measuring the aerosol asymmetry parameter g instrument ......black hole signals of four detectors...
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Measuring the Aerosol Asymmetry Parameter g Instrument
Description and Initial MeasurementsGuoxun Tian ([email protected]), Hans Moosmüller, and W.Patrick Arnott,
Desert Research Institute, Nevada System of Higher Education, Reno, NV.
Introduction
In addition to aerosol scattering and absorption coefficients, the angular distribution of light scattered by aerosol particles is needed to determine the aerosol contribution to radiative forcing. This angular distribution is commonly
parameterized into a single value, the asymmetry parameter g. It is defined as the intensity-weighted average cosine of the scattering angle with values ranging from –1 for pure backscattering to +1 for pure forward scattering.
No instruments for the direct measurement of aerosol g in the atmosphere are available. Commonly the asymmetry parameter g is determined from measurements of the aerosol size distribution and refractive index using Mie
calculations under the assumption of spherical particles. The problem is that size distribution and refractive index are often poorly known and the particles may not be spherical.
Here a g-meter which can measure aerosol g directly is introduced. It is made of a quadrant detector conjunction with a laser beam. An accurate g value can be achieved by the signals of four detectors. The initial measurement will be
discussed.
Schematic diagram
1) Concept of Asymmetry parameter g 2) 1-D Physical meaning of g
4) Schematic diagram and picture of
the g-Meter
3)Design of the g meter
The angular distribution of light scattered by aerosol is needed to determine the
aerosol contribution to radiative forcing. Phase function from Mie theory for
spherical particles (Needs size parameter x = πd/λ and complex refractive index)
00
2
04
cossin2
1cossin
4
1cos
4
1PddPdPdg
where is the angle between incident light and scattering direction and P() is the phase
function giving the angular distribution of the scattered light.
We can calculate back scattering percentage and forward
scattering percentage very easily if asymmetry parameter g
is known.
particle
Incoming photons
Forward scattered photons
back
scattered
photon
Here P↓↓=75%. P↓↑=25%.
P↓↓+ P↓↑ = 100%.
g≡ P↓↓ - P↓↑
g = P↓↓ - (1- P↓↓)
Solving, we have:
The g-meter needs to reproduce the (sinθcosθ) angular weighing
Laser beam propagating
through the center of a
quadrant torus detector.
2-dimensional cross-section
or simplified version
Laser is scattered by the aerosol, so four
detectors receive the scattered light and
produce four signals, S1, S2, S3 and S4
2
2
0
1 cos1cossin PdPdPCS laser
S2 C Plaser d P 1 cos 0
2
d P sin cos 2
S3 C Plaser d P 1 sin 2
S4 C Plaser d P 1 sin 0
2
4321
43214321
SSSS
SSSS
S
SSSSSg
Sg 1
2d P 1 sin cos
0
2
d P 1 sin cos 2
0
)(2
1wg gPdS
For gw cos sgn 2 1sin
sgn x
1 x 0
0 x 0
1 x 0
wg*165.1cossin
gw SgPdPdg *165.1)(2
1*165.1cossin
2
1
00
Multiple channel lock
in amplifier
Pow
er Mo
du
latio
n
Spatial
filter
Power
meter
Computer
Data
Black hole
Signals of four detectors
Aerosol outlet
Aerosol inlet
Laser
The laser is 532nm wavelength green laser. We use a virtual multiple channel
lock in amplifier to get the signal from the four detectors and power meter
and transfer the data to the computer. The spatial filter cleans the laser beam
and the black hole absorbs the incident laser. They greatly reduce the
background light.
5) Calibration and truncation angle analyze
Calibration(1): angular response
1. Mount the cylindrical detector on a rotation stage and rotate it around the cylinder axis.
2. Illuminate the detector with a planar wave (e.g., expanded laser beam) propagating
perpendicularly to the cylinder axis.
3. Record the angular response and normalize the angular response to sin(θ)cos(θ).
0 100 200 300
-0.6
-0.4
-0.2
0.0
0.2
0.4
0.6
Degree (C)
Sin(Q)Cos(Q)
Normalized Sg
Normalized Sg-Sin(Q)Cos(Q)
Calibration(2): sensitivity
Calibrate the reciprocal nephelometer with two gases ( Clean Air and CO2).
0.000010 0.000015 0.000020 0.000025 0.000030
0.14
0.15
0.16
0.17
0.18
0.19
0.20
gco2
=0.030223908
CO2
Clean Air
Scattering coefficient (1/Mm)
Vo
lta
ge
(v)
S1+S2-S3-S4
Y=0.13758+2092.8382*X
standard deviation of the voltage
Co2: 3.95302E-06 V
Air: 6.50221E-06 V
0 1000 2000 3000 4000 5000 6000 7000 8000
-0.4
-0.2
0.0
0.2
0.4
0.6
0.8
1.0
1.2
g
Diameter (nm)
gm (g from mie theory)
g'
fit line gf=0.19398+0.53284*g
'
truncation angle analyze (right fig)Since the tube is not infinite long, there are
different truncation angles for different detectors.
The fig on the right show the difference of g
caused by truncation angle.
Where black line is the g value from Mie theory,
red line shows the g value of g-meter without
truncation angle correction and green line is the
fit line of the black line and red line. It can be
seen easily that the green line does match the
black line.
6) Initial measurement
ultrasonic
Scanning Mobility
Particle Sizer (SMPS)
Aerosol
inlet
outlet
Aerosol
generator
(salt)
g meter
Aerosol
inlet
Aerosol
outlet
Aerosol
outlet
An SMPS is used to measure the size
distribution of salt particles from the aerosol
generator. We can calculate the g value with
Mie theory and measure it with g meter.
System diagram Initial measurement of salt particle
Size distribution 1
Measured g value: 0.82
Calculated g value: 0.74
Size distribution 2
Measured g value: 0.78
Calculated g value: 0.69
Initial measurement of latex sphereSMPS
0.6 V 0.7V 0.8V g-meter(theory) Mie
0.465um 0.874801 0.878528 0.887532 0.7508 0.7023
1.025um 0.643154 0.654732 0.653253 0.5249 0.3559
1.898um 0.896966 0.887687 0.890569 0.9125 0.6465
Diameter
Control voltage of four PMTg value