In fluid dynamics, Erdogan–Chatwin equation is a nonlinear diffusion equation for the scalar field, that accounts for shear-induced dispersion due to horizontal buoyancy forces. The equation was named after M. Emin Erdogan and Phillip C. Chatwin, who derived the equation in 1967.[1][2][3][4] The equation for the scalar field
reads[5]
![{\displaystyle {\frac {\partial c}{\partial t}}={\frac {\partial }{\partial x}}\left\{D\left[1+{\frac {\gamma g^{2}h^{8}\alpha ^{2}}{\nu ^{2}D^{2}}}\left({\frac {\partial c}{\partial x}}\right)^{2}\right]{\frac {\partial c}{\partial x}}\right\},}](//wikimedia.org/api/rest_v1/media/math/render/svg/98fb134cb83d2131d880697473a98177d5cd405d)
where
 | is the diffusion coefficient for the scalar ; |
 | is a numerical factor, which in planar problems assumes the value ; |
 | is the gravitational acceleration; |
 | is the width of the fluid layer in which dispersion is occurring; |
 | is the volumetric expansion coefficient defined by with being the fluid density; |
 | is the kinematic viscosity of the fluid. |
Suppose
is the characteristic length scale for
, then the characteristic time scale is given by
. And suppose
is a characteristic value for
. Then, we introudce the non-dimensional variables

then the Erdogan–Chatwin equation becomes[5]
![{\displaystyle {\frac {\partial \varphi }{\partial \tau }}={\frac {\partial }{\partial \xi }}\left\{\left[1+\gamma Ra^{2}\left({\frac {\partial \varphi }{\partial \xi }}\right)^{2}\right]{\frac {\partial \varphi }{\partial \xi }}\right\},}](//wikimedia.org/api/rest_v1/media/math/render/svg/d463b778862e42638b54da0cb22ff3c817032a35)
where
is a Rayleigh number. For
, the equation reduces to the linear heat equation,
and for
, the equation reduces to
.