Flux Density

Flux describes any effect that appears to pass or travel (whether it actually moves or not) through a surface or substance. Flux is a concept in applied mathematics and vector calculus which has many applications to physics. For transport phenomena, flux is a vector quantity, describing the magnitude and direction of the flow of a substance or property. In vector calculus flux is a scalar quantity, defined as the surface integral of the perpendicular component of a vector field over a surface.

Terminology

The word ''flux'' comes from Latin: ''fluxus'' means "flow", and ''fluere'' is "to flow". As '' fluxion'', this term was introduced into differential calculus by Isaac Newton.

The concept of heat flux was a key contribution of Joseph Fourier, in the analysis of heat transfer phenomena. His seminal treatise ''Théorie analytique de la chaleur'' (''The Analytical Theory of Heat''), defines ''fluxion'' as a central quantity and proceeds to derive the now well-known expressions of flux in terms of temperature differences across a slab, and then more generally in terms of temperature gradients or differentials of temperature, across other geometries. One could argue, based on the work of James Clerk Maxwell, that the transport definition precedes the definition of flux used in electromagnetism. The specific quote from Maxwell is:

According to the transport definition, flux may be a single vector, or it may be a vector field / function of position. In the latter case flux can readily be integrated over a surface. By contrast, according to the electromagnetism definition, flux ''is'' the integral over a surface; it makes no sense to integrate a second-definition flux for one would be integrating over a surface twice. Thus, Maxwell's quote only makes sense if "flux" is being used according to the transport definition (and furthermore is a vector field rather than single vector). This is ironic because Maxwell was one of the major developers of what we now call "electric flux" and "magnetic flux" according to the electromagnetism definition. Their names in accordance with the quote (and transport definition) would be "surface integral of electric flux" and "surface integral of magnetic flux", in which case "electric flux" would instead be defined as "electric field" and "magnetic flux" defined as "magnetic field". This implies that Maxwell conceived of these fields as flows/fluxes of some sort.

Given a flux according to the electromagnetism definition, the corresponding flux density, if that term is used, refers to its derivative along the surface that was integrated. By the Fundamental theorem of calculus, the corresponding flux density is a flux according to the transport definition. Given a current such as electric current—charge per time, current density would also be a flux according to the transport definition—charge per time per area. Due to the conflicting definitions of ''flux'', and the interchangeability of ''flux'', ''flow'', and ''current'' in nontechnical English, all of the terms used in this paragraph are sometimes used interchangeably and ambiguously. Concrete fluxes in the rest of this article will be used in accordance to their broad acceptance in the literature, regardless of which definition of flux the term corresponds to.

Flux as flow rate per unit area

In transport phenomena (heat transfer, mass transfer and fluid dynamics), flux is defined as the ''rate of flow of a property per unit area,'' which has the dimensions uantity�imesup>−1· reasup>−1. The area is of the surface the property is flowing "through" or "across". For example, the amount of water that flows through a cross section of a river each second divided by the area of that cross section, or the amount of sunlight energy that lands on a patch of ground each second divided by the area of the patch, are kinds of flux.

General mathematical definition (transport)

Here are 3 definitions in increasing order of complexity. Each is a special case of the following. In all cases the frequent symbol ''j'', (or ''J'') is used for flux, ''q'' for the physical quantity that flows, ''t'' for time, and ''A'' for area. These identifiers will be written in bold when and only when they are vectors.

First, flux as a (single) scalar:
$j = \frac$
where:
$I = \lim_\frac = \frac$
In this case the surface in which flux is being measured is fixed, and has area ''A''. The surface is assumed to be flat, and the flow is assumed to be everywhere constant with respect to position, and perpendicular to the surface.

Second, flux as a scalar field defined along a surface, i.e. a function of points on the surface:
$j(\mathbf) = \frac(\mathbf)$
$I(A,\mathbf) = \frac(A,\mathbf)$
As before, the surface is assumed to be flat, and the flow is assumed to be everywhere perpendicular to it. However the flow need not be constant. ''q'' is now a function of p, a point on the surface, and ''A'', an area. Rather than measure the total flow through the surface, q measures the flow through the disk with area ''A'' centered at ''p'' along the surface.

Finally, flux as a vector field:
$\mathbf(\mathbf) = \frac(\mathbf)$
$\mathbf(A,\mathbf) = \underset\, \mathbf_ \frac(A,\mathbf, \mathbf)$
In this case, there is no fixed surface we are measuring over. ''q'' is a function of a point, an area, and a direction (given by a unit vector, $\mathbf$), and measures the flow through the disk of area A perpendicular to that unit vector. ''I'' is defined picking the unit vector that maximizes the flow around the point, because the true flow is maximized across the disk that is perpendicular to it. The unit vector thus uniquely maximizes the function when it points in the "true direction" of the flow. trictly speaking, this is an abuse of notation because the "arg max" cannot directly compare vectors; we take the vector with the biggest norm instead.]

Properties

These direct definitions, especially the last, are rather unwieldy. For example, the argmax construction is artificial from the perspective of empirical measurements, when with a Weathervane or similar one can easily deduce the direction of flux at a point. Rather than defining the vector flux directly, it is often more intuitive to state some properties about it. Furthermore, from these properties the flux can uniquely be determined anyway.

If the flux j passes through the area at an angle θ to the area normal $\mathbf$, then
$\mathbf\cdot\mathbf= j\cos\theta$
where · is the dot product of the unit vectors. That is, the component of flux passing through the surface (i.e. normal to it) is ''j'' cos ''θ'', while the component of flux passing tangential to the area is ''j'' sin ''θ'', but there is ''no'' flux actually passing ''through'' the area in the tangential direction. The ''only'' component of flux passing normal to the area is the cosine component.

For vector flux, the surface integral of j over a surface ''S'', gives the proper flowing per unit of time through the surface.
$\frac = \iint_S \mathbf\cdot\mathbf\, dA = \iint_S \mathbf\cdot d\mathbf$
A (and its infinitesimal) is the vector area, combination of the magnitude of the area through which the property passes, ''A'', and a unit vector normal to the area, $\mathbf$. The relation is $\mathbf = A \mathbf$.
Unlike in the second set of equations, the surface here need not be flat.

Finally, we can integrate again over the time duration ''t''₁ to ''t''₂, getting the total amount of the property flowing through the surface in that time (''t''₂ − ''t''₁):
$q = \int_^\iint_S \mathbf\cdot d\mathbf A\, dt$

Transport fluxes

Eight of the most common forms of flux from the transport phenomena literature are defined as follows:

# Momentum flux, the rate of transfer of momentum across a unit area (N·s·m⁻²·s⁻¹). ( Newton's law of viscosity)
# Heat flux