By the end of this chapter you'll be able to…

  • 1State the five characteristics of particles of matter and justify each with one everyday observation
  • 2Distinguish solid, liquid and gas by particle arrangement, motion, force and macroscopic properties
  • 3Convert temperatures between Celsius and Kelvin scales
  • 4Explain melting, freezing, vaporisation, condensation, sublimation and deposition with particle-level reasoning
  • 5Define latent heat of fusion and vaporisation and use Q = mL in numerical problems
  • 6Explain why evaporation causes cooling and list the four factors affecting evaporation rate
  • 7Identify everyday examples of the fourth state (plasma) and fifth state (BEC) of matter
  • 8Solve numericals on heat-energy required for phase changes
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Why this chapter matters
Every later chapter in chemistry — atomic structure, chemical reactions, gases laws, thermodynamics — rests on this idea: matter is made of tiny moving particles. Get the particle theory deep in your bones and the rest of school chemistry feels obvious.

Matter in Our Surroundings — Class 9 (CBSE)

Look around. The chair, the air, your bones, the glass of water, even the dust on the screen — all of it is matter. This single chapter holds the most foundational idea in all of physical science: everything is made of tiny particles, and how those particles behave decides whether something is a solid, a liquid, a gas, or something stranger still.


1. The story — why we believe in particles we can't see

Ancient Indian philosopher Maharishi Kanada (≈ 600 BCE) and Greek philosopher Democritus (≈ 400 BCE) both proposed, independently, that all matter is made of tiny indivisible particles. They had no microscopes, no instruments — just careful thought. Cut a stone in half. Then in half again. Keep going. They reasoned: this can't continue forever. There must be a smallest possible piece.

They were right — but it took until the 19th century, with John Dalton's atomic theory, for science to firmly establish the idea. In your bottle of perfume left open across the room — the smell reaches your nose because particles of perfume are zipping through the air. You can't see a single perfume molecule. Yet trillions of them just landed on your nose receptors.

This chapter is about taking that simple "everything is made of particles" idea and using it to explain every visible behaviour of matter — why ice melts, why water boils, why steam is invisible until it cools, why solids hold shape but gases don't, why a cup of hot tea cools down, and how your body sweats to keep cool on a hot day.


2. The big picture — five things to take away

  1. Matter is made of tiny particles with empty space between them.
  2. The particles are in constant motion — they vibrate, slide, or fly around depending on the state.
  3. Particles attract each other — strongly in solids, less in liquids, very weakly in gases.
  4. Temperature changes the energy of these particles and thus changes the state.
  5. Latent heat is the hidden energy needed to break particle bonds — it changes phase without changing temperature.

3. What is matter?

Matter is anything that has mass and occupies space.

The air around you is matter — you can feel it pushing your hand if you wave it. The water in your bottle is matter. The light from a bulb? Light is NOT matter — it has no rest mass and doesn't occupy space.

Five characteristics of particles of matter

  1. Particles are very small — far too small to see with a normal microscope. A drop of water has more particles than there are stars in the Milky Way.
  2. Particles have space between them — when sugar dissolves in water, it disappears because sugar particles fit into spaces between water particles.
  3. Particles are continuously moving — they have kinetic energy. Hot tea cooling? That's energy leaving particles.
  4. Particles attract each other — try breaking iron with your hand vs breaking a piece of chalk. Iron's particles attract much more strongly.
  5. Particles intermix on their owndiffusion. Perfume reaches across a room not because someone fanned it but because particles diffuse.

4. The three classical states of matter

PropertySolidLiquidGas
ShapeFixedTakes containerTakes container
VolumeFixedFixedTakes container
Particle gapVery smallSlightly largerVery large
Particle motionVibrate onlySlide past each otherFly freely
Force between particlesStrongestModerateWeakest
CompressibilityNegligibleSlightHigh
DensityHighestMediumLowest
FluidityNoneHighHighest
ExamplesIron, ice, saltWater, milk, mercuryAir, oxygen, steam

A trick to remember states

  • Solid → Shape & Space fixed.
  • Liquid → Shape changes, Space fixed.
  • Gas → Shape & Space both change.

Why solids are rigid

Particles in a solid are held in fixed positions by strong attractive forces. They can vibrate about their mean positions but cannot move past each other. This rigidity is why your desk doesn't flow even though it's made of zillions of moving particles.

Why liquids flow

Particles in a liquid have enough energy to slip past each other but not enough to escape the surface entirely. A liquid takes the shape of its container but holds onto its volume.

Why gases fill any container

Gas particles move so fast (≈ 500 m/s at room temperature) and have so much space between them that they spread out to fill any container completely. Gases are highly compressible — squeezing a balloon shows you can reduce a gas's volume dramatically because all that space between particles can be removed.


5. Change of state — the fourth thing you must memorise

The state of matter depends on (a) temperature and (b) pressure.

When you heat a solid, particles gain energy and start vibrating harder. Eventually they overcome the strong inter-particle attraction and start to slip past each other → melting (solid → liquid). Keep heating and they gain enough energy to escape the surface entirely → boiling/vaporisation (liquid → gas).

Cool the gas and the reverse happens: condensation (gas → liquid), then freezing (liquid → solid).

There's also a direct path that skips the middle: sublimation is solid → gas without going through liquid (dry ice, camphor, ammonium chloride). The reverse, gas → solid, is deposition (frost on a winter window).

The six phase-change names — memorise

From → ToNameEnergy direction
Solid → LiquidMelting (fusion)Absorbed
Liquid → SolidFreezing (solidification)Released
Liquid → GasVaporisation (boiling/evaporation)Absorbed
Gas → LiquidCondensationReleased
Solid → GasSublimationAbsorbed
Gas → SolidDepositionReleased

Melting point and boiling point

The melting point is the fixed temperature at which a solid changes to liquid at atmospheric pressure. For ice: .

The boiling point is the fixed temperature at which a liquid changes to gas at atmospheric pressure. For water: .

Kelvin scale — convert with one formula

Why use Kelvin? Because is absolute zero — the temperature at which all particle motion theoretically stops. There can be no negative temperature in Kelvin.


6. Latent heat — the hidden energy

Here's the puzzling experimental fact: when ice is melting, even though you keep adding heat, the temperature stays at until all the ice has melted. Where is the heat going?

The heat is being used to break the bonds between water particles — to overcome the attractive forces that held them in the rigid ice structure. This hidden, non-temperature-changing heat is called latent heat.

  • Latent heat of fusion (): heat needed to convert of solid to liquid at its melting point. For ice: .
  • Latent heat of vaporisation (): heat needed to convert of liquid to vapour at its boiling point. For water: .

The formula:

where is heat absorbed/released, is mass, and is the appropriate latent heat.

Why steam burns more than boiling water

Both are at when they touch your skin. But steam additionally carries the latent heat of vaporisation () which it releases as it condenses on your skin. That's why a steam burn is much more severe than a hot-water burn at the same temperature.


7. Evaporation — the cousin of boiling

Evaporation is the conversion of liquid to gas at any temperature below the boiling point, occurring only at the surface.

Unlike boiling (which happens at a fixed temperature throughout the liquid), evaporation happens at any temperature — wet clothes dry on a cool morning, sweat evaporates from your skin in shade.

Factors affecting evaporation rate

  1. Surface area ↑ → evaporation ↑ (clothes spread out dry faster).
  2. Temperature ↑ → evaporation ↑ (warm day, faster drying).
  3. Humidity ↓ → evaporation ↑ (a dry day, faster drying).
  4. Wind speed ↑ → evaporation ↑ (wind sweeps away water vapour, more space for new vapour).

Why evaporation causes cooling

Particles with the highest kinetic energy escape the liquid surface during evaporation. The remaining particles have lower average kinetic energy — and average kinetic energy IS temperature. So the liquid cools.

This is why:

  • Sweat cools your body: sweat evaporates, taking heat from your skin.
  • Earthen pots ("matka") keep water cool: water seeps through tiny pores and evaporates from the outer surface, cooling the inside.
  • A wet handkerchief on your forehead feels cool on a hot day.
  • Acetone or spirit feels cold on the skin — they evaporate very quickly (low boiling point) and steal heat fast.

8. The fourth and fifth states — plasma and BEC

For most of the 19th century, scientists thought there were only three states: solid, liquid, gas. The 20th century added two more.

Plasma

At extremely high temperatures (typically above ), gas particles lose their electrons and become a soup of charged ions and free electrons — this is plasma, the fourth state of matter. Plasma is electrically conductive and responds to magnetic fields.

You see plasma every day:

  • The sun and stars are giant balls of plasma.
  • A fluorescent tube or neon sign has plasma glowing inside.
  • Lightning is a brief flash of plasma in the atmosphere.
  • The aurora borealis (northern lights) is plasma high in Earth's atmosphere.

Plasma is by far the most abundant state of matter in the universe (≈ 99% by mass) — it's just that on Earth, conditions favour solids, liquids and gases.

Bose-Einstein condensate (BEC)

In 1924, Indian physicist Satyendra Nath Bose and Albert Einstein theoretically predicted a strange new state of matter at temperatures so low (, much colder than outer space) that atoms lose their individual identity and merge into one giant "super-atom" governed by quantum mechanics. This is called the Bose-Einstein condensate (BEC) — the fifth state of matter.

BEC was finally created in 1995 by Eric Cornell, Carl Wieman and Wolfgang Ketterle, who won the 2001 Nobel Prize. BEC particles behave like a single quantum wave — they can flow without friction (superfluidity), let light pass through them at (instead of the usual ), and exhibit other bizarre quantum phenomena.


9. Solidified summary — what you must memorise

  • Matter = anything with mass + volume.
  • Particles: small, spaced, moving, attracting, intermixing.
  • 3 classical states (solid, liquid, gas) + 2 modern (plasma, BEC).
  • Temperature ↑ + pressure ↓ → favors gas. Temperature ↓ + pressure ↑ → favors solid.
  • Melting & boiling points are FIXED for a pure substance.
  • . Absolute zero is .
  • Latent heat: . Fusion = , vaporisation = for water.
  • Evaporation: surface-only liquid → gas, at any temp, causes cooling.
  • Plasma: super-hot ionised gas. BEC: ultra-cold quantum state predicted by Bose.

10. Closing thought

You started this chapter thinking matter was the boring obvious stuff around you. You're ending it knowing that:

  • The air in this room contains molecules in constant high-speed motion.
  • The water in your glass is the same molecules that fell as rain on a dinosaur 65 million years ago.
  • Inside your sun, hydrogen plasma is fusing into helium and pouring energy across the solar system.
  • And in a lab in Boulder, Colorado, physicists have created matter so cold that thousands of atoms behave like one big single atom.

Three pages ago you knew "matter is stuff". Now you understand stuff — and the leap from that to the rest of physics and chemistry is short.

Key formulas & results

Everything you need to memorise, in one card. Screenshot this for revision.

Celsius to Kelvin
T(K) = T(°C) + 273.15
Absolute zero = 0 K = −273.15 °C. No negative Kelvin.
Kelvin to Celsius
T(°C) = T(K) − 273.15
Latent heat formula
Q = m × L
Q in J, m in kg, L in J/kg. Use during phase changes only.
Latent heat of fusion (ice)
L_f = 334 kJ/kg = 3.34 × 10⁵ J/kg
Heat to melt 1 kg of ice at 0 °C.
Latent heat of vaporisation (water)
L_v = 2260 kJ/kg = 22.6 × 10⁵ J/kg
Heat to vaporise 1 kg of water at 100 °C.
Heat-temperature change
Q = m c ΔT
Used outside phase changes. c = specific heat capacity.
Density
ρ = m / V
SI unit kg/m³. Solids > liquids > gases (generally).
Atmospheric pressure
1 atm = 101.325 kPa = 76 cm Hg
Boiling point quoted at 1 atm by convention.
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Common mistakes & fixes

These are the exact errors that cost students marks in board exams. Read them once, save yourself the trouble.

WATCH OUT
Saying 'particles of gas are weightless'
Gas particles have mass — that's why air has measurable weight. They appear weightless because density is low, not because individual particles lack mass.
WATCH OUT
Confusing evaporation with boiling
Evaporation: surface-only, at any temp, slow. Boiling: throughout the liquid, only at boiling point, vigorous.
WATCH OUT
Forgetting to convert °C to K in numerical problems
Kelvin scale is mandatory for many physics formulas. Always check the question's units.
WATCH OUT
Saying steam at 100 °C and boiling water at 100 °C cause the same burn
Steam carries extra latent heat of vaporisation (~2260 kJ/kg) released on condensing → far worse burn.
WATCH OUT
Treating sublimation as a slow evaporation
Sublimation is solid directly to gas (no liquid step). Camphor, dry ice, naphthalene balls sublime.
WATCH OUT
Saying a solid has 'no spaces between particles'
Solid particles still have tiny spaces — that's why solids can expand on heating. They're packed tightly, not infinitely tightly.
WATCH OUT
Wrong unit conversion: 1 kJ ≠ 1000 J
1 kJ = 1000 J always. Many marks lost to this. Latent heat of fusion of ice = 334 kJ/kg = 334000 J/kg.

NCERT exercises

Every NCERT exercise from this chapter — what it covers and how many questions to expect.

Section 1.2 (in-text)
Section 1.2 (in-text)
Particle characteristics: salt in water, smell of perfume, intermixing in liquids/gases
4
Questions
Section 1.3 (in-text)
Section 1.3 (in-text)
Solid/liquid/gas comparison, compressibility, container-filling behaviour
3
Questions
Section 1.4 (in-text)
Section 1.4 (in-text)
Phase changes, melting and boiling points, latent heat numericals
6
Questions
Section 1.5 (in-text)
Section 1.5 (in-text)
Evaporation: cooling effect, factors affecting rate, sweat physiology
4
Questions
End-of-chapter
End-of-chapter
Mixed: conceptual, particle-level reasoning, numericals on Kelvin conversion and latent heat
12
Questions

Practice problems

Work through this chapter's problems as a readiness check — reveal each solution, mark yourself honestly, and get your gap report at the end.

Readiness check

Are you exam-ready for Matter in Our Surroundings?

16 problems from this chapter. Try each one, reveal the worked solution, mark yourself honestly — get your gap report at the end.

16 questions~11 min worth ~8 marks in West Bengal (WBBSE) exams

5-minute revision

The whole chapter, distilled. Read this the night before the exam.

  • Matter = mass + volume. Light, sound, heat are NOT matter.
  • Five particle properties: small, spaced, moving, attracting, intermixing.
  • 3 classical states: solid (fixed shape & vol), liquid (vol only), gas (neither).
  • Particle motion: vibrate (solid), slip (liquid), fly free (gas).
  • Conversion: T(K) = T(°C) + 273.15. Absolute zero = 0 K.
  • 6 phase-change names: melting, freezing, vaporisation, condensation, sublimation, deposition.
  • Latent heat formula Q = mL. Ice: L_f = 334 kJ/kg. Water: L_v = 2260 kJ/kg.
  • Evaporation: surface-only liquid → gas, at any temp, removes high-energy particles → cools surroundings.
  • Factors of evaporation: ↑ area, ↑ temp, ↓ humidity, ↑ wind → ↑ rate.
  • 4th state: plasma (sun, neon signs, lightning). 5th state: Bose-Einstein condensate (predicted by S.N. Bose, made in 1995).

West Bengal (WBBSE) marks blueprint

Where the marks come from in this chapter — so you can plan your prep.

Typical chapter weightage: 6–8 marks

Question typeMarks eachTypical countWhat it tests
MCQ / Assert-Reason12–3Factual recall, concept identification
Short answer (2-mark)22Define, state, or give one example
Short answer (3-mark)31Explain process or compare two concepts
Long answer (5-mark)51Describe in detail with diagram
Prep strategy
  • Draw and label diagrams for all biological/physical processes — diagram questions are reliable marks
  • Know both the DEFINITION and the EXAMPLE for every key term
  • For 5-mark answers: intro → body (3–4 points) → conclusion. Use subheadings
  • Practise CBSE sample papers: question patterns repeat year after year

Where this shows up in the real world

This chapter isn't just an exam topic — it lives in the world around you.

Refrigerators

Use the cooling effect of evaporation. A refrigerant evaporates inside the cold compartment (absorbing heat), then condenses outside the fridge (releasing heat) — repeat 24×7.

Sweating

Your body's built-in evaporative cooling. Each gram of sweat that evaporates carries away ~2.4 kJ of heat — that's how humans can survive in 40 °C+ heat.

Pressure cookers

Trap steam so internal pressure rises above 1 atm; water then boils at ~120 °C, cooking food faster. Reverse-engineering the boiling-point-vs-pressure relation.

Dry ice for cold chain

Sublimes directly to gas — no messy liquid leftover. Used to ship vaccines, ice cream and lab samples.

Earthen pots (matka)

Ancient Indian evaporative cooling tech — porous clay walls let water seep out and evaporate, cooling whatever's inside. Works without electricity.

Hot-air balloons

Air is matter and follows particle theory. Heat air → particles speed up, spread out → density drops → balloon rises (buoyancy).

Exam strategy

Battle-tested tips from teachers and toppers for this chapter.

1
For state-change numericals, ALWAYS split into 'phase changes' (use Q = mL) and 'temperature changes' (use Q = mcΔT). Combining them is the most common error.
2
Always convert grams to kilograms. L is given in kJ/kg — using grams will give you answers 1000× too large.
3
If a question asks for steam burns or 'how much energy', remember latent heat dwarfs sensible heat for water. Steam carries 2260 kJ/kg extra.
4
For 'why' questions about evaporation/diffusion, link your answer to PARTICLE motion + kinetic energy. CBSE marks the conceptual chain, not just the conclusion.
5
Memorise the four factors of evaporation in order. Most 3-mark questions ask for two; you should write three if time allows.
6
Don't confuse the names of the six phase changes — sublimation and deposition are commonly swapped.

Going beyond the textbook

For olympiad aspirants and curious learners — topics that build on this chapter.

STRETCH
Triple point and phase diagrams: at certain (P, T) all three states coexist; learn to read a P-T phase diagram (water vs CO₂).
STRETCH
Kinetic theory of gases: PV = nRT and how it explains gas laws (Boyle, Charles, Gay-Lussac) from particle motion.
STRETCH
Joule-Thomson effect: real gases cool when expanding through a valve — the basis of refrigeration cycles.
STRETCH
Superfluidity: at extreme cold (helium-4 below 2.17 K), liquids flow with zero viscosity — climbing the walls of containers.

Where else this chapter is tested

CBSE board isn't the only one — other exams test this chapter too.

NTSE / NMMSMedium — particle-theory MCQs and Kelvin conversions are routine
Olympiad (NSEJS)High — phase diagrams, latent heat numericals appear frequently
JEE FoundationMedium — foundation for thermodynamics in Class 11
NEET FoundationMedium — links to biology via osmosis, evaporation, fluid physiology

Questions students ask

The real ones — pulled from the Q&A community and tutor sessions.

Because the supplied heat is being used as 'latent heat' to break inter-particle bonds, not to raise particle kinetic energy. Temperature is the average kinetic energy, so it stays constant until all bonds in that phase are broken.

Plasma's particles are IONISED — electrons have been stripped off, leaving a soup of positive ions and free electrons. This makes plasma electrically conductive and responsive to magnetic fields — properties no normal gas has.

Yes — at water's 'triple point' (0.01 °C, 611.7 Pa), all three states coexist in equilibrium. This is a fixed physical constant used to define the Kelvin scale.

It's the EVAPORATION that cools, not the water itself being cold. The fastest-moving water molecules escape your skin, taking heat with them. A glass of water at body temperature has no driving force for net evaporation off your skin.

Pure water vapour (gas) is invisible. The white 'mist' you see is tiny liquid water droplets — vapour that has cooled and re-condensed in the cooler surrounding air. So the visible cloud isn't steam, it's condensed steam.

It isn't a special physical constant — it's just that 27 °C (a comfortable room temperature) happens to equal exactly 300.15 K. Convenient memorisation, nothing more.
Verified by the tuition.in editorial team
Last reviewed on 18 May 2026. Written and reviewed by subject-matter experts — read about our process.
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