In the various subfields of
physics, there exist two common usages of the term 'flux', both with rigorous mathematical frameworks.
★ In the study of
transport phenomena (
heat transfer,
mass transfer and
fluid dynamics), flux is defined as the amount that flows through a unit area per unit time, the
volumetric flow rate.
[1] Flux in this definition is a
vector.
★ In the field of
electromagnetism, flux is usually the
integral of a
vector quantity over a finite surface. The result of this integration is a
scalar quantity.
[2] The
magnetic flux is thus the integral of the magnetic vector field B over a surface, and the electric flux is defined similarly. Using this definition, the flux of the
Poynting vector over a specified surface is the rate at which electromagnetic energy flows through that surface. Confusingly, the Poynting vector is sometimes called the ''power flux'', which is an example of the first usage of flux, above.
[3] It has units of
watts per
square metre (W/m
2)
One could argue, based on the work of
James Clerk Maxwell[ Treatise on Electricity and Magnetism, , James Clerk, Maxwell, , 1892, ], that the transport definition precedes the more recent way the term is used in electromagnetism. The specific quote from Maxwell is "''In the case of fluxes, we have to take the integral, over a surface, of the flux through every element of the surface. The result of this operation is called the
surface integral of the flux. It represents the quantity which passes through the surface''".
In addition to these common mathematical definitions, there are many more loose usages found in fields such as biology.
Transport phenomena
Flux definition and theorems
Flux is surface bombardment rate. There are many fluxes used in the study of transport phenomena. Each type of flux has its own distinct unit of measurement along with distinct physical constants. Six of the most common forms of flux from the transport literature are defined as:
#''Momentum flux'', the rate of transfer of
momentum across a unit area (N·s·m
-2·s
-1). (Newtonian fluid,
viscous flow)
#''Heat flux'', the rate of
heat flow across a unit area (J·m
-2·s
-1). (
Fourier's Law)
[4] (This definition of heat flux fits Maxwell's original definition.
[ Treatise on Electricity and Magnetism, , James Clerk, Maxwell, , 1892, ])
#''Chemical flux'', the rate of movement of molecules across a unit area (mol·m
-2·s
-1). (
Fick's law of diffusion)
#''Volumetric flux'', the rate of
volume flow across a unit area (m
3·m
-2·s
-1). (
Darcy's law)
#''Mass flux'', the rate of
mass flow across a unit area (kg·m
-2·s
-1). (Either an alternate form of Fick's law that includes the molecular mass, or an alternate form of Darcy's law that includes the density)
#''Radiative flux'', the amount of energy moving in the form of
photons at a certain distance from the source per
steradian per second (J·m
-2·s
-1). Used in astronomy to determine the magnitude and spectral class of a star. Also acts as a generalization of heat flux, which is equal to the radiative flux when restricted to the infrared spectrum.
These fluxes are vectors at each point in space, and have a definite magnitude and direction. Also, one can take the
divergence of any of these fluxes to determine the accumulation rate of the quantity in a control volume around a given point in space. For
incompressible flow, the divergence of the volume flux is zero.
The fundamental laws that govern this process include:
★ Newton's law of viscosity
★ Fourier's law of convection
★ Fick's law of diffusion.
★ Darcy's law of groundwater flow
Chemical diffusion
Flux, or diffusion, for gaseous molecules can be related to the
function:
:
where
:''N'' is the total number of gaseous particles,
:''k'' is Boltzmann's constant,
:''T'' is the relative temperature in kelvins,
:
is the mean free path between the molecules ''a'' and ''b''.
Chemical molar flux of a component A in an
isothermal,
isobaric system is also defined in
Ficks's first law as:
:
where
:
is the molecular diffusion coefficient (m
2/s) of component A diffusing through component B,
:
is the concentration (
mol/m
3) of species A.
[5]
This flux has units of mol·m
−2·s
−1, and fits Maxwell's original definition of flux.
[ Treatise on Electricity and Magnetism, , James Clerk, Maxwell, , 1892, ]
Note:
("
nabla") denotes the
del operator.
Quantum mechanics
Main articles: Probability current
In
quantum mechanics, particles of mass m in the state
have a probability density defined as
:
.
So the probability of finding a particle in a unit of volume, say
, is
:
Then the number of particles passing through a perpendicular unit of area per unit time is
:
This is sometimes referred to as the "flux density".
[6]
Electromagnetism
Flux definition and theorems
An example of the second definition of flux is the magnitude of a river's current, that is, the amount of water that flows through a cross-section of the river each second. The amount of sunlight that lands on a patch of ground each second is also a kind of flux.
To better understand the concept of flux in Electromagnetism, imagine a butterfly net. The amount of air moving through the net at any given instant in time is the flux. If the wind speed is high, then the flux through the net is large. If the net is made bigger, then the flux would be larger even though the wind speed is the same. For the most air to move through the net, the opening of the net must be facing the direction the wind is blowing. If the net opening is parallel to the wind, then no wind will be moving through the net. (These examples are not very good because they rely on a transport process and as stated in the introduction, transport flux is defined differently than E+M flux.) Perhaps the best way to think of flux abstractly is "How much stuff goes through your thing", where the stuff is a field and the thing is the imaginary surface.

The flux visualized. The rings show the surface boundaries. The red arrows stand for the flow of charges, fluid particles, subatomic particles, photons, etc. The number of arrows that pass through each ring is the flux.
As a mathematical concept, flux is represented by the
surface integral of a vector field,
:
where
:'F' is a
vector field,
:'dA' is the
vector area of the surface ''S'', directed as the
surface normal,
:
is the resulting flux.
The surface has to be
orientable, i.e. two sides can be distinguished: the surface does not fold back onto itself. Also, the surface has to be actually oriented, i.e. we use a convention as to flowing which way is counted positive; flowing backward is then counted negative.
The surface normal is directed accordingly, usually by the
right-hand rule.
Conversely, one can consider the flux the more fundamental quantity and call the vector field the flux density.
Often a vector field is drawn by curves (field lines) following the "flow"; the magnitude of the vector field is then the line density, and the flux through a surface is the number of lines. Lines originate from areas of positive
divergence (sources) and end at areas of negative divergence (sinks).
See also the image at right: the number of red arrows passing through a unit area is the flux density, the
curve encircling the red arrows denotes the boundary of the surface, and the orientation of the arrows with respect to the surface denotes the sign of the
inner product of the vector field with the surface normals.
If the surface encloses a 3D region, usually the surface is oriented such that the 'outflux' is counted positive; the opposite is the 'influx'.
The
divergence theorem states that the net outflux through a closed surface, in other words the net outflux from a 3D region, is found by adding the local net outflow from each point in the region (which is expressed by the
divergence).
If the surface is not closed, it has an oriented curve as boundary.
Stokes theorem states that the flux of the
curl of a vector field is the
line integral of the vector field over this boundary. This path integral is also called
circulation, especially in fluid dynamics. Thus the curl is the circulation density.
We can apply the flux and these theorems to many disciplines in which we see currents, forces, etc., applied through areas.
Maxwell's equations
The flux of
electric and
magnetic field lines is frequently discussed in
electrostatics. This is because in
Maxwell's equations in integral form involve integrals like above for electric and magnetic fields.
For instance,
Gauss's law states that the flux of the electric field out of a closed surface is proportional to the
electric charge enclosed in the surface (regardless of how that charge is distributed). The constant of proportionality is the reciprocal of the
permittivity of free space.
Its integral form is:
:
where
:
is the electric field,
:
is the area of a differential square on the surface ''A'' with an outward facing
surface normal defining its direction,
:
is the charge enclosed by the surface,
:
is the
permittivity of free space
:
is the integral over the surface ''A''.
Either
or
is called the 'electric flux'.
Faraday's law of induction in integral form is:
:
The
magnetic field is denoted by
. Its flux is called the
magnetic flux. The time-rate of change of the magnetic flux through a loop of wire is minus the
electromotive force created in that wire. The direction is such that if current is allowed to pass through the wire, the electromotive force will cause a current which "opposes" the change in magnetic field by itself producing a magnetic field opposite to the change. This is the basis for
inductors and many
electric generators.
Poynting vector
The flux of the
Poynting vector through a surface is the electromagnetic
power, or
energy per unit
time, passing through that surface. This is commonly used in analysis of
electromagnetic radiation, but has application to other electromagnetic systems as well.
Biology
In general, 'flux' in
biology relates to movement of a substance between compartments. There are several cases where the concept of 'flux' is important.
★ The movement of molecules across a membrane: in this case, flux is defined by the rate of
diffusion or transport of a substance across a permeable
membrane. Except in the case of active transport, net flux is directly proportional to the
concentration difference across the membrane, the
surface area of the membrane, and the membrane
permeability constant.
★ In
ecology, flux is often considered at the
ecosystem level - for instance, accurate determination of
carbon fluxes (at a regional and global level) is essential for modeling the causes and consequences of
global warming.
★
Metabolic flux refers to the rate of flow of metabolites along a
metabolic pathway, or even through a single
enzyme. A calculation may also be made of carbon (or other elements, e.g. nitrogen) flux. It is dependent on a number of factors, including: enzyme concentration; the concentration of precursor, product, and intermediate metabolites;
post-translational modification of enzymes; and the presence of metabolic activators or repressors.
Metabolic control analysis and
flux balance analysis provide frameworks for understanding metabolic fluxes and their constraints.
See also
★
Explosively pumped flux compression generator
★
Fast Flux Test Facility
★
Flux capacitor (fictional device)
★
Fluid dynamics
★
Flux quantization
★
Flux pinning
★
Gauss's law
★
Inverse-square law
★
Latent heat flux
★
Luminous flux
★
Magnetic flux
★
Magnetic flux quantum
★
Neutron flux
★
Poynting flux
★
Poynting theorem
★
Radiant flux
★
Rapid single flux quantum
★
Sound energy flux
★
Volumetric flow rate
★
Fluence (flux for particle beams)
References
1. Transport Phenomena, , R. Byron, Bird, Wiley, 1960, ISBN 0-471-07392-X
2. Electromagnetic Fields and Waves, , Paul, Lorrain, , 1962,
3. Electromagnetic Fields, , Roald K., Wangsness, Wiley, 1986, ISBN 0-471-81186-6 p.357
4. Conduction of Heat in Solids, , H.S., Carslaw, Oxford University Press, 1959, ISBN 0-19-853303-9
5. Fundamentals of Momentum, Heat, and Mass Transfer, , , Welty, Wiley, 2001, ISBN 0-471-38149-7
6. Advanced Quantum Mechanics, Sakurai, J. J., , , Addison Wesley, 1967, ISBN 0-201-06710-2
Further reading
★
Flux Flummoxed: A Proposal for Consistent Usage, Stauffer, P.H., , , Ground Water, 2006