K. Ceulemans, J.-F. Müller, S. Compernolle

Presentatie over: "K. Ceulemans, J.-F. Müller, S. Compernolle"— Transcript van de presentatie:

1 K. Ceulemans, J.-F. Müller, S. Compernolle
Evaluation of a Detailed Chemical Mechanism for Alpha-Pinene Degradation and Subsequent Secondary Aerosol Formation K. Ceulemans, J.-F. Müller, S. Compernolle Belgian Institute for Space Aeronomy, Brussels, Belgium L. Vereecken, J. Peeters Katholieke Universiteit Leuven, Belgium ACM Conference Davis December 2008

2 Outline BOREAM: model for alpha-pinene oxidation and subsequent secondary aerosol formation Possible impact of gas-phase oligomerization reactions Evaluation against dark ozonolysis experiments

3 Alpha-Pinene Oxidation Model
Detailed explicit gas phase model with additional generic chemistry and aerosol formation module 10000 reactions, 2500 compounds Capouet et al., J. Geophys. Res., 2008 complete mechanism can be explored at KPP(Kinetic PreProcessor) /Rosenbrock as chemical solver

4 Explicit chemistry Oxidation by OH, O3 and NO3
mechanism based on advanced theoretical calculations and SARs Oxidation by OH, O3 and NO3 important updates from Vereecken et al., PCCP, 2007 leads to many different stable primary products

5 Primary products: explicit or through lumped generic species
APIN + OH APIN2OH APIN2OH JbCH3OHcHO2 JbCH3OHcHO2 + HO JbCH3OHcHOOH (primary product) JbCH3OHcHOOH + OH L10HPO2 (semi-generic: 10C, OH, OOH and O2-groups) JbCH3OHcHOOH + OH JbCH3OHcO Explicit chemistry Semi-generic chemistry L10HPO2 + NO L10HPO + NO2 L10HPO2 + HO L10HPP + O2 … L10HPP + OH L10KPP + HO2 L10KPP + OH LXeO2 + HO2 (LXeO2: generic low volatility peroxy-radical) P: hydroperoxide, H : alcohol , K: ketone O: oxyradical O2: peroxyradical generic chemistry LXeO2 + NO LXeO + NO2 LXeO2 + HO LXeOOH … LXeOOH + OH LXeO LXeO + O LXeCHO + HO2 LX indicates a generic species, e indicates the volatility class (11 classes provided) Products (explicit or generic) are allowed to partition to aerosol phase

6 Aerosol formation and Partitioning
Molecules can partition between particulate and gas phase Pankow partitioning coefficient: Vapor pressure: calculated with group contribution method (see talk of Steven Compernolle) Activity coefficient: takes into account mixture effects, calculated with UNIFAC-based method (Compernolle et al. ACPD 2008) Saturated vapor pressure Activity coefficient

7 Oligomerization reactions: gas-phase reactions of Criegee intermediates
Observed in several recent studies (Tobias & Ziemann 2001, Heaton et al. 2007) Example: SCI + pinic acid: produces a very condensable product

8 Oligomerization reactions: gas-phase reactions of Criegee intermediates
Tobias and Ziemann (2001) investigated the relative reaction rates of water vapour and other molecules with Stabilized Criegee Intermediates from tetradecene ozonolysis We take these rates and apply them to the most important species in alpha-pinene ozonolysis

9 Results: photo-oxidation: SOA yields
Capouet et al. JGR 2008 Simulations with additional acid formation channels in ozonolysis mechanism lead to better agreement in some (not all) low-VOC experiments Simulations with additional particle-phase association reactions (ROOH+R’CHO) has little impact except in high-VOC ozonolysis experiments

10 Model Validation: Dark ozonolysis experiments
New simulations for dark ozonolysis About 150 smog chamber experiments from 10 different studies were simulated Typical experimental conditions Excess ozone + OH-scavenger Very low or no NOx Temperatures generally between 0°C and 45°C RH variable, but many dry experiments ( < 10%)

11 Dark ozonolysis: modelled versus experimental SOA yields
SOA yield is predicted within a factor 2 for majority of experiments Some overstimations for Cocker et al. and Iinuma et al. at colder temperatures Some very serious underestimations for Hoffmann et al.1997: at high temperature (45°C)

12 Pathak et al. 2007: modelled versus experimental SOA
Dry, RH<10% but not exactly determined. Clear temperature dependence in model performance Overestimations of about factor 2 for 0-20°C Some very serious under-estimations at 30°C and 40°C with low initial VOC Example: Pathak01:(40°C,14.3 ppb) experimental yield: 9% modelled yield: 0.001% modelled with stabilized Criegee oligomers: 0.4 %

13 Results: temperature dependence of SOA yields is problematic
Experimental yields do not decrease strongly with temperature Modelled yields strongly decrease with temperature Serious underestimations at high temperature and no seed aerosol

14 Possible Importance of SCI oligomers at low RH
Song et al. 2007: Dark ozonolysis RH < 2% in all experiments Temperature 28°C Assuming very low RH significantly improves modelled yields, due to decreased competition of water vapor in formation of Criegee Intermediate oligomers Therefore: At very low RH gas phase reactions of Stabilized Criegee intermediates with acids and alcohols can significantly influence SOA yields Precise measurements of RH in smog chambers are important SOA yields deduced in very dry ozonolysis experiments might not be representative for real atmospheric conditions Exp Model RH 1% 0.01% Exp. Yield 2 0.16 0.35 3 0.18 0.36 0.38 4 0.015 0.20 0.15 5 0.19 0.37 0.43 6 0.21 0.46 7 0.08 0.28 8 0.14 0.34 9 0.17

15 Next step: model reduction
Currently BOREAM model contains about reactions and 2500 species Global models: chemical reactions consume large amount of CPU time Model reduction is needed: At most a few hundred reactions Less than 100 species Work in progress…

16 Conclusions Validation of dark ozonolysis experiments: majority of SOA yields reproduced up to factor 2 Overall temperature influence not well reproduced Oligomerization of Stabilized Criegee Intermediates can be important at very low RH Thank you for your attention!

17 Model reduction: requirements
Reduced model should be able to reproduce: Inorganics (NOx, HOx, O3) Small organics (CH2O, acetone, PAN) Some important products: Pinic, pinonic acid, pinonaldehyde SOA Validation through comparison with full mechanism Focus on atmospherically relevant scenarios

18 Reduction Techniques: Removing negligible reactions
Identify negligible reactions in atmospheric conditions Branching can depend strongly on NOx-regime Example: Peroxyradical in alpha-pinene + OH

19 Reduction Techniques: product merging
Products with Similar reactivity Similar products can be merged Example: in OH-addition on alpha-pinene The resulting peroxy radicals lead to similar products (nitrates, hydroperoxides and pinonaldehyde) Use of averaged reaction rates for the merged species

20 Reduction Techniques: Reducing length of long radical reaction chains
Some reactions produce a sequence of several peroxyradicals Radical reactions are very fast: considered instantaneous The chain ends through radical termination Is replaced by a single equation yielding LXO2, represents the peroxy radicals Stable endproducts

21 Reduction Techniques: Lumping
Not all different products can be treated explicitly in a reduced mechanism. Use generic species Example: generic nitrate LXONO2 + OH LXCHO + NO2 (OH oxydation) LXONO2 + hv LXO2 + NO2 (photolysis) LXONO LXNO2p (partitioning) Advantage: carbon balance conserved, some effects of aging are reproduced Disadvantage: simplifications lead to errors compared with full mechanism