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medium importance~1 Q in Tier 127 formulas⚡ 12 shortcuts6 subtopics

Heat, temperature and sound

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Temperature and heat

  • Scales: C/100 = (F − 32)/180 = (K − 273)/100. −40° is the same on Celsius and Fahrenheit.
  • Normal body temperature 37 °C = 98.6 °F = 310 K. Absolute zero = 0 K = −273.15 °C.
  • Water boils at 100 °C at sea level; boiling point falls at high altitude (lower pressure) — a pressure cooker raises pressure and hence boiling point.
  • Water has a high specific heat → coastal areas have moderate climate; used as a coolant.
  • Latent heat: burns from steam are worse than from boiling water because steam gives out extra latent heat of vaporisation on condensing.
  • Anomalous expansion: water is densest at 4 °C, so lakes freeze from the top and aquatic life survives below.
  • Evaporation causes cooling — earthen pots (matka), sweating.
  • Heat transfer: conduction (solids), convection (fluids — sea breeze by day, land breeze by night), radiation (no medium needed — Sun's heat). A thermos flask cuts all three.
  • Dark, rough surfaces are good absorbers and good emitters; light, shiny surfaces reflect heat (white clothes in summer).

Sound

  • Sound is a mechanical, longitudinal wave in air — it needs a medium and cannot travel in a vacuum.
  • Speed: solids > liquids > gases. In air about 332 m/s at 0 °C and about 343 m/s at 20 °C; it rises with temperature and humidity, but does not depend on pressure.
  • Human audible range 20 Hz – 20,000 Hz. Infrasonic < 20 Hz (earthquakes, elephants, whales). Ultrasonic > 20 kHz (bats, dolphins, SONAR, ultrasound scanning).
  • Pitch depends on frequency (women's and children's voices have higher pitch); loudness on amplitude; quality/timbre on the waveform.
  • Echo needs a gap of about 0.1 s → reflecting surface at least about 17 m away.
  • Doppler effect — apparent change in frequency when source and listener move relative to each other (siren pitch rises as it approaches; speed radars).
  • Mach number = object speed ÷ speed of sound; > 1 is supersonic (causes a sonic boom).
  • Resonance — soldiers break step while crossing a bridge.

Detailed notes

Heat and temperature are different

Heat is energy that flows from a hotter body to a colder one (unit: joule; older unit calorie). Temperature tells how hot a body is — the average energy of its particles (unit: kelvin). A bucket of warm water holds more heat than a cup of boiling water, though the cup is at a higher temperature.

Temperature scales

ScaleIce meltsWater boils
Celsius0 °C100 °C
Fahrenheit32 °F212 °F
Kelvin273 K (273.15)373 K
Conversions: F=95C+32F = \frac{9}{5}C + 32 and K=C+273K = C + 273. Celsius and Fahrenheit agree at −40°. Normal body temperature is 37 °C = 98.6 °F. The lowest possible temperature is 0 K (absolute zero) = −273.15 °C. A clinical thermometer reads about 35–42 °C; a pyrometer measures very high temperatures (furnaces).

Specific heat and latent heat

  • Specific heat is the heat needed to raise 1 kg of a substance by 1 °C. Water has a very high specific heat, so it heats and cools slowly. That is why coastal places have mild climates, why water is used in car radiators and hot-water bottles.
  • Latent heat is heat taken or given during a change of state without any change in temperature. Steam at 100 °C burns more than water at 100 °C because it also releases its large latent heat of vaporisation when it condenses on skin. Ice at 0 °C cools a drink better than water at 0 °C because melting absorbs latent heat.
  • Evaporation causes cooling: water in an earthen pot (matka) stays cool, sweating cools the body, a wet cloth feels cold. Evaporation is faster with more surface area, heat, wind and dry air.

Boiling, melting and pressure

Higher pressure raises the boiling point — a pressure cooker cooks faster because water boils above 100 °C inside it. On mountains air pressure is low, water boils below 100 °C, and food cooks slowly. Pressure lowers the melting point of ice (regelation — two ice blocks pressed together join).

Anomalous expansion of water

Most things expand on heating. Water contracts from 0 °C to 4 °C and then expands, so it is densest at 4 °C. In winter the top of a lake freezes first and floating ice insulates the water below, which stays near 4 °C — fish survive. Pipes burst in frost because water expands on freezing. Gaps in railway tracks and sagging electric wires in summer are examples of ordinary thermal expansion.

Three ways heat travels

  • Conduction — through solids, particle to particle (hot spoon handle). Metals conduct well; wood, plastic and air are insulators.
  • Convection — by movement of the liquid or gas itself. Sea breeze (day) and land breeze (night), boiling water, room heaters.
  • Radiation — no medium needed; the Sun's heat reaches us this way. Dark, rough surfaces absorb and emit well; white clothes keep us cool in summer. A thermos flask blocks all three: vacuum (conduction and convection) and silvered walls (radiation).

Sound — a mechanical wave

Sound is produced by vibration and travels as a longitudinal wave that needs a medium; it cannot travel in vacuum (astronauts use radio). Speed of sound: about 343 m/s in air at 20 °C (≈ 332 m/s at 0 °C), ≈ 1500 m/s in water, ≈ 5000 m/s or more in steel — solids > liquids > gases. Speed rises with temperature and humidity; pressure alone does not change it.

Frequency ranges and characteristics

  • Human audible range: 20 Hz to 20,000 Hz. Below 20 Hz = infrasonic (earthquakes, elephants, whales). Above 20 kHz = ultrasonic (bats, dolphins, SONAR, ultrasound scans, cleaning).
  • Pitch depends on frequency (women and children have higher-pitched voices). Loudness depends on amplitude, measured in decibel (dB). Quality (timbre) depends on the waveform — it lets us tell a sitar from a flute at the same note.

Echo, Doppler effect and resonance

  • Echo: reflected sound heard separately if it returns after at least 0.1 s — needs a reflector about 17 m away. Distance = speed × time ÷ 2.
  • Doppler effect: an approaching horn sounds higher-pitched, a receding one lower.
  • Resonance: a body vibrates strongly when pushed at its natural frequency — soldiers break step on bridges; tuning a radio.
  • Sonic boom: produced by objects moving faster than sound (supersonic).

Quick revision

  • F = 9C/5 + 32; K = C + 273; −40 °C = −40 °F; body 37 °C = 98.6 °F.
  • Water: highest specific heat, densest at 4 °C.
  • Steam burns worse — latent heat. Pressure cooker — higher boiling point.
  • Conduction (solids), convection (fluids, breezes), radiation (Sun, no medium).
  • Sound: solids fastest, vacuum none; 20 Hz–20 kHz; pitch ↔ frequency, loudness ↔ amplitude.

Types of questions asked

Every way this subtopic shows up in exams — how to recognise it, the formula or logic to use, and a solved example.

Type 1: Temperature scale conversionvery common3 practice Q
How to spot it:

A temperature in one scale to convert, or 'at what temperature do two scales read the same / one reads double the other'.

C5=F−329=K−2735\frac{C}{5}=\frac{F-32}{9}=\frac{K-273}{5}
  1. Write C/5 = (F − 32)/9.
  2. Substitute the given value (or the condition, e.g. F = C or F = 2C) and solve.
  3. For Kelvin just add 273. Why: 100 Celsius divisions cover the same range as 180 Fahrenheit divisions, so the ratio is 5 : 9 with a 32° offset.

Example: Convert 25 °C to Fahrenheit.

F = 9/5 × 25 + 32 = 45 + 32 = 77 °F.

Type 2: Everyday heat effect → reasonvery common4 practice Q
How to spot it:

'Why does steam burn more / pressure cooker cook faster / earthen pot cool water / fish survive frozen lakes / coastal climate mild?'

  1. Change of state with no temperature change → latent heat.
  2. Slow heating/cooling of water → high specific heat.
  3. Boiling point up with pressure, down at altitude.
  4. Cooling without a fridge → evaporation.
  5. Lakes freeze from the top → anomalous expansion (max density at 4 °C).

Example: Why does food take longer to cook on high mountains?

Air pressure is low, so water boils below 100 °C; food gets less heat and cooks slowly.

Type 3: Mode of heat transfercommon2 practice Q
How to spot it:

A situation (sea breeze, Sun's heat, hot spoon handle, thermos flask, white clothes) and options conduction/convection/radiation.

  1. Heat moves through a solid without the solid moving → conduction.
  2. The warm fluid itself moves (breezes, boiling) → convection.
  3. No medium / across empty space / colour matters → radiation.

Example: Land breeze blowing at night is an example of —

Convection — the sea is warmer at night, air over it rises, and cooler air from the land moves in.

Type 4: Speed of sound and the mediumcommon2 practice Q
How to spot it:

'Sound travels fastest in…', 'cannot travel through…', 'speed of sound increases with…'.

  1. Order: solids > liquids > gases; vacuum = no sound.
  2. Temperature and humidity raise the speed in air; pressure alone does not change it.
  3. Remember air ≈ 343 m/s, water ≈ 1500 m/s, steel ≈ 5000 m/s.

Example: Why is the sound of an approaching train heard earlier by putting an ear to the rail?

Sound travels much faster in steel (a solid) than in air.

Type 5: Frequency ranges; pitch, loudness, qualityvery common3 practice Q
How to spot it:

Audible range, infrasonic/ultrasonic users (bats, dolphins, elephants), or which property of a wave decides pitch/loudness/timbre.

  1. Audible 20 Hz–20 kHz; below = infrasonic; above = ultrasonic.
  2. Pitch ↔ frequency; loudness ↔ amplitude (dB); quality ↔ waveform.
  3. Ultrasound uses: SONAR, medical scans, bats' echolocation.

Example: Sound waves of frequency 10 Hz are called —

Infrasonic — they are below the 20 Hz lower limit of human hearing.

Type 6: Echo, Doppler effect and resonanceoccasional3 practice Q
How to spot it:

Echo-distance numericals, 'pitch of approaching horn rises', 'soldiers break step on a bridge'.

d=v×t2d=\frac{v\times t}{2}
  1. Echo: sound goes to the reflector and back, so distance = v × t ÷ 2.
  2. Change in heard pitch because source/listener moves → Doppler effect.
  3. Large vibration at the natural frequency → resonance.

Example: An echo returns in 3 s; speed of sound is 330 m/s. How far is the reflecting wall?

d = 330 × 3 ÷ 2 = 495 m.

Formulas

Temperature scales
C100=F−32180=K−273100\frac{C}{100} = \frac{F-32}{180} = \frac{K-273}{100}

−40 °C = −40 °F

Heat absorbed
Q=mc ΔTQ = mc\,\Delta T

c = specific heat

Latent heat
Q=mLQ = mL

no temperature change during phase change

Wave speed
v=fλv = f\lambda

speed = frequency × wavelength

Echo distance
d=v t2d = \frac{v\,t}{2}

sound travels to the wall and back

Shortcut tricks

⚡ Sound speed order: 'Steel Shouts, Water Whispers, Air Awaits'

Solids fastest, liquids next, gases slowest; vacuum — no sound at all (astronauts use radio).

⚡ Pitch–frequency, Loudness–amplitude

'Pitch = Frequency' (PF like 'Provident Fund'), 'Loudness = Amplitude' (LA like 'Los Angeles').

Example: The pitch of a sound depends on its?

Frequency.

Where students lose marks

  • Thinking sound speed rises with pressure — it rises with temperature and humidity, not pressure.

  • Calling bats' sounds infrasonic — they are ultrasonic.

  • Saying boiling point rises at hill stations — it falls because air pressure is lower.

Practice sets — 20 questions

Sets of 10, mixed across the question types above. Each answer comes with a step-by-step explanation.

Topic test · 10 questions

Suggested time 3 min · wrong answers go to your mistake notebook automatically.