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Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
Problems and Solutions Specific to Ambient Aerosol
Measurements
Alfred Wiedensohler
Leibniz Institute for Tropospheric Research
WMO-GAW World Calibration Centre for Aerosol Physics
Metrology of Airborne Nanoparticles, Standardisation and Applications (MANSA)
NPL, June 8-9, 2010
Background
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
- Long-term observations of physical aerosol properties became common
due to an increase interest in regional climate and air quality
- Especially, measurements of number size distributions, light scattering
and light absorption (black carbon) are of great interest
- An important goal of the community is to obtain comparable data sets
- Measurements have to be thus performed under the comparable
conditions
- The data have to be traceable and its treatment transparent and
reproducible
- The goal is now to standardize aerosol sampling, measurement
guidelines and data handling
EUSAAR
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
- The EU-infrastructure project EUSSAR is funded since 2006
- The aim of EUSSAR was to establish 20 aerosol supersites for continuous observations of key aerosol properties in Europe
- These properties are i) number size distributions, ii) light scattering, iii) light absorption, and iv) organic/elemental carbon
- One main focus is to standardize these measurements and to ensure
quality assurance and control
- The quality assurance includes comparable sampling protocols and data
analysis
- The quality control includes comparisons against “reference instruments”and stations audits
- The data delivered to the data base EBAS should be transparent and traceable
General Sampling Considerations
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
- Sample air should be brought into the laboratory through a vertical stack
with an aerosol inlet that is well above ground level
- Because gas analysers have other requirements, a dedicated inlet stack is
required for the aerosol samples
- The size of the entrance configuration should be well designed to provide a
high inlet sampling efficiency for aerosol particles over a wide range of
wind speeds
- The sample flow should be laminar in the sample tube to avoid additional
losses of small particles due to diffusion and turbulent inertial deposition.
The ideal flow should have a Reynolds number of about 2000
- The inlet material should be weather- and sunlight-resistant, conductive,
and non-corrosive such as stainless-steel
Water Take-Up
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
- Atmospheric aerosol particles can take up a significant amount of water at
relative humidities below saturation called hygroscopic growth
- This hygroscopic growth influences physical aerosol measurements
- Increase of particles size – factor ~1.5 at 80% RH
- Increase in light scattering – factor ~2 at 80% RH
- Increase of the noise level of filter-based light absorption measurements
- The sampling philosophy is thus to determine the physical aerosol properties
at a relative humidity lower than 40-50% - dry state
Humidity Control
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
How to reach the RH requirement?
- In case the room temperature is higher than 20°C, no dryer is needed if the
ambient dew point temperature never exceeds 10°C
- Aerosol dryers are needed for each instrument if the dew point temperature
is always below the room temperature
- The whole inlet flow have to be dried before entering the room in case that
the dew point temperature is occasionally above the room temperature
- There are basically FOUR possibilities to dry the aerosol
- Aerosol diffusion dryer
- Membrane dryer
- Drying by dilution with dry particle-free air
- Drying by heating (careful!)
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
Aerosol diffusion dryer
- A diffusion dryer works on the base of silica
- Advantage: no dry air is needed
- Disadvantage: the silica has to be frequently changed
Membrane dryer
- A membrane dryer (e.g. Nafion) is based on the principal that water vapor is
transported through a membrane surrounded by a counter flow with low
humidity
- Advantage: no frequent maintenance
- Disadvantage: dry air is needed
Dilution
- The aerosol is dried by dilution with dry particle-free air
- The dilution ratio has to be exactly known
Heating
- Heating is not recommended to avoid the evaporation of semi-volatile material
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
Sketch of an automated
aerosol diffusion dryer for long-
term operation
Diffusion Dryer
Nano-Particle Measurements
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
- In the following, the focus will be on the characterization of Nanometer
particles (number size distribution measurements)
- The knowledge of particle number size distribution is essential to better
understand the aerosol in terms of climate effects and air quality
- Mobility size spectrometers are widely used to determine the number size
distribution of Nanometer particles
- To use mobility size spectrometers following calibrations are mandatory
- Sizing calibration (latex calibration)
- Calibration of the Condensation Particle Counter
- Flow calibrations by an independent volume flow meter
Standardization for Long-Term Observations (EUSAAR)
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
Additional requirements for long term measurements
- The hard- and software set-up has to be modified according a
standardized set-up for mobility size spectrometers (next slide)
- Aerosol and sheath air volume flow rates have to be measured and logged
- Dryers should be mounted in the aerosol and sheath air flow
- Relative humidity (below 40 %) and temperature in the aerosol and sheath
air flows have to be measured and logged
- Absolute pressure in the system has to be measured and logged
- The inversion routines and correction functions for particle losses should
be transparent and traceable
- Recommendation: These standardizations should be also adopted for the
commercial mobility size spectrometers
Standard SMPS Set-Up (EUSAAR)
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
The Main Question
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
How to reach high quality measurements and final data?
- Follow the recommendations for sampling and humidity control
- Modify the existing mobility size spectrometers
- Test your inversion software (in case you use a custom-made)
- Perform regular calibrations
- Perform regular comparisons against reference instruments
- Allow independent audits of your station
- Educate operators and people producing the final data
EUSAAR Networking
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
What did EUSAAR to reach the aim of a network?
- Modification of custom-built and commercial mobility size spectrometers
according to the standard set-up
- Comparisons of inversion routines
- Standardization of calibrations
- Intercomparison workshops
- Mobile reference instruments for on-site intercomparisons
- Training courses
- Stations audits
- Standardization for a traceable three-level data format for EBAS
Comparison of Inversion Routines
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
1 10 100 1000
2000
4000
6000
8000
10000
12000
14000
dN
/ d
log
Dp [cm
-3]
Dp [nm]
IFT
LUND
BOL
NILU
UHEL
JRC
PSI
LAMP
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
1 10 100 1000
2000
4000
6000
8000
10000
12000
14000
dN
/ d
log
Dp [
cm
-3]
Dp [nm]
IFT
McMurry
Brechtel
GRIMM ISO15900
GRIMM Reichelt
TSI ISO15900
Latex Calibration
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
0.10 0.15 0.20 0.25 0.30
0
5000
10000
15000
20000
25000
30000
NILU
FMI
UHEL
NUIG
UBIR
IFT REF
IFT TDMPS
TNO
PSI
LAMP
JRC
± 3.5%
dN
/ d
log
Dp [cm
-3]
Dp [µm]
CPC Calibration
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
0 5 10 15 20 25 30 35 40 45
0
20
40
60
80
100
Co
un
tin
g E
ffic
ien
cy o
f b
uta
no
l C
PC
s
for
silv
er
pa
rtic
les
[%]
Particle Diameter Dp [nm]
IFT TDMPS, 3010, ∆T=17
NILU DMPS, 3010, ∆T=25
UHEL DMPS, 3010, ∆T>25
ISPRA DMPS, 3772, ∆T=17
IFT SMPS, 3010, ∆T=17
FMI TDMPS, 3772, ∆T=25
FMI TDMPS, 3772, ∆T=25
LAMP SMPS, 3010, ∆T=17
NUI SMPS, 3010, ∆T=17
Intercomparison of Mobility Size Spectrometers
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
0.01 0.1 0.5
0
1000
2000
3000
4000
5000 NILU
FMI
UHEL
IFT REF
IFT TDMPS
TNO
PSI
dN
/ d
log
Dp [
cm
-3]
Dp [µm]
Comparison Number Concentration - reference CPC
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
174.00 174.02 174.04 174.06 174.08 174.10
0
1000
2000
3000
4000
5000 NILU
FMI
UHEL
IFT REF
IFT TDMPS
TNO
PSI
IFT CPC
int.
co
nc.
[cm
-3]
time [DOY]
Comparison Number Concentration > 100 nm
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
174.00 174.02 174.04 174.06 174.08 174.10
0
200
400
600
800
1000
1200
1400 NILU
FMI
UHEL
IFT REF
IFT TDMPS
TNO
PSI
int.
co
nc. [c
m-3]
time [DOY]
Mobile Reference Mobility Size Spectrometer
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
On-Site Latex Size Calibration
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
100 200 300 400
0.1
1
10
p1
p5
p25
Median
p75
p95
p99
raw
co
nce
ntr
atio
n [#
/cm
³]
Mobility diameter [nm]
ref. SMPS
SMPS_HP
Hohenpeissenberg
On-Site Size Distribution Intercomparisons
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
Hyytiälä, Finland, one month average
Data Structure
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
- Traditionally, highly time-resolved data is stored as one-hour averages in
the EMEP data base (EBAS)
- For aerosol properties, this data is converted to standard temperature and
pressure
- This traditional data shows no transparency how the data were treated or
corrected
- Traceability back to raw data is not possible
- We developed a three-level data structure for the aerosol properties
mentioned above within EUSAAR
EUSAAR Three-Level Data Structure
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
The data treatment for each level is described in a separate document
The user obtains a optimum transparency and traceability of the data
Level-0
- Standardized raw and system data in original time resolution
Level-1
- Corrected data in original time resolution
Level-2
- Final one-hour averaged data are normalized to standard temperature and
pressure
Summary
Leibniz Institute for
Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol
Measurements
Recommendations
- Follow the guidelines for sampling and humidity control
- Modify your instrument (e.g. mobility size spectrometer) in hard- and
software
- Perform frequent calibrations
- Compare your instrument against a reference instrument (workshop or on-
site)
- Allow site audits
- Send your operators/young scientists to comparison workshops and/or
training courses for capacity building