|Part of a series on|
A continuity equation in physics is an equation that describes the transport of some quantity. It is particularly simple and powerful when applied to a conserved quantity, but it can be generalized to apply to any extensive quantity. Since mass, energy, momentum, electric charge and other natural quantities are conserved under their respective appropriate conditions, a variety of physical phenomena may be described using continuity equations.
Continuity equations are a stronger, local form of conservation laws. For example, a weak version of the law of conservation of energy states that energy can neither be created nor destroyed—i.e., the total amount of energy in the universe is fixed. This statement does not rule out the possibility that a quantity of energy could disappear from one point while simultaneously appearing at another point. A stronger statement is that energy is locally conserved: energy can neither be created nor destroyed, nor can it "teleport" from one place to another—it can only move by a continuous flow. A continuity equation is the mathematical way to express this kind of statement. For example, the continuity equation for electric charge states that the amount of electric charge in any volume of space can only change by the amount of electric current flowing into or out of that volume through its boundaries.
Continuity equations more generally can include "source" and "sink" terms, which allow them to describe quantities that are often but not always conserved, such as the density of a molecular species which can be created or destroyed by chemical reactions. In an everyday example, there is a continuity equation for the number of people alive; it has a "source term" to account for people being born, and a "sink term" to account for people dying.
Any continuity equation can be expressed in an "integral form" (in terms of a flux integral), which applies to any finite region, or in a "differential form" (in terms of the divergence operator) which applies at a point.
Flows governed by continuity equations can be visualized using a Sankey diagram.
Definition of flux
A continuity equation is useful when a flux can be defined. To define flux, first there must be a quantity q which can flow or move, such as mass, energy, electric charge, momentum, number of molecules, etc. Let ρ be the volume density of this quantity, that is, the amount of q per unit volume.
The way that this quantity q is flowing is described by its flux. The flux of q is a vector field, which we denote as j. Here are some examples and properties of flux:
- The dimension of flux is "amount of q flowing per unit time, through a unit area". For example, in the mass continuity equation for flowing water, if 1 gram per second of water is flowing through a pipe with cross-sectional area 1 cm2, then the average mass flux j inside the pipe is (1 gram / second) / cm2, and its direction is along the pipe in the direction that the water is flowing. Outside the pipe, where there is no water, the flux is zero.
- If there is a velocity field u which describes the relevant flow—in other words, if all of the quantity q at a point x is moving with velocity u(x)—then the flux is by definition equal to the density times the velocity field:
- For example, if in the mass continuity equation for flowing water, u is the water's velocity at each point, and ρ is the water's density at each point, then j would be the mass flux.
- If there is an imaginary surface S, then the surface integral of flux over S is equal to the amount of q that is passing through the surface S per unit time:
- in which ∬S dS is a surface integral.
(Note that the concept that is here called "flux" is alternatively termed "flux density" in some literature, in which context "flux" denotes the surface integral of flux density. See the main article on Flux for details.)
The integral form of the continuity equation states that:
- The amount of q in a region increases when additional q flows inward through the surface of the region, and decreases when it flows outward;
- The amount of q in a region increases when new q is created inside the region, and decreases when q is destroyed;
- Apart from these two processes, there is no other way for the amount of q in a region to change.
Mathematically, the integral form of the continuity equation expressing the rate of increase of q within a volume V is:
- S is any imaginary closed surface, that encloses a volume V,
- S dS denotes a surface integral over that closed surface,
- q is the total amount of the quantity in the volume V,
- j is the flux of q,
- t is time,
- Σ is the net rate that q is being generated inside the volume V per unit time. When q is being generated, it is called a source of q, and it makes Σ more positive. When q is being destroyed, it is called a sink of q, and it makes Σ more negative. This term is sometimes written as or the total change of q from its generation or destruction inside the control volume.
In a simple example, V could be a building, and q could be the number of people in the building. The surface S would consist of the walls, doors, roof, and foundation of the building. Then the continuity equation states that the number of people in the building increases when people enter the building (an inward flux through the surface), decreases when people exit the building (an outward flux through the surface), increases when someone in the building gives birth (a source, Σ > 0), and decreases when someone in the building dies (a sink, Σ < 0).
By the divergence theorem, a general continuity equation can also be written in a "differential form":
- ∇⋅ is divergence,
- ρ is the amount of the quantity q per unit volume,
- j is the flux of q,
- t is time,
- σ is the generation of q per unit volume per unit time. Terms that generate q (i.e. σ > 0) or remove q (i.e. σ < 0) are referred to as a "sources" and "sinks" respectively.
This general equation may be used to derive any continuity equation, ranging from as simple as the volume continuity equation to as complicated as the Navier–Stokes equations. This equation also generalizes the advection equation. Other equations in physics, such as Gauss's law of the electric field and Gauss's law for gravity, have a similar mathematical form to the continuity equation, but are not usually referred to by the term "continuity equation", because j in those cases does not represent the flow of a real physical quantity.
In electromagnetic theory, the continuity equation is an empirical law expressing (local) charge conservation. Mathematically it is an automatic consequence of Maxwell's equations, although charge conservation is more fundamental than Maxwell's equations. It states that the divergence of the current density J (in amperes per square metre) is equal to the negative rate of change of the charge density ρ (in coulombs per cubic metre),
Consistency with Maxwell's equations
Taking the divergence of both sides (the divergence and partial derivative in time commute) results in
but the divergence of a curl is zero, so that
But Gauss's law (another Maxwell equation), states that
which can be substituted in the previous equation to yield the continuity equation
Current is the movement of charge. The continuity equation says that if charge is moving out of a differential volume (i.e. divergence of current density is positive) then the amount of charge within that volume is going to decrease, so the rate of change of charge density is negative. Therefore, the continuity equation amounts to a conservation of charge.
If magnetic monopoles exist, there would be a continuity equation for monopole currents as well, see the monopole article for background and the duality between electric and magnetic currents.
In fluid dynamics, the continuity equation states that the rate at which mass enters a system is equal to the rate at which mass leaves the system plus the accumulation of mass within the system. The differential form of the continuity equation is:
The time derivative can be understood as the accumulation (or loss) of mass in the system, while the divergence term represents the difference in flow in versus flow out. In this context, this equation is also one of the Euler equations (fluid dynamics). The Navier–Stokes equations form a vector continuity equation describing the conservation of linear momentum.
If the fluid is incompressible (volumetric strain rate is zero), the mass continuity equation simplifies to a volume continuity equation:
which means that the divergence of the velocity field is zero everywhere. Physically, this is equivalent to saying that the local volume dilation rate is zero, hence a flow of water through a converging pipe will adjust solely by increasing its velocity as water is largely incompressible.
Energy and heat
- u, local energy density (energy per unit volume),
- q, energy flux (transfer of energy per unit cross-sectional area per unit time) as a vector,
An important practical example is the flow of heat. When heat flows inside a solid, the continuity equation can be combined with Fourier's law (heat flux is proportional to temperature gradient) to arrive at the heat equation. The equation of heat flow may also have source terms: Although energy cannot be created or destroyed, heat can be created from other types of energy, for example via friction or joule heating.
If there is a quantity that moves continuously according to a stochastic (random) process, like the location of a single dissolved molecule with Brownian motion, then there is a continuity equation for its probability distribution. The flux in this case is the probability per unit area per unit time that the particle passes through a surface. According to the continuity equation, the negative divergence of this flux equals the rate of change of the probability density. The continuity equation reflects the fact that the molecule is always somewhere—the integral of its probability distribution is always equal to 1—and that it moves by a continuous motion (no teleporting).
Quantum mechanics is another domain where there is a continuity equation related to conservation of probability. The terms in the equation require the following definitions, and are slightly less obvious than the other examples above, so they are outlined here:
- The wavefunction Ψ for a single particle in position space (rather than momentum space), that is, a function of position r and time t, Ψ = Ψ(r, t).
- The probability density function is
- The probability of finding the particle within V at t is denoted and defined by
- The probability current (aka probability flux) is
With these definitions the continuity equation reads:
Either form may be quoted. Intuitively, the above quantities indicate this represents the flow of probability. The chance of finding the particle at some position r and time t flows like a fluid; hence the term probability current, a vector field. The particle itself does not flow deterministically in this vector field.
Consistency with Schrödinger equation The 3-d time dependent Schrödinger equation and its complex conjugate (i → −i throughout) are respectively:
Multiplying the Schrödinger equation by Ψ* then solving for Ψ* ∂Ψ/, and similarly multiplying the complex conjugated Schrödinger equation by Ψ then solving for Ψ ∂Ψ*/;
substituting into the time derivative of ρ:
so the continuity equation is:
The integral form follows as for the general equation.
in the usual case where there are no sources or sinks, that is, for perfectly conserved quantities like energy or charge. This continuity equation is manifestly ("obviously") Lorentz invariant.
Examples of continuity equations often written in this form include electric charge conservation
where J is the electric 4-current; and energy–momentum conservation
where T is the stress–energy tensor.
In general relativity, where spacetime is curved, the continuity equation (in differential form) for energy, charge, or other conserved quantities involves the covariant divergence instead of the ordinary divergence.
For example, the stress–energy tensor is a second-order tensor field containing energy–momentum densities, energy–momentum fluxes, and shear stresses, of a mass-energy distribution. The differential form of energy–momentum conservation in general relativity states that the covariant divergence of the tress-energy tensor is zero:
The right-hand side strictly vanishes for a flat geometry only.
As a consequence, the integral form of the continuity equation is difficult to define and not necessarily valid for a region within which spacetime is significantly curved (e.g. around a black hole, or across the whole universe).
Quarks and gluons have color charge, which is always conserved like electric charge, and there is a continuity equation for such color charge currents (explicit expressions for currents are given at gluon field strength tensor).
There are many other quantities in particle physics which are often or always conserved: baryon number (proportional to the number of quarks minus the number of antiquarks), electron number, mu number, tau number, isospin, and others. Each of these has a corresponding continuity equation, possibly including source / sink terms.
One reason that conservation equations frequently occur in physics is Noether's theorem. This states that whenever the laws of physics have a continuous symmetry, there is a continuity equation for some conserved physical quantity. The three most famous examples are:
- The laws of physics are invariant with respect to time-translation—for example, the laws of physics today are the same as they were yesterday. This symmetry leads to the continuity equation for conservation of energy.
- The laws of physics are invariant with respect to space-translation—for example, the laws of physics in Brazil are the same as the laws of physics in Argentina. This symmetry leads to the continuity equation for conservation of momentum.
- The laws of physics are invariant with respect to orientation—for example, floating in outer space, there is no measurement you can do to say "which way is up"; the laws of physics are the same regardless of how you are oriented. This symmetry leads to the continuity equation for conservation of angular momentum.
See Noether's theorem for proofs and details.
- Pedlosky, Joseph (1987). Geophysical fluid dynamics. Springer. pp. 10–13. ISBN 978-0-387-96387-7.
- Clancy, L.J.(1975), Aerodynamics, Section 3.3, Pitman Publishing Limited, London
- Fielding, Suzanne. "The Basics of Fluid Dynamics" (PDF). Durham University. Retrieved 22 December 2019.
- For this derivation see for example McMahon, D. (2006). Quantum Mechanics Demystified. McGraw Hill. ISBN 0-07-145546-9.
- D. McMahon (2006). Relativity DeMystified. McGraw Hill (USA). ISBN 0-07-145545-0.
- C.W. Misner; K.S. Thorne; J.A. Wheeler (1973). Gravitation. W.H. Freeman & Co. ISBN 0-7167-0344-0.
- Michael Weiss; John Baez. "Is Energy Conserved in General Relativity?". Retrieved 2014-04-25.
- J.A. Wheeler; C. Misner; K.S. Thorne (1973). Gravitation. W.H. Freeman & Co. pp. 558–559. ISBN 0-7167-0344-0.
- Hydrodynamics, H. Lamb, Cambridge University Press, (2006 digitalization of 1932 6th edition) ISBN 978-0-521-45868-9
- Introduction to Electrodynamics (3rd Edition), D.J. Griffiths, Pearson Education Inc, 1999, ISBN 81-7758-293-3
- Electromagnetism (2nd edition), I.S. Grant, W.R. Phillips, Manchester Physics Series, 2008 ISBN 0-471-92712-0
- Gravitation, J.A. Wheeler, C. Misner, K.S. Thorne, W.H. Freeman & Co, 1973, ISBN 0-7167-0344-0