Hello Marshall and folks,

Hach  Water Analysis Handbook, 3rd edition, 1997, P 1277, ¶ 4:

 "A minute particle interacts with incident light by absorbing the light
energy and then, as if a point light source itself, reradiating the light
energy in all directions.  This omni directional reradiation constitutes the
"scattering" of the incident light.  The special distribution of scattered
light depends on the ratio of particle size to wavelength of incident light.
Particles much smaller than the wavelength of incident light exhibit a
fairly symmetrical scattering distribution with approximately equal amounts
of light scattered both forward and backward.

Next ¶

As particle sizes increase in relation to wavelength, light scattered from
different points of the sample particle create interference patterns that
are additive in the forward direction.  This constructive interference
results in forward-scattered light of a higher intensity than light
scattered in other directions [P. 1278] In additions smaller particles
scatter shorter (blue) wavelengths more intensely while having little effect
on longer (red) wavelengths.  Conversely, larger particles scatter long
wavelengths more readily than they scatter short wavelengths of light."
End excerpt.

The text goes on about particle shape, particle color, and lots of other
variables, leading one towards boggle....
If you don't have a copy of the book I will---when the new scanner is
operational---send you a copy of the 6 pages from the book if you like. No
math is included in the text. Hach will send you the entire book if you ask.

James Osbourne Holmes

FTNWO

 -----Original Message-----
From:   Marshall Dudley [mailto:[email protected]]
Sent:   Wednesday, November 22, 2000 2:06 PM
To:     [email protected]
Subject:        Re: CS>development work

"James Osbourne, Holmes" wrote:

> I think it is a bit more complex:  some are absorbed;

Right.

> some are reflected;

Right.

>
> some are refracted and the angles of reflection vary with wavelength;

True, this is lumped together with reflected as scattering, and is
ultimately
what is termed Tyndall effect.

> some
> are absorbed and re-emitted at a different wavelength.

I am not aware of any being absorbed and re-emitted, except for the energy
from
the light creates heat and the silver will have the black body radiation
associated with the temperature. Normally absorbed and re-emitted is
considered
fluorescence, and I don't think silver behaves this way.  Do you have any
cites
or references on this?

> All of this changes
> with particle size and concentration of particles.

It changes with particle size, as I have quoted previously, the Tyndall
increases to the third power with the size.  The increase in Tyndall and
absorption are both linear with concentration (provided the concentration
does
not reach a point where aggregation occurs)..

> Some devices take
> advantage of this behavior to determine particle size based on the changes
> between the light in and light out.

Yes, I have used this myself.  Using the Hack scanning spectrophotometer, I
scan
a specimen and can get a crude idea of the particle size distribution from
the
absorption spectrum from infrared to uv.  If I could obtain some samples
with
defined and narrow particle size ranges to calibrate from, I  think I could
do a
very good job of using this technique to profile particle size of CS
samples,
but have not been able to source any such standards.

Marshall


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