Fundamentholfundamenthol

Change of State And Calorimetry

PhysicsThermal Properties Of MatterFor NEET aspirants

Calorimetry is the measurement of heat using one rule: in an isolated system, heat lost by hot bodies equals heat gained by cold bodies. Change of state adds latent heat, , absorbed or released at constant temperature. Together, change of state and calorimetry give the mixture problems (ice, water and steam) that appear in almost every NEET and JEE Main paper. This page covers the law of mixtures, latent heats, the heating curve, the effect of pressure, phase diagrams and a fail-safe method for ice-water problems.

On this page1Principle of calorimetry2Calorimeter3States and changes4Latent heat5Heating curve6Pressure effects7Phase diagrams8Mixture method
Key Formulas - Quick Reference
  1. ★ Must learnPrinciple of calorimetry: heat lost heat gained,
  2. Mixture temperature (no phase change):
  3. ★ Must learnLatent heat: , at constant temperature
  4. ★ Must learnIce: ; water:
  5. ;
  6. Heating curve at constant power : slope ; flat time
  7. Calorimeter of water equivalent : add to the mass of water in the heat balance
  8. Triple point of water: , ()

1. Principle of Calorimetry (Law of Mixtures)

★ Must learn

When bodies at different temperatures are mixed in an insulated container, heat flows until they reach a common temperature . If no heat is lost to the surroundings, heat lost by the hot bodies = heat gained by the cold bodies. This is energy conservation applied to heat.

Written with signs, the total heat exchanged is zero: , which gives the weighted average

valid when no body changes state. The "weights" are the heat capacities , so lies nearer the temperature of the body with the larger heat capacity.

Principle of calorimetry: heat lost by the hot body equals heat gained by the cold body On a vertical temperature axis the hot body 1 falls from T1 to the mixture temperature Tm and the cold body 2 rises from T2 to Tm. Heat lost m1 s1 times T1 minus Tm equals heat gained m2 s2 times Tm minus T2. temperature T1 Tm T2 1 hot body cools heat lost = m1 s1 (T1 − Tm) 2 cold body warms heat gained = m2 s2 (Tm − T2) common final temperature Tm
Figure 1: Principle of calorimetry (law of mixtures). Both bodies end at the same temperature , which always lies between and ; if no heat escapes, heat lost heat gained.

1.1 The calorimeter

A calorimeter is a thin copper or aluminium can (small heat capacity, reaches the common temperature quickly) with a stirrer and a thermometer, kept inside an insulating jacket with a lid. The can itself takes part in the exchange: include its heat capacity , or its water equivalent , on the side it belongs to.

Calorimeter used in the method of mixtures A copper calorimeter can holding water, with a stirrer and a thermometer passing through an insulating lid. The can sits inside an outer insulating jacket so that little heat is exchanged with the surroundings. stirrer thermometer copper can (good conductor) insulating jacket water / liquid insulating lid
Figure 2: A calorimeter: a thin copper can (small heat capacity, conducts quickly) with stirrer and thermometer, kept in an insulating jacket so that heat lost = heat gained holds inside it.
Exam Trick

Equal masses of the same liquid: is the plain average. For equal heat capacities, . For identical portions at different temperatures, is the mean of the temperatures. Always check that your lies between the extreme temperatures.

2. States of Matter and Change of State

Matter exists as solid, liquid or gas. A change from one state to another is a change of state (phase change). While it happens, the heat supplied breaks or loosens the bonds between molecules (increases their potential energy) instead of making them move faster, so the temperature stays constant until the change is complete.

ChangeDirectionTemperature nameHeat
Melting (fusion)solid → liquidmelting pointabsorbed
Freezing (solidification)liquid → solidfreezing point (same as melting point)released
Vaporisation (boiling)liquid → vapourboiling pointabsorbed
Condensationvapour → liquidsame as boiling pointreleased
Sublimationsolid → vapour directlysublimation pointabsorbed
Depositionvapour → solid directlyreleased
Solid, liquid and gas and the changes of state between them Three boxes show particles in a solid in a regular lattice, a liquid close together but disordered, and a gas far apart moving randomly. Arrows show melting and freezing, boiling and condensing, and sublimation from solid to gas with deposition back. Solid fixed shape, fixed volume Liquid fixed volume, flows Gas fills its container melting freezing boiling condensing sublimation (camphor, iodine, dry ice) deposition (frost)
Figure 3: Changes of state. Red arrows absorb heat (melting, vaporisation, sublimation); blue arrows release the same latent heat (freezing, condensation, deposition). Temperature stays constant during each change.
Evaporation

At all temperatures, from the surface only, slow and silent. Faster with larger area, wind, higher temperature and lower humidity. Causes cooling (sweat, earthen pots).

Boiling

At one temperature for a given pressure (vapour pressure outside pressure), throughout the liquid with bubbles, fast. Temperature stays fixed while it lasts.

3. Latent Heat

★ Must learn

The latent heat of a substance is the heat absorbed or released per unit mass during a change of state at constant temperature:

SI unit . Latent heat of fusion : solid ↔ liquid at the melting point. Latent heat of vaporisation : liquid ↔ vapour at the boiling point. Both are measured at 1 atm unless stated.

For water, take ( to ) and () unless the question gives other values. for every substance, because separating molecules completely (liquid to gas, with a large expansion against the atmosphere) needs far more energy than loosening them (solid to liquid).

SubstanceMelting point (°C) ()Boiling point (°C) ()
Water03331002256
Ethanol−11410478854
Mercury−3911.8357272
Lead32824.51750868
Gold106364.526601580
Nitrogen−21025.5−196201
Oxygen−21913.8−183213
  • Steam burns are worse than boiling-water burns: of steam at gives on condensing before it even starts cooling, about nine times what of boiling water gives cooling to body temperature.
  • Ice at cools better than water at : each gram absorbs while melting, without warming.
  • Specific heat "during" a phase change would be : the heat goes into latent heat, not into temperature.
Key idea
During a change of state the temperature is constant; the heat changes the molecular potential energy, not the kinetic energy.

4. The Heating Curve

Supply heat steadily to ice below and plot temperature against heat supplied (or time, at constant power). The graph has sloping parts (one state warming) and flat parts (a change of state):

  1. Ice warms: slope .
  2. Ice melts at : flat, length .
  3. Water warms: slope , half as steep as for ice, since .
  4. Water boils at : flat, length , the longest part ().
  5. Steam warms: slope , about as steep as for ice.
Heating curve of 100 g of ice at minus 10 degrees Celsius to steam at 120 degrees Celsius Temperature against heat supplied, drawn to scale for 100 grams of ice. The ice warms to 0 degrees with 0.5 kilocalorie, melts at constant temperature with 8 kilocalories, the water warms to 100 degrees with 10 kilocalories, boils at constant temperature with 54 kilocalories, and the steam warms to 120 degrees with 1 kilocalorie. A zoomed panel shows the first 20 kilocalories. Q (kcal) T (°C) water + steam: Q = mLv 54 kcal, T constant steam zoomed → 18.5 72.5 0 100 120 Q T 8.5 18.5 0 100 ice + water (Lf) ice water first 20 kcal, stretched
Figure 4: Heating curve drawn to scale for Solved Example 3. Flat parts are phase changes (); sloping parts have slope , so ice and steam () climb twice as steeply as water (). Boiling alone takes of the .
Exam Trick

Read a heating curve like a v-t graph. At constant power : slope of a sloping part (steeper means smaller heat capacity), and length of a flat part . So and .

Step by step heat needed to turn ice at minus 10 degrees into steam at 120 degrees A ladder of five steps: warm the ice to 0 degrees, 500 calories; melt it, 8000 calories; warm the water to 100 degrees, 10000 calories; boil it, 54000 calories; warm the steam to 120 degrees, 1000 calories. Total 73.5 kilocalories. 100 g ice at −10 °C 100 g ice at 0 °C 100 g water at 0 °C 100 g water at 100 °C 100 g steam at 100 °C 100 g steam at 120 °C Q1 = ms ΔT = 100 × 0.5 × 10 = 500 cal Q2 = mLf = 100 × 80 = 8000 cal Q3 = ms ΔT = 100 × 1 × 100 = 10 000 cal Q4 = mLv = 100 × 540 = 54 000 cal Q5 = ms ΔT = 100 × 0.5 × 20 = 1000 cal Total Q = 73 500 cal = 73.5 kcal
Figure 5: Break every heating problem into stages: for each state and at each change of state, then add. The latent-heat steps (bold) usually dominate.
Quick Recall: tap to check
Why is the water part of the heating curve less steep than the ice part?
Slope and water's specific heat is twice that of ice.
Which flat step of the heating curve of water is longer, and why?
Boiling: is much larger than .
At what temperature does water evaporate?
At all temperatures; boiling happens only at the boiling point.

5. Effect of Pressure: Boiling Point and Melting Point

5.1 Boiling point rises with pressure

A liquid boils when its saturated vapour pressure equals the external pressure. Raise the pressure and a higher temperature is needed; lower it and the liquid boils sooner.

  • Pressure cooker: about 2 atm inside, water boils near , so food cooks faster.
  • Hill stations: lower air pressure, water boils below , so cooking takes longer.
  • In a closed flask of hot water, pouring cold water on the flask condenses the vapour, lowers the pressure, and the water boils again.
Boiling point of water against the external pressure Saturated vapour pressure of water against temperature. Water boils when its vapour pressure equals the outside pressure: about 90 degrees Celsius at 0.7 atmosphere on a hill station, 100 degrees at 1 atmosphere and about 120 degrees at 2 atmospheres in a pressure cooker. T (°C) p (kPa) 0 50 100 150 100 200 300 400 500 hill station ≈ 0.7 atm: 90 °C sea level 1 atm: 100 °C pressure cooker ≈ 2 atm: 120 °C
Figure 6: A liquid boils when its vapour pressure equals the pressure above it (curve from the Antoine equation for water). Lower pressure on mountains lowers the boiling point; a pressure cooker raises it, so food cooks faster.

5.2 Melting point and regelation

Substances that expand on melting (wax, most solids) have their melting point raised by pressure. Substances that contract on melting (ice, cast iron, bismuth) have it lowered by pressure: ice melts at about below for each extra atmosphere.

Regelation is the melting of ice under pressure and its refreezing when the pressure is removed. A loaded wire passes through a block of ice without cutting it into two; pressing snow makes a snowball; ice skates glide on a thin film of water under the blade.

Regelation: a loaded wire passes through a block of ice A block of ice rests on two supports. A thin wire loaded with a weight W hangs over it. The high pressure under the wire lowers the melting point so the ice there melts; the water flows above the wire, where the pressure is normal, and freezes again. The wire cuts through but the block stays whole. W ice melts under the wire water above refreezes (pressure removed) The wire passes through, yet the block stays in one piece
Figure 7: Regelation. Pressure lowers the melting point of ice (about per atm), so ice melts under the wire and refreezes above it. The same effect helps ice skates glide and snowballs stick.

6. Triple Point and Phase Diagrams

A phase diagram plots pressure against temperature and shows which state is stable. It has three curves:

  • Sublimation curve (solid ↔ vapour), fusion curve (solid ↔ liquid) and vaporisation curve (liquid ↔ vapour). On a curve two phases coexist; between curves one phase exists.
  • The three curves meet at the triple point, the unique temperature and pressure at which solid, liquid and vapour coexist in equilibrium. For water: () and (). For : () and .
  • The vaporisation curve ends at the critical point (, for water); above it liquid and vapour cannot be told apart and .
Phase diagrams of water and carbon dioxide Two pressure against temperature phase diagrams, not to scale. Each has solid, liquid and vapour regions separated by the sublimation, vaporisation and fusion curves, meeting at the triple point, with the vaporisation curve ending at the critical point. For water the fusion curve slopes to the left; the triple point is 0.01 degrees Celsius and 0.006 atmosphere. For carbon dioxide the fusion curve slopes to the right and the triple point is at 5.11 atmospheres, above 1 atmosphere, so solid carbon dioxide sublimes at minus 78.5 degrees. T p 1 atm solid liquid vapour Water 0 °C 100 °C TP 0.01 °C, 0.006 atm C 374 °C, 218 atm T p 1 atm solid liquid vapour Carbon dioxide −78.5 °C TP −56.6 °C, 5.11 atm C 31.1 °C, 73 atm
Figure 8: Phase diagrams (schematic, not to scale). Three curves meet at the triple point (TP), where solid, liquid and vapour coexist; the vaporisation curve ends at the critical point (C). Water's melting line slopes backwards (ice melts under pressure); 's triple point lies above 1 atm, so dry ice sublimes.

Because the triple point of is above 1 atm, liquid cannot exist at atmospheric pressure: solid ("dry ice") sublimes directly at . Water's fusion curve slopes to the left because ice is less dense than water.

JEE Advanced

The slope of a phase boundary is given by the Clausius-Clapeyron equation, , where , are specific volumes before and after the change. For ice to water, , so : the melting point falls as pressure rises. For boiling, and .

7. Solving Mixture Problems with a Phase Change

When ice or steam is involved, the final state is not known in advance. Test at the phase-change temperature before writing the full balance:

  1. Find the heat the hot side can give while cooling to (or to for steam problems).
  2. Find the heat the cold side needs to reach and change state completely.
  3. Compare. If the hot side has more, the whole of the cold side changes state and is found from the full balance. If less, is the phase-change temperature and only part changes state: mass changed .
Flowchart for solving ice and water mixing problems First find the heat the water can give while cooling to zero degrees, then the heat the ice needs to warm to zero and melt completely. If the available heat is greater, all ice melts and the final temperature is above zero; if equal, final temperature is zero; if smaller, the final temperature is zero and only part of the ice melts. greater equal smaller Ice (mi at Ti ≤ 0 °C) + water (mw at Tw) Qavail = mw sw Tw (water cooling to 0 °C) Qneed = mi si (0 − Ti) + mi Lf (ice warmed to 0 °C and all melted) Compare Qavail with Qneed All ice melts; Tm > 0 from the full heat balance Exactly melts; Tm = 0 °C Tm = 0 °C; melted = (Qavail − mi si |Ti|)/Lf negative? then water freezes instead
Figure 9: The test. Never write one heat balance with an unknown until you know whether all the ice melts; otherwise you may get an impossible answer such as with liquid water.
Exam Trick

Steam mixed with cold water: test at . Heat to bring all the water to versus heat all the steam gives on condensing () plus cooling to . If the water needs less, and some steam remains. One gram of steam can heat about of water from to ().

Quick Recall: tap to check
ice at is mixed with water at . Final state?
Water can give only (less than ): , ice melts.
What is the triple point of water?
and , where ice, water and vapour coexist.
Why does dry ice not melt at 1 atm?
Its triple point is at ; below that there is no liquid phase, so it sublimes.
Mind map of change of state and calorimetry Mind map with change of state and calorimetry at the centre and branches for calorimetry, latent heat, heating curve, effects of pressure, phase diagrams and problem-solving checks. Change of State and Calorimetry Calorimetry heat lost = heat gained Tm = Σ m s T / Σ m s calorimeter: add its W Latent heat Q = mL at constant T Lf (ice) = 80 cal/g = 336 kJ/kg Lv (water) = 540 cal/g = 2256 kJ/kg Heating curve flat: phase change slope = 1/(ms) boiling step is largest Pressure effects boiling point rises with p ice melting point falls with p regelation, pressure cooker Phase diagram triple point 273.16 K critical point: no Lv CO2: dry ice sublimes Problem checks 0 °C test for ice + water steam: 100 °C test Tm between T1 and T2
Figure 10: Mind map of this concept for quick revision.

8. Solved Examples

Solved Example 1
Equal masses of three liquids A, B and C are at , and . When A and B are mixed the temperature is ; when B and C are mixed it is . What is the temperature when A and C are mixed?
Solution:

A and B: ...(1)

B and C: ...(2)

From (1) and (2): .

A and C: .

Answer: .

Mixing temperatures of three liquids A, B and C on a number line Number line of temperature from 8 to 21 degrees Celsius. Liquids A, B and C start at 10, 15 and 20 degrees. A plus B mix to 13 degrees, B plus C to 16 degrees and A plus C to 140 over 11, about 12.7 degrees. T (°C) 8 9 10 11 12 13 14 15 16 17 18 19 20 21 A B C A + B → 13 °C B + C → 16 °C A + C → 140/11 ≈ 12.7 °C Each mixture lies between the two starting temperatures, nearer the liquid with the larger ms
Figure 11: Solved Example 1 on a number line. The mixture temperature is a weighted average , so it sits closer to the liquid with the larger heat capacity.
Solved Example 2
Three liquids of masses , , , specific heats , , and temperatures , , are mixed. Find the temperature of the mixture at thermal equilibrium (no change of state, no loss).
Solution:

The total heat exchanged is zero: .

Answer:

Writing every term as avoids deciding in advance which liquids gain and which lose heat.

Solved Example 3
Find the heat needed to convert of ice at into steam at . (, , , )
Solution:

Ice : .

Melting: .

Water : .

Boiling: .

Steam : .

Answer: (heat absorbed; see Figures 4 and 5).

Solved Example 4
of water at is mixed with of steam at . Find the final temperature and composition of the mixture. (, )
Solution:

Test at . Heat the water needs to reach : .

Heat the steam gives cooling to : . The remaining must come from condensing steam; all of it could give , far more than needed. So .

Steam condensed .

Answer: with about of steam and of water.

Solved Example 5
of ice at is added to of water at . Find the final temperature and the mass of ice left. ()
Solution:

Heat the water can give cooling to : .

Heat to melt all the ice: . Since , not all ice melts and .

Ice melted .

Answer: ; of ice remains (with of water).

Solved Example 6
of ice at is put into of water at . Find the final temperature. (, )
Solution:

Test: ice needs to become water at ; the water can give . So all the ice melts and .

Balance: .

Answer: .

Solved Example 7
A sphere of aluminium of mass at is put into a copper calorimeter of mass containing of water at . The final temperature is . Find the specific heat of aluminium. (, )
Solution:

Heat gained by water and calorimeter: .

Heat lost by aluminium: .

Answer: .

Solved Example 8
Calculate the heat needed to convert of ice at into steam at at 1 atm. (, , , )
Solution:

; .

; .

Answer: .

Solved Example 9
A metal piece at is dropped into of water at in a calorimeter of water equivalent . The final temperature is . Find the specific heat of the metal.
Solution:

Heat gained by water and calorimeter: .

Heat lost by the metal: .

Answer: .

Solved Example 10
What mass of steam at must be passed into of water at to raise its temperature to ? ()
Solution:

Each gram of steam gives (condensing) (cooling from to ) .

Water needs . So .

Answer: .

Solved Example 11
Ice at is heated at a constant rate and melts completely in . How much more time does the water take to reach ? ()
(A) 8 min
(B) 10 min
(C) 12.5 min
(D) 54 min
Solution:

Answer: (B). At constant power, time heat: , so .

Solved Example 12
Why does of steam at burn more than of water at ? Compare the heat each gives to skin at .
Solution:

Steam: (condensing) (cooling to ) . Water: only.

Answer: steam gives about , nearly ten times the from boiling water, because of its latent heat.

Practice Questions
  1. of ice at is mixed with of water at . Find the final temperature and the ice melted.Answer: ;
  2. of steam at is passed into of water at (negligible container). Find the final temperature.Answer: about
  3. How much heat (in kJ) turns of ice at into water at ? (, )Answer:
  4. A metal piece at is dropped into of water at ; the final temperature is . Find the metal's specific heat.Answer: about
  5. Why does the temperature stay constant while ice melts, although heat is supplied?Answer: The heat increases the potential energy of the molecules (breaks the lattice), not their kinetic energy
  6. Why does food cook faster in a pressure cooker?Answer: Higher pressure raises the boiling point to about
  7. In the heating curve at constant power, the melting step lasts and the boiling step . Find .Answer:

Common Mistakes to Avoid

Watch out
  • Writing one heat balance with unknown for ice + water without the test, and getting with liquid water left.
  • Using for ice or steam. Take .
  • Forgetting the calorimeter (or its water equivalent) on the heat-gaining side.
  • Adding latent heat when there is no change of state, or forgetting it when there is one.
  • Assuming steam condenses completely. Test at first: often only part of it condenses.
  • Mixing units: calories with kilograms or joules with grams. With and , masses must be in grams and heat in calories.
  • Saying pressure always raises the melting point. It lowers the melting point of ice (it contracts on melting).
  • Confusing evaporation (any temperature, surface) with boiling (one temperature, throughout the liquid).

Frequently Asked Questions

What is the principle of calorimetry?

The principle of calorimetry says that when bodies at different temperatures are mixed in an insulated container, the heat lost by the hotter bodies equals the heat gained by the colder bodies, until all reach a common temperature. It is the law of conservation of energy for heat.

What is latent heat?

Latent heat is the heat absorbed or released per unit mass when a substance changes state at constant temperature, . For water and .

Why does temperature remain constant during a change of state?

During melting or boiling the heat supplied is used to overcome the attraction between molecules, which raises their potential energy. Their average kinetic energy, and so the temperature, does not change until the whole substance has changed state.

Why is the latent heat of vaporisation greater than the latent heat of fusion?

Melting only loosens the molecules, which stay close together. Vaporisation separates them completely and the vapour expands a lot against the atmosphere, so much more energy is needed per kilogram.

What is the triple point of water?

The triple point of water is the single temperature and pressure, and about , at which ice, liquid water and water vapour coexist in equilibrium. It is used as the fixed point of the Kelvin scale.

What is regelation?

Regelation is the melting of ice under increased pressure and its refreezing when the pressure is removed. It happens because pressure lowers the melting point of ice. A loaded wire passing through an ice block without splitting it is the classic demonstration.

How are calorimetry questions asked in NEET?

NEET asks direct mixture problems, usually ice with water or steam with water, the heat needed to turn ice into steam, and reading a heating curve. Always check whether all the ice melts before finding the final temperature.

What calorimetry problems come in JEE Main?

JEE Main uses mixtures with phase changes, water equivalent of a calorimeter, heating curves at constant power, the ratio of latent heats from graph lengths, and energy conversion from falling or moving bodies into melting ice.

Previous year questions on Change of State And Calorimetry

6 questions from past papers, each with a step-by-step solution.

Ready to master Thermal Properties Of Matter?

Take a full mock test, practice concept-by-concept, and get an AI-powered rank prediction — all on Fundamenthol.