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Equality of mixed derivatives of smooth equilibrium potentials gives (∂T/∂V)_S=−(∂p/∂S)_V, (∂T/∂p)_S=(∂V/∂S)_p, (∂S/∂V)_T=(∂p/∂T)_V and (∂S/∂p)_T=−(∂V/∂T)_p.
Mathematical statementPhysics · ChemistryHeat capacities, expansion and compressibilityFor a fixed amount of simple compressible matter, C_V=(∂U/∂T)_V and C_p=(∂H/∂T)_p.
ModelPhysicsHeat-engine efficiency and Carnot boundA cyclic heat engine drawing heat Q_h from a reservoir T_h and rejecting Q_c to T_c delivers W=Q_h−Q_c.
ModelPhysics · ChemistryThermal equilibrium and low-temperature entropy limitThermal equilibrium is transitive, permitting a common temperature scale.
ModelPhysicsMicrocanonical ensemble and state countingFor an isolated equilibrium system with fixed energy shell, volume and particle number, the microcanonical model gives equal probability to accessible microstates.
ModelPhysics · ChemistryThermodynamic observables from the partition functionFor canonical Z=Σ_i exp(−βE_i), F=−k_BT lnZ, U=−∂_β lnZ and S=k_B(lnZ+βU).
ModelPhysics · ChemistryGrand-canonical particle exchange and potentialFor a system exchanging energy and particles with reservoirs at T and μ, p_i,N=exp[−β(E_i,N−μN)]/Ξ and Ξ=Σ_N,i exp[−β(E_i,N−μN)].
ModelPhysics · ChemistryClassical equipartition and quantum freeze-outIn a classical canonical model, each independent quadratic term in an unrestricted coordinate or momentum contributes k_BT/2 to the mean energy.
ModelPhysicsMaxwell equilibrium velocity distributionFor a dilute classical ideal gas in its rest frame, the probability density of a particle velocity is (m/(2πk_BT))³ᐟ²exp[−m|v|²/(2k_BT)].
ModelPhysics · Chemistry · Earth & cosmosPhase coexistence and Clapeyron slopePure phases coexist at common T and p when their molar Gibbs energies are equal.
ModelPhysics · Earth & cosmosPlanck spectrum and electromagnetic mode countingThermal radiation in a vacuum cavity at temperature T has spectral energy density per angular frequency u_ω=ħω³/[π²c³(exp(ħω/(k_BT))−1)].
ModelPhysicsCoulomb field from static chargeIn vacuum electrostatics, a point charge q at r′ produces E(r)=q(r−r′)/(4πε₀|r−r′|³).
ModelPhysicsPoisson and Laplace electrostatic boundary problemsElectrostatic potential obeys ∇²φ=−ρ/ε₀ in vacuum; charge-free regions obey Laplace's equation.
ModelPhysicsGrounded-sphere image-charge solutionFor a charge q at r₀ outside a grounded conducting sphere of radius a centered at the origin, an image q′=−qa/|r₀| at r′=a²r₀/|r₀|² gives the exterior potential q/(4πε₀|r−r₀|)+q′/(4πε₀|r−r′|).
ModelPhysicsElectric dipole and multipole expansionOutside a localized charge distribution, the potential expands in powers of inverse distance.
ModelPhysicsMagnetostatic Biot–Savart fieldA localized steady current distribution in vacuum produces B(r)=μ₀/(4π)∫J(r′)×(r−r′)/|r−r′|³d³r′.
ModelPhysics · ChemistryPolarization, bound charge and electric displacementMacroscopic electric polarization P gives bound volume charge ρ_b=−∇·P and surface charge σ_b=P·n at a material boundary.
ModelPhysicsMagnetization, bound current and magnetic field strengthMagnetization M contributes bound volume current J_b=∇×M and surface current K_b=M×n.
ModelPhysicsElectromagnetic interface jump conditionsFor a stationary interface with unit normal n from medium 1 to 2, n·(D₂−D₁)=σ_free, n·(B₂−B₁)=0, n×(E₂−E₁)=0 and n×(H₂−H₁)=K_free.
ModelPhysicsPlane waves in dielectric matterIn a homogeneous nonmagnetic isotropic dielectric, a monochromatic plane wave has k²=ε_r(ω)ω²/c² and B₀=k×E₀/ω.
ModelPhysics · ChemistryLorentz oscillator model of dielectric responseA damped bound-electron oscillator gives ε_r(ω)=1+Ne²/[ε₀m(ω₀²−ω²−iγω)] for the exp(−iωt) convention.
ApproximationPhysicsNormal-incidence Fresnel reflection and transmissionAt normal incidence on a lossless nonmagnetic dielectric interface, the electric-amplitude reflection coefficient is r=(n₁−n₂)/(n₁+n₂).
ModelPhysicsNonrelativistic charge radiationA nonrelativistic accelerated point charge radiates total power P=q²a²/(6πε₀c³).
ModelPhysicsLorentz coordinate transformationFor inertial frames in standard configuration with S′ moving at v along S's x axis, x′=γ_v(x−vt), t′=γ_v(t−vx/c²), y′=y and z′=z, where γ_v=(1−v²/c²)⁻¹ᐟ².
ModelPhysicsProper time, time dilation and length contractionAlong a timelike worldline in an inertial coordinate frame, dτ=dt√(1−u²/c²), and elapsed proper time is its integral.
ModelPhysicsRelativistic velocity transformationWith S′ moving at v along x, a particle's velocities obey u′_x=(u_x−v)/(1−vu_x/c²) and u′_y,z=u_y,z/[γ_v(1−vu_x/c²)].
ModelPhysicsRelativistic energy, momentum and invariant massA particle of invariant mass m has p=γ_u m u, E=γ_u mc² and K=(γ_u−1)mc²; E²−|p|²c²=m²c⁴.
ModelPhysics · Earth & cosmosLongitudinal relativistic Doppler shiftFor a light source and observer receding directly from each other at relative speed v, f_obs=f_source√[(1−v/c)/(1+v/c)].
ModelPhysics · ChemistryCrystal lattice, basis and primitive cellA Bravais lattice consists of translations R=Σ_i n_i a_i with integer n_i and independent primitive vectors.
DefinitionPhysics · ChemistryReciprocal lattice, Brillouin zone and Bragg conditionReciprocal vectors obey a_i·b_j=2πδ_ij and G=Σ_i h_i b_i with integer h_i.
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