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CBSE · Class 11 · Physics

Physics Formula Sheet

110 formulas across 14 chapters — with variables explained and exam tips where needed.

Ch 2Units and Measurements(8 formulas)

Dimensional formula of velocity

[v] = [M⁰LT⁻¹]

Dimensional formula of force

[F] = [MLT⁻²]

Dimensional formula of energy

[E] = [ML²T⁻²]

Dimensional formula of pressure

[P] = [ML⁻¹T⁻²]

Significant figures: addition/subtraction

Result has fewest decimal places of any operand

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For multiplication/division, result has fewest significant figures

Absolute error

Δa = |a_mean − aᵢ|

Relative error

Relative error = Δa / a_mean

Percentage error

% error = (Δa / a_mean) × 100

Ch 3Motion in a Straight Line(7 formulas)

First equation of motion

v = u + at

u = initial velocity, v = final velocity, a = acceleration, t = time

Second equation of motion

s = ut + ½at²

s = displacement

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Use this when time is given and displacement is asked

Third equation of motion

v² = u² + 2as

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Use this when time is not given

Average velocity

v_avg = (u + v)/2 (only for uniform acceleration)

Displacement in nth second

sₙ = u + a(2n − 1)/2

Relative velocity

v_AB = v_A − v_B

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If moving in same direction: subtract; opposite direction: add

Free fall acceleration

a = g = 9.8 m/s² (downward)

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Take downward as positive; then u = 0 for a body dropped from rest

Ch 4Motion in a Plane(8 formulas)

Projectile: Range

R = u²sin2θ / g

u = initial speed, θ = angle of projection, g = 9.8 m/s²

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Maximum range occurs at θ = 45°

Projectile: Maximum height

H_max = u²sin²θ / 2g

Projectile: Time of flight

T = 2u sinθ / g

Projectile: Horizontal velocity

v_x = u cosθ (constant throughout)

Projectile: Vertical velocity

v_y = u sinθ − gt

Centripetal acceleration

aₓ = v²/r = ω²r

v = speed, r = radius, ω = angular velocity

Centripetal force

F = mv²/r = mω²r

Relation: linear and angular velocity

v = ωr

Ch 5Laws of Motion(7 formulas)

Newton's Second Law

N

F = ma

F = net force (N), m = mass (kg), a = acceleration (m/s²)

Impulse

N·s or kg·m/s

J = FΔt = Δp = m(v − u)

Static friction (max)

f_s = μₛN

μₛ = coefficient of static friction, N = normal force

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Static friction ≤ μₛN; it equals applied force until this limit

Kinetic friction

f_k = μₖN

μₖ = coefficient of kinetic friction

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μₖ < μₛ always — kinetic friction is less than maximum static friction

Pseudo force (non-inertial frame)

F_pseudo = −ma_frame

a_frame = acceleration of non-inertial frame

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Directed opposite to the frame's acceleration

Normal force on inclined plane

N = mg cosθ

Acceleration on frictionless incline

a = g sinθ

Ch 6Work, Energy and Power(8 formulas)

Work done by constant force

J

W = Fs cosθ

F = force, s = displacement, θ = angle between F and s

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W = 0 if F ⊥ s (e.g. centripetal force does no work)

Kinetic energy

J

KE = ½mv²

Gravitational potential energy

J

PE = mgh

Work-energy theorem

W_net = ΔKE = KE_final − KE_initial

Conservation of mechanical energy

KE + PE = constant (no friction)

Power

W (Watt)

P = W/t = Fv cosθ

Spring potential energy

PE = ½kx²

k = spring constant, x = compression/extension

Elastic collision: kinetic energy

KE conserved | v₁' = (m₁−m₂)u₁/(m₁+m₂) | v₂' = 2m₁u₁/(m₁+m₂)

Ch 7System of Particles and Rotational Motion(11 formulas)

Torque

N·m

τ = r × F = rF sinθ

Angular momentum

kg·m²/s

L = Iω = mvr sinθ

Newton's second law (rotation)

τ = Iα

I = moment of inertia, α = angular acceleration

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Rotational analogue of F = ma

Moment of inertia: thin rod (centre)

I = ML²/12

Moment of inertia: thin rod (end)

I = ML²/3

Moment of inertia: disc (centre)

I = MR²/2

Moment of inertia: ring (centre)

I = MR²

Moment of inertia: solid sphere

I = 2MR²/5

Parallel axis theorem

I = I_cm + Md²

d = distance from CM to new axis

Rolling body KE

KE_total = ½mv² + ½Iω² = ½mv²(1 + I/mR²)

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For a sphere: KE = 7/10 mv²; for a cylinder: KE = 3/4 mv²

Conservation of angular momentum

L = Iω = constant (when τ_net = 0)

Ch 8Gravitation(8 formulas)

Newton's law of gravitation

N

F = Gm₁m₂/r²

G = 6.674×10⁻¹¹ N·m²/kg²

Acceleration due to gravity at surface

g = GM/R²

M = mass of Earth, R = radius of Earth

Variation of g with height h

g_h = g(1 − 2h/R) for h << R

Variation of g with depth d

g_d = g(1 − d/R)

Orbital velocity

v₀ = √(GM/r)

r = orbital radius

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At surface r = R, so v₀ = √(gR)

Escape velocity

v_e = √(2GM/R) = √(2gR)

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Escape velocity = √2 × orbital velocity at surface

Kepler's third law

T² ∝ r³ or T² = (4π²/GM) r³

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More massive central body → faster orbital period

Gravitational potential energy

U = −GMm/r

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Negative value: bound system; approaches 0 as r → ∞

Ch 9Mechanical Properties of Solids(7 formulas)

Stress

N/m² or Pa

Stress = F/A

F = applied force, A = cross-sectional area

Strain

Strain = ΔL/L (longitudinal) or Δx/L (shear)

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Strain is dimensionless

Young's modulus

Pa

Y = (F/A) / (ΔL/L) = Stress / Longitudinal strain

Bulk modulus

Pa

B = −ΔP / (ΔV/V)

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Negative sign: pressure increase → volume decrease

Modulus of rigidity

η = Shear stress / Shear strain

Hooke's Law

Stress ∝ Strain (within elastic limit)

Elastic potential energy per unit volume

u = ½ × stress × strain = ½ Y (strain)²

Ch 10Mechanical Properties of Fluids(8 formulas)

Pressure at depth h

Pa

P = P₀ + ρgh

P₀ = atmospheric pressure, ρ = fluid density

Pascal's law

Pressure applied to enclosed fluid is transmitted equally in all directions

Bernoulli's equation

P + ½ρv² + ρgh = constant

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Energy conservation for ideal fluid flow — fast flow → low pressure

Continuity equation

A₁v₁ = A₂v₂

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Narrower pipe → faster flow

Stokes' law (viscous drag)

F = 6πηrv

η = coefficient of viscosity, r = radius of sphere, v = velocity

Terminal velocity

v_t = 2r²(ρ − σ)g / 9η

σ = density of fluid

Surface tension

N/m

T = F/L

Excess pressure inside bubble (soap)

ΔP = 4T/r

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Soap bubble has two surfaces; liquid drop has one surface so ΔP = 2T/r

Ch 11Thermal Properties of Matter(7 formulas)

Linear thermal expansion

ΔL = αLΔT

α = coefficient of linear expansion, L = original length, ΔT = temperature change

Volumetric thermal expansion

ΔV = γVΔT

γ = 3α for isotropic solids

Heat absorbed / released

J

Q = mcΔT

m = mass, c = specific heat capacity, ΔT = temperature change

Latent heat

J

Q = mL

L = specific latent heat

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Temperature stays constant during phase change

Stefan-Boltzmann law

W

P = εσAT⁴

σ = 5.67×10⁻⁸ W/m²·K⁴, ε = emissivity, A = area, T = temperature in K

Wien's displacement law

λ_max T = 2.898×10⁻³ m·K

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Hotter body emits at shorter (bluer) wavelengths

Newton's law of cooling

dT/dt = −k(T − T₀)

T₀ = ambient temperature, k = cooling constant

Ch 12Thermodynamics(7 formulas)

First law of thermodynamics

ΔU = Q − W

ΔU = change in internal energy, Q = heat added to system, W = work done by system

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Sign convention: Q +ve when added to system; W +ve when done BY system

Work done by gas (isobaric)

W = PΔV = P(V₂ − V₁)

Efficiency of Carnot engine

η = 1 − T₂/T₁

T₁ = source temperature (K), T₂ = sink temperature (K)

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Always use temperatures in Kelvin

COP of refrigerator

COP = T₂ / (T₁ − T₂) = Q₂/W

Q₂ = heat extracted from cold reservoir

Entropy change

J/K

ΔS = Q/T (reversible process)

Relation for Cp and Cv

Cp − Cv = R

R = 8.314 J/mol·K

Adiabatic process

PVᵞ = constant | TV^(γ−1) = constant

γ = Cp/Cv

Ch 13Kinetic Theory of Gases(8 formulas)

Ideal gas law

PV = nRT

n = moles, R = 8.314 J/mol·K, T = temperature in K

Kinetic energy per molecule

KE = 3/2 kT

k = 1.38×10⁻²³ J/K (Boltzmann constant)

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Average KE depends only on temperature, not mass

RMS speed

v_rms = √(3RT/M) = √(3kT/m)

M = molar mass, m = mass of one molecule

Average speed

v_avg = √(8RT/πM)

Most probable speed

v_mp = √(2RT/M)

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Speeds order: v_mp < v_avg < v_rms

Degrees of freedom: monatomic gas

f = 3 | U = 3/2 nRT

Degrees of freedom: diatomic gas

f = 5 | U = 5/2 nRT

Mean free path

λ = 1/(√2 πd²n)

d = diameter of molecule, n = number density

Ch 14Oscillations(8 formulas)

Displacement in SHM

x = A sin(ωt + φ)

A = amplitude, ω = angular frequency, φ = initial phase

Angular frequency of spring-mass

ω = √(k/m) → T = 2π√(m/k)

k = spring constant, m = mass

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T depends on mass and spring constant, not amplitude

Time period of simple pendulum

T = 2π√(l/g)

l = effective length

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T independent of mass and amplitude (for small oscillations)

Velocity in SHM

v = ω√(A² − x²)

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Maximum velocity v_max = ωA at x = 0

Acceleration in SHM

a = −ω²x

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Acceleration is always directed towards mean position

Total energy in SHM

E = ½kA² = ½mω²A²

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Total energy is constant; independent of position

Kinetic energy in SHM

KE = ½mω²(A² − x²)

Potential energy in SHM

PE = ½mω²x²

Ch 15Waves(8 formulas)

Wave speed

m/s

v = fλ

f = frequency (Hz), λ = wavelength (m)

Wave speed on string

v = √(T/μ)

T = tension, μ = linear mass density (kg/m)

Wave speed in gas

v = √(γP/ρ)

γ = ratio of specific heats, P = pressure, ρ = density

Speed of sound in air

v ≈ 331 + 0.6T m/s

T = temperature in °C

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Speed increases with temperature

Standing waves: nodes and antinodes

λ = 2L/n for both ends fixed | λ = 4L/(2n−1) for one end open

Fundamental frequency (string)

f₁ = v/2L = (1/2L)√(T/μ)

Doppler effect (source moving towards observer)

f' = f(v + v₀) / (v − v_s)

v₀ = observer speed, v_s = source speed

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Use +v₀ if observer moves towards source, −v₀ if away

Beats

Beat frequency = |f₁ − f₂|

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Beats are heard when two close frequencies are superimposed

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