Light Optical Aerosol Counter (LOAC) Project Overview

 
LOAC (Light Optical Aerosol Counter)
 
Jean-Baptiste RENARD (LPC2E-CNRS, Orléans, France)
 
                                                 
Light Optical Aerosols Counter
 
 
Project funded by the “Agence Nationale de la Recherche”
Collaboration between national research laboratory (LPC2E,
LSCE/CEA, LA), private companies (Environnement-SA,
Aerophile SAS, MeteoModem), and the French Space Agency
90 copies produced at the end of 2014
50 scientific flights under different kinds of balloons
 
Instrument and pump: 350 g
Electric consumption: ~3 W
No lenses => no risk of misalignment
Concentrations for 19 size classes
between 0.2 and 100 
m
Automatic check every 10 minutes and electronic
recalibration if necessary (ex. strong changes in
temperature)
 
Total weigh (gondola, batteries and LOAC): 1 kg for
use with meteo balloons
 
  
        
Principle of measurements
2 scattering angles measurements (field of view of few degrees)
~12°, insensitive to the refractive index of the particles (mainly diffraction)
 
=> accurate size determination and counting
~60°, strongly sensitive to the refractive index of the particles
 
=> indication of the nature of the particles
 
 
 
Detection of the maximum of
intensity for particle that
crosses the laser beam
Real-time stray light correction
 
Calibrated with beads and real irregular particles
Similar statistical approach for the detection of
irregular particles (all natural solid particles are
irregular)
 
At a given diameter, same scattered flux for different
natures of particles (at small scattering angles)
 
LOAC can be used for liquid and irregular
particles but not for perfect solid spheres
 
Small field of view (few degrees) at
small scattering angles
=> large irregular  particles are less
luminous than expected
 
Confirmation by modelling (Mie)
calculations including a roughness
surface coefficient
 
Determination of the main nature of the particles: Speciation
 
The 60° measurements are very sensitive to the refractive index of the particles
More absorbing are the particles, lower are the scattered flux
 The 60° size distribution is often
lower than the 12° real size distribution
 
 
The ratio of the 2 size distributions
varies with the nature of the particles
 
       The 12°/60° ratio is compared to charts obtained in laboratory for different
families of particles:
 
- Liquid droplets
 
- Minerals
 
- Carbons
 
This is an open data base and other natures
of particles can be considered (no more than
3 or 4 different natures)
Pollution carbon particles
Saharan sand plume
 
Size distribution
 
speciation
 
Size distribution
 
speciation
Sea salt
Inside a cloud
 
Size distribution
 
speciation
 
Size distribution
 
speciation
 
LOAC is used at ground and under all kinds of balloons:
tethered, meteo, low troposphere, stratosphere
 
 
 
 
 
 
“Modular” instrument : LOAC can work with different  kinds of pump (between 1.3
and 2.7 l/mn) and with different kinds of inlets depending on the sampling conditions
 
Permanent measurements at ground in the
south sunburn of Paris to study fog events
 
Beginning of the fog
 
End of the fog
 
Welas and Fog Monitor :
optical counters
 
Strong pollution event on 11 December 2013
and inversion layer at an altitude of 200 m
 
Permanent measurements on board the touristic balloon
“AOG” in Paris, from ground to an altitude of 250 m
 
Close to the ground,
various natures
 
At 200m, black carbon
 
    Counting measurements can be converted
to PM 2.5 and PM10 mass (
g/m
3
)
 
Mean densities used from speciation results:
    1.4 g/cm
3
 for carbon
    2.2 g/cm
3
 for minerals and salts
    0 g/cm
3
 for droplets
(small changes in case of humidity > 65%)
 
Comparison with microbalance measurements
from AirParif ambient air network
Very good agreement
 
LOAC has performed 19 flight under BPCL (long duration tropospheric
balloons) and BLD (Meteo balloon) during the Charmex campaign,
summer 2013, above the Mediterranean Sea
 
BPCL trajectory on 17 June
2013, altitude of 2000 m
 
Flight inside a Saharan sand plume
 
Detection of large particles
Particles transported during
several days
No sedimentation
 
Indirect detection of strong
electro-magnetic field inside
the plume
 
Vertical profiles of aerosol content with BLD (meteo) balloons
 
L
i
q
u
i
d
 
p
a
r
t
i
c
l
e
s
 
S
a
n
d
 
p
l
u
m
e
 
17 June 2013, Minorca
 
23 June 2014, Ury (France)
 
C
i
r
r
u
s
 
L
i
q
u
i
d
 
d
r
o
p
l
e
t
s
+
 
s
o
o
t
 
Fly on-board Unmanned Airborne Vehicles (Fly-N-Sense Society)
Environmental studies, analysis of local sources
 
CONCLUSIONS
 
LOAC can provide size distribution and main nature of the aerosols
Light instrument for ground and airborne measurements
Now a commercial instrument
 
Actual scientific campaigns:
Pollution studies 
in the Paris region (ground, tethered balloon)
VOLTAIRE
, long-term monitoring of the stratosphere (~25 flights per year
at different latitudes)
 
Future
Improved version of LOAC in development
STRATEOLE, long duration balloons (several months) in the lower
equatorial stratosphere (coordinated by LMD-CNRS)
LOAC for space application (CNES) : Studies of planetary atmospheres
 
Earth
 
Mars
 
Titan
 
Saturn
 
Contact for science application: 
jbrenard@cnrs-orleans.fr
 
LOAC is commercialized by the MeteoModem company:
http://www.meteomodem.com
 
LOAC on board Unmanned Airborne Vehicles is commercialized by
the Fly-N-Sense company : 
http://www.fly-n-sense.com/
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Light Optical Aerosol Counter (LOAC) is a project led by Jean-Baptiste Renard in France, involving a collaboration between research institutions, private companies, and the French Space Agency. The LOAC instrument, weighing 1 kg, is used with meteorological balloons to measure concentrations of aerosols in various size classes. It employs two scattering angles for accurate sizing and counting of particles, providing real-time stray light correction. Calibrated for irregular particles, LOAC can detect the nature of particles but is not suitable for perfect solid spheres. The project aims to determine the main nature of particles through speciation analysis.

  • LOAC
  • Aerosol Counter
  • Jean-Baptiste Renard
  • France
  • Research

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  1. LOAC (Light Optical Aerosol Counter) Jean-Baptiste RENARD (LPC2E-CNRS, Orl ans, France)

  2. Light Optical Aerosols Counter Project funded by the Agence Nationale de la Recherche Collaboration between national research laboratory (LPC2E, LSCE/CEA, LA), private companies (Environnement-SA, Aerophile SAS, MeteoModem), and the French Space Agency 90 copies produced at the end of 2014 50 scientific flights under different kinds of balloons

  3. Instrument and pump: 350 g Electric consumption: ~3 W No lenses => no risk of misalignment Concentrations for 19 size classes between 0.2 and 100 m Automatic check every 10 minutes and electronic recalibration if necessary (ex. strong changes in temperature) Total weigh (gondola, batteries and LOAC): 1 kg for use with meteo balloons

  4. Principle of measurements 2 scattering angles measurements (field of view of few degrees) ~12 , insensitive to the refractive index of the particles (mainly diffraction) => accurate size determination and counting ~60 , strongly sensitive to the refractive index of the particles => indication of the nature of the particles Detection of the maximum of intensity for particle that crosses the laser beam Real-time stray light correction

  5. Calibrated with beads and real irregular particles Similar statistical approach for the detection of irregular particles (all natural solid particles are irregular) At a given diameter, same scattered flux for different natures of particles (at small scattering angles) LOAC can be used for liquid and irregular particles but not for perfect solid spheres

  6. Small field of view (few degrees) at small scattering angles => large irregular particles are less luminous than expected Confirmation by modelling (Mie) calculations including a roughness surface coefficient

  7. Determination of the main nature of the particles: Speciation The 60 measurements are very sensitive to the refractive index of the particles More absorbing are the particles, lower are the scattered flux The 60 size distribution is often lower than the 12 real size distribution The ratio of the 2 size distributions varies with the nature of the particles

  8. The 12/60 ratio is compared to charts obtained in laboratory for different families of particles: - Liquid droplets - Minerals - Carbons This is an open data base and other natures of particles can be considered (no more than 3 or 4 different natures)

  9. Pollution carbon particles Saharan sand plume Size distribution Size distribution speciation speciation

  10. Sea salt Inside a cloud Size distribution Size distribution speciation speciation

  11. LOAC is used at ground and under all kinds of balloons: tethered, meteo, low troposphere, stratosphere Modular instrument : LOAC can work with different kinds of pump (between 1.3 and 2.7 l/mn) and with different kinds of inlets depending on the sampling conditions

  12. Beginning of the fog Permanent measurements at ground in the south sunburn of Paris to study fog events End of the fog Welas and Fog Monitor : optical counters

  13. Permanent measurements on board the touristic balloon AOG in Paris, from ground to an altitude of 250 m Strong pollution event on 11 December 2013 and inversion layer at an altitude of 200 m Close to the ground, various natures At 200m, black carbon

  14. Counting measurements can be converted to PM 2.5 and PM10 mass ( g/m3) Mean densities used from speciation results: 1.4 g/cm3for carbon 2.2 g/cm3for minerals and salts 0 g/cm3for droplets (small changes in case of humidity > 65%) Comparison with microbalance measurements from AirParif ambient air network Very good agreement

  15. LOAC has performed 19 flight under BPCL (long duration tropospheric balloons) and BLD (Meteo balloon) during the Charmex campaign, summer 2013, above the Mediterranean Sea BPCL trajectory on 17 June 2013, altitude of 2000 m

  16. Flight inside a Saharan sand plume Detection of large particles Particles transported during several days No sedimentation Indirect detection of strong electro-magnetic field inside the plume

  17. Vertical profiles of aerosol content with BLD (meteo) balloons 17 June 2013, Minorca 23 June 2014, Ury (France) Liquid particles Liquid droplets + soot Sand plume Cirrus

  18. Fly on-board Unmanned Airborne Vehicles (Fly-N-Sense Society) Environmental studies, analysis of local sources

  19. CONCLUSIONS LOAC can provide size distribution and main nature of the aerosols Light instrument for ground and airborne measurements Now a commercial instrument Actual scientific campaigns: Pollution studies in the Paris region (ground, tethered balloon) VOLTAIRE, long-term monitoring of the stratosphere (~25 flights per year at different latitudes)

  20. Future Improved version of LOAC in development STRATEOLE, long duration balloons (several months) in the lower equatorial stratosphere (coordinated by LMD-CNRS) LOAC for space application (CNES) : Studies of planetary atmospheres Earth Saturn Titan Mars

  21. Contact for science application: jbrenard@cnrs-orleans.fr LOAC is commercialized by the MeteoModem company: http://www.meteomodem.com LOAC on board Unmanned Airborne Vehicles is commercialized by the Fly-N-Sense company : http://www.fly-n-sense.com/

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