Physics Properties of Solids and Liquids

Properties of Solids and Liquids Formula Sheet

All key Physics formulas for Properties of Solids & Liquids — elasticity, fluid pressure, Bernoulli, viscosity, surface tension. JEE Main & Advanced quick revision.

7 min read Updated Jun 2026 #formula sheet#quick revision#jee-main

Every must-know formula, constant, and result for elasticity and fluid mechanics — compiled for last-minute JEE revision. Each section maps to a full topic page; follow the links if a result needs derivation.

Elasticity: Stress and Strain

Stress — internal restoring force per unit area; same dimensions as pressure, $[ML^{-1}T^{-2}]$, unit Pa.

$$\boxed{\text{Stress} = \frac{F}{A}}$$

Strain — relative deformation; dimensionless (a pure ratio).

$$\boxed{\text{Strain} = \frac{\text{Change in dimension}}{\text{Original dimension}}}$$
TypeStressStrain
Tensile / Compressive$F/A$ (longitudinal)$\dfrac{\Delta L}{L}$
Shearing (tangential)$F_{\text{tangential}}/A$$\theta = \dfrac{\Delta x}{L}$
Hydraulic (bulk)$-\Delta P$$\dfrac{\Delta V}{V}$

Hooke’s Law (within elastic limit):

$$\boxed{\text{Stress} = E \times \text{Strain}}$$

For a spring: $\boxed{F = kx}$

High-yield reminders

Strain is dimensionless — never give it units.

Hooke’s law holds only within the elastic limit, for small deformations, at constant temperature, in isotropic materials.

Hydraulic stress carries a negative sign ($-\Delta P$): increasing pressure compresses the body.

Elastic Potential Energy

$$\boxed{U = \tfrac{1}{2}kx^2}$$

For a stretched wire / rod:

$$\boxed{U = \tfrac{1}{2}\,\text{Stress}\times\text{Strain}\times\text{Volume} = \tfrac{1}{2}F\,\Delta L}$$

Energy density (per unit volume):

$$\boxed{u = \frac{U}{V} = \tfrac{1}{2}\,\text{Stress}\times\text{Strain}}$$

Full page: Stress and Strain

Elastic Moduli

$$\boxed{\text{Elastic Modulus} = \frac{\text{Stress}}{\text{Strain}}}$$

Common unit: Pa; dimensions $[ML^{-1}T^{-2}]$.

ModulusFormulaApplies to
Young’s $Y$$\dfrac{F/A}{\Delta L/L} = \dfrac{FL}{A\,\Delta L}$Solids
Bulk $K$$\dfrac{-\Delta P}{\Delta V/V} = -V\dfrac{\Delta P}{\Delta V}$Solids, liquids, gases
Shear (rigidity) $\eta$$\dfrac{F/A}{\theta} = \dfrac{F/A}{\Delta x/L}$Solids only
Poisson’s ratio $\sigma$$-\dfrac{\Delta d/d}{\Delta L/L}$Solids (dimensionless)
Compressibility $\kappa$$\dfrac{1}{K}$All materials

For a wire, $\Delta L = \dfrac{FL}{AY}$, so it behaves like a spring with $k = \dfrac{YA}{L}$.

Bulk modulus of an ideal gas:

$$\boxed{K_{\text{isothermal}} = P} \qquad \boxed{K_{\text{adiabatic}} = \gamma P}$$

where $\gamma = C_p/C_v$ (air: $\gamma \approx 1.4$).

Poisson’s ratio range: $0 < \sigma < 0.5$ (cork $\approx 0$, rubber $\approx 0.5$, most metals $\approx 0.2$–$0.4$).

Relations Between Elastic Constants (isotropic materials)

$$\boxed{Y = 2\eta(1+\sigma)} \qquad \boxed{Y = 3K(1-2\sigma)}$$$$\boxed{K = \frac{Y}{3(1-2\sigma)}} \qquad \boxed{\eta = \frac{Y}{2(1+\sigma)}}$$$$\boxed{K = \frac{\eta(2+2\sigma)}{3(1-2\sigma)}} \qquad \boxed{Y = \frac{9K\eta}{3K+\eta}}$$
High-yield reminders

Liquids and gases have no shear modulus ($\eta = 0$) — that is why they flow.

A vertical wire stretched by its own weight extends $\Delta L = \dfrac{\rho g L^2}{2Y}$ — half the value for the same weight hung at the end.

Order of stiffness (Young’s modulus): Steel > Iron > Copper > Aluminium > Glass $\approx$ Wood > Rubber.

Reference values (Young’s modulus): Steel $2\times10^{11}$ Pa, Iron $1.9\times10^{11}$, Copper $1.2\times10^{11}$, Aluminium $0.7\times10^{11}$, Rubber $\approx 5\times10^6$ Pa.

Full page: Elastic Moduli

Fluid Pressure and Pascal’s Law

$$\boxed{P = \frac{F}{A}}$$

Pressure in a fluid at rest is a scalar — same in all directions at a point.

Hydrostatic pressure at depth $h$:

$$\boxed{P = P_0 + \rho g h}$$

Gauge pressure:

$$\boxed{P_{\text{gauge}} = P - P_0 = \rho g h}$$

Pascal’s Law — hydraulic lift:

$$\boxed{\frac{F_1}{A_1} = \frac{F_2}{A_2}} \qquad \frac{F_2}{F_1} = \frac{A_2}{A_1}$$

Work conserved: $F_1 d_1 = F_2 d_2$.

Barometer / manometer: $P_0 = \rho_{Hg}\, g\, h$; open-tube manometer gives $P_{\text{gas}} - P_0 = \rho g h$.

Archimedes’ Principle and Buoyancy

$$\boxed{F_B = \rho_{\text{fluid}}\, V_{\text{displaced}}\, g}$$

Floating condition ($\rho_{\text{body}} < \rho_{\text{fluid}}$):

$$\boxed{\frac{V_{\text{submerged}}}{V_{\text{total}}} = \frac{\rho_{\text{body}}}{\rho_{\text{fluid}}}}$$

Apparent weight (sinking body):

$$\boxed{W_{\text{apparent}} = W_{\text{actual}} - F_B = Vg(\rho_{\text{body}} - \rho_{\text{fluid}})}$$
High-yield reminders

Hydrostatic pressure depends only on depth $h$, not on container shape or amount of liquid (hydrostatic paradox).

Buoyant force equals the weight of fluid displaced, not the weight of the body. They are equal only for a floating body.

Remember: 76 cm Hg = 760 mm Hg = 1 atm $= 1.013\times10^5$ Pa $\approx 10^5$ Pa; $\rho_{Hg} = 13600$ kg/m³.

Full page: Fluid Pressure and Pascal’s Law

Fluid Dynamics: Continuity and Bernoulli

Equation of continuity (incompressible, streamline flow):

$$\boxed{A_1 v_1 = A_2 v_2 = \text{constant}}$$

Bernoulli’s theorem (ideal fluid — non-viscous, incompressible, steady, streamline flow):

$$\boxed{P + \tfrac{1}{2}\rho v^2 + \rho g h = \text{constant}}$$

Equivalently, dividing by $\rho g$ (head form):

$$\boxed{\frac{P}{\rho g} + \frac{v^2}{2g} + h = \text{constant}}$$

Key Applications

ApplicationFormulaCondition
Torricelli’s efflux$v = \sqrt{2gh}$Hole at depth $h$, large tank
Venturi meter$v_1 = A_2\sqrt{\dfrac{2(P_1-P_2)}{\rho(A_1^2 - A_2^2)}}$Horizontal pipe
Flow rate$Q = A_1 v_1 = Av$
Aerofoil lift$F_{\text{lift}} = \tfrac{1}{2}\rho(v_{\text{top}}^2 - v_{\text{bottom}}^2)A$Wing area $A$
$$\boxed{v = \sqrt{2gh}} \qquad \text{(Torricelli — same as free fall from height } h)$$
High-yield reminders

Bernoulli connects two points on the same streamline only.

In a constriction: area $\downarrow$ → velocity $\uparrow$ (continuity) → pressure $\downarrow$ (Bernoulli).

In Torricelli’s theorem both the surface and the jet exit are at atmospheric pressure $P_0$ — the $P_0$ terms cancel.

Full page: Bernoulli’s Theorem

Viscosity, Stokes’ Law and Flow Through Pipes

Newton’s law of viscosity:

$$\boxed{F = -\eta A \frac{dv}{dy}}$$

$\eta$ = coefficient of viscosity. Unit: Pa·s (CGS: poise; $1$ poise $= 0.1$ Pa·s, $1$ cP $= 10^{-3}$ Pa·s). Dimensions $[ML^{-1}T^{-1}]$. Water at 20 °C: $\eta \approx 10^{-3}$ Pa·s.

Reynolds number (dimensionless):

$$\boxed{Re = \frac{\rho v D}{\eta}}$$

Laminar: $Re < 1000$; turbulent: $Re > 2000$; transition: $1000 < Re < 2000$.

Stokes’ law (small sphere, low velocity, $Re < 1$):

$$\boxed{F = 6\pi \eta r v}$$

Terminal velocity:

$$\boxed{v_t = \frac{2r^2 g(\rho_{\text{sphere}} - \rho_{\text{fluid}})}{9\eta}}$$

When $\rho_{\text{sphere}} \gg \rho_{\text{fluid}}$: $v_t = \dfrac{2r^2 \rho g}{9\eta}$.

Time to reach $\sim$90 % of $v_t$: $t_{90\%} \approx \dfrac{m}{3\pi\eta r}$.

Poiseuille’s law (laminar flow through a cylindrical pipe):

$$\boxed{Q = \frac{\pi r^4 (P_1 - P_2)}{8\eta L}}$$
High-yield reminders

$v_t \propto r^2$: a drop 10× smaller falls 100× slower. Also $v_t \propto (\rho_{\text{sphere}}-\rho_{\text{fluid}})$, $\propto 1/\eta$, $\propto g$.

Poiseuille flow $Q \propto r^4$: halving the radius cuts flow to $1/16$.

Temperature: liquid viscosity decreases with $T$; gas viscosity increases with $T$.

If $n$ identical drops of radius $r$ coalesce, the big drop radius is $R = n^{1/3}r$; e.g. 8 drops → $R = 2r$ → $v_t$ becomes $4\times$.

Full page: Viscosity and Stokes’ Law

Surface Tension and Capillarity

Two equivalent definitions, same value and units ($\text{N/m} = \text{J/m}^2$), dimensions $[MT^{-2}]$:

$$\boxed{\gamma = \frac{F}{L}} \qquad \boxed{\gamma = \frac{W}{A}}$$

Work to create new surface (surface energy):

$$\boxed{W = \gamma\,\Delta A} \qquad U = \gamma A$$

Excess Pressure

GeometryExcess pressureSurfaces
Liquid drop$\dfrac{2\gamma}{r}$1
Air bubble in liquid$\dfrac{2\gamma}{r}$1
Soap bubble$\dfrac{4\gamma}{r}$2 (inner + outer)
$$\boxed{\Delta P_{\text{drop}} = \frac{2\gamma}{r}} \qquad \boxed{\Delta P_{\text{soap bubble}} = \frac{4\gamma}{r}}$$

Capillary Rise

$$\boxed{h = \frac{2\gamma\cos\theta}{\rho g r}}$$

For perfect wetting ($\theta = 0°$, $\cos\theta = 1$): $h = \dfrac{2\gamma}{\rho g r}$.

Obtuse $\theta$ (e.g. mercury in glass) gives $\cos\theta < 0$ → capillary depression.

Angle of contact: measured through the liquid. $\theta < 90°$ → wets, concave meniscus, adhesion > cohesion (water on glass). $\theta > 90°$ → doesn’t wet, convex meniscus, cohesion > adhesion (mercury on glass, $\theta \approx 135°$–$140°$).

High-yield reminders

Soap bubble has two surfaces → factor of 4, not 2. Energy to blow it = $\gamma \times 8\pi r^2$.

Capillary rise: $h \propto 1/r$, $h \propto \gamma$, $h \propto 1/\rho$. Valid only for narrow tubes.

Excess pressure $\propto 1/r$ — tiny drops/bubbles have huge internal pressure; when two bubbles join, air flows from smaller (higher $P$) to larger.

Reference: $\gamma_{\text{water}} \approx 0.073$ N/m, $\gamma_{\text{mercury}} \approx 0.465$ N/m (highest), soap $\approx 0.025$ N/m. Surface tension decreases with temperature (zero at critical temperature).

Full page: Surface Tension and Capillarity

Coalescing Drops and Bubbles (Quick Results)

graph LR
    A["n small drops/bubbles
radius r"] --> B{Combine} B --> C["Liquid drops:
volume conserved
R = n^(1/3) r"] B --> D["Soap bubbles, isothermal:
surface energy/area conserved
R² = r₁² + r₂² + ..."]
  • Liquid drops coalescing — volume is conserved: $R^3 = \sum r_i^3$ (e.g. $n=8 \Rightarrow R = 2r$).
  • Soap bubbles coalescing (isothermal) — surface energy is conserved: $R^2 = r_1^2 + r_2^2$.

One-Glance Master Table

QuantityFormulaNotes
Stress$\sigma = F/A$Pa, $[ML^{-1}T^{-2}]$
Strain$\varepsilon = \Delta L/L$dimensionless
Hooke’s law$\sigma = E\varepsilon$; $F = kx$within elastic limit
Elastic PE$U = \tfrac12 kx^2 = \tfrac12 F\Delta L$
Young’s modulus$Y = FL/(A\Delta L)$solids
Bulk modulus$K = -V\Delta P/\Delta V$all states; gas: $K_{\text{iso}}=P$, $K_{\text{adi}}=\gamma P$
Shear modulus$\eta = (F/A)/\theta$solids only
Poisson’s ratio$\sigma = -(\Delta d/d)/(\Delta L/L)$$0$–$0.5$
Modulus relation$Y = 9K\eta/(3K+\eta)$isotropic
Hydrostatic pressure$P = P_0 + \rho gh$depends only on $h$
Hydraulic lift$F_1/A_1 = F_2/A_2$$F_1 d_1 = F_2 d_2$
Buoyant force$F_B = \rho_{\text{fluid}} V_{\text{disp}}\, g$upward
Floating fraction$V_{\text{sub}}/V = \rho_{\text{body}}/\rho_{\text{fluid}}$$\rho_{\text{body}}<\rho_{\text{fluid}}$
Continuity$Av = $ constincompressible
Bernoulli$P + \tfrac12\rho v^2 + \rho gh = $ constideal, same streamline
Torricelli$v = \sqrt{2gh}$efflux
Venturi$v_1 = A_2\sqrt{2\Delta P/[\rho(A_1^2-A_2^2)]}$horizontal
Newton’s viscosity$F = -\eta A\, dv/dy$$\eta$ in Pa·s
Reynolds number$Re = \rho v D/\eta$$<1000$ laminar, $>2000$ turbulent
Stokes’ law$F = 6\pi\eta r v$small sphere, $Re<1$
Terminal velocity$v_t = 2r^2 g(\rho_s-\rho_f)/(9\eta)$$\propto r^2$
Poiseuille$Q = \pi r^4 \Delta P/(8\eta L)$$Q\propto r^4$
Surface tension$\gamma = F/L = W/A$N/m $=$ J/m²
Excess pressure (drop)$\Delta P = 2\gamma/r$one surface
Excess pressure (bubble)$\Delta P = 4\gamma/r$two surfaces
Capillary rise$h = 2\gamma\cos\theta/(\rho gr)$narrow tubes