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Time-resolved and Online Determination of Reactive Oxygen Species (ROS) in Ambient Air Markus Kalberer, Stephen Fuller Department of Chemistry University of Cambridge, UK

Time-resolved and Online Determination of Reactive Oxygen Species … · 2018. 8. 14. · Barcelona, 25 April 2012 M. Kalberer Measuring ROS concentrations online • Many current

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  • Time-resolved and Online Determination of

    Reactive Oxygen Species (ROS) in Ambient Air

    Markus Kalberer, Stephen Fuller

    Department of Chemistry

    University of Cambridge, UK

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Overview

    • Oxidative stress - a possible mechanism of particle-induced

    health effects

    • A new instrument measuring reactive oxygen species (ROS)

    concentration on-line: design and instrument characterization

    • First applications of the instrument

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Ambient particle cause negative biological/health effects

    as observed in epidemiological and laboratory studies

    Health effects of aerosols

    London-Smog, 1952 Deaths SO2 aerosol particles (dust)

    Six cities study, Dockery et al. 1993

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    What particle properties are relevant for

    biological effects?

    particles e.g.,

    from combustion

    sources

    1m

    potential damaging properties

    - organic components

    - metals

    - mass, size, surface properties

    effects in the cell

    - ROS?

    - oxidative stress?

    - inflammation

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Oxidative stress in the lung

    H2O2

    O2-

    OH

    Respiratory

    tract lining

    fluid

    Lung epicelial

    cells

    Circulatory

    system

    glutathione

    vitamin C vitamin E

    Antioxidants ROS

    • Oxidative stress = disturbance of prooxidant- antioxidant balance leading to potential

    biomolecular damage

    • Oxidative stress can be induced by ROS in the lung lining layer

    • Antioxidant depletion may cause damage to cell membranes, proteins

    & DNA

    Antioxidants

    ROS

    anti-ox

    proteins org. peroxides & radicals

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    PM induced ROS in the lung

    Formation routes of ROS from aerosol particles:

    1. Particle bound ROS – e.g. H2O2, ROOH, radicals

    = reactive and short-lived

    2. (Catalytic) ROS production in the lung lining fluid by

    redox active components; e.g., quinones and metals

    3. Metabolism of organics (e.g. PAHs) may lead to ROS

    formation

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Measuring ROS concentrations in solution

    - the reaction system

    • DCFH is oxidised by ROS in the presence of Horseradish

    Peroxidase to the fluorescent product DCF; excited at 470 nm

    and emitting at 520 nm.

    • DCFH reacts with almost all ROS

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    HRP

    HRP-I

    HRP-II

    ROS (ox) (H2O2)

    DCF-H

    DCF

    DCF-H

    DCF

    ROS (red) (H2O)

    • The fluorescence is directly proportional to the concentration of DCF

    • While the DCFH assay gives a linear relationship with H2O2, organic

    peroxides react much slower with HRP.

    • This assay gives an indication of ROS activity related to an

    equivalent H2O2 concentration. NOT an absolute ROS

    concentration.

    I [DCF] [H2O2]

    (HRP = Horesradish Peroxidase)

    Measuring ROS concentrations in solution

    - the reaction system

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Measuring ROS concentrations online

    • Many current aerosol studies measuring composition use

    off-line filter collection techniques

    • The time delay between collection and analysis possibly

    allows for degradation and loss of reactive components

    • Online analysis allows for fast analysis that minimizes

    loss of reactive components and allows for higher time

    resolution

    • Online analysis allows for high time resolution

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Fast Online Quantification

    of Oxidizing Particle Components

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Water Bath

    37°C

    hydrophobic

    filter

    Continuous

    collection and

    solvent

    extraction

    Connected to LabView program

    0.25 ml / min

    5 slpm

    sampling

    Aqueous

    Aqueous

    To vacuum

    pump

    HRP solution

    To mix with

    DCFH solution

    Aerosol inlet

    15 c

    m

    Fast Online Quantification

    of Oxidizing Particle Components

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Particle into liquid sampling

    0

    0,2

    0,4

    0,6

    0,8

    1

    0 100 200 300 400 500

    Co

    llecti

    on

    Eff

    ecie

    ncy

    Aerodynamic Diameter / nm

    Collection Effeciency

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    ROS quantification

    Water Bath

    37°C

    Hydrophilic

    filter

    -Continuous

    filter collection

    and solvent

    extraction

    Connected to LabView program

    0.25 ml / min

    5 slpm

    sampling

    Aqueous

    Aqueous

    Fan cooled 5 W 470 nm LED

    Spectrometer

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Experimental set up

    Water Bath

    37°C

    Hydrophilic

    filter

    Continuous

    filter collection

    and solvent

    extraction

    Connected to LabView program

    0.25 ml / min

    5 slpm

    sampling

    Aqueous

    Aqueous

    Fan cooled 5 W 470 nm LED

    Spectrometer

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Sensitivity calibration with H2O2

    Fluorescence intensity after reaction has gone to completion after

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Normalised to equivalent

    fluorescein fluorescence to

    account for non linear

    spectrometer behaviour at

    higher concentrations

    Sensitivity calibration with H2O2

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Sensitivity calibration with H2O2

    R2 = 0.99

    0

    500

    1000

    1500

    2000

    0 100 200 300 400 500 600 700

    [Flu

    ore

    sc

    ien

    ] / n

    M

    [H2O2] / nM

    Dynamic range:

    ca. 2 orders of magnitude

    Detection limit:

    in liquid H2O2: ~ 10 nM

    ambient air (5lpm):

    4 nmol / m3

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Smog Chamber Experiments

    • Experiments at Paul Scherrer Institut (PSI), Switzerland

    • Primary moped emissions photochemically aged in smog

    chamber

    • Mopeds conforming to both Euro 1 and Euro 2 emissions

    regulations

    27 m3

    Chamber

    UV + NOx + O3

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Smog Chamber Experiments

    Secondary Organic Aerosol Formation

    Primary organic aerosol

    (POA)

    Soot

    Gaseous volatile organic

    compounds (VOCs)

    Oxidation by ozone and

    OH in the presence of

    UV light and NOx

    Oxidised VOCs

    condense to form

    secondary organic

    aerosol (SOA)

    Primary

    Processing

    Secondary

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Smog Chamber Experiments

    Charcoal Denuder

    Online ROS Instrument

    Remove gaseous

    oxidants

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Smog Chamber Experiments

    With photochemical

    SOA formation:

    increase of ROS

    ROS =

    ca. 1 nmol μg-1 SOA

    50

    40

    30

    20

    10

    0

    SO

    A m

    ass / µ

    g m

    -3

    2.52.01.51.00.50.0

    Time after lights on / hours

    50

    40

    30

    20

    10

    RO

    S c

    on

    ce

    ntr

    atio

    n /

    nM

    ole

    s m

    -3

    Euro 1 SOA mass

    Euro 2 SOA mass

    Euro 1 ROS concentration

    Euro 2 ROS concentration

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Smog Chamber Experiments: POA vs. SOA

    ROS concentration in POA (before photochemical aging): negligible

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Smog Chamber Experiments: Euro1 vs. Euro2

    ROS / g POA large differences between Euro 1 and Euro 2

    8

    6

    4

    2

    RO

    S c

    on

    ce

    ntr

    atio

    n n

    orm

    alis

    ed

    to

    PO

    A m

    ass

    / n

    Mo

    les m

    -3 µ

    g-1

    2.52.01.51.00.50.0

    Time after lights on / hours

    Euro 1

    Euro 2

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Ambient measurements

    ROS in ambient urban air (Cambridge)

    0

    20

    40

    60

    80

    100

    120

    140

    160

    180

    200

    11:52:48 12:21:36 12:50:24 13:19:12 13:48:00 14:16:48 14:45:36 15:14:24 15:43:12

    nM

    ole

    s m

    -3

    Time

    clean air ambient air clean

    air

    F

    luo

    res

    cen

    ce s

    ign

    al

    11:50 12:50 13:50 14:50 15:50

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Conclusions

    • Design of online instrument to quantify ROS

    • ROS “scavenged” within seconds: reactive ROS are not lost

    • Time resolution: ca. 10min

    • Detection limit: 10nmol (H2O2), 4 nmol / m3

    • ROS only observed in SOA from moped emissions

    ROS concentrations of ca. 1 nmol μg-1 SOA

    • No ROS in primary moped emissions

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Acknowledgements

    PSI, Villigen – Smog Chamber Experiments

    Stephen Platt

    Josef Dommen

    Andre Prevot

    Urs Baltensperger

  • M. Kalberer AirMonTech, Barcelona, 25 April 2012

    Thanks for your attention