GLOBAL KNOWLEDGE ARK

Reference library

Foundations

Explore concepts, laws, equations and methods, with clear explanations of their use and sources. Choose an area of study or find a specific entry.

More filters

Fluids & waves

Showing 1–30 of 34 reference entries

Physics · ChemistryIdeal-gas equation of state

A simple gas model relates pressure, amount, volume and temperature.

Model
PhysicsHydrostatic pressure

Static fluid pressure rises with depth under gravity.

Model
PhysicsArchimedes' buoyancy principle

The hydrostatic upward force equals displaced-fluid weight.

Model
PhysicsFluid mass continuity

Density change balances mass flux through a region.

Model
PhysicsBernoulli's streamline relation

An ideal steady flow balances pressure, motion and height.

Model
PhysicsIncompressible Navier–Stokes equation

Fluid inertia balances pressure, viscosity and gravity.

Model
PhysicsReynolds number

Compare inertial and viscous scales of a flow.

Model
PhysicsDriven damped oscillator

A linear restoring force, damping and periodic drive determine response.

Model
PhysicsIdeal-string wave equation

A local differential equation determines small string disturbances.

Model
Physics · Mathematics & logicWave superposition and interference

Linear disturbances add; their relative phase determines reinforcement.

Model
PhysicsFixed-end string modes

Boundary conditions select standing-wave frequencies.

Model
Physics · ChemistryHeat capacities, expansion and compressibility

For a fixed amount of simple compressible matter, C_V=(∂U/∂T)_V and C_p=(∂H/∂T)_p.

Model
Physics · Earth & cosmosCoriolis and centrifugal rotating-frame acceleration

For a frame rotating at constant Ω about a common inertial origin, a_inertial=a_rot+2Ω×v_rot+Ω×(Ω×r).

Model
PhysicsCompressible inviscid Euler momentum balance

For a smooth classical fluid with mass continuity, material acceleration is D_tv=∂_tv+(v·∇)v and inviscid momentum obeys ρD_tv=−∇P+ρg.

Model
Physics · Earth & cosmosAdiabatic fluid energy and thermodynamic closure

For 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.

Model
PhysicsLinear isentropic sound waves

Linearizing mass continuity and inviscid momentum around a uniform stationary fluid with δP=c_s²δρ gives ∂_t²δP=c_s²∇²δP.

Model
PhysicsReynolds stresses and turbulence closure

For constant-density incompressible flow, averaging u=U+u′ adds the Reynolds stress R_ij=⟨u′_iu′_j⟩ to the mean momentum equation.

Method
PhysicsDNS, filtered models and convergence evidence

DNS aims to resolve the dynamically relevant viscous scales of a specified flow; LES filters resolved scales and models subfilter stress.

Method
PhysicsNonlinear optical polarization and phase matching

A nonlinear polarization drives new frequency components.

Model
PhysicsKerr envelopes, dispersion and soliton limits

In a lossless scalar narrowband Kerr envelope convention, i∂_zA=−D∂²_tA+δ|A|²A represents second-order dispersion and self-phase modulation.

Model
PhysicsFDTD stability, boundaries and physical validation

Yee FDTD staggers electric/magnetic fields in space and time to approximate Maxwell curl evolution.

Method
PhysicsA mixing-layer benchmark and observable dependence

Nichols' worked compressible mixing-layer comparison specifies two streams, geometry, initial transients and statistical sampling before comparing RANS, LES and hybrid predictions with measurements downstream.

Method
PhysicsDensity and fluid pressure

Density is mass per volume; pressure is normal force per area.

Model
PhysicsAbsolute, gauge and differential pressure

A zero gauge reading need not be a vacuum.

Model
PhysicsPascal’s principle and ideal hydraulics

A pressure change is transmitted; pressure need not be equal at different heights.

Model
PhysicsNewtonian viscosity and Poiseuille flow

Viscosity relates shear stress to velocity gradient.

Model
Physics · ChemistrySurface tension and capillary rise

Interface forces can support pressure jumps and capillary columns.

Model
PhysicsSimple harmonic motion and period

Linear restoring acceleration produces sinusoidal motion.

Model
PhysicsSimple pendulum and the small-angle limit

The familiar pendulum period requires a small swing.

Model
PhysicsAmplitude, phase, wavelength and polarization direction

A wave’s pattern speed differs from the motion of its medium.

Model