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A second-order partial differential equation describing the process of diffusion, i.e. the process of equalization of the concentration in a medium with an initially non-homogeneous distribution of some substance. The diffusion equation has the form
 
A second-order partial differential equation describing the process of diffusion, i.e. the process of equalization of the concentration in a medium with an initially non-homogeneous distribution of some substance. The diffusion equation has the form
  
<table class="eq" style="width:100%;"> <tr><td valign="top" style="width:94%;text-align:center;"><img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323601.png" /></td> <td valign="top" style="width:5%;text-align:right;">(1)</td></tr></table>
+
$$ \tag{1 }
 +
L u  \equiv  c
 +
\frac{\partial  u }{\partial  t }
 +
- \mathop{\rm div} ( D \
 +
\mathop{\rm grad}  u )  = 0 ,
 +
$$
  
where <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323602.png" /> is the porosity coefficient, <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323603.png" /> is the diffusion coefficient and <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323604.png" /> is the concentration of the substance at a point <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323605.png" /> of the medium at the moment of time <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323606.png" />. The diffusion equation is derived by making up the balance of the substance using Nerst's diffusion law. It is assumed in so doing that sources of the substance and diffusion into an external medium are absent in the domain under consideration. Such a diffusion equation is said to be homogeneous. If the domain under consideration contains sources of the substance with a volume distribution density <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323607.png" />, the diffusion process is said to be inhomogeneous with right-hand side <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323608.png" />. If the substance falls apart or multiplies at a rate proportional to the initial concentration, a term <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d0323609.png" /> should be inserted in the right-hand side of the diffusion equation.
+
where $  c $
 +
is the porosity coefficient, $  D $
 +
is the diffusion coefficient and $  u ( x , t ) $
 +
is the concentration of the substance at a point $  x $
 +
of the medium at the moment of time $  t $.  
 +
The diffusion equation is derived by making up the balance of the substance using Nerst's diffusion law. It is assumed in so doing that sources of the substance and diffusion into an external medium are absent in the domain under consideration. Such a diffusion equation is said to be homogeneous. If the domain under consideration contains sources of the substance with a volume distribution density $  F ( x , t ) $,  
 +
the diffusion process is said to be inhomogeneous with right-hand side $  F ( x , t ) $.  
 +
If the substance falls apart or multiplies at a rate proportional to the initial concentration, a term $  \pm  {\lambda \partial  u } / {\partial  x } $
 +
should be inserted in the right-hand side of the diffusion equation.
  
The diffusion equation is of parabolic type. In order to find a unique solution, initial and boundary conditions are imposed. The initial condition for a diffusion equation is to specify the concentration <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236010.png" /> of the substance at the initial moment of time:
+
The diffusion equation is of parabolic type. In order to find a unique solution, initial and boundary conditions are imposed. The initial condition for a diffusion equation is to specify the concentration $  u _ {0} ( x) $
 +
of the substance at the initial moment of time:
  
<table class="eq" style="width:100%;"> <tr><td valign="top" style="width:94%;text-align:center;"><img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236011.png" /></td> <td valign="top" style="width:5%;text-align:right;">(2)</td></tr></table>
+
$$ \tag{2 }
 +
u ( x , 0 )  = u _ {0} ( x) .
 +
$$
  
If the substance then fills the entire space, one obtains the [[Cauchy problem|Cauchy problem]] (1), (2). If, on the other hand, the diffusion substance occupies a volume <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236012.png" /> bounded by the side surface <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236013.png" />, as well as the initial condition (2), a boundary condition is imposed on <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236014.png" />. The three fundamental linear boundary conditions for a diffusion equation are listed below.
+
If the substance then fills the entire space, one obtains the [[Cauchy problem|Cauchy problem]] (1), (2). If, on the other hand, the diffusion substance occupies a volume $  V $
 +
bounded by the side surface $  S $,  
 +
as well as the initial condition (2), a boundary condition is imposed on $  S $.  
 +
The three fundamental linear boundary conditions for a diffusion equation are listed below.
  
1) The concentration of the substance <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236015.png" /> is specified on <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236016.png" />; then
+
1) The concentration of the substance $  \theta ( x , t ) $
 +
is specified on $  S $;  
 +
then
  
<table class="eq" style="width:100%;"> <tr><td valign="top" style="width:94%;text-align:center;"><img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236017.png" /></td> </tr></table>
+
$$
 +
u ( x , t )  = \theta ( x , t )
 +
$$
  
 
is a boundary condition of the first kind.
 
is a boundary condition of the first kind.
  
2) The density <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236018.png" /> of the flow of the substance entering <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236019.png" /> through <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236020.png" /> is given; then
+
2) The density $  q ( x , t ) $
 +
of the flow of the substance entering $  V $
 +
through $  S $
 +
is given; then
  
<table class="eq" style="width:100%;"> <tr><td valign="top" style="width:94%;text-align:center;"><img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236021.png" /></td> </tr></table>
+
$$
 +
- D
 +
\frac{\partial  u ( x , t ) }{\partial  n }
 +
  = q ( x , t ) ,\ \
 +
x \in S ,
 +
$$
  
where <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236022.png" /> is the interior normal to the surface <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236023.png" />, is a boundary condition of the second kind (if <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236024.png" /> is impermeable, <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236025.png" />).
+
where $  n $
 +
is the interior normal to the surface $  S $,  
 +
is a boundary condition of the second kind (if $  S $
 +
is impermeable, $  q ( x , t ) \equiv 0 $).
  
3) If <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236026.png" /> is semi-permeable, and if the diffusion taking place into the external medium with a given concentration <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236027.png" /> through <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236028.png" /> is linear, then
+
3) If $  S $
 +
is semi-permeable, and if the diffusion taking place into the external medium with a given concentration $  \theta ( x , t ) $
 +
through $  S $
 +
is linear, then
  
<table class="eq" style="width:100%;"> <tr><td valign="top" style="width:94%;text-align:center;"><img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236029.png" /></td> </tr></table>
+
$$
 +
 
 +
\frac{\partial  u ( x , t ) }{\partial  n }
 +
  = - h ( u ( x , t ) - \theta
 +
( x , t ) ) ,\  x \in S ,
 +
$$
  
 
is a boundary condition of the third kind.
 
is a boundary condition of the third kind.
  
Other boundary conditions, including non-linear ones, may also be imposed on <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236030.png" />, as well as conditions involving derivatives of a higher order than those which appear in the diffusion equation. Since a diffusion equation is a special case of a differential equation describing physical equalization processes, it is analogous to the [[Thermal-conductance equation|thermal-conductance equation]], the [[Navier–Stokes equations|Navier–Stokes equations]] for the laminar flow of an incompressible liquid, the equation of pure electric conductance, etc.
+
Other boundary conditions, including non-linear ones, may also be imposed on $  S $,  
 +
as well as conditions involving derivatives of a higher order than those which appear in the diffusion equation. Since a diffusion equation is a special case of a differential equation describing physical equalization processes, it is analogous to the [[Thermal-conductance equation|thermal-conductance equation]], the [[Navier–Stokes equations|Navier–Stokes equations]] for the laminar flow of an incompressible liquid, the equation of pure electric conductance, etc.
  
 
====References====
 
====References====
<table><TR><TD valign="top">[1]</TD> <TD valign="top">  A.N. [A.N. Tikhonov] Tichonoff,  A.A. Samarskii,  "Differentialgleichungen der mathematischen Physik" , Deutsch. Verlag Wissenschaft.  (1959)  (Translated from Russian)</TD></TR></table>
+
<table><TR><TD valign="top">[1]</TD> <TD valign="top">  A.N. [A.N. Tikhonov] Tichonoff,  A.A. Samarskii,  "Differentialgleichungen der mathematischen Physik" , Deutsch. Verlag Wissenschaft.  (1959)  (Translated from Russian) {{MR|104888}} {{ZBL|}} </TD></TR></table>
 
 
 
 
  
 
====Comments====
 
====Comments====
Line 41: Line 94:
 
Another notation for the diffusion equation is
 
Another notation for the diffusion equation is
  
<table class="eq" style="width:100%;"> <tr><td valign="top" style="width:94%;text-align:center;"><img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236031.png" /></td> </tr></table>
+
$$
  
(where, of course, <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236032.png" /> and <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236033.png" /> is another notation for <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236034.png" />).
+
\frac{\partial  u }{\partial  t }
 +
- \nabla _ {\bullet }  ( D \nabla u )  =  0
 +
$$
 +
 
 +
(where, of course, $  \nabla u = \mathop{\rm grad} ( u) = ( \partial  u / {\partial  x _ {1} } \dots \partial  u / {\partial  x _ {n} } ) $
 +
and $  \nabla _ {\bullet }  $
 +
is another notation for $  \mathop{\rm div} $).
  
 
The non-linear equation (in one space variable)
 
The non-linear equation (in one space variable)
  
<table class="eq" style="width:100%;"> <tr><td valign="top" style="width:94%;text-align:center;"><img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236035.png" /></td> </tr></table>
+
$$
 +
 
 +
\frac{\partial  u }{\partial  t }
 +
+ u
 +
 
 +
\frac{\partial  u }{\partial  x }
 +
  = D
 +
 
 +
\frac{\partial  ^ {2} u }{\partial  x  ^ {2} }
 +
,
 +
$$
  
where <img align="absmiddle" border="0" src="https://www.encyclopediaofmath.org/legacyimages/d/d032/d032360/d03236036.png" /> is a constant, is referred to as the one-dimensional non-linear diffusion equation or the Burgers equation. The monograph [[#References|[a3]]] is devoted to this equation.
+
where $  D $
 +
is a constant, is referred to as the one-dimensional non-linear diffusion equation or the Burgers equation. The monograph [[#References|[a3]]] is devoted to this equation.
  
 
====References====
 
====References====
<table><TR><TD valign="top">[a1]</TD> <TD valign="top">  J. Crank,  "The mathematics of diffusion" , Clarendon Press  (1956)</TD></TR><TR><TD valign="top">[a2]</TD> <TD valign="top">  H.S. Carslaw,  J.C. Jaeger,  "Conduction of heat in solids" , Clarendon Press  (1959)</TD></TR><TR><TD valign="top">[a3]</TD> <TD valign="top">  J.M. Burgers,  "The nonlinear diffusion equation" , Reidel  (1974)</TD></TR></table>
+
<table><TR><TD valign="top">[a1]</TD> <TD valign="top">  J. Crank,  "The mathematics of diffusion" , Clarendon Press  (1956) {{MR|0082827}} {{ZBL|0071.41401}} </TD></TR><TR><TD valign="top">[a2]</TD> <TD valign="top">  H.S. Carslaw,  J.C. Jaeger,  "Conduction of heat in solids" , Clarendon Press  (1959) {{MR|0959730}} {{MR|0022294}} {{MR|0015635}} {{MR|1520543}} {{ZBL|0972.80500}} {{ZBL|0584.73001}} {{ZBL|0095.30201}} {{ZBL|0029.37801}} {{ZBL|0063.00722}}  {{ZBL|48.0573.09}} </TD></TR><TR><TD valign="top">[a3]</TD> <TD valign="top">  J.M. Burgers,  "The nonlinear diffusion equation" , Reidel  (1974) {{MR|}} {{ZBL|0302.60048}} </TD></TR></table>

Latest revision as of 11:53, 12 January 2021


A second-order partial differential equation describing the process of diffusion, i.e. the process of equalization of the concentration in a medium with an initially non-homogeneous distribution of some substance. The diffusion equation has the form

$$ \tag{1 } L u \equiv c \frac{\partial u }{\partial t } - \mathop{\rm div} ( D \ \mathop{\rm grad} u ) = 0 , $$

where $ c $ is the porosity coefficient, $ D $ is the diffusion coefficient and $ u ( x , t ) $ is the concentration of the substance at a point $ x $ of the medium at the moment of time $ t $. The diffusion equation is derived by making up the balance of the substance using Nerst's diffusion law. It is assumed in so doing that sources of the substance and diffusion into an external medium are absent in the domain under consideration. Such a diffusion equation is said to be homogeneous. If the domain under consideration contains sources of the substance with a volume distribution density $ F ( x , t ) $, the diffusion process is said to be inhomogeneous with right-hand side $ F ( x , t ) $. If the substance falls apart or multiplies at a rate proportional to the initial concentration, a term $ \pm {\lambda \partial u } / {\partial x } $ should be inserted in the right-hand side of the diffusion equation.

The diffusion equation is of parabolic type. In order to find a unique solution, initial and boundary conditions are imposed. The initial condition for a diffusion equation is to specify the concentration $ u _ {0} ( x) $ of the substance at the initial moment of time:

$$ \tag{2 } u ( x , 0 ) = u _ {0} ( x) . $$

If the substance then fills the entire space, one obtains the Cauchy problem (1), (2). If, on the other hand, the diffusion substance occupies a volume $ V $ bounded by the side surface $ S $, as well as the initial condition (2), a boundary condition is imposed on $ S $. The three fundamental linear boundary conditions for a diffusion equation are listed below.

1) The concentration of the substance $ \theta ( x , t ) $ is specified on $ S $; then

$$ u ( x , t ) = \theta ( x , t ) $$

is a boundary condition of the first kind.

2) The density $ q ( x , t ) $ of the flow of the substance entering $ V $ through $ S $ is given; then

$$ - D \frac{\partial u ( x , t ) }{\partial n } = q ( x , t ) ,\ \ x \in S , $$

where $ n $ is the interior normal to the surface $ S $, is a boundary condition of the second kind (if $ S $ is impermeable, $ q ( x , t ) \equiv 0 $).

3) If $ S $ is semi-permeable, and if the diffusion taking place into the external medium with a given concentration $ \theta ( x , t ) $ through $ S $ is linear, then

$$ \frac{\partial u ( x , t ) }{\partial n } = - h ( u ( x , t ) - \theta ( x , t ) ) ,\ x \in S , $$

is a boundary condition of the third kind.

Other boundary conditions, including non-linear ones, may also be imposed on $ S $, as well as conditions involving derivatives of a higher order than those which appear in the diffusion equation. Since a diffusion equation is a special case of a differential equation describing physical equalization processes, it is analogous to the thermal-conductance equation, the Navier–Stokes equations for the laminar flow of an incompressible liquid, the equation of pure electric conductance, etc.

References

[1] A.N. [A.N. Tikhonov] Tichonoff, A.A. Samarskii, "Differentialgleichungen der mathematischen Physik" , Deutsch. Verlag Wissenschaft. (1959) (Translated from Russian) MR104888

Comments

For the role of diffusion equations in the theory of stochastic processes see Diffusion process.

Another notation for the diffusion equation is

$$ \frac{\partial u }{\partial t } - \nabla _ {\bullet } ( D \nabla u ) = 0 $$

(where, of course, $ \nabla u = \mathop{\rm grad} ( u) = ( \partial u / {\partial x _ {1} } \dots \partial u / {\partial x _ {n} } ) $ and $ \nabla _ {\bullet } $ is another notation for $ \mathop{\rm div} $).

The non-linear equation (in one space variable)

$$ \frac{\partial u }{\partial t } + u \frac{\partial u }{\partial x } = D \frac{\partial ^ {2} u }{\partial x ^ {2} } , $$

where $ D $ is a constant, is referred to as the one-dimensional non-linear diffusion equation or the Burgers equation. The monograph [a3] is devoted to this equation.

References

[a1] J. Crank, "The mathematics of diffusion" , Clarendon Press (1956) MR0082827 Zbl 0071.41401
[a2] H.S. Carslaw, J.C. Jaeger, "Conduction of heat in solids" , Clarendon Press (1959) MR0959730 MR0022294 MR0015635 MR1520543 Zbl 0972.80500 Zbl 0584.73001 Zbl 0095.30201 Zbl 0029.37801 Zbl 0063.00722 Zbl 48.0573.09
[a3] J.M. Burgers, "The nonlinear diffusion equation" , Reidel (1974) Zbl 0302.60048
How to Cite This Entry:
Diffusion equation. Encyclopedia of Mathematics. URL: http://encyclopediaofmath.org/index.php?title=Diffusion_equation&oldid=17166
This article was adapted from an original article by L.I. Kamynin (originator), which appeared in Encyclopedia of Mathematics - ISBN 1402006098. See original article