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SEMI E104-0303 © SEMI 2000, 2003 17 A3-5 Aerosol Neutralization A3-5.1 Wh en dispers ing th e suspension, the particles are charged. This su rface charge should be rem oved after drying the aerosol fl ow t o avoid electr…

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SEMI E104-0303 © SEMI 2000, 2003 16
APPENDIX 3
AEROSOL GENERATION AND AEROSOL DILUTION
NOTICE: The material in this appendix is an official part of SEMI E104 and was approved by full letter ballot
procedures on July 28, 2000 by the European Regional Standards Committee.
A3-1 Monodisperse Particle Suspension
A3-1.1 Monodisperse suspensions of particles (PSL)
are available in sizes from 0.02 µm. These particles are
grown by emulsion polymerization and are stabilized in
aqueous suspensions with an anionic surfactant. They
carry a negative charge which contributes to their
stability. The suspension normally contains 10% solids
and 2% dissolved, highly viscous stabilizer. The solid
contains up to 8% emulsifier and inorganics.
A3-1.2 After evaporation, these solids and the
stabilizer will both increase the diameter of the single
particle and generate a residual nucleus out of an empty
droplet. These residual particles are called secondary
aerosol. The diameter of residual nucleus could be up to
0.25 µm according to the PSL size and dilution of the
suspension. Most of these secondary aerosol particles
might be too small to be detectable with commonly
used particle detectors, but they will have an influence
on the noise level because of there high number.
A3-1.3 Out of a high-concentration suspension it is not
possible to aerosolize only individual particles.
Droplets containing more than one of the suspended
particles will become undesirable agglomerates upon
evaporation.
A3-1.4 For this, an adequate dilution of the suspension
is necessary to avoid the formation of aggregates and
the enlargement of the particles.
A3-2 Generation and Dilution of PSL
Suspension
A3-2.1 A diluted PSL suspension for particle
generation in an aerosol generator can be created by the
following procedure:
Shaking and/or ultrasonic treatment of the PSL
bottle distributed by the PSL manufacturer.
Placing one drop of PSL in one liter of deionized
or destilled water or Isopropanol. The water could
be cleaned using a filter with a pore size no more
than 10% of the size of the particles being used.
Shaking and/or ultrasonic treatment of the
suspension to disperse the particles.
A3-2.2 The suspension will probably need to be diluted
further to provide a required particle concentration.
This is necessary to avoid the formation of
agglomerates and to restrict the size of the secondary
aerosol particles. An equation to calculate the required
particle concentration is given in “The Generation of
Aerosols of Fine Particles” by O. Raabe (see Section
11).
A3-2.3 The particle suspensions distributed by the PSL
manufacturer shows no detectable variation in particle
characteristics when they are stored in a cool place over
the years. Diluted suspensions for atomization feature
an aging process. Diluted suspensions of polymer
spheres smaller than 1 µm should not be stored for
more than one week.
NOTE A3-1: Care should be taken to avoid contamination of
the polymer spheres and the suspension.
A3-3 Aerosol Generation
A3-3.1 The diluted suspension is nebulized in the
aerosol generator. Great account is taken of
concentration and size distribution of the generated
droplets and of the volume flow rate V´
G
. To achieve a
constant aerosol production, the volume flow rate and
the droplet size distribution should be constant and
independent of the supplies of suspension in the
reservoir. The variation in particle concentration should
be no more than 10% as measured by the reference
particle counter over a time period of 15 minutes or
more.
NOTE A3-2: Care should be taken to avoid contamination of
the aerosol generator.
A3-4 Aerosol Drying
A3-4.1 The water of the generated droplets will
completely evaporate when the relative humidity of the
aerosol flow behind the nebulizer is lower than 70%.
The volume flow of the suspension in the nozzle
increases the humidity of the filtered compressed air
which has a relative humidity of 10%15% in spite of
predrying. The use of a diffusion dryer or another
appropriate instrument allows a higher relative
humidity of the aerosol flow behind the aerosol
generator. The diffusion dryer uses silica gel desiccant
to remove the moisture. The desiccant shall either be
new or freshly regenerated. It is not wise to get the
aerosol in direct contact with the desiccant. Polymer
spheres will be precipitated and additional particles out
of the desiccant will change the particle size
distribution of the aerosol.
SEMI E104-0303 © SEMI 2000, 2003 17
A3-5 Aerosol Neutralization
A3-5.1 When dispersing the suspension, the particles
are charged. This surface charge should be removed
after drying the aerosol flow to avoid electrostatic
interactions with each other or the line walls. With the
help of the discharging distance of an electrostatic
neutralizer, the aerosol is exposed to a bipolar ion
source. Some electrostatic neutralizers may produce a
large number of ultra-fine particles which will combine
with the calibration aerosol and affects the signal-to-
noise-ratio of the LPPD and the reference particle
counter.
A3-6 Aerosol Size Separation
A3-6.1 When calibrating with ultra-fine particles, a
particle size separation might be necessary to remove
the residue particles and agglomerates. An electrostatic
classifier is most effective for particle sizes less than 1
µm. This instrument electrically charges the incoming
aerosol. With electrostatic deflection, it separates
selected particles of one mobility. The residue particles
and the larger aggregate particles would be stripped out
of the particle stream consisting of the desired polymer
particles. To charge the aerosol, the electrostatic
classifier uses a radioactive neutralizer. The aerosol
exiting the instrument will contain singly charged
particles. This low charge level makes the use of an
additional aerosol neutralizer unnecessary.
Nevertheless, conductive tubing should be used
between the aerosol generator and the LPPD and
reference particle counter to minimize electrostatic
particle loss.
A3-7 Aerosol Dilution
A3-7.1 The particle concentration of the aerosol
generated by the nebulizer might be too high. The
aerosol should be further diluted to achieve the required
concentration and to avoid coincidence errors. The
dilution could be executed with a mixing chamber in
which the aerosol is mixed with zero gas. The internal
chamber pressure should be stable and very close to
ambient atmospheric pressure at operational flow rates.
The spatial particle distribution in the exiting aerosol
should be as homogenous as possible.
SEMI E104-0303 © SEMI 2000, 2003 18
APPENDIX 4
AEROSOL TRANSPORT AND AEROSOL SAMPLING
NOTICE: The material in this appendix is an official part of SEMI E104 and was approved by full letter ballot
procedures on July 28, 2000 by the European Regional Standards Committee.
A4-1 Aerosol Transport
A4-1.1 Aerosol loss in lines occurs both for small and
larger particles. Larger particles (approximately 5 µm
and larger) are lost as a result of gravitational settling in
horizontal lines and inertial effects in all lines. Smaller
particles are lost to the line walls by diffusion and by
electrostatic charge effects.
A4-1.2 A limitation of particle loss could be achieved
with tubing as short and as straight as possible with no
bends with a radius of curvature less than 100 mm. The
tubing of the calibration setup should be smooth,
conductive, and electrically grounded. Stainless,
polished steel for rigid lines and Polyurethane or
polyvinyl chloride for flexible lines is found acceptable
for handling most aerosols with low electrostatic
particle loss. If long transit lines are required, they
should be sized to permit a Reynolds number in the
range of 5,000 to 25,000 at the sample flow rate to
minimize particle residence time in the tubing without
causing excessive turbulence at high flow rates.
A4-2 Aerosol Sample Acquisition
A4-2.1 The term isokinetic sampling often is used in
aerosol measurement and characterization. Isokinetic
sampling of particles in a moving aerosol is performed
by matching the sample probe inlet velocity (flow speed
and
direction) to the velocity of the moving aerosol. At
velocities less than 15 m/s, anisokinetic sampling errors
are negligible for most particles smaller than
approximately 5 µm. Losses of larger particles might be
significant. The larger the particle, the larger the loss
due to inertial effects. Isokinetic sampling is not
possible in environmental conditions with varying
velocity, motionless air, and turbulent, random, or non-
unidirectional flow. For better sampling inlet efficiency,
isokinetic or at least isoaxial sampling is recommended
at calibration.
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