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.
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).
$$\boxed{\text{Strain} = \frac{\text{Change in dimension}}{\text{Original dimension}}}$$| Type | Stress | Strain |
|---|---|---|
| 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: $\boxed{F = kx}$
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 $[ML^{-1}T^{-2}]$.
| Modulus | Formula | Applies 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)
$$\boxed{Y = 2\eta(1+\sigma)} \qquad \boxed{Y = 3K(1-2\sigma)}$$$$\boxed{K = \frac{Y}{3(1-2\sigma)}} \qquad \boxed{\eta = \frac{Y}{2(1+\sigma)}}$$$$\boxed{K = \frac{\eta(2+2\sigma)}{3(1-2\sigma)}} \qquad \boxed{Y = \frac{9K\eta}{3K+\eta}}$$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):
$$\boxed{W_{\text{apparent}} = W_{\text{actual}} - F_B = Vg(\rho_{\text{body}} - \rho_{\text{fluid}})}$$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
| Application | Formula | Condition |
|---|---|---|
| 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 $A$ |
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):
$$\boxed{Q = \frac{\pi r^4 (P_1 - P_2)}{8\eta L}}$$$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
| Geometry | Excess pressure | Surfaces |
|---|---|---|
| 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) |
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, $\theta \approx 135°$–$140°$).
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
| Quantity | Formula | Notes |
|---|---|---|
| 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 = $ const | incompressible |
| Bernoulli | $P + \tfrac12\rho v^2 + \rho gh = $ const | ideal, 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 |