Comprehensive Physics Study Guide: Class 11th
Units and Measurements
Fundamentals of Units:
- Unit Definition: An internationally accepted standard for the measurement of physical quantities. No measurement is complete without a numeric value and its corresponding unit.
- Fundamental (Base) Units: Units for quantities that cannot be derived from others (e.g., length, mass, time).
- Derived Units: Units formed by combinations of fundamental units (e.g., \text{m/s} for speed).
- System of Units: The combined set of fundamental and derived units.
- SI System (Systeme Internationale d'Unites): Developed in 1971, it includes 7 base units:
- Length: metre (\text{m})
- Mass: kilogram (\text{kg})
- Time: second (\text{s})
- Electric Current: ampere (\text{A})
- Thermodynamic Temperature: kelvin (\text{K})
- Amount of Substance: mole (\text{mol})
- Luminous Intensity: candela (\text{cd})
- Supplementary Dimensionless Units: Radian (\text{rad}) for plane angle and Steradian (\text{sr}) for solid angle.
Measurement of Length:
- Instruments:
- Metre scale: 10^{-3} \text{m} to 10^{2} \text{m}
- Vernier callipers: 10^{-4} \text{m}
- Screw gauge/Spherometer: 10^{-5} \text{m}
- Parallax Method: Used for measuring large distances (stars/planets). Parallax is the apparent displacement of an object against a background when viewed from two different points.
- Formula: \alpha = \frac{d}{D}, where \alpha is the angular size, d is the diameter, and D is the distance.
- Instruments:
Dimensional Analysis:
- Dimensional Formula: The expression showing which base quantities represent a physical quantity. Examples:
- Force: [MLT^{-2}]
- Energy/Work: [ML^{2}T^{-2}]
- Power: [ML^{2}T^{-3}]
- Applications: Deriving equations, checking dimensional correctness using the Principle of Homogeneity, and unit conversion.
- Dimensional Formula: The expression showing which base quantities represent a physical quantity. Examples:
Motion in a Straight Line
Kinematics vs. Dynamics:
- Kinematics: Describes motion without considering causes (forces).
- Dynamics: Examines the forces that cause motion.
Distance and Displacement:
- Distance: Total path traversed; scalar; always positive.
- Displacement: Shortest distance between initial (x1) and final (x2) positions (\Delta x = x2 - x1); vector; can be positive, negative, or zero.
Speed and Velocity:
- Average Velocity: Displacement per unit time: \bar{v} = \frac{\Delta x}{\Delta t}.
- Average Speed: Total path length per total time.
- Instantaneous Velocity: The limit of average velocity as \Delta t \to 0: v = \frac{dx}{dt}.
Acceleration:
- Average Acceleration: Change in velocity over time: \bar{a} = \frac{\Delta v}{\Delta t}.
- Instantaneous Acceleration: a = \frac{dv}{dt}.
Kinematic Equations for Uniform Acceleration:
- v = v_0 + at
- x = v_0t + \frac{1}{2}at^{2}
- v^{2} = v_0^{2} + 2ax
- X{nth} = v0 + \frac{a}{2}(2n - 1)
Motion in a Plane
Vector Operations:
- Resolution: Splitting a vector into components: A = Ax\hat{i} + Ay\hat{j}, where Ax = A\cos\theta and Ay = A\sin\theta.
- Addition: Done via the Triangle Law or Parallelogram Law: R = \sqrt{A^{2} + B^{2} + 2AB\cos\theta}.
Projectile Motion:
- Motion under gravity consisting of horizontal (constant velocity) and vertical (constant acceleration) components.
- Time of Maximum Height: tm = \frac{v0\sin\theta_0}{g}.
- Total Time of Flight: T = \frac{2v0\sin\theta0}{g}.
- Maximum Height: H = \frac{(v0\sin\theta0)^{2}}{2g}.
- Horizontal Range: R = \frac{v0^{2}\sin2\theta0}{g}.
Uniform Circular Motion:
- Constant speed (v) but changing direction.
- Centripetal Acceleration: Acceleration directed toward the center: a_c = \frac{v^{2}}{R} = \omega^{2}R.
Laws of Motion
Newton's First Law (Law of Inertia): A body remains at rest or in uniform motion unless an external force acts on it. Inertia depends on mass.
Newton's Second Law: Force is proportional to the rate of change of momentum: F = \frac{dp}{dt} = ma.
- Momentum (p): Product of mass and velocity (p = mv).
- Impulse (I): Force \times time: I = F\Delta t = \Delta p.
Newton's Third Law: To every action, there is an equal and opposite reaction acting on different bodies (F{AB} = -F{BA}).
Friction:
- Static Friction (fs): Opposes impending motion (f{s,max} = \mu_s R).
- Kinetic Friction (fk): Opposes actual relative motion (fk = \mu_k R).
Work, Energy, and Power
Work: Formally defined as the dot product of force and displacement: W = F \cdot d = Fd\cos\theta.
- Work-Energy Theorem: Work done by the net force equals the change in kinetic energy: W = \Delta K = \frac{1}{2}mvf^{2} - \frac{1}{2}mvi^{2}.
Forms of Energy:
- Kinetic Energy (K): Energy due to motion (K = \frac{p^{2}}{2m} = \frac{1}{2}mv^{2}).
- Potential Energy (V): Stored energy due to position. For a spring: U = \frac{1}{2}kx^{2}. For gravity: U = mgh.
- Mass-Energy Equivalence: E = mc^{2}.
Power (P): Rate of doing work. P = \frac{dW}{dt} = F \cdot v. SI Unit is Watt (1 \text{ hp} = 746 \text{ W}).
Collisions:
- Elastic: Both momentum and kinetic energy are conserved.
- Inelastic: Momentum conserved, but kinetic energy is lost.
System of Particles and Rotational Motion
Centre of Mass (COM): The point where the entire mass of a system is concentrated for treating translational motion.
- Coordinates: R{cm} = \frac{\sum mi ri}{\sum mi}.
Rotational Dynamics:
- Torque (\tau): Turning effect of a force: \tau = r \times F = rF\sin\theta.
- Angular Momentum (L): L = r \times p = I\omega.
- Moment of Inertia (I): Rotational analogue of mass: I = \sum mi ri^{2} = Mk^{2} (where k is radius of gyration).
Theorems of MI:
- Perpendicular Axis Theorem: Iz = Ix + I_y (for planar bodies).
- Parallel Axis Theorem: I = I_{cm} + Ma^{2}.
Gravitation
Universal Law of Gravitation: F = G \frac{m1 m2}{r^{2}}, where G = 6.67 \times 10^{-11} \text{ Nm}^{2}\text{/kg}^{2}.
Acceleration due to gravity (g):
- Surface: g = \frac{GM}{R^{2}} \approx 9.8 \text{ m/s}^{2}.
- Height (h): g' = g\left(1 + \frac{h}{R}\right)^{-2}.
- Depth (d): g' = g\left(1 - \frac{d}{R}\right).
Kepler’s Laws:
- 1. Law of Orbits: Planets move in elliptical orbits with the sun at one focus.
- 2. Law of Areas: Areal velocity is constant (\frac{dA}{dt} = \text{constant}).
- 3. Law of Periods: T^{2} \propto a^{3}.
Escape Velocity (ve): Minimum speed to escape a planet's pull: ve = \sqrt{\frac{2GM}{R}} = \sqrt{2gR}. (For Earth, 11.2 \text{ km/s}).
Mechanical Properties of Solids and Fluids
Solids:
- Stress: Force/Area (\frac{F}{A}). Types: Longitudinal, Shearing, Volumetric.
- Strain: Change in dimension/Original dimension. Types: Longitudinal, Shearing (\theta), Volumetric (\frac{\Delta V}{V}).
- Hooke's Law: Stress \propto Strain.
- Moduli: Young's Modulus (Y), Shear Modulus (\eta), Bulk Modulus (B).
Fluids:
- Pascal’s Law: Pressure applied to a confined fluid is transmitted equally in all directions.
- Bernoulli's Principle: For streamline flow: P + \frac{1}{2}\rho v^{2} + \rho gh = \text{constant}.
- Viscosity: Internal friction in fluids. Stokes Law: F = 6\pi\eta rv.
- Surface Tension (S): Force per unit length on liquid surface. Capillary Rise: h = \frac{2S\cos\theta}{r\rho g}.
Thermal Properties and Thermodynamics
Thermal Expansion:
- Linear: \Delta L = \alpha L\Delta T
- Volume: \Delta V = \gamma V\Delta T
- Relation: \gamma = 3\alpha
Laws of Thermodynamics:
- Zeroth Law: Defines temperature; if A and B are in equilibrium with C, they are in equilibrium with each other.
- First Law: \Delta Q = \Delta U + \Delta W (Energy conservation).
- Second Law: Entropy of the universe always increases; defines heat flow (hot to cold).
Thermodynamic Processes:
- Isothermal: constant T (PV = \text{constant}).
- Adiabatic: constant heat exchange (PV^{\gamma} = \text{constant}).
- Isobaric/Isochoric: constant pressure/volume.
Kinetic Theory of Gases:
- Provides molecular basis for pressure (P = \frac{1}{3}nmv^{2}) and temperature (KE = \frac{3}{2}k_B T).
Oscillations and Waves
Simple Harmonic Motion (SHM): Acceleration is proportional to displacement (a = -\omega^{2}x).
- Simple Pendulum Period: T = 2\pi \sqrt{\frac{L}{g}}.
- Total Energy in SHM: E = \frac{1}{2}kA^{2}.
Waves:
- Transverse Waves: Particles oscillate perpendicular to propagation (e.g., string waves).
- Longitudinal Waves: Particles oscillate parallel to propagation (e.g., sound waves).
- Speed of Sound: v = \sqrt{\frac{\gamma P}{\rho}}.
- Doppler Effect: Change in observed frequency due to relative motion of source and observer.