Mason–Weaver equation

Mason–Weaver equation

The Mason–Weaver equation (named after Max Mason and Warren Weaver) describes the sedimentation and diffusion of solutes under a uniform force, usually a gravitational field. Assuming that the gravitational field is aligned in the z direction (Fig. 1), the Mason–Weaver equation may be written where t is the time, c is the solute concentration (moles per unit length in the z-direction), and the parameters D, s, and g represent the solute diffusion constant, sedimentation coefficient and the (presumed constant) acceleration of gravity, respectively. is conserved, i.e., .

Comment
enThe Mason–Weaver equation (named after Max Mason and Warren Weaver) describes the sedimentation and diffusion of solutes under a uniform force, usually a gravitational field. Assuming that the gravitational field is aligned in the z direction (Fig. 1), the Mason–Weaver equation may be written where t is the time, c is the solute concentration (moles per unit length in the z-direction), and the parameters D, s, and g represent the solute diffusion constant, sedimentation coefficient and the (presumed constant) acceleration of gravity, respectively. is conserved, i.e., .
Depiction
Mason Weaver cell.png
Has abstract
enThe Mason–Weaver equation (named after Max Mason and Warren Weaver) describes the sedimentation and diffusion of solutes under a uniform force, usually a gravitational field. Assuming that the gravitational field is aligned in the z direction (Fig. 1), the Mason–Weaver equation may be written where t is the time, c is the solute concentration (moles per unit length in the z-direction), and the parameters D, s, and g represent the solute diffusion constant, sedimentation coefficient and the (presumed constant) acceleration of gravity, respectively. The Mason–Weaver equation is complemented by the boundary conditions at the top and bottom of the cell, denoted as and , respectively (Fig. 1). These boundary conditions correspond to the physical requirement that no solute pass through the top and bottom of the cell, i.e., that the flux there be zero. The cell is assumed to be rectangular and aligned with the Cartesian axes (Fig. 1), so that the net flux through the side walls is likewise zero. Hence, the total amount of solute in the cell is conserved, i.e., .
Is primary topic of
Mason–Weaver equation
Label
enMason–Weaver equation
Link from a Wikipage to another Wikipage
Acceleration
Amplitude
Boltzmann constant
Boltzmann distribution
Boundary conditions
Buoyancy
Buoyant mass
Cartesian coordinate system
Category:Laboratory techniques
Category:Partial differential equations
Concentration
Convective flux
Density
Diffusion
Diffusion constant
Dimensionless
Drag (physics)
Drag coefficient
Eigenfunction
Eigenfunctions
Eigenvalue
Einstein relation (kinetic theory)
File:Mason Weaver cell.png
Flux
Force
Fourier series
Fundamental frequency
Gravitation
Harmonic
Harmonic oscillator
Kelvin
Lamm equation
Mass
Max Mason
Mechanical equilibrium
Molecule
Ordinary differential equation
Orthonormal
Partial specific volume
Phase (waves)
Sedimentation
Sedimentation coefficient
Separation of variables
Solute
Solutes
Solvent
Sturm–Liouville theory
Temperature
Terminal velocity
Velocity
Warren Weaver
Weight function
SameAs
2KdHu
Ecuación de Mason-Weaver
Equação de Mason-Weaver
Équation de Mason-Weaver
m.0cjj8h
Q2470526
Уравнение Масона — Вивера
Subject
Category:Laboratory techniques
Category:Partial differential equations
Thumbnail
Mason Weaver cell.png?width=300
WasDerivedFrom
Mason–Weaver equation?oldid=1117737999&ns=0
WikiPageLength
11392
Wikipage page ID
4709796
Wikipage revision ID
1117737999
WikiPageUsesTemplate
Template:Reflist