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Fluids & waves
Showing 1–30 of 34 reference entries
A simple gas model relates pressure, amount, volume and temperature.
ModelPhysicsHydrostatic pressureStatic fluid pressure rises with depth under gravity.
ModelPhysicsArchimedes' buoyancy principleThe hydrostatic upward force equals displaced-fluid weight.
ModelPhysicsFluid mass continuityDensity change balances mass flux through a region.
ModelPhysicsBernoulli's streamline relationAn ideal steady flow balances pressure, motion and height.
ModelPhysicsIncompressible Navier–Stokes equationFluid inertia balances pressure, viscosity and gravity.
ModelPhysicsReynolds numberCompare inertial and viscous scales of a flow.
ModelPhysicsDriven damped oscillatorA linear restoring force, damping and periodic drive determine response.
ModelPhysicsIdeal-string wave equationA local differential equation determines small string disturbances.
ModelPhysics · Mathematics & logicWave superposition and interferenceLinear disturbances add; their relative phase determines reinforcement.
ModelPhysicsFixed-end string modesBoundary conditions select standing-wave frequencies.
ModelPhysics · ChemistryHeat capacities, expansion and compressibilityFor a fixed amount of simple compressible matter, C_V=(∂U/∂T)_V and C_p=(∂H/∂T)_p.
ModelPhysics · Earth & cosmosCoriolis and centrifugal rotating-frame accelerationFor a frame rotating at constant Ω about a common inertial origin, a_inertial=a_rot+2Ω×v_rot+Ω×(Ω×r).
ModelPhysicsCompressible inviscid Euler momentum balanceFor a smooth classical fluid with mass continuity, material acceleration is D_tv=∂_tv+(v·∇)v and inviscid momentum obeys ρD_tv=−∇P+ρg.
ModelPhysics · Earth & cosmosAdiabatic fluid energy and thermodynamic closureFor a smooth inviscid, nonconducting fixed-composition fluid, D_ts=0 and ρD_te=−P∇·v, where e and s are internal energy and entropy per mass.
ModelPhysicsLinear isentropic sound wavesLinearizing mass continuity and inviscid momentum around a uniform stationary fluid with δP=c_s²δρ gives ∂_t²δP=c_s²∇²δP.
ModelPhysicsReynolds stresses and turbulence closureFor constant-density incompressible flow, averaging u=U+u′ adds the Reynolds stress R_ij=⟨u′_iu′_j⟩ to the mean momentum equation.
MethodPhysicsDNS, filtered models and convergence evidenceDNS aims to resolve the dynamically relevant viscous scales of a specified flow; LES filters resolved scales and models subfilter stress.
MethodPhysicsNonlinear optical polarization and phase matchingA nonlinear polarization drives new frequency components.
ModelPhysicsKerr envelopes, dispersion and soliton limitsIn a lossless scalar narrowband Kerr envelope convention, i∂_zA=−D∂²_tA+δ|A|²A represents second-order dispersion and self-phase modulation.
ModelPhysicsFDTD stability, boundaries and physical validationYee FDTD staggers electric/magnetic fields in space and time to approximate Maxwell curl evolution.
MethodPhysicsA mixing-layer benchmark and observable dependenceNichols' worked compressible mixing-layer comparison specifies two streams, geometry, initial transients and statistical sampling before comparing RANS, LES and hybrid predictions with measurements downstream.
MethodPhysicsDensity and fluid pressureDensity is mass per volume; pressure is normal force per area.
ModelPhysicsAbsolute, gauge and differential pressureA zero gauge reading need not be a vacuum.
ModelPhysicsPascal’s principle and ideal hydraulicsA pressure change is transmitted; pressure need not be equal at different heights.
ModelPhysicsNewtonian viscosity and Poiseuille flowViscosity relates shear stress to velocity gradient.
ModelPhysics · ChemistrySurface tension and capillary riseInterface forces can support pressure jumps and capillary columns.
ModelPhysicsSimple harmonic motion and periodLinear restoring acceleration produces sinusoidal motion.
ModelPhysicsSimple pendulum and the small-angle limitThe familiar pendulum period requires a small swing.
ModelPhysicsAmplitude, phase, wavelength and polarization directionA wave’s pattern speed differs from the motion of its medium.
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