A church (or local church) is a Christian organization or congregation that meets in a particular location, often for worship. Many are formally organized, with constitutions and by-laws, maintain offices, are served by clergy or lay leaders, and, in nations where this is permissible, often seek non-profit corporate status. The term is distinct from the use of the word "church" to mean a church building.
Local churches often relate with, affiliate with, or consider themselves to be constitutive parts of denominations,
which are also called churches in many traditions. Depending on the
tradition, these organizations may connect local churches to larger
church traditions, ordain and defrock clergy, define terms of membership and exercise church discipline, and have organizations for cooperative ministry such as educational institutions and missionary societies. Non-denominational
churches are not part of denominations, but may consider themselves
part of larger church movements without institutional expression.
History
The word church is used in the sense of a distinct congregation in a given city in slightly under half of the 200 uses of the term in the New Testament. John Locke
defined a church as "a voluntary society of men, joining themselves
together of their own accord in order to the public worshipping of God in such manner as they judge acceptable to him".
The word church may rarely be used for other religious
communities. For non-Christian communities the term may be considered
archaic or even offensive, negating existing terms such as synagogue or mosque used to refer to their community or place of worship.
Etymology
The Greek word ekklēsia,
literally "called out" or "called forth" and commonly used to indicate a
group of individuals called to gather for some function, in particular
an assembly of the citizens of a city, as in Acts 19:32–41, is the New Testament term referring to the Christian Church (either a particular local congregation or the whole body of the faithful). In the Septuagint, the Greek word "ἐκκλησία" is used to translate the Hebrew "קהל" (qahal). In most Romance and Celtic languages, the word for church derives from the Greek word or its Latin form ecclesia (Spanish iglesia, French église, Italian chiesa, Irish eaglais, Welsh eglwys).
The English language word "church" is from the Old English word cirice, derived from West Germanic*kirika, which in turn comes from the Greek κυριακήkuriakē, meaning "of the Lord" (possessive form of κύριοςkurios "ruler" or "lord"). Kuriakē in the sense of "church" is most likely a shortening of κυριακὴ οἰκίαkuriakē oikia ("house of the Lord") or ἐκκλησία κυριακήekklēsia kuriakē ("congregation of the Lord"). Some grammarians and scholars say that the word has uncertain roots and may derive from the Anglo-Saxon
"kirke" from the Latin "circus" and the Greek "kuklos" for "circle",
which shape is the form in which many religious groups met and gathered. Christian churches were sometimes called κυριακόνkuriakon (adjective meaning "of the Lord") in Greek starting in the fourth century, but ekklēsia and βασιλικήbasilikē were more common.
The word is one of many direct Greek-to-Germanic loans of Christian terminology, via the Goths. The Slavic terms for "church" (Old Church Slavonicцрькꙑ [crĭky], Russianцерковь [cerkov’], Slovenian cerkev) are via the Old High German cognate chirihha.
Description
Among congregational churches, since each local church is autonomous,
there are no formal lines of responsibility to organizational levels of
higher authority. Deacons
of each church are elected by the congregation. In some Baptist
congregations, for example, deacons function much like a board of
directors or executive committee authorized to make important decisions.
Although these congregations typically retain the right to vote on
major decisions such as purchasing or selling property, large spending,
and the hiring or firing of pastors and other paid ministers. In many
such local churches, the role of deacons includes pastoral and nurturing
responsibilities. Typically, congregational churches have informal
worship styles, less structured services, and may tend toward modern
music and celebrations.
Local churches united with others under the oversight of a bishop are normally called "parishes", by Roman Catholic, Eastern Orthodox, Anglican, and Lutherancommunions.
Each parish usually has one active parish church, though seldom and
historically more than one. The parish church has always been
fundamental to the life of every parish community, especially in rural
areas. For example, in the Church of England,
parish churches are the oldest churches to be found in England. A
number are substantially of Anglo-Saxon date and all subsequent periods
of architecture are represented in the country. Most parishes have
churches that date back to the Middle Ages. Thus, such local churches
tend to favor traditional, formal worship styles, liturgy, and classical
music styles, although modern trends are common as well.
Local parishes of the Roman Catholic Church, like episcopal
parishes, favor formal worship styles, and still more traditional
structure in services. The importance of formal office is also a
distinctive trait; thus a solemn mass may include the presence of
officers of the Knights of Columbus
as an escort for the regional bishop when he is present. Likewise,
vestments are valued to inculcate the solemnity of the Holy Eucharist
and are typically more elaborate than in other churches.
A local church may also be a mission,
that is a smaller church under the sponsorship of a larger
congregation, a bishop, or a greater church hierarchy. Often
congregational churches prefer to call such local mission churches
"church plants."
A local church may also work in association with parachurch organizations.
While parachurch organizations/ministries are vital to accomplishing
specific missions on behalf of the church they do not normally take the
place of the local church.
Church asylum
The door of this Spanish church is inscribed ES YGLESIA DE REFUGIO ("[This] is an asylum church").
The Catholic Church has long offered housing to asylum seekers in the
form of church asylum. In this tradition, the church provides sanctuary
to asylum seekers for a short duration on their congregation's premises.
During the nineteenth century in the United States, many churches, particularly the African Methodist Episcopal Zion Church,
sheltered those escaping Southern slavery. Many of these churches
assisted fugitive slaves and aligned themselves with the growing
abolitionist movement in the northern United States.
The microscopic equations have universal applicability
but are unwieldy for common calculations. They relate the electric and
magnetic fields to total charge and total current, including the
complicated charges and currents in materials at the atomic scale.
The macroscopic equations define two new auxiliary fields
that describe the large-scale behaviour of matter without having to
consider atomic-scale charges and quantum phenomena like spins. However,
their use requires experimentally determined parameters for a
phenomenological description of the electromagnetic response of
materials.
Maxwell's equations are named after the physicist and mathematician James Clerk Maxwell,
who, in 1861 and 1862, published an early form of the equations that
included the Lorentz force law. The publication of the equations marked
the unification
of a theory for previously separately described phenomena: magnetism,
electricity, light, and associated radiation. The modern form of the
equations in their most common formulation is credited to Oliver Heaviside.
Since the mid-20th century, it has been understood that Maxwell's
equations do not give an exact description of electromagnetic
phenomena, but are instead a classical limit of the more precise theory of quantum electrodynamics.
Summary
The two most commonly used variants of Maxwell's equations are the microscopic and macroscopic differential form in SI units.
Gauss's law describes the relationship between an electric field and electric charges: an electric field points away from positive charges and towards negative charges, and the net outflow of the electric field through a closed surface
is proportional to the enclosed charge, including bound charge due to
polarization of material. The coefficient of the proportion is the permittivity of free space.
Gauss's law for magnetism:
magnetic field lines never begin nor end but form loops or extend to
infinity as shown here with the magnetic field due to a ring of current.
Gauss's law for magnetism states that electric charges have no magnetic analogues, called magnetic monopoles; no north or south magnetic poles exist in isolation. Instead, the magnetic field of a material is attributed to a dipole,
and the net outflow of the magnetic field through a closed surface is
zero. Magnetic dipoles may be represented as loops of current or
inseparable pairs of equal and opposite "magnetic charges". Precisely,
the total magnetic flux through a Gaussian surface is zero, and the magnetic field is a solenoidal vector field.
In a geomagnetic storm, solar wind plasma impacts Earth's magnetic field causing a time-dependent change in the field, thus inducing electric fields in Earth's atmosphere and conductive lithosphere which can destabilize power grids. (Not to scale.)
The Maxwell–Faraday version of Faraday's law of induction describes how a time-varying magnetic field corresponds to the negative curl of an electric field. In integral form, it states that the work per unit charge required to
move a charge around a closed loop equals the rate of change of the
magnetic flux through the enclosed surface.
The original law of Ampère states that magnetic fields relate to electric current. Maxwell's addition states that magnetic fields also relate to changing electric fields, which Maxwell called displacement current.
The integral form states that electric and displacement currents are
associated with a proportional magnetic field along any enclosing curve.
Maxwell's modification of Ampère's circuital law is important
because the laws of Ampère and Gauss must otherwise be adjusted for
static fields. As a consequence, it predicts that a rotating magnetic field occurs with a changing electric field. A further consequence is the existence of self-sustaining electromagnetic waves which travel through empty space.
The speed calculated for electromagnetic waves, which could be predicted from experiments on charges and currents, matches the speed of light; indeed, lightis one form of electromagnetic radiation (as are X-rays, radio waves,
and others). Maxwell understood the connection between electromagnetic
waves and light in 1861, thereby unifying the theories of electromagnetism and optics.
Microscopic formulation in terms of electric and magnetic fields (in vacuum version)
In the electric and magnetic field formulation there are four
equations that determine the fields for given charge and current
distribution. A separate law of nature, the Lorentz force
law, describes how the electric and magnetic fields act on charged
particles and currents. By convention, a version of this law in the
original equations by Maxwell is no longer included. The vector calculus formalism below, the work of Oliver Heaviside, has become standard. It is rotationally invariant, and therefore
mathematically more transparent than Maxwell's original 20 equations in x, y and z components. The relativistic formulations are more symmetric and Lorentz invariant. For the same equations expressed using tensor calculus or differential forms (see § Alternative formulations).
The differential and integral formulations are mathematically
equivalent; both are useful. The integral formulation relates fields
within a region of space to fields on the boundary and can often be used
to simplify and directly calculate fields from symmetric distributions
of charges and currents. On the other hand, the differential equations
are purely local and are a more natural starting point for
calculating the fields in more complicated (less symmetric) situations,
for example using finite element analysis.
Key to the notation
Symbols in bold represent vector quantities, and symbols in italics represent scalar quantities, unless otherwise indicated.
The equations introduce the electric field, E, a vector field, and the magnetic field, B, a pseudovector field, each generally having a time and location dependence.
The sources are
the total electric charge density (total charge per unit volume), ρ, and
the total electric current density (total current per unit area), J.
The universal constants appearing in the equations (the first two ones explicitly only in the SI formulation) are:
the ∇⋅ symbol (pronounced "del dot") denotes the divergence operator,
the ∇× symbol (pronounced "del cross") denotes the curl operator.
Integral equations
In the integral equations,
Ω is any volume with closed boundary surface ∂Ω, and
Σ is any surface with closed boundary curve ∂Σ,
The equations are a little easier to interpret with time-independent
surfaces and volumes. Time-independent surfaces and volumes are "fixed"
and do not change over a given time interval. For example, since the
surface is time-independent, we can bring the differentiation under the integral sign in Faraday's law:
Maxwell's equations can be formulated with possibly time-dependent
surfaces and volumes by using the differential version and using Gauss'
and Stokes' theorems as appropriate.
is a surface integral over the boundary surface ∂Ω, with the loop indicating the surface is closed
The definitions of charge, electric field, and magnetic field can be altered to simplify theoretical calculation, by absorbing dimensioned factors of ε0 and μ0 into the units (and thus redefining these). With a corresponding change in the values of the quantities for the Lorentz force law this yields the same physics, i.e. trajectories of charged particles, or work
done by an electric motor. These definitions are often preferred in
theoretical and high energy physics where it is natural to take the
electric and magnetic field with the same units, to simplify the
appearance of the electromagnetic tensor:
the Lorentz covariant object unifying electric and magnetic field would
then contain components with uniform unit and dimension. Such modified definitions are conventionally used with the Gaussian (CGS) units. Using these definitions, colloquially "in Gaussian units", the Maxwell equations become:
The equations simplify slightly when a system of quantities is chosen in the speed of light, c, is used for nondimensionalization, so that, for example, seconds and lightseconds are interchangeable, and c = 1.
Volume Ω and its closed boundary ∂Ω, containing (respectively enclosing) a source (+) and sink (−) of a vector field F. Here, F could be the E field with source electric charges, but not the B field, which has no magnetic charges as shown. The outward unit normal is n.
The integral version of Gauss's equation can thus be rewritten as
Since Ω is arbitrary (e.g. an arbitrary small ball with arbitrary center), this is satisfied if and only if the integrand is zero everywhere. This is
the differential equations formulation of Gauss equation up to a trivial rearrangement.
Similarly rewriting the magnetic flux in Gauss's law for magnetism in integral form gives
which is satisfied for all Ω if and only if everywhere.
Circulation and curl
Surface Σ with closed boundary ∂Σ. F could be the E or B fields. Again, n is the unit normal. (The curl of a vector field does not literally look like the "circulations", this is a heuristic depiction.)
By the Kelvin–Stokes theorem we can rewrite the line integrals of the fields around the closed boundary curve ∂Σ to an integral of the "circulation of the fields" (i.e. their curls) over a surface it bounds, i.e.
Hence the Ampère–Maxwell law, the modified version of Ampère's circuital law, in integral form can be rewritten as
Since Σ can be chosen arbitrarily, e.g. as
an arbitrary small, arbitrary oriented, and arbitrary centered disk, we
conclude that the integrand is zero if and only if the Ampère–Maxwell law in differential equations form is satisfied.
The equivalence of Faraday's law in differential and integral form follows likewise.
The line integrals and curls are analogous to quantities in classical fluid dynamics: the circulation of a fluid is the line integral of the fluid's flow velocity field around a closed loop, and the vorticity of the fluid is the curl of the velocity field.
Charge conservation
The invariance of charge can be derived as a corollary of Maxwell's
equations. The left-hand side of the Ampère–Maxwell law has zero
divergence by the div–curl identity. Expanding the divergence of the right-hand side, interchanging derivatives, and applying Gauss's law gives:
i.e.,
By the Gauss divergence theorem, this means the rate of change of charge
in a fixed volume equals the net current flowing through the boundary:
In particular, in an isolated system the total charge is conserved.
Vacuum equations, electromagnetic waves and speed of light
This 3D diagram shows a plane linearly polarized wave propagating from left to right, defined by E = E0 sin(−ωt + k ⋅ r) and B = B0 sin(−ωt + k ⋅ r) The oscillating fields are detected at the flashing point. The horizontal wavelength is λ. E0 ⋅ B0 = 0 = E0 ⋅ k = B0 ⋅ k
In a region with no charges (ρ = 0) and no currents (J = 0), such as in vacuum, Maxwell's equations reduce to:
The quantity has the dimension (T/L)2. Defining , the equations above have the form of the standard wave equations
Already during Maxwell's lifetime, it was found that the known values for and give , then already known to be the speed of light
in free space. This led him to propose that light and radio waves were
propagating electromagnetic waves, since amply confirmed. In the old SI system of units, the values of and are defined constants, (which means that by definition ) that define the ampere and the metre. In the new SI system, only c keeps its defined value, and the electron charge gets a defined value.
In addition, E and B are perpendicular to each other and to the direction of wave propagation, and are in phase with each other. A sinusoidal
plane wave is one special solution of these equations. Maxwell's
equations explain how these waves can physically propagate through
space. The changing magnetic field creates a changing electric field
through Faraday's law. In turn, that electric field creates a changing magnetic field through Maxwell's modification of Ampère's circuital law. This perpetual cycle allows these waves, now known as electromagnetic radiation, to move through space at velocity c.
Macroscopic formulation in terms of displacement and magnetizing fields (in matter version)
The above equations are the microscopic version of Maxwell's
equations, expressing the electric and the magnetic fields in terms of
the (possibly atomic-level) charges and currents present. This is
sometimes called the "general" form, but the macroscopic version below
is equally general, the difference being one of bookkeeping.
The microscopic version is sometimes called "Maxwell's equations
in vacuum": this refers to the fact that the material medium is not
built into the structure of the equations, but appears only in the
charge and current terms. The microscopic version was introduced by
Lorentz, who tried to use it to derive the macroscopic properties of
bulk matter from its microscopic constituents.
"Maxwell's macroscopic equations", also known as Maxwell's equations in matter, are more similar to those that Maxwell introduced himself.
Maxwell–Faraday equation (Faraday's law of induction)
In the macroscopic equations, the influence of bound charge Qb and bound current Ib is incorporated into the displacement fieldD and the magnetizing fieldH, while the equations depend only on the free charges Qf and free currents If. This reflects a splitting of the total electric charge Q and current I (and their densities ρ and J) into free and bound parts:
The cost of this splitting is that the additional fields D and H need to be determined through phenomenological constituent equations relating these fields to the electric field E and the magnetic field B, together with the bound charge and current.
See below for a detailed description of the differences between the microscopic equations, dealing with total charge and current including material contributions, useful in air/vacuum; and the macroscopic equations, dealing with free charge and current, practical to use within materials.
Left: A schematic view of how an assembly of microscopic dipoles produces opposite surface charges as shown at top and bottom. Right:
How an assembly of microscopic current loops add together to produce a
macroscopically circulating current loop. Inside the boundaries, the
individual contributions tend to cancel, but at the boundaries no
cancelation occurs.
When an electric field is applied to a dielectric material its molecules respond by forming microscopic electric dipoles – their atomic nuclei move a tiny distance in the direction of the field, while their electrons move a tiny distance in the opposite direction. This produces a macroscopicbound charge
in the material even though all of the charges involved are bound to
individual molecules. For example, if every molecule responds the same,
similar to that shown in the figure, these tiny movements of charge
combine to produce a layer of positive bound charge
on one side of the material and a layer of negative charge on the other
side. The bound charge is most conveniently described in terms of the polarizationP of the material, its dipole moment per unit volume. If P is uniform, a macroscopic separation of charge is produced only at the surfaces where P enters and leaves the material. For non-uniform P, a charge is also produced in the bulk.
Somewhat similarly, in all materials the constituent atoms exhibit magnetic moments that are intrinsically linked to the angular momentum of the components of the atoms, most notably their electrons. The connection to angular momentum
suggests the picture of an assembly of microscopic current loops.
Outside the material, an assembly of such microscopic current loops is
not different from a macroscopic current circulating around the
material's surface, despite the fact that no individual charge is
traveling a large distance. These bound currents can be described using the magnetizationM.
The very complicated and granular bound charges and bound
currents, therefore, can be represented on the macroscopic scale in
terms of P and M,
which average these charges and currents on a sufficiently large scale
so as not to see the granularity of individual atoms, but also
sufficiently small that they vary with location in the material. As
such, Maxwell's macroscopic equations ignore many details on a
fine scale that can be unimportant to understanding matters on a gross
scale by calculating fields that are averaged over some suitable volume.
Auxiliary fields, polarization and magnetization
The definitions of the auxiliary fields are:
where P is the polarization field and M is the magnetization
field, which are defined in terms of microscopic bound charges and
bound currents respectively. The macroscopic bound charge density ρb and bound current density Jb in terms of polarizationP and magnetizationM are then defined as
If we define the total, bound, and free charge and current density by
and use the defining relations above to eliminate D, and H, the "macroscopic" Maxwell's equations reproduce the "microscopic" equations.
In order to apply 'Maxwell's macroscopic equations', it is necessary to specify the relations between displacement fieldD and the electric field E, as well as the magnetizing field H and the magnetic field B. Equivalently, we have to specify the dependence of the polarization P (hence the bound charge) and the magnetization M (hence the bound current) on the applied electric and magnetic field. The equations specifying this response are called constitutive relations.
For real-world materials, the constitutive relations are rarely simple,
except approximately, and usually determined by experiment. See the
main article on constitutive relations for a fuller description.
For materials without polarization and magnetization, the constitutive relations are (by definition)
where ε0 is the permittivity of free space and μ0 the permeability of free space. Since there is no bound charge, the total and the free charge and current are equal.
An alternative viewpoint on the microscopic equations is that they are the macroscopic equations together with the statement that vacuum behaves like a perfect linear "material" without additional polarization and magnetization.
More generally, for linear materials the constitutive relations are
where ε is the permittivity and μ the permeability of the material. For the displacement field D
the linear approximation is usually excellent because for all but the
most extreme electric fields or temperatures obtainable in the
laboratory (high power pulsed lasers) the interatomic electric fields of
materials of the order of 1011 V/m are much higher than the external field. For the magnetizing field , however, the linear approximation can break down in common materials like iron leading to phenomena like hysteresis. Even the linear case can have various complications, however.
For homogeneous materials, ε and μ are constant throughout the material, while for inhomogeneous materials they depend on location within the material (and perhaps time).
For isotropic materials, ε and μ are scalars, while for anisotropic materials (e.g. due to crystal structure) they are tensors.
Materials are generally dispersive, so ε and μ depend on the frequency of any incident EM waves.
Even more generally, in the case of non-linear materials (see for example nonlinear optics), D and P are not necessarily proportional to E, similarly H or M is not necessarily proportional to B. In general D and H depend on both E and B, on location and time, and possibly other physical quantities.
In applications one also has to describe how the free currents and charge density behave in terms of E and B
possibly coupled to other physical quantities like pressure, and the
mass, number density, and velocity of charge-carrying particles. E.g.,
the original equations given by Maxwell (see History of Maxwell's equations) included Ohm's law in the form
Following are some of the several other mathematical formalisms of
Maxwell's equations, with the columns separating the two homogeneous
Maxwell equations from the two inhomogeneous ones. Each formulation has
versions directly in terms of the electric and magnetic fields, and
indirectly in terms of the electrical potentialφ and the vector potentialA.
Potentials were introduced as a convenient way to solve the homogeneous
equations, but it was thought that all observable physics was contained
in the electric and magnetic fields (or relativistically, the Faraday
tensor). The potentials play a central role in quantum mechanics,
however, and act quantum mechanically with observable consequences even
when the electric and magnetic fields vanish (Aharonov–Bohm effect).
Each table describes one formalism. See the main article for details of each formulation.
The direct spacetime formulations make manifest that the Maxwell equations are relativistically invariant,
where space and time are treated on equal footing. Because of this
symmetry, the electric and magnetic fields are treated on equal footing
and are recognized as components of the Faraday tensor.
This reduces the four Maxwell equations to two, which simplifies the
equations, although we can no longer use the familiar vector
formulation. Maxwell equations in formulation that do not treat space
and time manifestly on the same footing have Lorentz invariance as a
hidden symmetry. This was a major source of inspiration for the
development of relativity theory. Indeed, even the formulation that
treats space and time separately is not a non-relativistic approximation
and describes the same physics by simply renaming variables. For this
reason the relativistic invariant equations are usually called the
Maxwell equations as well.
Potentials (any gauge) any spacetime (with topological restrictions)
Potentials (Lorenz gauge) any spacetime (with topological restrictions)
In the tensor calculus formulation, the electromagnetic tensorFαβ is an antisymmetric covariant order 2 tensor; the four-potential, Aα, is a covariant vector; the current, Jα, is a vector; the square brackets, [ ], denote antisymmetrization of indices; ∂α is the partial derivative with respect to the coordinate, xα. In Minkowski space coordinates are chosen with respect to an inertial frame; (xα) = (ct, x, y, z), so that the metric tensor used to raise and lower indices is ηαβ = diag(1, −1, −1, −1). The d'Alembert operator on Minkowski space is ◻ = ∂α∂α as in the vector formulation. In general spacetimes, the coordinate system xα is arbitrary, the covariant derivative∇α, the Ricci tensor, Rαβ and raising and lowering of indices are defined by the Lorentzian metric, gαβ and the d'Alembert operator is defined as ◻ = ∇α∇α. The topological restriction is that the second real cohomology
group of the space vanishes (see the differential form formulation for
an explanation). This is violated for Minkowski space with a line
removed, which can model a (flat) spacetime with a point-like monopole
on the complement of the line.
In the differential form formulation on arbitrary space times, F = 1/2Fαβdxα ∧ dxβ is the electromagnetic tensor considered as a 2-form, A = Aαdxα is the potential 1-form, is the current 3-form, d is the exterior derivative, and is the Hodge star
on forms defined (up to its orientation, i.e. its sign) by the
Lorentzian metric of spacetime. In the special case of 2-forms such as F, the Hodge star
depends on the metric tensor only for its local scale. This means that,
as formulated, the differential form field equations are conformally invariant, but the Lorenz gauge condition breaks conformal invariance. The operator is the d'Alembert–Laplace–Beltrami operator on 1-forms on an arbitrary Lorentzian spacetime.
The topological condition is again that the second real cohomology
group is 'trivial' (meaning that its form follows from a definition). By
the isomorphism with the second de Rham cohomology this condition means that every closed 2-form is exact.
Maxwell's equations are partial differential equations
that relate the electric and magnetic fields to each other and to the
electric charges and currents. Often, the charges and currents are
themselves dependent on the electric and magnetic fields via the Lorentz force equation and the constitutive relations.
These all form a set of coupled partial differential equations which
are often very difficult to solve: the solutions encompass all the
diverse phenomena of classical electromagnetism. Some general remarks follow.
As for any differential equation, boundary conditions and initial conditions are necessary for a unique solution. For example, even with no charges and no currents anywhere in spacetime, there are the obvious solutions for which E and B
are zero or constant, but there are also non-trivial solutions
corresponding to electromagnetic waves. In some cases, Maxwell's
equations are solved over the whole of space, and boundary conditions
are given as asymptotic limits at infinity. In other cases, Maxwell's equations are solved in a finite region of
space, with appropriate conditions on the boundary of that region, for
example an artificial absorbing boundary representing the rest of the universe, or periodic boundary conditions, or walls that isolate a small region from the outside world (as with a waveguide or cavity resonator).
Jefimenko's equations and Panofsky-Phillips equations (or the closely related Liénard–Wiechert potentials)
are the explicit solution to Maxwell's equations for the electric and
magnetic fields created by any given distribution of charges and
currents. It assumes specific initial conditions to obtain the so-called
"retarded solution", where the only fields present are the ones created
by the charges. However, Jefimenko's equations are unhelpful in
situations when the charges and currents are themselves affected by the
fields they create.
Maxwell's equations seemoverdetermined, in that they involve six unknowns (the three components of E and B)
but eight equations (one for each of the two Gauss's laws, three vector
components each for Faraday's and Ampère's circuital laws). (The
currents and charges are not unknowns, being freely specifiable subject
to charge conservation.)
This is related to a certain limited kind of redundancy in Maxwell's
equations: It can be proven that any system satisfying Faraday's law and
Ampère's circuital law automatically also satisfies the two
Gauss's laws, as long as the system's initial condition does, and
assuming conservation of charge and the nonexistence of magnetic
monopoles. This explanation was first introduced by Julius Adams Stratton in 1941.
Although it is possible to simply ignore the two Gauss's laws in a
numerical algorithm (apart from the initial conditions), the imperfect
precision of the calculations can lead to ever-increasing violations of
those laws. By introducing dummy variables characterizing these
violations, the four equations become not overdetermined after all. The
resulting formulation can lead to more accurate algorithms that take all
four laws into account.
Both identities , which reduce eight equations to six independent ones, are the true reason of overdetermination.
Equivalently, the overdetermination can be viewed as implying
conservation of electric and magnetic charge, as they are required in
the derivation described above but implied by the two Gauss's laws.
For linear algebraic equations, one can make 'nice' rules to
rewrite the equations and unknowns. The equations can be linearly
dependent. But in differential equations, and especially partial
differential equations (PDEs), one needs appropriate boundary
conditions, which depend in not so obvious ways on the equations. Even
more, if one rewrites them in terms of vector and scalar potential, then
the equations are underdetermined because of gauge fixing.
Maxwell's equations as the classical limit of QED
Maxwell's equations and the Lorentz force law (along with the rest of
classical electromagnetism) are extraordinarily successful at
explaining and predicting a variety of phenomena. However, they do not
account for quantum effects, and so their domain of applicability is
limited. Maxwell's equations are thought of as the classical limit of quantum electrodynamics (QED).
Some observed electromagnetic phenomena cannot be explained with
Maxwell's equations if the source of the electromagnetic fields are the
classical distributions of charge and current. These include photon–photon scattering and many other phenomena related to photons or virtual photons, "nonclassical light" and quantum entanglement of electromagnetic fields (see Quantum optics). E.g. quantum cryptography
cannot be described by Maxwell theory, not even approximately. The
approximate nature of Maxwell's equations becomes more and more apparent
when going into the extremely strong field regime (see Euler–Heisenberg Lagrangian) or to extremely small distances.
Finally, Maxwell's equations cannot explain any phenomenon involving individual photons interacting with quantum matter, such as the photoelectric effect, Planck's law, the Duane–Hunt law, and single-photon light detectors.
However, many such phenomena may be explained using a halfway theory of
quantum matter coupled to a classical electromagnetic field, either as
external field or with the expected value of the charge current and
density on the right hand side of Maxwell's equations. This is known as
semiclassical theory or self-field QED and was initially discovered by
de Broglie and Schrödinger and later fully developed by E.T. Jaynes and
A.O. Barut.
Variations
Popular variations on the Maxwell equations as a classical theory of
electromagnetic fields are relatively scarce because the standard
equations have stood the test of time remarkably well.
Maxwell's equations posit that there is electric charge, but no magnetic charge (also called magnetic monopoles), in the universe. Indeed, magnetic charge has never been observed, despite extensive searches, and may not exist. If they did exist, both Gauss's law for magnetism
and Faraday's law would need to be modified, and the resulting four
equations would be fully symmetric under the interchange of electric and
magnetic fields.