. Every number here is recomputed in `verify_hs2-calorimetry-mixing-problems.py` from cw=4180c_w = 4180, cice=2100c_{\text{ice}} = 2100, csteam=2010c_{\text{steam}} = 2010, cCu=386c_{\text{Cu}} = 386, Lf=3.34×105L_f = 3.34\times10^{5}, Lv=2.26×106L_v = 2.26\times10^{6} J/kg. The list a verifier reproduces: the mix at 40 ∘C40\ ^\circ\mathrm{C} with 16 72016\,720 J crossing the ledger; the metal at 418418 J/kg·K, and 430.9430.9 once the cup is counted; the water equivalent 9.239.23 g and the shifted mix at 39.4 ∘C39.4\ ^\circ\mathrm{C}; the ice budget 31 35031\,350 J against 33 40033\,400 J, giving 93.993.9 g melted, 6.16.1 g surviving, Tf=0 ∘CT_f = 0\ ^\circ\mathrm{C}, and a threshold start of 26.6 ∘C26.6\ ^\circ\mathrm{C}; the 5050 g branch at 10.0 ∘C10.0\ ^\circ\mathrm{C}; the steam mix at 49.6 ∘C49.6\ ^\circ\mathrm{C}, against 23.8 ∘C23.8\ ^\circ\mathrm{C} without the latent term; the cold-ice case melting 87.687.6 g; and the ratios Lf/cw=79.9L_f/c_w = 79.9 K, Lv/cw=540.7L_v/c_w = 540.7 K.

Prerequisites. Specific Heat Capacity · The Principle of Calorimetry · Latent Heat and Change of State. Leads to. Heating Curves and Latent-Heat Numericals — the same ledger drawn as a graph, where the plateaus you tested for become flat stretches you can measure.

The deep dive. Calorimetry takes cc as a measured number. Why cc has the value it does is a statistical-mechanics question, opened by the undergraduate article "Heat Capacity of Classical Gases", which counts a molecule's degrees of freedom and predicts cc from first principles. Not needed for any board exam; irresistible once the bookkeeping feels easy.

Why does the temperature refuse to change while ice is melting?

Because the incoming energy is not going into molecular motion — it is going into pulling the crystal apart. Temperature is a measure of the average kinetic energy of the molecules; latent heat goes instead into potential energy, breaking the bonds that lock water molecules into a lattice. Heat flows in, bonds break, the thermometer sits at 0 ∘C0\ ^\circ\mathrm{C} and does nothing. That is what "latent" (hidden) means, and it is why a drink with ice in it stays cold for so long: until the last ice is gone, every joule arriving is spent on melting rather than on warming.

How do I know whether all the ice melts, without solving the whole problem?

Two multiplications. Compute the heat available — everything the warm water can give as it cools to 0 ∘C0\ ^\circ\mathrm{C}, mwcwTwm_w c_w T_w — and the heat demanded to melt the entire block, miLfm_i L_f. If available exceeds demanded, all the ice melts and the surplus warms the mixture above zero. If not, the melt is incomplete, the final temperature is exactly 0 ∘C0\ ^\circ\mathrm{C}, and the mass that melts is (available)/LfL_f. For 300300 g of water at 25 ∘C25\ ^\circ\mathrm{C} and 100100 g of ice: 31 35031\,350 J available against 33 40033\,400 J demanded — not enough, so 93.993.9 g melts and 6.16.1 g of ice survives.

My equation gave a negative final temperature. What went wrong?

Nothing, arithmetically — and everything, physically. A negative TfT_f means you assumed all the ice melts when the energy budget cannot pay for it. The equation dutifully invented liquid water below freezing to make the books balance. Treat it as a diagnostic, not a disaster: go back, run the budget test, and you will find the heat ran out mid-melt. The real answer is Tf=0 ∘CT_f = 0\ ^\circ\mathrm{C} with ice left over. The same story plays out at the top of the scale: an answer above 100 ∘C100\ ^\circ\mathrm{C} in a steam problem means some steam never condensed and the true answer is 100 ∘C100\ ^\circ\mathrm{C}.

Do I have to convert temperatures to kelvin?

Not for mc ΔTmc\,\Delta T, because a difference of one degree Celsius is exactly a difference of one kelvin — the two scales have the same size division, they just start in different places. So a temperature drop of 75 ∘C75\ ^\circ\mathrm{C} is a drop of 7575 K, and calorimetry may be worked entirely in Celsius, which is what every board's marking scheme does. The rule breaks the moment a formula uses the absolute temperature itself rather than a difference — Stefan's T4T^4 radiation law, or the gas laws. There, kelvin is compulsory.

Is the water equivalent a real mass of water?

No — it is an accounting alias. The water equivalent w=mcalccal/cww = m_{\text{cal}}c_{\text{cal}}/c_w is the mass of water that would have the same heat capacity as the calorimeter, so that you can drop the cup from the problem and pretend the vessel simply contained a little extra water. No water is added; nothing physical changes. A 100100 g copper cup has w=9.23w = 9.23 g, meaning it soaks up heat like nine grams of water would. Some questions hand you ww directly (in grams) instead of mcalm_{\text{cal}} and ccalc_{\text{cal}} — when they do, just add it to the water's mass and carry on.

Why is a steam burn so much worse than a boiling-water burn?

Both start at 100 ∘C100\ ^\circ\mathrm{C}, so it is not about temperature — it is about the latent term. A gram of boiling water landing on 37 ∘C37\ ^\circ\mathrm{C} skin can only cool, giving up 1 g×4.18×63=2631\ \mathrm{g} \times 4.18 \times 63 = 263 J. A gram of steam must first condense, releasing 22602260 J, and only then cool: 2260+263=25232260 + 263 = 2523 J, about 9.69.6 times as much energy delivered into the same patch of skin. That factor of nearly ten is the whole reason LvL_v dominates every steam calorimetry problem you will ever be set.

What if the calorimeter and the water start at different temperatures?

Then treat them as separate bodies, exactly as the ledger intends — one may be losing while the other is gaining. The water-equivalent shortcut assumes the cup starts at the water's temperature, which it does in every standard question because the water has been sitting in it. If a question deliberately gives the cup a different start, abandon the shortcut and write its own mcalccal(Tstart−Tf)m_{\text{cal}}c_{\text{cal}}(T_{\text{start}} - T_f) term on whichever side it belongs to. The master equation never breaks; only the shortcuts do.

Before this

Where this leads