Class 11 – Chapter 0: All Important Maths Formulas
1) Algebraic Identities
\[ (a+b)^2 = a^2 + 2ab + b^2 \] \[ (a-b)^2 = a^2 - 2ab + b^2 \] \[ (a+b)(a-b) = a^2 - b^2 \] \[ (x+a)(x+b) = x^2 + (a+b)x + ab \] \[ (a+b+c)^2 = a^2 + b^2 + c^2 + 2(ab+bc+ca) \] \[ (a+b)^3 = a^3 + b^3 + 3ab(a+b) \] \[ (a-b)^3 = a^3 - b^3 - 3ab(a-b) \] \[ a^3 + b^3 = (a+b)(a^2 - ab + b^2) \] \[ a^3 - b^3 = (a-b)(a^2 + ab + b^2) \] \[ a^3 + b^3 + c^3 - 3abc = (a+b+c)(a^2+b^2+c^2-ab-bc-ca) \]2) Factorisation / Quadratic
\[ ax^2 + bx + c = 0 \implies x = \frac{-b \pm \sqrt{\,b^2 - 4ac\,}}{2a} \] \[ x^2 + (p+q)x + pq = (x+p)(x+q) \] \[ b^2 - 4ac = \Delta \text{ (discriminant)} \]3) Indices (Exponents)
\[ a^m \cdot a^n = a^{m+n}, \quad \frac{a^m}{a^n} = a^{m-n} \] \[ (a^m)^n = a^{mn}, \quad (ab)^n = a^n b^n \] \[ a^0 = 1 \ (a\neq0), \quad a^{-n} = \frac{1}{a^n} \]4) Surds
\[ \sqrt{ab} = \sqrt a\,\sqrt b \ (a,b \ge 0), \quad \sqrt{\tfrac{a}{b}} = \frac{\sqrt a}{\sqrt b} \ (b>0) \] \[ \sqrt a \cdot \sqrt a = a, \quad (\sqrt a + \sqrt b)^2 = a+b+2\sqrt{ab} \]5) Logarithms
\[ \log_a (mn) = \log_a m + \log_a n \] \[ \log_a \!\left(\frac{m}{n}\right) = \log_a m - \log_a n \] \[ \log_a (m^k) = k\,\log_a m \] \[ \log_a 1 = 0,\quad \log_a a = 1 \] \[ \log_a b = \frac{\log_c b}{\log_c a} \ (\text{change of base}) \] \[ a^{\log_a m} = m \]6) Series: AP & GP
\[ \text{AP: } a,\,a+d,\,a+2d,\dots \] \[ n\text{th term: } a_n = a + (n-1)d \] \[ \text{Sum of }n\text{ terms: } S_n = \frac{n}{2}\,[2a + (n-1)d] \] \[ \text{GP: } a,\,ar,\,ar^2,\dots \] \[ n\text{th term: } a_n = a\,r^{\,n-1} \] \[ \text{Sum of }n\text{ terms }(r\neq1):\; S_n = a\,\frac{1-r^{\,n}}{1-r} \] \[ \text{Infinite GP }(|r|<1):\; S_\infty = \frac{a}{1-r} \]7) Binomial Basics
\[ (x+y)^n = \sum_{k=0}^{n} \binom{n}{k} x^{\,n-k} y^{\,k} \] \[ \binom{n}{k} = \frac{n!}{k!\,(n-k)!}, \quad \binom{n}{k} = \binom{n}{n-k} \]8) Trigonometry – Pythagorean & Identities
\[ \sin^2\theta + \cos^2\theta = 1 \] \[ 1 + \tan^2\theta = \sec^2\theta,\quad 1 + \cot^2\theta = \csc^2\theta \] \[ \sin(2\theta) = 2\sin\theta\cos\theta \] \[ \cos(2\theta) = \cos^2\theta - \sin^2\theta = 1-2\sin^2\theta = 2\cos^2\theta-1 \] \[ \tan(2\theta) = \frac{2\tan\theta}{1-\tan^2\theta} \] \[ \sin(A\pm B)=\sin A\cos B \pm \cos A\sin B \] \[ \cos(A\pm B)=\cos A\cos B \mp \sin A\sin B \] \[ \tan(A\pm B)=\frac{\tan A \pm \tan B}{1 \mp \tan A \tan B} \]Trigonometric Ratios (Standard Angles)
Values of sin θ, cos θ, tan θ, cosec θ, sec θ, and cot θ at standard angles:
| \(\theta\) | \(\sin\theta\) | \(\cos\theta\) | \(\tan\theta\) | \(\csc\theta\) | \(\sec\theta\) | \(\cot\theta\) |
|---|---|---|---|---|---|---|
| \(0^\circ\) | 0 | 1 | 0 | Undefined | 1 | Undefined |
| \(30^\circ\) | \(\frac{1}{2}\) | \(\frac{\sqrt{3}}{2}\) | \(\frac{1}{\sqrt{3}}\) | 2 | \(\frac{2}{\sqrt{3}}\) | \(\sqrt{3}\) |
| \(45^\circ\) | \(\frac{\sqrt{2}}{2}\) | \(\frac{\sqrt{2}}{2}\) | 1 | \(\sqrt{2}\) | \(\sqrt{2}\) | 1 |
| \(60^\circ\) | \(\frac{\sqrt{3}}{2}\) | \(\frac{1}{2}\) | \(\sqrt{3}\) | \(\frac{2}{\sqrt{3}}\) | 2 | \(\frac{1}{\sqrt{3}}\) |
| \(90^\circ\) | 1 | 0 | Undefined | 1 | Undefined | 0 |
| \(120^\circ\) | \(\frac{\sqrt{3}}{2}\) | \(-\frac{1}{2}\) | \(-\sqrt{3}\) | \(\frac{2}{\sqrt{3}}\) | -2 | \(-\frac{1}{\sqrt{3}}\) |
| \(135^\circ\) | \(\frac{\sqrt{2}}{2}\) | \(-\frac{\sqrt{2}}{2}\) | -1 | \(\sqrt{2}\) | \(-\sqrt{2}\) | -1 |
| \(150^\circ\) | \(\frac{1}{2}\) | \(-\frac{\sqrt{3}}{2}\) | \(-\frac{1}{\sqrt{3}}\) | 2 | \(-\frac{2}{\sqrt{3}}\) | \(-\sqrt{3}\) |
| \(180^\circ\) | 0 | -1 | 0 | Undefined | -1 | Undefined |
| \(270^\circ\) | -1 | 0 | Undefined | -1 | Undefined | 0 |
| \(360^\circ\) | 0 | 1 | 0 | Undefined | 1 | Undefined |
9) Coordinate Geometry
\[ \text{Distance: } d = \sqrt{(x_2-x_1)^2 + (y_2-y_1)^2} \] \[ \text{Midpoint: } M\!\left(\frac{x_1+x_2}{2},\,\frac{y_1+y_2}{2}\right) \] \[ \text{Section (internal }m:n\text{): } \left(\frac{mx_2+nx_1}{m+n},\,\frac{my_2+ny_1}{m+n}\right) \] \[ \text{Slope: } m = \frac{y_2-y_1}{x_2-x_1} \] \[ \text{Point–slope: } y-y_1 = m(x-x_1) \] \[ \text{Slope–intercept: } y = mx + c \] \[ \text{Two-point: } \frac{y-y_1}{y_2-y_1} = \frac{x-x_1}{x_2-x_1} \] \[ \text{Intercept form: } \frac{x}{a} + \frac{y}{b} = 1 \] \[ \text{General form: } Ax + By + C = 0 \]10) Circle (Basics)
\[ (x - h)^2 + (y - k)^2 = r^2 \] \[ x^2 + y^2 + 2gx + 2fy + c = 0 \ \Rightarrow \ \text{center }(-g,-f),\ r=\sqrt{g^2+f^2-c} \]11) Triangle Geometry (2D)
\[ \text{Area: } \Delta = \frac{1}{2}\,|x_1(y_2-y_3)+x_2(y_3-y_1)+x_3(y_1-y_2)| \] \[ \text{Heron: } \Delta = \sqrt{s(s-a)(s-b)(s-c)},\ s=\frac{a+b+c}{2} \] \[ \text{Centroid: } \left(\frac{x_1+x_2+x_3}{3},\,\frac{y_1+y_2+y_3}{3}\right) \]12) Mensuration (Quick)
\[ \text{Area(circle)}=\pi r^2,\ \text{Circumference}=2\pi r \] \[ \text{Surface Area(sphere)}=4\pi r^2,\ \text{Volume(sphere)}=\frac{4}{3}\pi r^3 \] \[ \text{Volume(cylinder)}=\pi r^2 h,\ \text{Volume(cone)}=\frac{1}{3}\pi r^2 h \]13) Probability (Basics)
\[ P(E) = \frac{\text{favourable outcomes}}{\text{total outcomes}} \] \[ P(\bar E) = 1 - P(E) \] \[ P(A \cup B) = P(A) + P(B) - P(A \cap B) \]14) Inequalities (Basics)
\[ |x| = \begin{cases} x, & x \geq 0 \\ -x, & x < 0 \end{cases} \] \[ |x| < a \quad (a > 0) \quad \Rightarrow \quad -a < x < a \] \[ |x| > a \quad (a > 0) \quad \Rightarrow \quad x < -a \ \text{or} \ x > a \]Differentiation Formulas
1. \(\frac{d}{dx}(c) = 0\)
2. \(\frac{d}{dx}(x) = 1\)
3. \(\frac{d}{dx}(x^n) = n x^{n-1}\)
4. \(\frac{d}{dx}(e^x) = e^x\)
5. \(\frac{d}{dx}(a^x) = a^x \ln(a)\)
6. \(\frac{d}{dx}(\ln x) = \frac{1}{x}\)
7. \(\frac{d}{dx}(\log_a x) = \frac{1}{x \ln a}\)
8. \(\frac{d}{dx}(\sin x) = \cos x\)
9. \(\frac{d}{dx}(\cos x) = -\sin x\)
10. \(\frac{d}{dx}(\tan x) = \sec^2 x\)
11. \(\frac{d}{dx}(\cot x) = -\csc^2 x\)
12. \(\frac{d}{dx}(\sec x) = \sec x \tan x\)
13. \(\frac{d}{dx}(\csc x) = -\csc x \cot x\)
14. \(\frac{d}{dx}(\sin^{-1}x) = \frac{1}{\sqrt{1-x^2}}\)
15. \(\frac{d}{dx}(\cos^{-1}x) = -\frac{1}{\sqrt{1-x^2}}\)
16. \(\frac{d}{dx}(\tan^{-1}x) = \frac{1}{1+x^2}\)
17. \(\frac{d}{dx}(\cot^{-1}x) = -\frac{1}{1+x^2}\)
18. \(\frac{d}{dx}(\sec^{-1}x) = \frac{1}{|x|\sqrt{x^2-1}}\)
19. \(\frac{d}{dx}(\csc^{-1}x) = -\frac{1}{|x|\sqrt{x^2-1}}\)
Integration Formulas
1. \(\int 0 \, dx = C\)
2. \(\int 1 \, dx = x + C\)
3. \(\int x^n \, dx = \frac{x^{n+1}}{n+1} + C, \; n \neq -1\)
4. \(\int e^x \, dx = e^x + C\)
5. \(\int a^x \, dx = \frac{a^x}{\ln a} + C\)
6. \(\int \frac{1}{x} \, dx = \ln|x| + C\)
7. \(\int \sin x \, dx = -\cos x + C\)
8. \(\int \cos x \, dx = \sin x + C\)
9. \(\int \sec^2 x \, dx = \tan x + C\)
10. \(\int \csc^2 x \, dx = -\cot x + C\)
11. \(\int \sec x \tan x \, dx = \sec x + C\)
12. \(\int \csc x \cot x \, dx = -\csc x + C\)
13. \(\int \frac{1}{\sqrt{1-x^2}} \, dx = \sin^{-1}x + C\)
14. \(\int \frac{-1}{\sqrt{1-x^2}} \, dx = \cos^{-1}x + C\)
15. \(\int \frac{1}{1+x^2} \, dx = \tan^{-1}x + C\)
16. \(\int \frac{-1}{1+x^2} \, dx = \cot^{-1}x + C\)
17. \(\int \frac{1}{|x|\sqrt{x^2-1}} \, dx = \sec^{-1}x + C\)
18. \(\int \frac{-1}{|x|\sqrt{x^2-1}} \, dx = \csc^{-1}x + C\)
Units and Measurements - Class 11 Physics Notes
Physics is a science based on the measurement of physical quantities. Every observation and experiment requires measurement in a well-defined unit. To make communication universal, the International System of Units (SI system) is used worldwide.
1. Physical Quantities and Measurement
Physical Quantity: Any quantity that can be measured and expressed in terms of a unit.
Examples: Length, Mass, Time, Temperature, Electric Current, etc.
Measurement: Comparison of a physical quantity with a standard reference unit.
Example: If the length of a rod is 2 m, it means the rod is 2 times the chosen unit of length (1 m).
2. Systems of Units
Historically, different unit systems were used:
| System | Length | Mass | Time |
|---|---|---|---|
| CGS | cm | g | s |
| FPS | foot | pound | s |
| MKS | metre | kg | s |
| SI | metre | kg | s |
SI System (International System of Units)
Introduced in 1960, the SI system is the most widely accepted. It defines 7 fundamental quantities:
| Base Quantity | SI Unit | Symbol |
|---|---|---|
| Length | metre | m |
| Mass | kilogram | kg |
| Time | second | s |
| Electric current | ampere | A |
| Temperature | kelvin | K |
| Luminous intensity | candela | cd |
| Amount of substance | mole | mol |
👉 All other quantities like velocity, force, energy, pressure are derived quantities, expressed using these base units.
3. Significant Figures
Significant figures represent the precision and reliability of a measurement.
Rules for Counting Significant Figures
- All non-zero digits are significant.
Example: 456 → 3 significant figures. - Zeros between non-zero digits are significant.
Example: 1002 → 4 significant figures. - Leading zeros are not significant.
Example: 0.0045 → 2 significant figures. - Trailing zeros after a decimal are significant.
Example: 2.300 → 4 significant figures.
Importance: They show the reliability of experimental data.
4. Accuracy, Precision, and Errors
Accuracy: Closeness of a measured value to the true value.
Precision: Closeness of repeated measurements with each other.
Examples:
– If a clock shows 2:59 when the actual time is 3:00 → Accurate.
– If multiple readings are 2:59, 2:59, 2:59 → Precise.
Types of Errors
- Systematic Errors: Due to faulty instruments, poor calibration, or observer bias.
Example: Meter scale with worn-out edges. - Random Errors: Due to unpredictable variations.
Example: Fluctuation in temperature readings. - Least Count Error: Due to limitation of instrument resolution.
Formulas for Errors
\[
\text{Absolute Error} = | \text{Measured Value – True Value} |
\]
\[
\text{Mean Absolute Error} = \frac{\text{Sum of absolute errors}}{n}
\]
\[
\text{Relative Error} = \frac{\text{Mean Absolute Error}}{\text{True Value}}
\]
\[
\text{Percentage Error} = \text{Relative Error} \times 100
\]
5. Dimensional Analysis
Dimensions express a physical quantity in terms of fundamental quantities (M, L, T).
Examples:
Velocity = distance / time = \([M^0L^1T^{-1}]\)
Force = mass × acceleration = \([M^1L^1T^{-2}]\)
Uses of Dimensional Analysis
- Conversion of units from one system to another.
- Checking correctness of physical equations.
- Deriving relations between physical quantities.
Limitations
- Cannot find dimensionless constants (π, e).
- Cannot be applied to empirical formulas.
- Cannot give information about additive or multiplicative constants.
Summary - Key Points
- Measurement is comparison with a standard unit.
- SI system has 7 base quantities.
- Significant figures show precision of data.
- Accuracy ≠ Precision.
- Errors are unavoidable but can be minimized.
- Dimensional analysis is useful for unit conversion and equation verification.
Class 11 Physics Notes – Chapter 2: Motion in a Straight Line
Introduction
The study of motion without considering its cause is called Kinematics. Motion along a straight line is the simplest type, also called one-dimensional motion.
Points to Remember
- Scalar: only magnitude (distance, speed).
- Vector: magnitude + direction (displacement, velocity, acceleration).
Position, Path Length and Displacement
- Position: Location of a particle on a straight line w.r.t origin.
- Path length (Distance): Actual length of the path travelled; a scalar.
- Displacement: Change in position of the particle; a vector.
Formula: \(\Delta x = x_2 - x_1\)
Points to Remember
- Distance ≥ Displacement (always).
- Displacement can be zero even if distance is not zero.
Speed and Its Types
Speed = Rate of change of distance (scalar).
- Uniform Speed: Equal distances in equal intervals of time.
- Non-Uniform Speed: Unequal distances in equal intervals of time.
- Average Speed: \(\text{Average speed} = \frac{\text{Total distance}}{\text{Total time}}\)
- Instantaneous Speed: Speed at a given instant (speedometer reading).
Velocity and Its Types
Velocity = Rate of change of displacement (vector).
- Uniform Velocity: Equal displacements in equal intervals of time in the same direction.
- Non-Uniform Velocity: Unequal displacements OR change in direction.
- Average Velocity: \(v_{avg} = \frac{\Delta x}{\Delta t}\)
- Instantaneous Velocity: \(v = \frac{dx}{dt}\)
- Relative Velocity: \(v_{AB} = v_A - v_B\)
Points to Remember
- Speed ≥ |Velocity| (in magnitude).
- Velocity can be positive, negative or zero; speed cannot be negative.
- Uniform speed ≠ Uniform velocity (velocity depends on direction).
Acceleration
Acceleration = Rate of change of velocity.
Formulas: \(a_{avg} = \frac{\Delta v}{\Delta t}, \quad a = \frac{dv}{dt}\)
Points to Remember
- If velocity increases → acceleration positive.
- If velocity decreases → acceleration negative (retardation).
- Acceleration can be zero even if velocity is not zero (uniform velocity motion).
Equations of Motion (for uniform acceleration)
- \( v = u + at \)
- \( s = ut + \frac{1}{2}at^2 \)
- \( v^2 - u^2 = 2as \)
Where u = initial velocity, v = final velocity, a = acceleration, s = displacement, t = time
Points to Remember
- Valid only for constant acceleration.
- Derivable using calculus or graphs.
Graphs in Straight Line Motion
- Position–Time Graph (x–t): slope = velocity. Straight line → uniform velocity, Curve → variable velocity.
- Velocity–Time Graph (v–t): slope = acceleration, area under graph = displacement.
- Acceleration–Time Graph (a–t): area under graph = change in velocity.
Points to Remember
- Steeper slope = higher velocity/acceleration.
- v–t graph is most important for exam problems.
Relative Velocity in One Dimension
Formula: \(v_{AB} = v_A - v_B\)
- Same direction → difference of speeds.
- Opposite direction → sum of speeds.
Summary / Quick Revision Box
- Distance = scalar, Displacement = vector.
- Speed = scalar, Velocity = vector.
- Instantaneous velocity = slope of x–t graph.
- Acceleration = slope of v–t graph.
- Displacement = area under v–t graph.
- Change in velocity = area under a–t graph.
- Three equations of motion valid only for uniform acceleration.
- Relative velocity (1D): \( v_{AB} = v_A - v_B \).
Chapter 3: Motion in a Plane (Vectors and 2D Motion)
1. Scalars and Vectors
Scalar: Physical quantity having only magnitude (e.g., mass, time, speed, temperature).
Vector: Physical quantity having both magnitude and direction (e.g., displacement, velocity, force).
2. Types of Vectors
- Zero Vector: Magnitude = 0, direction arbitrary.
- Unit Vector: Vector with magnitude = 1, represents direction.
- Equal Vectors: Same magnitude and direction.
- Like Vectors: Same direction.
- Unlike Vectors: Opposite direction.
- Position Vector: Denotes the position of a point relative to origin.
- Co-initial Vectors: Vectors starting from the same point.
- Collinear Vectors: Parallel vectors.
- Coplanar Vectors: Vectors lying in the same plane.
3. Vector Operations
(a) Addition of Vectors
Triangle Law: If two vectors are represented as two sides of a triangle taken in order, then their sum is represented by the third side taken in opposite order.
Parallelogram Law: If two vectors are represented by adjacent sides of a parallelogram, their sum is represented by the diagonal.
(b) Subtraction of Vectors
(c) Resolution of a Vector
If a vector \(\vec{A}\) makes angle \(\theta\) with x-axis:
4. Scalar Product (Dot Product)
Work done:
Properties:
- If vectors are perpendicular → \(\vec{A} \cdot \vec{B} = 0\)
- If vectors are parallel → \(\vec{A} \cdot \vec{B} = AB\)
5. Vector Product (Cross Product)
Here, \(\hat{n}\) is a unit vector perpendicular to the plane of \(\vec{A}, \vec{B}\). Direction is given by the Right-Hand Rule.
Magnitude:
Applications:
- Torque: \(\vec{\tau} = \vec{r} \times \vec{F}\)
- Angular momentum: \(\vec{L} = \vec{r} \times \vec{p}\)
6. Geometrical Applications of Vectors
(a) Area of a Triangle:
(b) Area of a Parallelogram:
(c) Area of a Rectangle:
(d) Area of a Rhombus:
where \(d_1, d_2\) are diagonals.
7. Direction Cosines and Direction Ratios
If a vector \(\vec{A}\) makes angles \(\alpha, \beta, \gamma\) with x, y, z axes:
Relation:
Direction Ratios (DRs): Any numbers proportional to \((l, m, n)\).
8. Projectile Motion
(a) Horizontal Projectile
When a body is projected horizontally with velocity \(u\) from a height \(h\):
- Time of flight: \(T = \sqrt{\frac{2h}{g}}\)
- Horizontal range: \(R = uT = u \sqrt{\frac{2h}{g}}\)
- Path equation: \(y = \frac{1}{2} g \left(\frac{x}{u}\right)^2\)
(b) Oblique Projectile
When a body is projected with velocity \(u\) at an angle \(\theta\) with the horizontal:
- Time of flight: \(T = \frac{2u \sin \theta}{g}\)
- Maximum height: \(H = \frac{u^2 \sin^2 \theta}{2g}\)
- Horizontal range: \(R = \frac{u^2 \sin 2\theta}{g}\)
- Equation of trajectory: \(y = x \tan \theta - \frac{gx^2}{2u^2 \cos^2 \theta}\)
- Path: Parabola
Laws of Motion & Dynamics – Class 11 Physics Notes
1. Intuitive Concept of Force
Force is any influence that can change the state of rest or motion of a body. Represented by \(\vec{F}\), measured in Newton (N).
Types of Force:
- Contact forces: Push, pull, tension
- Non-contact forces: Gravity, magnetic, electrostatic
Effect of Force: Changes velocity (causes acceleration) and can deform a body.
2. Inertia & Newton’s First Law of Motion
Inertia: Tendency of a body to resist changes in motion. Depends on mass: larger mass → larger inertia.
Newton’s First Law: A body remains at rest or in uniform motion unless acted upon by an external force.
Examples:
- Passenger falls forward when a bus stops suddenly
- Book remains on a table until pushed
Applications: Seat belts, vehicle brakes, safety measures in transport
3. Momentum & Newton’s Second Law
Momentum:
\(\vec{p} = m \vec{v}\)
Newton’s Second Law:
\(\vec{F} = \frac{d\vec{p}}{dt} = m\vec{a} \quad (\text{if } m \text{ is constant})\)
Impulse:
\(\vec{J} = \vec{F} \Delta t = \Delta \vec{p}\)
Applications: Catching a ball, vehicle collisions, airbags
4. Newton’s Third Law of Motion
Statement: For every action, there is an equal and opposite reaction. Forces act on different bodies.
Examples: Recoil of a gun, rocket propulsion, swimming
5. Law of Conservation of Linear Momentum
Statement: Total momentum of a system remains constant if no external force acts:
\(\vec{p}_\text{initial} = \vec{p}_\text{final}\)
Applications:
- Elastic and inelastic collisions
- Recoil of gun
- Rocket motion
6. Equilibrium of Concurrent Forces
Particle is in equilibrium if:
\(\sum \vec{F} = 0\)
Resolve forces along axes:
\(\sum F_x = 0, \quad \sum F_y = 0\)
Example: Hanging lamp supported by two ropes
7. Friction
Definition: Force opposing relative motion between surfaces. Originates from microscopic roughness and interlocking of surfaces.
Types:
- Static friction (\(f_s\)) – prevents motion at rest
- Kinetic friction (\(f_k\)) – opposes sliding motion
- Rolling friction – smaller than sliding friction
Laws of Friction:
- Friction ∝ Normal force: \( f \propto N \)
- Independent of contact area
- Static friction > Kinetic friction
Limiting friction: \( f_\text{max} = \mu N \)
Angle of Friction (\(\theta\)): \(\tan \theta = \mu\)
Angle of Repose (\(\alpha\)): \(\tan \alpha = \mu\)
Lubrication: Reduces friction using oil or grease
Applications: Vehicles, machinery, ramps
8. Dynamics of Uniform Circular Motion
Centripetal Force: Force towards center keeping body in circular motion:
\[
F_c = \frac{mv^2}{r}
\]
Centripetal acceleration:
\[
a_c = \frac{v^2}{r}
\]
Examples:
- Vehicle on a level circular road: friction provides centripetal force
- Vehicle on a banked road (frictionless): \(\tan \theta = \frac{v^2}{rg}\)
Applications: Banking of roads, roller coasters, satellites, planets
9. Pulley System (Two-Mass)
Two masses \( m_1 \) and \( m_2 \) connected by a light string over frictionless pulley (\( m_1 > m_2 \))
Forces:
- \( m_1 \) downward: \( m_1 g - T = m_1 a \)
- \( m_2 \) upward: \( T - m_2 g = m_2 a \)
Acceleration: \( a = \frac{(m_1 - m_2) g}{m_1 + m_2} \)
Tension: \( T = \frac{2 m_1 m_2 g}{m_1 + m_2} \)
Applications: Lifting weights, cranes, elevators
10. Important Formulas
| Concept | Formula |
|---|---|
| Momentum | \(\vec{p} = m \vec{v}\) |
| Force | \(\vec{F} = m\vec{a}\) |
| Impulse | \(\vec{J} = \vec{F} \Delta t = \Delta \vec{p}\) |
| Friction | \(f \leq \mu N\) |
| Limiting friction | \(f_\text{max} = \mu N\) |
| Circular motion | \(F_c = \frac{mv^2}{r}, a_c = \frac{v^2}{r}\) |
| Banked road | \(\tan \theta = \frac{v^2}{rg}\) |
| Pulley acceleration | \(a = \frac{(m_1 - m_2) g}{m_1 + m_2}\) |
| Pulley tension | \(T = \frac{2 m_1 m_2 g}{m_1 + m_2}\) |
| Weight | \(W = mg\) |
| Normal reaction (inclined plane) | \(N = W \cos \theta\) |
Unit IV: Work, Energy, and Power – Class 11 Physics Notes
1. Work Done by a Force
Definition: Work is done when a force displaces a body in the direction of the force.
Formula (constant force):
\[
W = \vec{F} \cdot \vec{d} = Fd \cos \theta
\]
\(\theta\) = angle between force and displacement. Work is positive if along displacement, negative if opposite.
Variable force:
\[
W = \int_{x_1}^{x_2} F(x) \, dx
\]
Unit: Joule (1 J = 1 N·m)
Example: Pushing a block, lifting a weight, stretching a spring.
2. Kinetic Energy and Work-Energy Theorem
Kinetic Energy (KE):
\[
KE = \frac{1}{2} m v^2
\]
Work-Energy Theorem: Work done by net force = change in kinetic energy:
\[
W_\text{net} = KE_f - KE_i = \Delta KE
\]
Example: A car accelerating or braking.
3. Power
Definition: Rate of doing work:
\[
P = \frac{dW}{dt}
\]
Average Power:
\[
P_\text{avg} = \frac{W}{\Delta t}
\]
Unit: Watt (1 W = 1 J/s)
Example: A motor lifting a weight, running engine power.
4. Potential Energy (PE)
Gravitational PE:
\[
PE = m g h
\]
Elastic potential energy of a spring:
\[
PE_\text{spring} = \frac{1}{2} k x^2
\]
\(k\) = spring constant, \(x\) = displacement from equilibrium
5. Conservative and Non-Conservative Forces
5.1 Conservative Forces
Work done is independent of path:
\[
\oint \vec{F} \cdot d\vec{r} = 0
\]
Can be expressed as:
\[
\vec{F} = -\nabla U
\]
Examples: Gravity, spring force, electrostatic force
Mechanical Energy Conservation:
\[
KE + PE = \text{constant}
\]
5.2 Non-Conservative Forces
Work depends on the path; energy dissipates as heat or sound.
Examples: Friction, air resistance, viscous forces
Work-energy relation:
\[
W_\text{nc} = \Delta KE + \Delta PE
\]
Applications: Braking vehicles, sliding blocks, dissipative systems
6. Motion in a Vertical Circle
Particle of mass \(m\) in vertical circle of radius \(r\):
- Minimum speed at top: \(v_\text{top} = \sqrt{r g}\)
- Tension at top:
\[ T + mg = \frac{mv^2}{r} \]
Applications: Pendulum, roller coaster loops, satellites.
7. Collisions
7.1 Elastic Collision
Both momentum and kinetic energy conserved.
1D Elastic Collision Formulas:
\[
v_1' = \frac{m_1 - m_2}{m_1 + m_2} v_1 + \frac{2 m_2}{m_1 + m_2} v_2
\]
\[
v_2' = \frac{2 m_1}{m_1 + m_2} v_1 - \frac{m_1 - m_2}{m_1 + m_2} v_2
\]
7.2 Inelastic Collision
Momentum conserved, kinetic energy not conserved.
2D collision momentum conservation along axes:
\[
m_1 \vec{v}_1 + m_2 \vec{v}_2 = m_1 \vec{v}_1' + m_2 \vec{v}_2'
\]
8. Important Formulas
| Concept | Formula |
|---|---|
| Work (constant force) | \( W = F d \cos \theta \) |
| Work (variable force) | \( W = \int F(x) dx \) |
| Kinetic Energy | \( KE = \frac{1}{2} m v^2 \) |
| Work-Energy Theorem | \( W_\text{net} = \Delta KE \) |
| Power | \( P = \frac{dW}{dt}, \quad P_\text{avg} = \frac{W}{\Delta t} \) |
| Gravitational PE | \( PE = m g h \) |
| Elastic PE | \( PE_\text{spring} = \frac{1}{2} k x^2 \) |
| Mechanical energy conservation | \( KE + PE = \text{constant} \) |
| Circular motion (tension at top) | \( T + mg = \frac{mv^2}{r} \) |
| 1D Elastic collision | \( v_1', v_2' \) formulas above |
| Momentum (2D collision) | \( m_1 \vec{v}_1 + m_2 \vec{v}_2 = m_1 \vec{v}_1' + m_2 \vec{v}_2' \) |
Chapter 6: System of Particles and Rotational Motion
1. Centre of Mass of a Two-Particle System
Definition: The point where the total mass of the system is considered concentrated for translational motion.
- Equal masses: COM at midpoint.
- COM closer to heavier mass.
- Exam Tip: Used in collision and external force problems.
2. Momentum Conservation and Centre of Mass Motion
Conservation: If no external force, \( \vec{P}_{initial} = \vec{P}_{final} \).
- Isolated system: COM velocity constant.
- Applications: Rocket propulsion, explosions (COM at rest if initial momentum zero).
- Exam Tip: Solve collision velocities in COM frame.
3. Centre of Mass of a Rigid Body
Uniform Rod: COM at midpoint,
- Symmetric bodies: COM at centre of symmetry.
- Exam Tip: Use integration for non-uniform density; symmetry for uniform bodies.
4. Moment of a Force and Torque
Unit: N·m.
- Causes rotational motion.
- Direction: Right-hand rule.
- Exam Tip: Zero torque if force through axis or parallel to \( \vec{r} \).
5. Angular Momentum
- Unit: kg·m²/s.
- Exam Tip: Use perpendicular components in calculations.
6. Law of Conservation of Angular Momentum
Law: If no external torque,
Applications:
- Ice skater: Pulling arms in increases \( \omega \).
- Diving: Tucking body increases rotation speed.
- Planetary motion, boomerang.
- Exam Tip: Use \( I_1 \omega_1 = I_2 \omega_2 \)
7. Equilibrium of Rigid Bodies
Types: Stable, unstable, neutral.
- Exam Tip: Solve ladder problems by balancing torques about pivot.
8. Rigid Body Rotation and Equations of Rotational Motion
Angular Quantities: Displacement \( \theta \), velocity
Equations (Constant \( \alpha \)):
- \( \omega = \omega_0 + \alpha t \)
- \( \theta = \omega_0 t + \frac{1}{2} \alpha t^2 \)
- \( \omega^2 = \omega_0^2 + 2 \alpha \theta \)
- Exam Tip: Analogous to \( F = ma \).
9. Comparison of Linear and Rotational Motions
| Linear | Rotational |
|---|---|
| Displacement: \( x \) | Angular displacement: \( \theta \) |
| Velocity: \( v = \frac{dx}{dt} \) | Angular velocity: \( \omega = \frac{d\theta}{dt} \) |
| Acceleration: \( a = \frac{dv}{dt} \) | Angular acceleration: \( \alpha = \frac{d\omega}{dt} \) |
| Mass: \( m \) | Moment of inertia: \( I \) |
| Force: \( F = ma \) | Torque: \( \tau = I \alpha \) |
| Momentum: \( p = mv \) | Angular momentum: \( L = I \omega \) |
| Kinetic Energy: \( \frac{1}{2} m v^2 \) | Rotational KE: \( \frac{1}{2} I \omega^2 \) |
| Work: \( F \cdot s \) | Work: \( \tau \cdot \theta \) |
- Exam Tip: Use analogies for problem-solving.
10. Moment of Inertia and Radius of Gyration
Values for Objects:
- Thin rod (centre, perpendicular): \( I = \frac{1}{12} M L^2 \)
- Thin rod (end): \( I = \frac{1}{3} M L^2 \)
- Rectangular lamina (centre): \( I = \frac{1}{12} M (a^2 + b^2) \)
- Thin ring (diameter): \( I = \frac{1}{2} M R^2 \)
- Thin ring (axis): \( I = M R^2 \)
- Disc (diameter): \( I = \frac{1}{4} M R^2 \)
- Disc (axis): \( I = \frac{1}{2} M R^2 \)
- Solid sphere (diameter): \( I = \frac{2}{5} M R^2 \)
- Hollow sphere (diameter): \( I = \frac{2}{3} M R^2 \)
- Theorems: Parallel axis: \( I = I_{cm} + M d^2 \); Perpendicular axis:\( I_z = I_x + I_y \).
- Exam Tip: Choose axis carefully; apply theorems to shift axes.
Summary / Quick Revision Box
- COM: Weighted average position; \( M \vec{a_{cm}} = \vec{F_{ext}} \).
- Momentum: Conserved if no external force.
- Torque: \( \vec{\tau} = \vec{r} \times \vec{F} = I \alpha \).
- Angular Momentum: \( \vec{L} = I \omega \), conserved if no external torque.
- Equilibrium: \( \sum \vec{F} = 0 \),\( \sum \vec{\tau} = 0 \).
- Rotational Equations: Analogous to linear; use for constant \( \alpha \).
- Linear vs Rotational: Analogous quantities (e.g., \( m \leftrightarrow I \)).
- Moment of Inertia: Depends on mass distribution; use standard values.
- Radius of Gyration: \( k = \sqrt{\frac{I}{M}} \).
Chapter 7: Gravitation
1. Kepler’s Laws of Planetary Motion
First Law (Law of Ellipses): Planets move in elliptical orbits with the Sun at one focus.
Second Law (Law of Equal Areas): The line joining a planet to the Sun sweeps equal areas in equal time intervals.
Third Law (Law of Periods): The square of the orbital period is proportional to the cube of the semi-major axis.
- Exam Tip: Use third law to find orbital period or radius; applies to satellites too.
2. Universal Law of Gravitation
Newton’s Law: Every particle attracts every other particle with a force proportional to the product of their masses and inversely proportional to the square of the distance between them.
G: Gravitational constant, \( G = 6.67 \times 10^{-11} \, \text{N·m}^2/\text{kg}^2 \).
- Vector form: \( \vec{F} = -\frac{G m_1 m_2}{r^2} \hat{r} \)
- Exam Tip: Use for calculating force between masses; direction is along the line joining them.
3. Acceleration Due to Gravity
Definition: Acceleration of an object due to Earth’s gravitational pull, \( g = 9.8 \, \text{m/s}^2 \) (surface value).
Variation with Altitude (h):
Variation with Depth (d):
- At Earth’s centre: \( g_d = 0 \) (d = R).
- Exam Tip: Use approximate formulas for small \( h \) or \( d \); note \( g \) decreases with altitude and depth.
4. Gravitational Potential Energy
Definition: Energy due to the position of a mass in a gravitational field.
- Negative sign indicates bound system; zero at infinity.
- Exam Tip: Use to calculate work done in moving masses; change in \( U = -\text{Work} \).
5. Gravitational Potential
Definition: Potential energy per unit mass at a point in the gravitational field.
- Unit: J/kg.
- Relation: \( U = m V \).
- Exam Tip: Use to find potential at a point; useful for energy conservation problems.
6. Escape Speed
Definition: Minimum speed required for an object to escape Earth’s gravitational field.
- For Earth: \( v_e \approx 11.2 \, \text{km/s} \).
- Exam Tip: Independent of object’s mass; use conservation of energy to derive.
7. Orbital Velocity of a Satellite
Definition: Speed required for a satellite to maintain a circular orbit.
- For near-Earth orbit: \( v_o \approx 7.9 \, \text{km/s} \).
- Exam Tip: Derived from balancing gravitational force and centripetal force.
8. Energy of an Orbiting Satellite
Kinetic Energy:
Potential Energy:
Total Energy:
- Negative total energy indicates bound orbit.
- Exam Tip: Use total energy to compare orbits; smaller \( r \) means lower (more negative) energy.
Chapter 8: Mechanical Properties of Solids
1. Elasticity
Definition: Property of a material to regain its original shape and size after removal of deforming force.
- Elastic Limit: Maximum stress a material can withstand without permanent deformation.
- Types: Perfectly elastic (returns to original shape completely, e.g., quartz), partially elastic (partial recovery, e.g., rubber).
- Exam Tip: Elasticity is key for materials in springs, bridges, and structures.
2. Stress-Strain Relationship
Stress: Internal force per unit area resisting deformation.
Types of Stress:
- Normal Stress: Perpendicular to surface (tensile or compressive).
- Shear Stress: Parallel to surface.
Strain: Relative deformation due to stress.
Types of Strain:
- Longitudinal Strain: \( \frac{\Delta L}{L} \)
- Shear Strain: Angular deformation (qualitative).
- Volumetric Strain: \( \frac{\Delta V}{V} \)
- Stress-Strain Curve: Shows elastic region (linear), yield point, and plastic region.
- Exam Tip: Linear portion obeys Hooke’s law; beyond yield point, permanent deformation occurs.
3. Hooke’s Law
Statement: Within elastic limit, stress is directly proportional to strain.
- \( k \): Modulus of elasticity (depends on type of stress/strain).
- Exam Tip: Applies only in elastic region; used to calculate moduli.
4. Young’s Modulus
Definition: Measure of stiffness under tensile or compressive stress.
- Unit: N/m² or Pa.
- Higher \( Y \): Stiffer material (e.g., steel > rubber).
- Exam Tip: Use for problems involving stretching/compressing wires or rods.
5. Bulk Modulus
Definition: Measure of resistance to uniform compression (volume change).
- Unit: N/m² or Pa.
- Negative sign: Volume decreases with pressure.
- Exam Tip: Liquids have high \( K \); gases have low \( K \).
6. Shear Modulus of Rigidity (Qualitative Idea)
Definition: Measure of resistance to shear deformation.
- Unit: N/m² or Pa.
- Qualitative: Describes how materials resist shape change without volume change (e.g., twisting of a shaft).
- Exam Tip: Focus on concept; numerical problems less common.
7. Poisson’s Ratio
Definition: Ratio of transverse strain to longitudinal strain under tensile stress.
- Negative sign: Lateral contraction with longitudinal extension.
- Range: Typically 0 to 0.5 for most materials.
- Exam Tip: Understand concept; rarely used in numericals but important for material properties.
8. Elastic Energy
Definition: Potential energy stored in a deformed elastic body.
- Analogous to spring energy: \( U = \frac{1}{2} k x^2 \).
- Exam Tip: Calculate for stretched wires or compressed materials; use in energy conservation problems.
9. Application of Elastic Behavior of Materials (Qualitative Idea)
- Construction: High Young’s modulus materials (e.g., steel) used in bridges, buildings for rigidity.
- Springs: Elastic energy storage for mechanical devices.
- Shock Absorbers: Materials with controlled elasticity to absorb vibrations.
- Medical: Elastic properties in prosthetics or implants to mimic tissues.
- Exam Tip: Focus on examples like beams bending or wires stretching; relate to moduli.
Summary / Quick Revision Box
- Elasticity: Ability to regain shape; elastic limit key for deformation.
- Stress: \( \frac{F}{A} \), types: normal, shear.
- Strain: \( \frac{\text{Change}}{\text{Original}} \), types: longitudinal, shear, volumetric.
- Hooke’s Law: \( \text{Stress} \propto \text{Strain} \).
- Young’s Modulus: \( Y = \frac{F L}{A \Delta L} \).
- Bulk Modulus: \( K = -\frac{P V}{\Delta V} \).\( G = \frac{\text{Shear stress}}{\text{Shear strain}} \)
Chapter 9: Mechanical Properties of Fluids
1. Pressure Due to a Fluid Column
Definition: Pressure exerted by a fluid due to its weight at a given depth.
- \( \rho \): Density of fluid, \( g \): Acceleration due to gravity, \( h \): Depth.
- Unit: N/m² or Pa.
- Exam Tip: Use for calculating pressure in liquids like water or oil at different depths.
2. Pascal’s Law and Its Applications
Pascal’s Law: Pressure applied to an enclosed fluid is transmitted equally in all directions.
Applications:
- Hydraulic Lift: Uses pressure transmission to lift heavy loads.
- Hydraulic Brakes: Pressure applied to brake fluid transmits force to brake pads.
- Exam Tip: Solve for force amplification in hydraulic systems using area ratios.
3. Effect of Gravity on Fluid Pressure
Effect: Pressure increases with depth due to weight of fluid column.
- \( P_0 \): Atmospheric pressure at surface.
- Exam Tip: Use for problems involving pressure at depth in open containers or dams.
4. Viscosity
Definition: Internal friction in a fluid resisting relative motion of its layers.
- \( \eta \): Coefficient of viscosity, \( A \): Area, \( \frac{dv}{dx} \): Velocity gradient.
- Unit: Pa·s or kg/(m·s).
- Examples: Honey (high viscosity), water (low viscosity).
- Exam Tip: Understand viscosity’s role in fluid flow resistance.
5. Stokes’ Law and Terminal Velocity
Stokes’ Law: Drag force on a small sphere moving through a viscous fluid.
Terminal Velocity: Constant velocity when net force on falling object is zero.
- \( r \): Radius of sphere, \( \rho \): Density of sphere, \( \sigma \): Density of fluid.
- Exam Tip: Use for objects like raindrops or small particles in fluids.
6. Streamline and Turbulent Flow, Critical Velocity
Streamline Flow: Smooth, layered flow; particles follow fixed paths.
Turbulent Flow: Chaotic, irregular flow with eddies.
Critical Velocity: Velocity above which flow becomes turbulent.
- \( R_e \): Reynolds number (dimensionless), \( \eta \): Viscosity, \( d \): Pipe diameter.
- Exam Tip: Low \( R_e \) (<2000) for streamline, high \( R_e \) (>3000) for turbulent.
7. Bernoulli’s Theorem and Its Applications
Theorem: For an incompressible, non-viscous fluid in streamline flow, total energy per unit volume is constant.
Applications:
- Torricelli’s Law: Speed of liquid exiting a hole in a tank.
- Dynamic Lift: Lift on airplane wings or spinning balls due to pressure difference.
- Exam Tip: Apply to venturi meters, airfoils, or liquid flow problems.
8. Surface Energy and Surface Tension
Surface Tension: Force per unit length acting on the surface of a liquid.
Surface Energy: Energy required to increase surface area by unit area.
- Unit: N/m or J/m².
- Exam Tip: Relate surface tension to cohesive forces in liquids.
9. Angle of Contact
Definition: Angle between tangent to liquid surface and solid surface inside the liquid.
- \( \theta < 90^\circ \): Concave meniscus (e.g., water-glass).
- \( \theta > 90^\circ \): Convex meniscus (e.g., mercury-glass).
- Exam Tip: Determines capillary action; depends on liquid-solid interaction.
10. Excess Pressure Across a Curved Surface
Excess Pressure: Pressure difference across a curved liquid surface.
- Drop: \( P = \frac{2 T}{R} \)
- Soap Bubble: \( P = \frac{4 T}{R} \)(two surfaces).
- Exam Tip: Use for problems involving bubbles or droplets; note factor of 4 for soap bubbles.
11. Application of Surface Tension: Capillary Rise
Capillary Rise: Rise or fall of liquid in a narrow tube due to surface tension.
- \( h \): Height of rise, \( \theta \): Angle of contact, \( r \): Radius of tube.
- Rise: \( \theta < 90^\circ \); Fall: \( \theta > 90^\circ \).
- Exam Tip: Use for problems involving water rising in plants or capillary tubes.
Summary / Quick Revision Box
- Pressure: \( P = \rho g h \),\( P = P_0 + \rho g h \).
- Pascal’s Law: \( \frac{F_1}{A_1} = \frac{F_2}{A_2} \)(hydraulic systems).
- Viscosity: \( F = \eta A \frac{dv}{dx} \).
- Stokes’ Law: \( F_d = 6 \pi \eta r v \), Terminal velocity:\( v_t = \frac{2 r^2 (\rho - \sigma) g}{9 \eta} \).
- Flow: Streamline at low \( R_e \), turbulent at high \( R_e \); \( v_c = \frac{R_e \eta}{\rho d} \).
- Bernoulli’s: \( P + \rho g h + \frac{1}{2} \rho v^2 = \text{constant} \).
- Torricelli’s Law: \( v = \sqrt{2 g h} \).
- Surface Tension: \( T = \frac{F}{l} \), Energy:\( E = T \times \Delta A \).
- Excess Pressure: Drop: \( P = \frac{2 T}{R} \), Bubble:\( P = \frac{4 T}{R} \).
- Capillary Rise: \( h = \frac{2 T \cos \theta}{\rho g r} \).
Chapter 9: Mechanical Properties of Fluids
1. Pressure Due to a Fluid Column
Definition: Pressure exerted by a fluid due to its weight at a given depth.
- \( \rho \): Density of fluid, \( g \): Acceleration due to gravity, \( h \): Depth.
- Unit: N/m² or Pa.
- Exam Tip: Use for calculating pressure in liquids like water or oil at different depths.
2. Pascal’s Law and Its Applications
Pascal’s Law: Pressure applied to an enclosed fluid is transmitted equally in all directions.
Applications:
- Hydraulic Lift: Uses pressure transmission to lift heavy loads.
- Hydraulic Brakes: Pressure applied to brake fluid transmits force to brake pads.
- Exam Tip: Solve for force amplification in hydraulic systems using area ratios.
3. Effect of Gravity on Fluid Pressure
Effect: Pressure increases with depth due to weight of fluid column.
- \( P_0 \): Atmospheric pressure at surface.
- Exam Tip: Use for problems involving pressure at depth in open containers or dams.
4. Viscosity
Definition: Internal friction in a fluid resisting relative motion of its layers.
- \( \eta \): Coefficient of viscosity, \( A \): Area, \( \frac{dv}{dx} \): Velocity gradient.
- Unit: Pa·s or kg/(m·s).
- Examples: Honey (high viscosity), water (low viscosity).
- Exam Tip: Understand viscosity’s role in fluid flow resistance.
5. Stokes’ Law and Terminal Velocity
Stokes’ Law: Drag force on a small sphere moving through a viscous fluid.
Terminal Velocity: Constant velocity when net force on falling object is zero.
- \( r \): Radius of sphere, \( \rho \): Density of sphere, \( \sigma \): Density of fluid.
- Exam Tip: Use for objects like raindrops or small particles in fluids.
6. Streamline and Turbulent Flow, Critical Velocity
Streamline Flow: Smooth, layered flow; particles follow fixed paths.
Turbulent Flow: Chaotic, irregular flow with eddies.
Critical Velocity: Velocity above which flow becomes turbulent.
- \( R_e \): Reynolds number (dimensionless), \( \eta \): Viscosity, \( d \): Pipe diameter.
- Exam Tip: Low \( R_e \) (<2000) for streamline, high \( R_e \) (>3000) for turbulent.
7. Bernoulli’s Theorem and Its Applications
Theorem: For an incompressible, non-viscous fluid in streamline flow, total energy per unit volume is constant.
Applications:
- Torricelli’s Law: Speed of liquid exiting a hole in a tank.
- Dynamic Lift: Lift on airplane wings or spinning balls due to pressure difference.
- Exam Tip: Apply to venturi meters, airfoils, or liquid flow problems.
8. Surface Energy and Surface Tension
Surface Tension: Force per unit length acting on the surface of a liquid.
Surface Energy: Energy required to increase surface area by unit area.
- Unit: N/m or J/m².
- Exam Tip: Relate surface tension to cohesive forces in liquids.
9. Angle of Contact
Definition: Angle between tangent to liquid surface and solid surface inside the liquid.
- \( \theta < 90^\circ \): Concave meniscus (e.g., water-glass).
- \( \theta > 90^\circ \): Convex meniscus (e.g., mercury-glass).
- Exam Tip: Determines capillary action; depends on liquid-solid interaction.
10. Excess Pressure Across a Curved Surface
Excess Pressure: Pressure difference across a curved liquid surface.
- Drop: \( P = \frac{2 T}{R} \)
- Soap Bubble: \( P = \frac{4 T}{R} \)(two surfaces).
- Exam Tip: Use for problems involving bubbles or droplets; note factor of 4 for soap bubbles.
11. Application of Surface Tension: Capillary Rise
Capillary Rise: Rise or fall of liquid in a narrow tube due to surface tension.
- \( h \): Height of rise, \( \theta \): Angle of contact, \( r \): Radius of tube.
- Rise: \( \theta < 90^\circ \); Fall: \( \theta > 90^\circ \).
- Exam Tip: Use for problems involving water rising in plants or capillary tubes.
Summary / Quick Revision Box
- Pressure: \( P = \rho g h \),\( P = P_0 + \rho g h \).
- Pascal’s Law: \( \frac{F_1}{A_1} = \frac{F_2}{A_2} \)(hydraulic systems).
- Viscosity: \( F = \eta A \frac{dv}{dx} \).
- Stokes’ Law: \( F_d = 6 \pi \eta r v \), Terminal velocity:\( v_t = \frac{2 r^2 (\rho - \sigma) g}{9 \eta} \).
- Flow: Streamline at low \( R_e \), turbulent at high \( R_e \); \( v_c = \frac{R_e \eta}{\rho d} \).
- Bernoulli’s: \( P + \rho g h + \frac{1}{2} \rho v^2 = \text{constant} \).
- Torricelli’s Law: \( v = \sqrt{2 g h} \).
- Surface Tension: \( T = \frac{F}{l} \), Energy:\( E = T \times \Delta A \).
- Excess Pressure: Drop: \( P = \frac{2 T}{R} \), Bubble:\( P = \frac{4 T}{R} \).
- Capillary Rise: \( h = \frac{2 T \cos \theta}{\rho g r} \).
Chapter 10: Thermal Properties of Matter
1. Heat and Temperature
Heat: Form of energy transferred due to temperature difference.
- Unit: Joule (J).
- Temperature: Measure of average kinetic energy of particles.
- Unit: Kelvin (K) or Celsius (°C).
- Relation: \( T_K = T_C + 273.15 \).
- Exam Tip: Use Kelvin for calculations involving gases or thermodynamic laws.
2. Thermal Expansion
Definition: Increase in size of a substance due to increase in temperature.
Solids:
- Linear Expansion: \( \Delta L = L_0 \alpha \Delta T \)
- Area Expansion: \( \Delta A = A_0 \beta \Delta T \), where \( \beta \approx 2\alpha \)
- Volume Expansion: \( \Delta V = V_0 \gamma \Delta T \), where \( \gamma \approx 3\alpha \)
- \( \alpha \): Coefficient of linear expansion, \( \beta \): Area, \( \gamma \): Volume.
Liquids: Only volume expansion,
Gases: Significant volume expansion, governed by gas laws.
Anomalous Expansion of Water: Water contracts from 0°C to 4°C, expands above 4°C; max density at 4°C.
- Exam Tip: Use for bimetallic strips, liquid thermometers; note water’s anomaly for biological applications.
3. Specific Heat Capacity
Definition: Heat required to raise the temperature of unit mass by 1°C.
- \( c \): Specific heat capacity, Unit: J/(kg·K).
- \( C_p \): Specific heat at constant pressure (gases).
- \( C_v \): Specific heat at constant volume (gases).
- Relation: \( C_p - C_v = R \)(R: gas constant).
- Exam Tip: Use in calorimetry to calculate heat transfer.
4. Calorimetry
Principle: Heat lost by hot body = Heat gained by cold body (no phase change).
- Assumes no heat loss to surroundings.
- Exam Tip: Solve for final equilibrium temperature in mixing problems.
5. Change of State - Latent Heat Capacity
Definition: Heat required to change the phase of unit mass without temperature change.
- \( L \): Latent heat (fusion or vaporization), Unit: J/kg.
- Latent Heat of Fusion: Solid to liquid (e.g., ice to water).
- Latent Heat of Vaporization: Liquid to gas (e.g., water to steam).
- Exam Tip: Include latent heat in calculations when phase changes occur.
6. Heat Transfer - Conduction
Definition: Transfer of heat through a material without movement of the material.
- \( k \): Thermal conductivity, \( A \): Area, \( \Delta T \): Temperature difference, \( d \): Thickness, \( t \): Time.
- Unit of \( k \): W/(m·K).
- Exam Tip: Use for heat flow through rods or slabs; high \( k \) for conductors (metals).
7. Heat Transfer - Convection
Definition: Heat transfer by movement of fluid particles due to density differences.
- Examples: Boiling water, sea breezes.
- Exam Tip: Qualitative understanding; focus on natural vs. forced convection.
8. Heat Transfer - Radiation
Definition: Heat transfer via electromagnetic waves, no medium required.
- Examples: Heat from Sun, infrared from heaters.
- Exam Tip: All bodies emit and absorb radiation; depends on temperature and surface.
9. Thermal Conductivity
Definition: Ability of a material to conduct heat.
- High \( k \): Metals (e.g., copper); Low \( k \): Insulators (e.g., wood).
- Exam Tip: Compare materials for heat transfer efficiency in conduction problems.
10. Blackbody Radiation (Qualitative Idea)
Definition: Ideal body that absorbs all incident radiation and emits maximum radiation at a given temperature.
- Emission depends on temperature; hotter objects emit more energy.
- Exam Tip: Understand concept; relate to real objects like stars or furnaces.
11. Wien’s Displacement Law
Definition: Wavelength of maximum intensity of blackbody radiation is inversely proportional to temperature.
- \( b \): Wien’s constant (\( 2.898 \times 10^{-3} \, \text{m·K} \)).
- Exam Tip: Use to find peak wavelength of stars or hot objects.
12. Stefan’s Law
Definition: Total power radiated by a blackbody is proportional to the fourth power of its temperature.
- \( \sigma \): Stefan-Boltzmann constant (\( 5.67 \times 10^{-8} \, \text{W}/(\text{m}^2 \cdot \text{K}^4) \)).
- For non-blackbody: \( P = e \sigma A T^4 \), where \( e \): Emissivity (0 to 1).
- Exam Tip: Use for calculating radiated power; adjust for emissivity in real objects.
Summary / Quick Revision Box
- Heat: Energy transfer; Temperature: \( T_K = T_C + 273.15 \).
- Thermal Expansion: Solids: \( \Delta L = L_0 \alpha \Delta T \), Liquids/Gases:\( \Delta V = V_0 \gamma \Delta T \).
- Specific Heat: \( Q = m c \Delta T \), \( C_p - C_v = R \).
- Calorimetry: \( m_1 c_1 \Delta T_1 = m_2 c_2 \Delta T_2 \).
- Latent Heat: \( Q = m L \).
- Conduction: \( Q = \frac{k A \Delta T t}{d} \).
- Convection: Fluid movement; qualitative.
- Radiation: Via EM waves; no medium needed.
- Wien’s Law: \( \lambda_{\text{max}} T = b \).
- Stefan’s Law: \( P = \sigma A T^4 \).
Chapter 11: Thermodynamics
1. Thermal Equilibrium and Definition of Temperature
Thermal Equilibrium: State where two systems in contact have no net heat flow, as their temperatures are equal.
Temperature: Measure of average kinetic energy of particles, indicating hotness or coldness.
- Unit: Kelvin (K), \( T_K = T_C + 273.15 \).
- Exam Tip: Use Kelvin for thermodynamic calculations; thermal equilibrium is key for temperature measurement.
2. Zeroth Law of Thermodynamics
Statement: If two systems are in thermal equilibrium with a third system, they are in thermal equilibrium with each other.
- Establishes temperature as a measurable property.
- Exam Tip: Basis for thermometers; ensures consistent temperature scales.
3. Heat, Work, and Internal Energy
Heat (Q): Energy transferred due to temperature difference.
- Unit: Joule (J).
Work (W): Energy transfer due to mechanical interaction (e.g., gas expansion).
Internal Energy (U): Total energy (kinetic + potential) of particles in a system.
- Depends on temperature, pressure, volume (state variables).
- Exam Tip: Distinguish between heat (process) and internal energy (state); use \( W \) for gas expansion/compression.
4. First Law of Thermodynamics
Statement: Change in internal energy of a system equals heat added minus work done by the system.
- \( Q \): Heat added to system, \( W \): Work done by system.
- Sign convention: \( Q \) positive if added, \( W \) positive if done by system.
- Exam Tip: Apply to calculate \( \Delta U \), \( Q \), or \( W \) in processes like expansion or heating.
5. Second Law of Thermodynamics
Statement: Heat cannot flow spontaneously from a colder to a hotter body, or, total entropy of an isolated system always increases.
- Kelvin-Planck: No engine can convert all heat into work (no 100% efficient heat engine).
- Clausius: No process can transfer heat from cold to hot without work.
- Exam Tip: Focus on irreversibility and entropy increase; relates to efficiency of engines.
6. Thermodynamic State Variables and Equation of State
State Variables: Properties defining system’s state (e.g., pressure \( P \), volume \( V \), temperature \( T \), internal energy \( U \)).
Equation of State: Relates state variables for a system.
- \( n \): Moles, \( R \): Gas constant (\( 8.314 \, \text{J}/(\text{mol·K}) \)).
- Exam Tip: Use to find unknown state variables; valid for ideal gases.
7. Thermodynamic Processes
Isothermal Process: Constant temperature (\( \Delta T = 0 \)).
- \( PV = \text{constant} \)
- \( \Delta U = 0 \), \( Q = W \)
- Work: \( W = nRT \ln\left(\frac{V_f}{V_i}\right) \)
Adiabatic Process: No heat transfer (\( Q = 0 \)).
- \( PV^\gamma = \text{constant} \), where \( \gamma = \frac{C_p}{C_v} \)
- \( \Delta U = -W \)
- Work: \( W = \frac{P_i V_i - P_f V_f}{\gamma - 1} \)
Reversible Process: Can be reversed without changing system or surroundings (idealized).
Irreversible Process: Cannot be reversed (e.g., friction, mixing).
Cyclic Process: System returns to initial state (\( \Delta U = 0 \)).
- Examples: Carnot cycle, heat engines.
- Exam Tip: Identify process type; use specific formulas for work and \( \Delta U \).
Summary / Quick Revision Box
- Thermal Equilibrium: No net heat flow; basis for temperature.
- Zeroth Law: Defines temperature consistency.
- Heat/Work: \( W = P \Delta V \), Internal energy: State function.
- First Law: \( \Delta U = Q - W \).
- Second Law: Entropy increases; no 100% efficient engine.
- Equation of State: \( PV = nRT \).
- Isothermal: \( PV = \text{constant} \),\( W = nRT \ln\left(\frac{V_f}{V_i}\right) \).
- Adiabatic: \( PV^\gamma = \text{constant} \),\( \Delta U = -W \).
- Cyclic: \( \Delta U = 0 \), \( Q_{\text{net}} = W_{\text{net}} \).
Chapter 12: Kinetic Theory
1. Equation of State of a Perfect Gas
Definition: Relation between pressure, volume, and temperature for an ideal gas.
- \( P \): Pressure, \( V \): Volume, \( n \): Number of moles, \( R \): Gas constant (\( 8.314 \, \text{J}/(\text{mol·K}) \)), \( T \): Temperature (K).
- Alternate Form: \( PV = NkT \), where \( N \): Number of molecules, \( k \): Boltzmann constant (\( 1.38 \times 10^{-23} \, \text{J/K} \)).
- Exam Tip: Use to find unknown state variables; ensure \( T \) in Kelvin.
2. Work Done in Compressing a Gas
Definition: Work done on/by a gas during volume change at constant pressure.
- \( \Delta V = V_f - V_i \); negative for compression (\( \Delta V < 0 \)), positive for expansion.
- For varying pressure: \( W = -\int_{V_i}^{V_f} P \, dV \).
- Exam Tip: Negative work for compression; use graph area under \( P-V \) curve for non-constant pressure.
3. Kinetic Theory of Gases - Assumptions
Assumptions:
- Molecules are point masses with no volume.
- Molecules move randomly, obey Newton’s laws.
- Collisions are elastic and instantaneous.
- No intermolecular forces except during collisions.
- Molecules are in constant random motion.
- Exam Tip: Understand assumptions to justify ideal gas behavior.
4. Concept of Pressure
Definition: Pressure is force per unit area due to molecular collisions with container walls.
- \( m \): Mass of a molecule, \( N \): Number of molecules, \( V \): Volume, \( \langle v^2 \rangle \): Mean square speed.
- Alternate Form: \( P = \frac{1}{3} \rho \langle v^2 \rangle \), where \( \rho = \frac{m N}{V} \).
- Exam Tip: Relate pressure to molecular speed and density for derivations.
5. Kinetic Interpretation of Temperature
Concept: Temperature is proportional to average kinetic energy of gas molecules.
- \( \langle v^2 \rangle \): Mean square speed, \( k \): Boltzmann constant, \( T \): Temperature (K).
- Exam Tip: Use to link temperature to molecular motion; higher \( T \), faster molecules.
6. RMS Speed of Gas Molecules
Definition: Root mean square speed, measure of molecular speed.
- \( M \): Molar mass (\( M = m N_A \)), \( N_A \): Avogadro’s number.
- Exam Tip: Lighter gases (low \( M \)) have higher \( v_{\text{rms}} \); use for speed comparisons.
7. Degrees of Freedom
Definition: Number of independent ways a molecule can store energy (translational, rotational, vibrational).
- Monatomic gas: 3 (translational).
- Diatomic gas: 5 (3 translational, 2 rotational at room temperature).
- Exam Tip: Use to calculate specific heat capacities; more degrees, higher energy storage.
8. Law of Equi-partition of Energy
Statement: Each degree of freedom contributes \( \frac{1}{2} k T \) to the average energy of a molecule.
- Total energy per molecule: \( U = \frac{f}{2} k T \), where \( f \): Degrees of freedom.
- Application to Specific Heat:
- Monatomic: \( f = 3 \), \( C_v = \frac{3}{2} R \),\( C_p = \frac{5}{2} R \).
- Diatomic: \( f = 5 \), \( C_v = \frac{5}{2} R \),\( C_p = \frac{7}{2} R \).
- Exam Tip: Use to derive \( C_v \), \( C_p \), and \( \gamma = \frac{C_p}{C_v} \).
9. Concept of Mean Free Path
Definition: Average distance a molecule travels between collisions.
- \( d \): Molecular diameter, \( \frac{N}{V} \): Number density.
- Exam Tip: Smaller \( \lambda \) in dense gases; affects diffusion and viscosity.
10. Avogadro’s Number
Definition: Number of molecules in one mole of a substance.
- Relates microscopic (molecules) to macroscopic (moles): \( N = n N_A \).
- Exam Tip: Use in calculations involving number of molecules or gas constant (\( R = N_A k \)).
Summary / Quick Revision Box
- Equation of State: \( PV = nRT \)or\( PV = NkT \).
- Work: \( W = -P \Delta V \).
- Pressure: \( P = \frac{1}{3} \frac{m N}{V} \langle v^2 \rangle \).
- Temperature: \( \frac{1}{2} m \langle v^2 \rangle = \frac{3}{2} k T \).
- RMS Speed: \( v_{\text{rms}} = \sqrt{\frac{3 R T}{M}} \).
- Degrees of Freedom: Monatomic (3), Diatomic (5).
- Equi-partition: Each degree contributes \( \frac{1}{2} k T \).
- Specific Heat: Monatomic: \( C_v = \frac{3}{2} R \), Diatomic:\( C_v = \frac{5}{2} R \).
- Mean Free Path: \( \lambda = \frac{1}{\sqrt{2} \pi d^2 \frac{N}{V}} \).
- Avogadro’s Number: \( N_A = 6.022 \times 10^{23} \).
Chapter 14: Waves
1. Wave Motion
Definition: Transfer of energy through a medium or space without transfer of matter.
Transverse Waves: Particle displacement is perpendicular to wave propagation (e.g., waves on a string, light).
Longitudinal Waves: Particle displacement is parallel to wave propagation (e.g., sound waves).
- Characteristics: Wavelength (\( \lambda \)), frequency (\( f \)), amplitude (\( A \)), speed (\( v \)).
- Exam Tip: Identify wave type by particle motion direction relative to wave travel.
2. Speed of a Travelling Wave
Relation:
Speed on a String:
- \( T \): Tension, \( \mu \): Mass per unit length.
Speed of Sound (Longitudinal):
- \( B \): Bulk modulus, \( \rho \): Density.
- For gases: \( v = \sqrt{\frac{\gamma P}{\rho}} \), where \( \gamma \): Adiabatic index, \( P \): Pressure.
- Exam Tip: Use appropriate formula for medium (string or fluid); speed depends on medium properties.
3. Displacement Relation for a Progressive Wave
Definition: Equation describing displacement of particles in a wave.
- \( A \): Amplitude, \( k = \frac{2\pi}{\lambda} \): Wave number, \( \omega = 2\pi f \): Angular frequency, \( \phi \): Phase constant.
- Travelling left: \( y = A \sin(kx + \omega t + \phi) \).
- Velocity: \( v_y = \frac{\partial y}{\partial t} = -A \omega \cos(kx - \omega t + \phi) \).
- Exam Tip: Use to find displacement, velocity, or phase at specific \( x \) and \( t \).
4. Principle of Superposition of Waves
Principle: Net displacement is the vector sum of displacements of individual waves.
- Leads to interference (constructive/destructive) and standing waves.
- Exam Tip: Apply to calculate resultant amplitude in overlapping waves.
5. Reflection of Waves
Definition: Wave bounces back after hitting a boundary.
- Fixed End: Phase change of \( \pi \), inverted wave.
- Free End: No phase change, same orientation.
- Exam Tip: Note phase change for standing wave formation.
6. Standing Waves in Strings
Definition: Waves formed by superposition of incident and reflected waves, creating nodes and antinodes.
Boundary Condition: Nodes at fixed ends (\( x = 0, L \)).
Fundamental Mode (1st Harmonic):
Higher Harmonics:
- \( n \): Harmonic number (1, 2, 3, …).
- Exam Tip: Calculate frequency or wavelength for strings fixed at both ends.
7. Standing Waves in Organ Pipes
Closed Organ Pipe (One End Closed):
- Node at closed end, antinode at open end.
- Fundamental Mode: \( \lambda_1 = 4L \), \( f_1 = \frac{v}{4L} \).
- Harmonics: \( f_n = n \frac{v}{4L} \), \( n = 1, 3, 5, \ldots \) (odd harmonics only).
Open Organ Pipe (Both Ends Open):
- Antinodes at both ends.
- Fundamental Mode: \( \lambda_1 = 2L \), \( f_1 = \frac{v}{2L} \).
- Harmonics: \( f_n = n \frac{v}{2L} \), \( n = 1, 2, 3, \ldots \).
- Exam Tip: Distinguish between open and closed pipes; use sound speed for frequencies.
8. Beats
Definition: Interference of two waves with slightly different frequencies, causing amplitude variation.
Beat Frequency:
- Application: Tuning instruments (e.g., tuning forks).
- Exam Tip: Calculate beat frequency from frequency difference; relate to sound intensity variation.
No comments:
Post a Comment