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Physics — Second Secondary

Physics — Second Secondary

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Physics — Second Secondary 2026/2027

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Text lesson

Chapter 6: Gas Laws

Physics — Second Secondary

Chapter 6: Gas Laws

Overview

Overview

(Unit Four→Heat — Second Secondary, Term 1)

🌳 Concept tree

Chapter 6→Gas Laws

├── What you will learn

  1. Kinetic Picture of a Gas
  2. │ ├── 1.1 Molecules in the three states of matter

│ ├── 1.2 Brownian motion

│ └── 1.3 Intermolecular spaces
├── Lesson 2The Variables of a Gas
├── Lesson 3Boyle's Law

│ ├── 3.1 The experiment

│ ├── 3.2 Boyle's law

│ └── 3.3 Worked examples

  1. Charles's Law
  2. │ ├── 4.1 Do all gases expand equally?

│ ├── 4.2 Charles's apparatus

│ ├── 4.3 Charles's law

│ └── 4.4 Worked examples

├── Lesson 5→The Pressure Law (Gay-Lussac's Law)

│ ├── 5.1 The experiment

│ ├── 5.2 Jolly's apparatus

│ ├── 5.3 The pressure law

│ └── 5.4 Worked examples

  • ├── Lesson 6 Absolute Zero and the Kelvin Scale
  • │ ├── 6.1 Absolute zero from Charles's law and from the pressure law

│ ├── 6.2 Remarks

│ └── 6.3 Relation between Celsius and Kelvin

├── Lesson 7→The General Gas Law

│ ├── 7.1 Combining the three laws

│ ├── 7.2 Enrichment: the ideal gas equation

  • │ ├── 7.3 Standard temperature and pressure (STP)

│ └── 7.4 Worked examples

└── Summary and relations

Chapter 6: Gas Laws · 1 / 11
What you will learn

What you will learn

  • Brownian motion and what it tells us about gas molecules; intermolecular spaces.
  • The three variables of a gas (volume, pressure, temperature) and three separate experiments.
  • Boyle’s law (volume–pressure at constant temperature).
  • Charles’s law (volume–temperature at constant pressure); the coefficient of volume expansion.
  • The pressure law (Gay-Lussac’s law) (pressure–temperature at constant volume); Jolly’s apparatus; the coefficient of pressure increase.
  • Absolute zero and the Kelvin scale.
  • The general gas law, and the ideal gas equation PV = nRT (enrichment).
  • Solving problems on gases.
Chapter 6: Gas Laws · 2 / 11
Lesson 1: Kinetic Picture of a Gas

Lesson 1: Kinetic Picture of a Gas

1.1 Molecules in the three states of matter

  1. The molecules of every substance are in continuous motion
  2. but the kind of motion depends on the state:
gasrandom translational motion in all directions (and collisions);
liquidtranslational and vibrational motion;
solidvibrational motion about fixed positions only.
  • If we look through a microscope at the smoke rising from a burning candle, we see tiny carbon particles moving here and there in random zig-zag motion.
  • This motion is called Brownian motion after the Scottish botanist Robert Brown, who discovered in 1827 that pollen grains suspended in water move constantly and randomly.
  • Explanation.
  • The molecules of air (or any gas) move randomly in all directions with different speeds and collide with each other and with the smoke particles.
  • At any instant the number (or force) of the collisions on one side of a carbon particle may be larger than on the opposite side, so the particle is pushed a short distance in one direction.
  • A moment later the unbalance is in another direction.
  • The motion of the molecules is caused by heat and is never-ending.
  • Conclusion.
  • Gas molecules are in continuous random motion; they collide with each other and with the walls of the container.
  • (The collisions with the walls are the cause of gas pressure.)

1.3 Intermolecular spaces

  • Experiment.
  • Hold a beaker full of ammonia gas (NH₃) upside down over a beaker of hydrogen chloride gas (HCl) (with a cover separating them, which is then removed).
  • A white cloud of ammonium chloride (NH₄Cl) forms and spreads until it fills both beakers.
  • Explanation.
  • HCl molecules, although heavier (denser), rise upward through the spaces between ammonia molecules; NH₃ molecules, although lighter, move downward through the spaces between HCl molecules.
  • Where they meet, they combine to form NH₄Cl, which diffuses to fill both beakers.
  • Conclusion.
  • There are relatively large spaces between gas molecules (intermolecular spaces).
  • This also explains why gases are easily compressed pressure pushes the molecules closer together, so the volume decreases.
Chapter 6: Gas Laws · 3 / 11
Lesson 2: The Variables of a Gas

Lesson 2: The Variables of a Gas

  • Experiments on the expansion of a gas with heat are not simple because a gas changes its volume if the pressure, the temperature or both change.
  • (For solids and liquids this difficulty does not arise their compressibility is very small.)
  • To study a gas we have to consider three variables — volume (V), pressure (P) and temperature (T) — and do three separate experiments, in each of which the relationship between two variables is studied while the third is held constant (and the mass of the gas is fixed):
Experiment Constant Law
Volume against pressure temperature Boyle’s law
Volume against temperature pressure Charles’s law
Pressure against temperature volume Pressure law (Gay-Lussac’s law)
Chapter 6: Gas Laws · 4 / 11
Lesson 3: Boyle’s Law

Lesson 3: Boyle’s Law

3.1 The experiment

  • Apparatus.
  • A graduated glass tube (A) (like an inverted burette whose scale starts at the top) connected by a rubber tube to a second movable tube (B).
  • Both contain mercury.
  • The apparatus stands on a vertical board with levelling screws.
  • Tube (B) can be raised, lowered and fixed at any height.
  • A stopcock closes the top of tube (A).
  • Procedure
  1. With the tap of (A) open, move (B) until the mercury in (A) is about halfway. Both tubes are open to the air, so the mercury is at the same level in both.
  2. Close the tap. The trapped air has volume V₁ and pressure P₁ = Pa (atmospheric pressure in cm Hg, read from a barometer).
  3. Raise (B) a few centimetres. The mercury level in (B) is now higher than in (A) by h. Measure the new volume V₂. The pressure is P₂ = Pa + h.
  4. Repeat at least once more with another height of (B) above (A) (P₃, V₃).
  5. Lower (B) so that its mercury level is lower than that in (A) by h. Measure V₄; the pressure is P₄ = Pa − h.
  6. Repeat once more (P₅, V₅).
  7. Plot volume (vertical axis) against 1/P (horizontal axis). The graph is a straight line through the origin.
  • So V ∝ 1/P.
  • (Keep the temperature constant wait before taking each reading so that the gas returns to room temperature, and change the pressure slowly.)

3.2 Boyle’s law

  • Boyle’s law At constant temperature, the volume of a fixed mass of gas is inversely proportional to its pressure.
  • V ∝ 1/P → P V = constant (fixed mass, constant temperature)
  • or for two states P₁V₁ = P₂V₂.
  • The graph of P against V (constant T) is a curve (a hyperbola); the graph of V against 1/P is a straight line through the origin; the graph of PV against P is a horizontal line.

3.3 Worked examples

Example 1.→A gas occupies 600 cm3 at 76 cm Hg. It is compressed at constant temperature to 400 cm3. P₂ = P₁V₁/V₂ = 76 × 600/400 = 114 cm Hg.

✍️ Worked examples

Comparison aspectMain ideaKeywords
Example 2.The pressure of a gas is tripled at constant temperature. Its volume becomes one-thirdpressuretripledconstanttemperature
Example 3.8 cm3 of air is at the bottom of a lake at a depth where the total pressure is 3 atm. The temperature is the same at the surface. At the surface (1 atm): V = 3 × 8 = 24 cm3bottomlakedepthtotal
Example 4 (barometer-tube).
  • A tube holds 40 cm3 of air at atmospheric pressure of 76 cm Hg. The air is pushed to 25 cm3 by raising the movable tube. P = 76 × 40/25 = 121.6 cm Hg
  • so h = 121.6 − 76 = 45.6 cm Hg
holdsatmosphericpressurepushed
Chapter 6: Gas Laws · 5 / 11
Lesson 4: Charles’s Law

Lesson 4: Charles’s Law

4.1 Do all gases expand equally?

  • Gases expand when heated and contract when cooled. Do equal volumes of different gases expand by different amounts?
  • Experiment.
  • Two flasks of exactly equal volume, each closed with a stopper through which passes a right-angle glass tube holding a small thread of mercury (2–3 cm long).
  • Fill one with oxygen and the other with air or carbon dioxide.
  • Place both in the same basin of water and add hot water.
  • The two mercury threads move equal distances.
  • Conclusion. Equal volumes of different gases, under the same pressure, expand by equal amounts for the same rise of temperature; so their coefficient of volume expansion is the same.
  • Coefficient of volume expansion of a gas at constant pressure (αv): the increase in volume of unit volume of the gas at 0 °C when its temperature rises by one degree Celsius at constant pressure.

4.2 Charles’s apparatus

  • A glass tube about 30 cm long and 1 mm wide, closed at one end, with a drop of mercury trapping a certain amount of dry air.
  • The tube is fixed along with a thermometer to a graduated ruler inside a cylindrical glass jacket.
  • Procedure
  1. Surround the tube with melting crushed ice until the trapped air is at 0 °C. Because the tube has a uniform cross-section, the length of the air column is a measure of its volume (V₀).
  2. Remove the ice water and pass steam through the jacket until the air reaches 100 °C. Measure the length of the air column (volume V₁₀₀).
  3. Plot volume against temperature (°C). A straight line is obtained. If it is extended backwards, it cuts the temperature axis at −273 °C.
  4. The coefficient of volume expansion is
αv = (V₁₀₀ − V₀) / (V₀ × 100)→For air (and for all gases) it is found to be 1/273 per °C (per kelvin).

4.3 Charles’s law

  • Charles’s law (first form):
  • At constant pressure, the volume of a fixed mass of gas increases by 1/273 of its volume at 0 °C for every 1 °C rise in temperature.
  • This fraction is the same for all gases.
  • Thus Vt = V₀ (1 + t/273), where t is in °C.
  • Second form (Kelvin scale). Using similar triangles in the graph (V against t, extended to −273 °C): V₁/T₁ = V₂/T₂, i.e.
  • V / T = constant (fixed mass, constant pressure), so V ∝ T
  • At constant pressure, the volume of a fixed mass of gas is directly proportional to its absolute (Kelvin) temperature.

4.4 Worked examples

Example 1.→A gas has volume 300 cm3 at 0 °C. At 91 °C (constant pressure): V = 300 × (273 + 91)/273 = 300 × 364/273 = 400 cm3.
Comparison aspectMain ideaKeywords
Example 2.2 litres of a gas at 27 °C (300 K) is heated to 127 °C (400 K) at constant pressure. V₂ = 2 × 400/300 = 2.67 litreslitresheatedconstantpressure
Example 3 (find the temperature).A gas of volume 500 cm3 at 7 °C (280 K) is heated at constant pressure until its volume becomes 750 cm3. T₂ = 280 × 750/500 = 420 K = 147 °Cvolumeheatedconstantpressure
Example 4.Show the coefficient. A gas has 200 cm3 at 0 °C and 273.2 cm3 at 100 °C. αv = (273.2 − 200)/(200 × 100) = 3.66 × 10−3 °C−1 ≈ 1/273.Showcoefficient
Chapter 6: Gas Laws · 6 / 11
Lesson 5: The Pressure Law (Gay-Lussac’s Law)

Lesson 5: The Pressure Law (Gay-Lussac’s Law)

5.1 The experiment

  • Simple experiment.
  • A glass flask closed with a stopper through which a U-shaped tube (A, B) containing mercury passes.
  • At first the mercury is at the same level (x and y) in both arms, so the gas pressure is atmospheric; temperature t₁.
  1. Immerse the flask in warm water at t₂. The mercury falls in arm A (connected to the flask) and rises in B.
  2. Add mercury through a funnel until the level in A returns to mark x, so the volume of the gas is again the same (constant volume).
  3. the pressure of the gas has increased by h cm Hg when the temperature rose from t₁ to t₂.
  4. Repeat with different gases and the same rise in temperature. Findings: (a) at constant volume, the pressure increases with temperature; (b) equal pressures of different gases increase by equal amounts for equal rises in temperature.
  • Coefficient of pressure increase of a gas at constant volume (βP): the increase in the pressure of a unit pressure measured at 0 °C when the temperature rises by 1 °C at constant volume.
  • ΔP ∝ P₀ Δt → ΔP = βP P₀ Δt → βP = ΔP/(P₀ Δt) = (P₁₀₀ − P₀)/(P₀ × 100)
  • A spherical thin glass bulb (A) connected to a long capillary tube (B) (bent at two right angles), fixed on a vertical board that stands on a base with levelling screws.
  • The other end of the capillary is joined by a rubber tube to a wide tube (C) which can be moved up and down along the board; there is a graduated scale.
  • Procedure
  1. Read the atmospheric pressure from a barometer.
  2. Put mercury in the bulb’s side to take up part of the volume (about 1/7 of the bulb), so that the volume of the remaining air stays practically constant at all temperatures (mercury expands about 7 times as much as glass).
  3. Immerse bulb (A) in a beaker of water; pour mercury into (C) until the mercury in the other branch rises to a fixed mark X.
  4. Heat the water to boiling, wait for the temperature to become steady.
  5. Move (C) until the mercury in the bulb-side arm returns to mark X (so the volume is again constant). The gas pressure P = Pa + h, where h is the height difference between the surfaces in the two arms.
  6. Let the water cool to about 90 °C, adjust (C) so that the mercury returns to X, measure the temperature and height difference and calculate P again.
  7. Repeat at several temperatures.
  8. Plot pressure (vertical) against temperature in °C (horizontal). A straight line is obtained which, when extended backwards, cuts the temperature axis at −273 °C.
  9. Calculate βP = (P₁₀₀ − P₀)/(P₀ × 100). It is found to be 1/273 per °C for air and the same for all gases.

5.3 The pressure law

Comparison aspectMain ideaKeywords
The pressure law
  • At constant volume
  • the pressure of a fixed mass of gas increases by 1/273 of its pressure at 0 °C for every 1 °C rise in temperature
constantvolumefixedmass
Second form (Kelvin scale).
  • From similar triangles: P₁/T₁ = P₂/T₂
  • i.e
similartriangles
P / T = constant
  • (fixed mass
  • constant volume)
  • so P ∝ T
fixedmassvolume
•
  • At constant volume
  • the pressure of a fixed mass of gas is directly proportional to its absolute temperature
constantvolumepressurefixed
•Note that the coefficient of volume expansion at constant pressure αv and the coefficient of pressure increase at constant volume βP are equal for all gases: both = 1/273 K−1.Notecoefficientvolumeexpansion

5.4 Worked examples

Example 1.→A gas has a pressure of 45 cm Hg at 27 °C (300 K). Its volume is constant. At 127 °C (400 K): P₂ = 45 × 400/300 = 60 cm Hg.
Comparison aspectMain ideaKeywords
Example 2.A sealed container of air is at 0 °C with pressure 80 cm Hg. It is cooled to −91 °C (182 K): P = 80 × 182/273 = 53.3 cm Hgsealedcontainerpressurecooled
Example 3 (car tyre).
  • A tyre has air at 2.0 atm at 7 °C (280 K). After driving
  • the air is at 47 °C (320 K). Assuming constant volume
  • P = 2.0 × 320/280 = 2.29 atm. (That is why tyre pressure should be checked when the tyres are cold.)
AfterdrivingAssumingconstant
Example 4 (find the temperature).The pressure of a gas at constant volume rises from 1 atm at 27 °C to 1.5 atm. T₂ = 300 × 1.5 = 450 K = 177 °Cpressureconstantvolumerises
Chapter 6: Gas Laws · 7 / 11
Lesson 6: Absolute Zero and the Kelvin Scale

Lesson 6: Absolute Zero and the Kelvin Scale

6.1 Absolute zero from Charles’s law and from the pressure law

  • The line on the volume–temperature (°C) graph, when extended, cuts the temperature axis at −273 °C (the volume appears to vanish there).
  • The line on the pressure–temperature (°C) graph (Jolly’s experiment), when extended, also cuts the temperature axis at −273 °C (the pressure appears to vanish).
  • Absolute zero (zero kelvin) is therefore the lowest theoretically attainable temperature, −273 °C; the temperature at which the volume of an ideal gas becomes zero at constant pressure, or the pressure of an ideal gas becomes zero at constant volume.
  • Example of the method. For a gas whose volume is 273 cm3 at 0 °C and 373 cm3 at 100 °C, the line V = 273 + t reaches V = 0 at t = −273 °C.

6.2 Remarks

  • Redrawn against the absolute temperature T (kelvin), the V–T and P–T graphs are straight lines through the origin: V = 0 and P = 0 at 0 K.
  • In practice, a real gas does not reach these values on strong cooling it liquefies (and may solidify) and no longer obeys the gas laws. An ideal gas is defined as a gas whose volume (at constant pressure) or pressure (at constant volume) would become zero at absolute zero, so that it obeys the gas laws at all temperatures.
  • The temperature on the Kelvin scale is always positive; Celsius temperature can be positive or negative.

6.3 Relation between Celsius and Kelvin

  1. −273 °C ↔ 0 K
  2. 0 °C ↔ 273 K
  3. 100 °C ↔ 373 K. Hence
T (K) = t (°C) + 273→human body 37 °C = 310 K; room 27 °C = 300 K; 100 K = −173 °C. A change of 1 °C equals a change of 1 K.
Chapter 6: Gas Laws · 8 / 11
Lesson 7: The General Gas Law

Lesson 7: The General Gas Law

7.1 Combining the three laws

  • For a fixed mass of gas:
Comparison aspectMain ideaKeywords
BoyleV ∝ 1/P (T constant)constant
CharlesV ∝ T (P constant) Combining: V ∝ T/P → PV/T = constantconstantCombining
•For two states of the same mass of gasstatessamemass
P₁V₁/T₁ = P₂V₂/T₂
  • (T in kelvin
  • P in any consistent unit
  • V in any consistent unit)
kelvinconsistentunit
Special cases
  • T constant → Boyle’s law
  • P constant → Charles’s law
  • V constant → pressure law
constantBoyleCharlespressure

7.2 Enrichment: the ideal gas equation

  • In general, PV = nRT, where

n = number of moles of the gas,

P in pascals, V in m3, T in kelvin,

Comparison aspectMain ideaKeywords
R = 8.31 J/(mol·K)
  • the universal gas constant. A mole is the amount of a substance whose mass in grams equals its molecular mass: one mole of oxygen (O₂) has a mass of 32 g
  • nitrogen (N₂) 28 g
  • carbon dioxide (CO₂) 44 g
universalconstantmoleamount
Examplethe volume of one mole of any gas at STP is V = nRT/P = 1 × 8.31 × 273/1.013 × 105 = 0.0224 m3 = 22.4 litresvolumemole0224litres

7.3 Standard temperature and pressure (STP)

STP→0 °C (273 K) and 76 cm Hg (1 atm = 1.013 × 105 Pa).
7.4 Worked examples
Example 1 (to STP).A gas has volume 450 cm3 at 27 °C and 60 cm Hg. Find its volume at STP.
P₁V₁/T₁ = P₂V₂/T₂60 × 450/300 = 76 × V₂/273 → V₂ = 60 × 450 × 273/(300 × 76) = 323 cm3.
Comparison aspectMain ideaKeywords
Example 2 (find T).A gas of 3 L at 2 atm and 27 °C changes to 6 L at 1.5 atm. T₂ = T₁ P₂V₂/(P₁V₁) = 300 × (1.5 × 6)/(2 × 3) = 300 × 1.5 = 450 K = 177 °CchangesP₂V₂P₁V₁
Example 3 (find P).
  • A fixed mass of gas at 76 cm Hg
  • 300 K
  • and 500 cm3 is compressed to 250 cm3 and heated to 360 K: P₂ = 76 × 500 × 360/(300 × 250) = 182.4 cm Hg
fixedmasscompressedheated
Example 4 (gas that escapes).
  • An open flask of air is heated from 7 °C (280 K) to 147 °C (420 K) at constant pressure. The volume of the flask is constant
  • so the amount of gas ∝ 1/T. Fraction left = 280/420 = 2/3
  • fraction that escaped = 1/3 = 33.3 % of the original amount
openflaskheatedconstant

✍️ Worked examples

  • Example 5 (mixture of two gases — partial pressures).
  • Gas A 6 L at 20 cm Hg.
  • Gas B 4 L at 30 cm Hg.
  • Both are transferred (at constant temperature) to a 3-L container.
  • A: PA VA = P’_A × 3 → P’_A = 20 × 6/3 = 40 cm Hg.
  • B: P’_B = 30 × 4/3 = 40 cm Hg.
    The pressure of a mixture equals the sum of the pressures each gas would produce alone: P = 40 + 40 = 80 cm Hg.
  • Example 6 (ideal gas equation). Two moles of a gas at 300 K in a 0.01 m3 container: P = nRT/V = 2 × 8.31 × 300/0.01 = 4.99 × 105 Pa (about 4.9 atm).
  • Example 7 (helium balloon). A helium balloon rises in the air. As it rises the surrounding pressure falls (and the temperature falls less than the pressure), so by PV/T = constant its volume increases, until it may burst.
Chapter 6: Gas Laws · 9 / 11
Summary and relations

Summary and relations

  • Gas molecules are in continuous random motion, colliding with each other and with the walls; there are spaces between molecules (compressibility). Evidence: Brownian motion, diffusion of NH₃ and HCl.
  • Boyle PV = const (T const).
  • Charles V/T = const (P const); V increases by 1/273 of V₀ per °C; αv = (V₁₀₀ − V₀)/(V₀ × 100) = 1/273 K−1.
  • Pressure law P/T = const (V const); P increases by 1/273 of P₀ per °C; βP = (P₁₀₀ − P₀)/(P₀ × 100) = 1/273 K−1.
  • T(K) = t(°C) + 273; absolute zero = −273 °C.
  • General gas law P₁V₁/T₁ = P₂V₂/T₂; PV = nRT with R = 8.31 J/(mol·K).
  • .egp-ex{margin:18px 0;border:1px solid rgba(79,63,224,.2);border-radius:16px;overflow:hidden;background:#fff}.egp-ex-h{padding:10px 16px;font-weight:800;background:linear-gradient(90deg,#4f3fe0,#22c1c3);color:#fff}.egp-ex-tabs{display:flex;flex-wrap:wrap;gap:6px;padding:10px 12px;background:#f7f6ff}.egp-ex-b{border:1px solid rgba(79,63,224,.3);background:#fff;border-radius:20px;padding:5px 14px;font-weight:700;cursor:pointer}.egp-ex-b.on{background:#4f3fe0;color:#fff}.egp-ex-p{padding:12px 16px}
Chapter 6: Gas Laws · 10 / 11
Part 11

Part 11

  • 📖

📌 Comprehensive Scientific Terminology & Definitions:

Comparison aspectMain ideaKeywords
Boyle’s Law
  • At constant temperature
  • the volume of a fixed mass of an ideal gas is inversely proportional to its pressure: P ∝ 1 / V
  • meaning P₁ V₁ = P₂ V₂ = constant
constanttemperaturevolumefixed
Charles’s Law
  • At constant pressure
  • the volume of a fixed mass of an ideal gas is directly proportional to its absolute temperature in Kelvin: V ∝ T
  • meaning V₁ / T₁ = V₂ / T₂ = constant
constantpressurevolumefixed
Pressure Law (Gay-Lussac’s Law)
  • At constant volume
  • the pressure of a fixed mass of an ideal gas is directly proportional to its absolute temperature in Kelvin: P ∝ T
  • meaning P₁ / T₁ = P₂ / T₂ = constant
constantvolumefixedmass
Absolute Zero (0 Kelvin / -273.15°C)
  • The theoretical temperature at
  • the volume (at constant P) or pressure (at constant V) of an ideal gas would extrapolate to zero
  • molecular kinetic energy reaches its minimum possible value
theoreticaltemperaturevolumeconstant
Ideal Gas Equation
  • Equation of state combining all three empirical gas laws: P V = n R T
  • where n is the number of moles and R is the universal gas constant (8.314 J/mol·K)
statecombiningthreeempirical

⚖️ Governing Scientific Laws, Principles & Mathematical Formulas:

Comparison aspectMain ideaKeywords
Boyle’s Law (T = const)P₁ V₁ = P₂ V₂
Charles’s Law (P = const)V₁ / T₁ = V₂ / T₂ (where T = t°C + 273.15)
Pressure Law (V = const)P₁ / T₁ = P₂ / T₂
General Combined Gas Law(P₁ V₁) / T₁ = (P₂ V₂) / T₂
Ideal Gas LawP V = n R T = (m / M) R T
Volume Expansion Coefficientα_v = (Vt – V0) / (V0 × t) = 1 / 273.15 K−1

🔍 In-Depth Explanations, Deductions & Core Concepts:

Comparison aspectMain ideaKeywords
•
  • Why do all gases have the identical thermal expansion coefficient (α_v = 1/273)? Because intermolecular spacing in gases is enormous and cohesive intermolecular forces are negligible
  • so all ideal gases expand identically regardless of chemical identity
gasesidenticalthermalexpansion
Why can gas volume never actually reach zero at absolute zero?Because real gases condense into liquids and freeze into solids long before reaching 0 K as attractive van der Waals forces overcome kinetic energyBecauserealgasescondense
Why do car tires sometimes burst on hot highways?
  • Friction raises the temperature of the enclosed air. Since tire volume is approximately rigid (constant V)
  • air pressure climbs proportionally with absolute temperature (P ∝ T) until structural failure occurs
Frictionraisestemperatureenclosed
Gas Law Constant Parameter Proportionality Governing Formula
Boyle’s Law Temperature (T) Inverse: P ∝ 1/V P₁ V₁ = P₂ V₂
Charles’s Law Pressure (P) Direct: V ∝ T(K) V₁ / T₁ = V₂ / T₂
Pressure Law Volume (V) Direct: P ∝ T(K) P₁ / T₁ = P₂ / T₂
💡 High-Yield Exam Traps & Key Takeaways:
Always convert Celsius to KelvinT(K) = t(°C) + 273.15.
For gas mixtures at constant TPtotal Vtotal = P₁ V₁ + P₂ V₂.
Chapter 6: Gas Laws · 11 / 11