The Tyndall effect, also known as Tyndall scattering, is light scattering by particles
in a colloid or particles in a fine suspension.
It is named after the 19th-century physicist John Tyndall.
It is similar to Rayleigh scattering, in that the intensity of the scattered light depends
on the fourth power of the frequency, so blue light is scattered much more strongly than
red light.
An example in everyday life is the blue colour sometimes seen in the smoke emitted by motorcycles,
in particular two-stroke machines where the burnt engine oil provides the particles.
Under the Tyndall effect, the longer-wavelength light is more transmitted while the shorter-wavelength
light is more reflected via scattering.
An analogy to this wavelength dependency is that longwave electromagnetic waves such as
radio waves are able to pass through the walls of buildings, while shortwave electromagnetic
waves such as light waves are stopped and reflected by the walls.
The Tyndall effect is seen when light-scattering particulate-matter is dispersed in an otherwise-light-transmitting
medium, when the cross-section of an individual particulate is the range of roughly between
40 and 900 nanometers, i.e., somewhat below or near the wavelength of visible light.
It is particularly applicable to colloidal mixtures and suspensions; for example, the
Tyndall effect is used commercially to determine the size and density of particles in aerosols
and other colloidal matter.
Difference from Rayleigh scattering
Rayleigh scattering is defined by a mathematical formula that requires the light-scattering
particles to be far smaller than the wavelength of the light.
For a dispersion of particles to qualify for the Rayleigh formula, the particle sizes need
to be below roughly 40 nanometres, and the particles may be individual molecules.
Colloidal particles are bigger, and are in the rough vicinity of the size of a wavelength
of light.
Tyndall scattering, i.e. colloidal particle scattering, is much more intense than Rayleigh
scattering due to the bigger particle sizes involved.
The importance of the particle size factor for intensity can be seen in the large exponent
it has in the mathematical statement of the intensity of Rayleigh scattering.
There is no equivalent mathematical statement for Tyndall scattering.
But, if the colloid particles are spheroid, Tyndall scattering is mathematically analysable
in terms of Mie theory, which admits particle sizes in the rough vicinity of the wavelength
of light.
Blue irises
A blue iris in an eye is due to Tyndall scattering in a turbid layer in the iris.
Brown and black irises have the same layer except with more melanin in it.
The melanin absorbs light.
In the absence of melanin, the layer is translucent and a noticeable portion of the light that
enters this turbid layer re-emerges via a scattered path.
That is, there is backscatter, the redirection of the lightwaves back out to the open air.
Scattering takes place to a greater extent at the shorter wavelengths.
The longer wavelengths tend to pass straight through the turbid layer with unaltered paths,
and then encounter the next layer further back in the iris, which is a light absorber.
Thus, the longer wavelengths are not reflected back to the open air as much as the shorter
wavelengths are.
Since the shorter wavelengths are the blue wavelengths, this gives rise to a blue hue
in the light that comes out of the eye.
The blue iris is an example of a structural color, in contradistinction to a pigment color.
The complete absence of pigment in eyes causes the eye to appear red, due to the visibility
of the red of the retina through the iris.
Some phenomena that are not Tyndall scattering On a day when the sky is overcast, the sunlight
passes through the turbid layer of the clouds, resulting in scattered, diffuse light on the
ground.
This does not exhibit Tyndall scattering because the cloud droplets are larger than the wavelength
of light and scatter all colors approximately equally.
On a day when the sky is cloud-free, the sky's color is blue in consequence of light scattering,
but this is not termed Tyndall scattering because the scattering particles are the molecules
of the air, which are much smaller than the wavelength of the light.
On occasion, the term Tyndall effect is incorrectly applied to light scattering by macroscopic
dust particles in the air.
See also Light scattering
Nephelometer; aka turbidimeter Rayleigh scattering
Transparency and translucency Ultramicroscope
References