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Leibniz Institute for Tropospheric Research Problems 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

05 Alfred Wiedensohler - National Physical Laboratory · Alfred Wiedensohler ... - In case the room temperature is higher than 20 °C, ... training courses for capacity building

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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

Leibniz Institute for

Tropospheric ResearchProblems and Solutions Specific to Ambient Aerosol

Measurements

Thank you very much for your attention

Melpitz: PM10 inlet and dryer