Thermal Properties of Matter
Class 11 · Thermal Properties of Matter

Radiation (Stefan–Boltzmann)

P = εσAT⁴ — blackbody vs polished surface.

Key Notes

01

Radiation: heat transfer by ELECTROMAGNETIC WAVES (mostly infrared at terrestrial T). Doesn't need a medium.

02

Stefan-Boltzmann law: power radiated per unit area P/A = εσT⁴, with σ = 5.67×10⁻⁸ W/m²·K⁴ and ε = emissivity (0 ≤ ε ≤ 1).

03

Black body: ε = 1, perfect absorber and emitter. Sun is approximately a black body at ~5800 K.

04

Net radiative exchange: P_net = εσA(T_body⁴ − T_surroundings⁴).

05

Wien's law: λ_max·T = 2.898 × 10⁻³ m·K. Peak wavelength of emitted radiation.

06

Sun's peak: λ_max ≈ 500 nm (visible). Human body (310 K): peak ~ 9.4 μm (infrared).

07

Radiation is how Earth gets energy from Sun (no medium between). Also how Earth loses heat to space.

08

Greenhouse effect: atmosphere absorbs outgoing IR, traps heat ⇒ Earth's surface stays warmer.

Formulas

Stefan-Boltzmann law

Power radiated by surface area A at temperature T.

Net exchange

Body at T_b in surroundings at T_s.

Wien's displacement law

Peak wavelength shifts inversely with T.

Solar constant

Solar power per m² at Earth's orbit, before atmosphere.

Important Points

Radiation does NOT need a medium — works through vacuum (unlike conduction & convection).

Power radiated ∝ T⁴ — doubles for only ~19% T increase. Hot objects radiate vastly more.

Wien's law: hotter ⇒ shorter peak wavelength (blue/UV); cooler ⇒ infrared.

Emissivity ε depends on surface: black 1, polished metal 0.05.

Earth would be ~33°C colder without greenhouse effect — water vapor and CO₂ trap IR.

All bodies at T > 0 K emit radiation continuously. We see colors because surfaces absorb/emit selectively.

Radiation (Stefan–Boltzmann) notes from sciphylab (also known as SciPhy, SciPhy Lab, SciPhy Labs, Physics Lab). Class 11 physics revision for JEE Mains, JEE Advanced, NEET UG, AP Physics 1/2/C, SAT, and CUET-UG.