Topics
Units and Measurements
- Quantitative Science
- System of Units
- Derived Quantities and Units
- Rules and Conventions for Writing SI Units and Their Symbols
- Measurement of Length
- Measurement of Mass
- Measurement of Time
- Dimensions and Dimensional Analysis
- Accuracy, Precision and Uncertainty in Measurement
- Errors in Measurements>Systematic Errors
- Errors in Measurements>Random Errors
- Estimation of Errors
- Combination of Errors
- Significant Figures
- Definitions of SI Units and Constants
Mathematical Methods
- Vector Analysis
- Scalar
- Vector
- Vector Operations>Multiplication of a Vector by a Scalar
- Vector Operations>Addition and Subtraction of Vectors
- Vector Operations>Triangle Law for Vector Addition
- Vector Operations>Law of parallelogram of vectors
- Resolution of Vectors
- Multiplication of Vectors
- Scalar Product(Dot Product)
- Vector Product (Cross Product)
- Concept of Calculus
- Differential Calculus
- Integral Calculus
Motion in a Plane
- Concept of Motion
- Rectilinear Motion
- Displacement
- Path Length
- Average Velocity
- Average Speed
- Instantaneous Velocity
- Instantaneous Speed
- Acceleration in Linear Motion
- Relative Velocity
- Motion in Two Dimensions-Motion in a Plane
- Average and Instantaneous Velocities
- Acceleration in a Plane
- Equations of Motion in a Plane with Constant Acceleration
- Relative Velocity in Two Dimensions
- Projectile Motion
- Uniform Circular Motion (UCM)
- Key Parameters of Circular Motion
- Centripetal Acceleration
- Conical Pendulum
Laws of Motion
- Fundamental Principles of Motion and Mechanics
- Types of Motion
- Aristotle’s Fallacy
- Newton’s Laws of Motion
- Newton's First Law of Motion
- Newton’s Second Law of Motion
- Newton's Third Law of Motion
- Inertial and Non-inertial Frames of Reference
- Types of Forces>Fundamental Forces in Nature
- Types of Forces>Contact and Non-Contact Forces
- Types of Forces>Real and Pseudo Forces
- Types of Forces>Conservative and Non-Conservative Forces
- Types of Forces>Work Done by a Variable Force
- Work Energy Theorem
- Principle of Conservation of Linear Momentum
- Collisions
- Elastic and Inelastic Collisions
- Perfectly Inelastic Collision
- Coefficient of Restitution e
- Expressions for Final Velocities in Elastic Head-On Collision
- Loss of Kinetic Energy in Perfectly Inelastic Head-On Collision
- Collision in Two Dimensions
- Impulse of a Force
- Necessity of Defining Impulse
- Rotational Analogue of a Force: Moment of a Force Or Torque
- Couple and Its Torque
- Proof of Independence of the Axis of Rotation
- Mechanical Equilibrium
- States of Equilibrium
- Centre of Mass>Mathematical Understanding of Centre of Mass
- Centre of Mass>Velocity of Centre of Mass
- Centre of Mass>Acceleration of Centre of Mass
- Centre of Mass>Characteristics of Centre of Mass
- Centre of Gravity
Gravitation
- Concept of Gravitation
- Kepler’s Laws
- Law of Orbit or Kepler's First Law
- Law of Areas or Kepler's Second Law
- Law of Periods or Kepler's Third Law
- Newton's Universal Law of Gravitation
- Measurement of the Gravitational Constant (G)
- Acceleration Due to Gravity (Earth’s Gravitational Acceleration)
- Variation in the Acceleration>Variation in Gravity with Altitude
- Variation in the Acceleration>Variation in Gravity with Depth
- Variation in the Acceleration>Variation in Gravity with Latitude and Rotation of the Earth
- Variation in the Acceleration>Effect of the shape of the Earth
- Gravitational Potential Energy
- Expression for Gravitational Potential Energy
- Connection of Potential Energy Formula with mgh
- Potential and Potential Difference
- Escape Velocity
- Earth Satellites
- Projection of Satellite
- Weightlessness in a Satellite
- Time Period of Satellite
- Binding Energy of an Orbiting Satellite
Mechanical Properties of Solids
- Mechanical Properties of Solids
- Elastic Behavior of Solids
- Stress and Strain
- Types of Stress and Corresponding Strain
- Hooke’s Law
- Elastic Modulus>Young’s Modulus
- Elastic Modulus>Bulk Modulus
- Elastic Modulus>Modulus of Rigidity
- Elastic Modulus>Poisson’s Ratio
- Stress-strain Curve
- Strain Energy
- Hardness of Material
- Friction in Solids
- Origin of Friction
- Types of Friction>Static Friction
- Types of Friction>Kinetic Friction
- Types of Friction>Rolling Friction
Thermal Properties of Matter
- Thermal Properties of Matter
- Temperature and Heat
- Measurement of Temperature
- Absolute Zero and Absolute Temperature
- Ideal Gas Equation
- Thermal Expansion
- Linear Expansion
- Areal Expansion
- Volume Expansion
- Relation Between Coefficient of Expansion
- Specific Heat Capacity
- Specific Heat Capacity of Solids and Liquids
- Specific Heat Capacity of Gas
- Heat Equation
- Thermal Capacity
- Calorimetry
- Change of State
- Analysis of Observation>From Point A to B
- Analysis of Observation>From Point B to D
- Temperature Effects and Considerations
- Evaporation vs Boiling
- Boiling Point and Pressure
- Factors Affecting Cooking
- Sublimation
- Phase Diagram
- Gas and Vapour
- Latent Heat
- Heat Transfer
- Conduction
- Thermal Conductivity
- Coefficient of Thermal Conductivity
- Thermal Resistance
- Applications of Thermal conductivity
- Convection
- Application of Convection
- Free and Forced Convection
- Radiation
- Newton’s Law of Cooling
Sound
- Sound Waves
- Common Properties of All Waves
- Transverse Waves
- Longitudinal Waves
- Mathematical Expression of a Wave
- The Speed of Travelling Waves
- The Speed of Transverse Waves
- The Speed of Longitudinal Waves
- Newton's Formula for Velocity of Sound
- Laplace’s Correction
- Factors Affecting Speed of Sound
- Principle of Superposition of Waves
- Echo
- Reverberation
- Acoustics
- Qualities of Sound
- Doppler Effect
- Source Moving and Listener Stationary
- Listener Approaching a Stationary Source with Velocity
- Both Source and Listener are Moving
- Common Properties between Doppler Effect of Sound and Light
- Major Differences between Doppler Effects of Sound and Light
Optics
- Fundamental Concepts of Light
- Nature of Light
- Ray Optics Or Geometrical Optics
- Cartesian Sign Convention
- Reflection>Reflection from a Plane Surface
- Reflection>Reflection from Curved Mirrors
- Total Internal Reflection
- Refraction of Light
- Applications of Total Internal Reflection
- Refraction at a Spherical Surface and Lenses
- Thin Lenses and Their Combination
- Refraction at a Single Spherical Surface
- Lens Makers' Equation
- Dispersion of Light
- Analysis of Prism
- Thin Prisms
- Some Natural Phenomena Due to Sunlight
- Defects of Lenses
- Optical Instruments
- Simple Microscope or a Reading Glass
- Compound Microscope
- Telescope
Electrostatics
- Concept of Electrostatics
- Electric Charge
- Basic Properties of Electric Charge
- Additive Nature of Charge
- Quantization of Charge
- Conservation of Charge
- Force between Charges
- Coulomb’s Law
- Scalar Form of Coulomb’s Law
- Relative Permittivity or Dielectric Constant
- Definition of Unit Charge from the Coulomb’s Law
- Coulomb's Law in Vector Form
- Principle of Superposition
- Electric Field
- Electric Field Intensity Due to a Point-Charge
- Practical Way of Calculating Electric Field
- Electric Lines of Force
- Electric Flux
- Gauss’s Law
- Electric Dipole
- Couple Acting on an Electric Dipole in a Uniform Electric Field
- Electric Intensity at a Point Due to an Electric Dipole
- Continuous Charge Distribution
Electric Current Through Conductors
- Concept of Electric Currents in Conductors
- Electric Current
- Flow of Current Through a Conductor
- Drift Speed
- Ohm's Law
- Limitations of Ohm’s Law
- Electrical Power
- Resistors
- Rheostat
- A combination of resistors in both series and parallel
- Specific Resistance
- Variation of Resistance with Temperature
- Electromotive Force (emf)
- Cells in Series
- Cells in Parallel
- Types of Cells
Magnetism
- Concept of Magnetism
- Magnetic Lines of Force
- The Bar Magnet
- Magnetic Field due to a Bar Magnet
- Magnetic Field Due to a Bar Magnet at an Arbitrary Point
- Gauss' Law of Magnetism
- The Earth’s Magnetism
Electromagnetic Waves and Communication System
- Foundations of Electromagnetic Theory
- EM Wave
- Sources of EM Waves
- Characteristics of EM Waves
- Electromagnetic Spectrum
- Radio Waves
- Microwaves
- Infrared waves
- Visible Light
- Ultraviolet rays
- X-rays
- Gamma Rays
- Propagation of EM Waves
- Ground (surface) Wave
- Space wave
- Sky wave propagation
- Communication System
- Elements of a Communication System
- Commonly Used Terms in Electronic Communication System
- Modulation
Semiconductors
- Concept of Semiconductors
- Electrical Conduction in Solids
- Band Theory of Solids
- Intrinsic Semiconductor
- Extrinsic Semiconductor
- n-type semiconductor
- p-type semiconductor
- Charge neutrality of extrinsic semiconductors
- p-n Junction
- A p-n Junction Diode
- Basics of Semiconductor Devices
- Applications of Semiconductors and P-n Junction Diode
- Thermistor
- Introduction
- Definition: Absolute Zero
- Definition: Kelvin Scale
- Definition: Triple Point
- Definition: Ideal Gas
- Definition: Universal Gas Constant (R)
- Definition: Extrapolation
- Definition: Kelvin
- Conversion Formulas
- Gases Respond to Temperature
- The Discovery of Absolute Zero
- The Kelvin (Absolute) Temperature Scale
- Temperature Scales & Conversion
- The Ideal Gas Equation
- Example 1
- Example 2
- Key Points: Absolute Zero and Absolute Temperature
Introduction
Every gas thermometer in a hospital, every weather balloon, and every rocket engine relies on how gas pressure, volume, and temperature are related. This topic lays the foundation for thermodynamics — and it all starts with defining temperature properly.
Definition: Absolute Zero
The lowest theoretically possible temperature (0 K = −273.15 °C), where ideal gas molecules have zero kinetic energy.
Definition: Kelvin Scale
The SI absolute temperature scale starting at absolute zero. Written as K (no degree symbol °).
Definition: Triple Point
The unique temperature & pressure at which solid, liquid, and gas phases of a substance coexist in equilibrium.
Definition: Ideal Gas
A hypothetical gas whose molecules have no volume and exert no intermolecular forces; obeys PV = μRT exactly.
Definition: Universal Gas Constant (R)
A constant in the ideal gas equation; R = 8.31 J mol⁻¹ K⁻¹.
Definition: Extrapolation
Extending a graph line beyond the measured data to predict values.
Definition: Kelvin
One kelvin = 1/273.16 of the difference between absolute zero and the triple point of water.
Conversion Formulas
Master Conversion Formula:
\[\frac {T_C}{100}\] = \[\frac {(T_{F}-32)}{180}\] = \[\frac {(T_{K}-273.15)}{100}\]
Gases Respond to Temperature
Experiments with gases at low densities reveal a simple and powerful pattern:
- At constant pressure: The volume of a gas is directly proportional to its temperature (°C). → Charles' Law
- At constant volume: The pressure of a gas is directly proportional to its temperature (°C). → Gay-Lussac's Law
V ∝ TC (at constant P)
P ∝ TC (at constant V)
The Graphs Show:
When we plot these relationships, we get straight lines — but with important properties:
- The lines do not pass through the origin (non-zero y-intercept).
- Different gases have different slopes.
- Gases expand linearly with temperature: equal temperature rises cause equal increases in volume (or pressure).

Fig: Volume vs Temperature at Constant Pressure
The Discovery of Absolute Zero
If we extrapolate the P–T graph backwards — imagining the gas doesn't liquefy — we ask: "At what temperature would the gas pressure drop to zero?"
The answer, from extrapolation, is:
This is called absolute zero.
Why This Is Remarkable:
- All gases, regardless of type, produce lines that converge to the same point: −273.15 °C.
- This point does not depend on which specific gas is used — it is a universal property of nature.
- No temperature lower than absolute zero is physically possible.
- In practice, absolute zero has never been achieved — only approached.
The Kelvin (Absolute) Temperature Scale
The old two-fixed-point system (ice point + steam point) had a practical problem: the boiling point of water is very sensitive to pressure changes, making calibration difficult. In 1954, scientists adopted a one-fixed-point scale based on the triple point of water.
The triple point is the unique combination of temperature and pressure at which all three phases of a substance — solid, liquid, and gas — coexist in perfect equilibrium.
| Property | Value |
|---|---|
| Triple point temperature | 273.16 K (= 0.01 °C) |
| Triple point pressure | 6.11 × 10⁻³ atm (= 611 Pa) |
The Kelvin
- The size of one kelvin is identical to one degree Celsius.
- Kelvin is written as K (no degree symbol °). Named after Lord Kelvin (1824–1907).
TK = TC + 273.15
Common Mistake:
Students often write "°K" — this is incorrect. The correct notation is simply K (e.g., 300 K, not 300°K).Why Is It Called "Absolute"?
- Based on a universal property of ideal gases, not on any particular substance.
- Its zero point represents the lowest physically possible temperature.
- Unlike the Celsius or Fahrenheit scales, the Kelvin scale has no negative values.
Temperature Scales & Conversion
Scale Comparison Table
| Fixed Point | Kelvin (K) | Celsius (°C) | Fahrenheit (°F) |
|---|---|---|---|
| Absolute zero | 0 | −273.15 | −459.67 |
| Triple point of water | 273.16 | 0.01 | 32.018 |
| Ice point (melting) | 273.15 | 0 | 32 |
| Steam point (boiling) | 373.15 | 100 | 212 |
| Human body temperature | ~310 | ~37 | ~98.6 |

Three Temperature Scales — Side by Side
"Celsius Adds 273" — To go from Celsius to Kelvin, always add 273.15. To go the other way, subtract. The interval sizes are identical: a change of 1 °C = a change of 1 K.
The Ideal Gas Equation
Building the Equation Step by Step
The ideal gas equation combines two experimental gas laws:
| Law | Statement | Mathematical Form |
|---|---|---|
| Boyle's Law | At constant T, P and V are inversely proportional. | PV = constant |
| Charles' Law | At constant P, V is directly proportional to T. | V/T = constant |
Combining both laws:
\[\frac {PV}{T}\] = constant
For μ moles of any ideal gas, this constant equals μR, giving us:
PV = μRT
| Symbol | Quantity | SI Unit |
|---|---|---|
| P | Pressure | Pascal (Pa) |
| V | Volume | m³ |
| μ | Number of moles | mol |
| R | Universal gas constant | 8.31 J mol⁻¹ K⁻¹ |
| T | Absolute temperature | Kelvin (K) only |
The ideal gas equation only works with Kelvin. If the problem gives temperature in Celsius, you must convert to Kelvin first: T(K) = T(°C) + 273.15. Using °C directly will yield an incorrect answer.
Example 1
= \[\frac {9}{5}\](24.57 − 273.15) + 32
= \[\frac {9}{5}\](−248.58) + 32
= −447.44 + 32 = −415.44 °F
Example 2
100y − 3200 = 180y − 49167
80y = 45967
y = 574.59
Key Points: Absolute Zero and Absolute Temperature
- Gases expand linearly with temperature, making them useful for thermometers. This consistent behaviour suggests the existence of a lowest temperature limit.
- Absolute zero (−273.15 °C or 0 K) is the temperature where an ideal gas would have zero pressure. It is the lowest possible temperature.
- The Kelvin scale begins at absolute zero and uses the triple point of water (273.16 K) as a reference point. It is the SI temperature scale.
- The ideal gas equation (PV = μRT) combines all gas laws into a single relationship among pressure, volume, and temperature. It works best for gases at low pressure and high temperature.
