The dimensionless ratio of a material's density to a specified reference density, with reference conditions stated. Gases are commonly compared with dry air and liquids with water.
A nonnegative mass density proportional to rp has finite local mass near a straight axis if ∫0εrp+1dr converges, namely p>−2. Near a three-dimensional center the corresponding condition is convergence of ∫0εrp+2dr, namely p>−3. These follow from the cylindrical volume element and spherical volume element. At equality the divergence is logarithmic. An unbounded density does not by itself imply infinite mass.
The spatial dependence of density, such as ρ(r) for spherical matter. Hydrostatic equilibrium relates a gas profile and temperature to its confining gravitational mass.
The flux of mass carried by a continuum moving with velocity v. In the nonrelativistic limit, ∂tρ+∇⋅jm=0 is local mass conservation. A stationary mass current can produce a stationary gravitomagnetic field without emitting gravitational radiation.
The mean mass density of a body is its total mass divided by its volume. A nonuniform density distribution can have the same mean as a uniform one; orbital information that determines only M/V does not determine the internal density profile.
For a spherical surface of radius R with exterior mass density ρ(r)=ρ0e−(r−R)/h0, integrate the spherical volume element to obtain M=4πρ0∫0∞(R+h)2e−h/h0dh. The moments ∫0∞hne−h/h0dh=n!h0n+1 give the displayed expression. Its leading thin-atmosphere approximation is surface area times column mass, 4πR2ρ0h0; the two positive correction terms account for the growth of shell area with altitude.
Gas density is the mass density of a gas. For an ideal gas sample of amount of substance n, mean molar mass M and volume V, combine m=nM with pV=nRT to obtainHere R is the molar gas constant. For a homogeneous mixture of gases, M=∑ixiMi, where xi is the mole fraction of component i. Equal pressure and temperature make a gas density ratio equal to a mean-molar mass ratio within this model. Argon detection in a binary gas mixture gives a worked example and a temperature confounder.
ρ=Vm=RTpM.
In an idealized rigid-globe weighing, subtract the evacuated assembly's mass from the filled assembly's mass, then divide by the internal volume. Establish the filled sample's pressure and temperature before comparing gases. The subtraction removes the container's large contribution, making a small gas contribution accessible. A real measurement also needs corrections or bounds for residual gas, adsorption, leaks, changing vessel volume and external buoyancy. The Rayleigh-Ramsay argon density experiment shows why preparation-route comparisons add information beyond repeated weighings of one sample.
Linear mass density is mass per unit length, measured in kgm−1. A uniform string of mass m and length L has μ=m/L; with constant tension T, its transverse wave speed is T/μ. Mass density instead measures mass per unit volume.
The gas clumping factor measures unresolved inhomogeneity in electron number density within a chosen averaging region. Nonnegative variance gives Ce≥1. At a uniform temperature, thermal bremsstrahlung scales with ⟨ne2⟩, whereas the thermal Sunyaev-Zeldovich effect scales with ⟨ne⟩. A homogeneous cluster distance from Sunyaev-Zeldovich and X-ray signals inference then gives dA,inferred=dA,true/Ce, for the same geometry and temperature. Correlated temperature variations require additional weighted averages.
Projected surface mass density is mass per unit projected area, obtained by integrating mass density along the line of sight. It determines the enclosed cylindrical mass used by a thin gravitational lens equation. It need not equal a physical disk's density, and its aperture mass differs from a spherical three-dimensional enclosed mass.
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Incoming links (557)
- Adams-Williamson equation
- Adiabatic bulk modulus
- Agarose gel electrophoresis
- Age of a flat barotropic matter-vacuum universe
- AGN Emission Lines by Hagai Netzer
- Airy isostasy
- Angular-frequency Planck energy density
- Astrophysical volume filling factor
- Atomic and nuclear properties of tungsten by the Particle Data Group
- Boltzmann ion densities in a symmetric electrolyte
- Boosted uniform line charge
- Bose condensation temperature from a fermionic density scale
- Bulk-density upper limit from a transit and an RV nondetection
- Buoyant density
- Circular bending energy of an elastic filament
- Classical Gases by David Tong
- Cold neutral medium
- Collective diffusion
- Collision stopping power
- Compensation depth
- Contact-angle change of capillary rise
- Contact-interaction Hartree-Fock spin energy
- Cosmic-ray altitude attenuation model
- Critical mass from a virial pressure turning point
- Curie heat-capacity density from an Arrott plot
- Curie response of an arbitrary independent spin
- Deccan Traps
- Degeneracy onset from thermal wavelength
- Density-depth degeneracy of free-free radiation
- Density-gradient centrifugation
- Density profile
- Density-weighted mean
- Diapycnal mixing
- Dissociation fraction versus conserved density
- Divergence
- Dopant density
- Drag coefficient
- Dynamic topography
- Earth crust
- Eclogitization
- Eddy buoyancy flux
- Effective carrier convention in the Nernst-Einstein relation
- Effects of Microstructural Factors on Irradiation Growth in Zirconium-Base Alloys by Noriyuki Sadaoka and Motomasa Fuse
- Elasticity tensor
- Electron-hydrogen normalization of the cooling function
- Elementary charge
- Emission measure
- Energy in a rectangular membrane mode
- Entropic polymer depletion near nonadsorbing walls
- Entropy mode
- Entropy-related corotation torque
- Ertel's theorem
- Fermi-window convolution of the grand potential
- Fibre-laser gain-volume rate equations
- Field-induced triplon condensation
- Finite-time rate-zonal separation
- First sound
- Flat barotropic matter-vacuum solution
- Flexural gravity admittance
- Focal length of a rotating liquid mirror
- Geodesic motion of uncharged dust
- Geoid
- Geophysical density contrast
- Geostrophic wind
- Gravitationally focused growth of a planetary core
- Gravity inversion
- Gravity-topography admittance
- Greenstone
- Harmonic heating response of quasi-geostrophic flow
- Heat balance with volumetric heat generation
- Henry Cavendish
- High-density two-level radiative cooling
- Hydrometer
- Hydrostatic temperature of an inverse-square halo
- Incompressible flow
- Influence function of a quantile
- Integral
- Intrinsic phase averages in a two-fluid pipe model
- Ionization-chamber charge-loss model
- Isobaric ideal-gas internal-energy density
- Isobaric thermal stability of a two-level coolant
- Isochoric thermal stability of a collisionally excited line
- Isopycnic centrifugation
- Isostatic adjustment
- Isostatic ridge elevation in a plate model
- Joule-heated cylindrical wire
- Larmor-Langevin susceptibility
- Lawson criterion
- Lenard cathode-ray window experiment
- Lindblad resonance
- Linear displacement equations for a magnetized atmosphere
- Linear-gradient isopycnic focusing
- Linearized planar screening solution
- Line-of-sight projection
- Liquid water
- Liquid-water content
- Lithology
- Local isostatic response to an added surface layer
- Localized interchange criterion for a magnetized atmosphere
- Longitudinal solenoid field under an axial boost
- Long-wave and short-wave branches at marginal Toomre stability
- Long-wavelength undular magnetic buoyancy criterion
- Magnetic-to-electric energy ratio in a driven disc capacitor
- Marginal-sea overflow
- Material-arm winding in a differentially rotating galaxy
- Melt depletion
- Melting pressure inferred from flotation and latent heats
- Multiphase flow
- Multiphase interstellar medium
- Neutral current filament in a boosted frame
- Nonlinear counterion accumulation in planar screening
- Nonlinear planar Poisson-Boltzmann profile
- Nonuniqueness of geophysical inversion
- On-shell divergence of a quartic scalar dilation current
- Oppenheimer-Snyder cloud
- Oppenheimer-Snyder model
- Oscillation of a uniformly wound coil
- Particle velocity-relaxation time
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- Perrin sedimentation experiment
- Perseus cluster
- Plasma wakefield acceleration
- Plumb-line deflection from cylindrical gravity
- Potential of an inverse-radius spherical charge density
- Pratt isostasy
- Preliminary Reference Earth Model
- Pressure-truncated singular isothermal gas sphere
- Proper distance prior for parallax inference
- P-star density for two exponential rates
- Quadratic drag
- Radial density inversion of the Earth
- Range-conditioned uniform location inference
- Rate-zonal centrifugation
- Redshift shell volume at the present epoch
- Reduced pressure in a rotating fluid
- Relative centrifugal force
- Relative density
- Ridge-push force in a plate model
- Rigid rotation minimizes kinetic energy at fixed angular momentum
- Rock physics
- Salt-advection feedback
- Sedimentation coefficient
- Sedimentation scale height
- Seismic parameter
- Seismic velocity
- Selection-normalized astronomical likelihood
- Shear-wave impedance
- Slab buoyancy
- Solar model
- Spherical Thomas–Fermi condensate
- Spherical top-hat collapse model
- Step-flux residual circulation in a stratified channel
- Stokes equation
- Stokes flow
- Stokes settling velocity
- Stokes's law
- Streakline
- Stress glut tensor
- Stretch and twist coefficients of an elastic filament
- Strong-collision ion-neutral Alfvén modes
- Subslab mantle buoyancy
- Synchronous coordinates for irrotational dust
- Tangent-axis inertia of a spherical shell
- Terrain correction
- Tex unit
- Thermal and compositional interfacial buoyancy criterion
- Thermal radiation processes by Jelle S. Kaastra and others
- Thermal relic density bound for a tunable fermion
- Three-level forbidden-line density diagnostic
- Tidal water loading of a spring balance
- Toroidal interchange field threshold in a thin Keplerian disk
- Translational magnetic damping of a square wire loop
- Transport of fossil remains
- Triplon
- Triplon condensation field scaling
- Two-box overturning model
- Two coupled real Klein-Gordon fields
- Two-step catalytic waiting time
- U-tube liquid oscillation
- Vapor density
- Volcanic loading
- Water-mass transformation
- William Ramsay
- Zeeman discovery experiment of 1896
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