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    In the various subfields of physics, there exist two common usages of the term flux, both with rigorous mathematical frameworks.
      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. The magnetic flux is thus the integral of the magnetic vector field 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. It has units of watts/metre2.

    One could argue, based on the work of James Clerk Maxwell 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 mathematically defined definitions, there are many more loose usages found in fields such as biology.


        Flux
                Flux definition and theorems
                Chemical diffusion
                Quantum mechanics
                Flux definition and theorems
                Maxwells equations
                Poynting vector
            Biology
            See also
            Further reading

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    Flux definition and theorems
    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. Five 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) (This definition of heat flux fits Maxwell's original definition.)
      Volumetric flux, the rate of volume flow across a unit area (m3·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)

    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

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    Chemical diffusion
    Flux, or diffusion, for gaseous molecules can be related to the function:

    Phi = 4pisigma_^2sqrt


    where
    N is the total number of gaseous particles,

    k is Boltzmann's constant,

    T is the relative temperature in kelvins,

    sigma_ 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:

    overrightarrow = -D_

    abla c_A

    where
    D_ is the molecular diffusion coefficient (m2/s) of component A diffusing through component B,

    c_A is the concentration (mol/m3) of species A .


    This flux has units of mol·m−2·s−1, and fits Maxwell's original definition of flux.

    Note:
    abla ("nabla") denotes the del operator.

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    Quantum mechanics

    In quantum mechanics, particles of mass m in the state psi(r,t) have a probability density defined as

    ho = psi^
      psi = |psi|^2 ,.
    So the probability of finding a particle in a unit of volume, say d^3x, is
    |psi|^2 d^3x ,

    Then the number of particles passing through a perpendicular unit of area per unit time is
    mathbf = -i rac left(psi^
    abla psi - psi
    abla psi^
    ight) ,
    This is sometimes referred to as the "flux density".

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    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.



    As a mathematical concept, flux is represented by the surface integral of a vector field,

    Phi_f = int_S mathbf cdot mathbf


    where
    F is a vector field,

    dA is the vector area of the surface S, directed as the surface normal,

    Phi_f  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.

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    Maxwells 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:

    oint_A epsilon_0 mathbf cdot dmathbf = Q_A


    where
    mathbf is the electric field,

    dmathbf is the area of a differential square on the surface A with an outward facing surface normal defining its direction,

    Q_A is the charge enclosed by the surface,

    epsilon_0 is the permittivity of free space

    oint_A is the integral over the surface A.


    Either oint_A epsilon_0 mathbf cdot dmathbf or oint_A mathbf cdot dmathbf is called the electric flux.

    Faraday's law of induction in integral form is:

    oint_C mathbf cdot dmathbf = -int_ cdot dmathbf = - rac


    The magnetic field density, also called magnetic flux density, is denoted by mathbf . 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.

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    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.

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    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.

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    See also

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    Further reading




     
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    This article is licensed under the GNU Free Documentation License [copyleft]. It uses material from the Wikipedia article "Flux". link