Detailed chemical modelling based on the Master Chemical Mechanism (MCM) Mike Jenkin EMMA Group Department of Environmental Science and Technology

Slides:



Advertisements
Similar presentations
Atmospheric chemistry
Advertisements

Prof. Dudley Shallcross ACRG Tim Harrison Bristol ChemLabS 2008 A Pollutants Tale.
Functional Groups What is the family name?.
Organic Chem Quizzer Basic Skills. 1. Name the functional group. a)-OH b)-NH 2 c)C=O d)COOH e)C=C.
History of the Master Chemical Mechanism (MCM) and its development protocols Mike Jenkin EPSR Group Department of Environmental Science and Technology.
LECTURE 12 AOSC 434 AIR POLLUTION RUSSELL R. DICKERSON.
Oxidation-Reduction & Organometallic
Intercomparison of secondary organic aerosol models based on SOA/O x ratio Yu Morino, Kiyoshi Tanabe, Kei Sato, and Toshimasa Ohara National Institute.
Application of the PTM-MCM to the TORCH-1 campaign Steve Utembe, Mike Jenkin and David Johnson EPSR Group Department of Environmental Science and Technology.
Development of a Secondary Organic Aerosol Formation Mechanism: Comparison with Smog Chamber Experiments and Atmospheric Measurements Luis Olcese, Joyce.
The Framework of Modeling SOA Formation from Toluene Oxidation Di Hu and Richard Kamens Department of Environmental Sciences and Engineering, University.
Secondary Organic Aerosol Formation from Gas and Particle Phase Reactions of Aromatic Hydrocarbons Di Hu PhD Committee Meeting March 24, 2004.
Developing Secondary Organic Aerosol (SOA) Code for the MCM David Johnson (Mike Jenkin and Steve Utembe) Department of Environmental Science and Technology,
History of the Master Chemical Mechanism (MCM) and its development protocols Mike Jenkin Centre for Environmental Policy
METO 621 Lesson 24. The Troposphere In the Stratosphere we had high energy photons so that oxygen atoms and ozone dominated the chemistry. In the troposphere.
Evaluation of MCM v3, using environmental chamber data P. G. Pinho 1, C.A. Pio 1 and M.E. Jenkin 2 1 Departamento de Ambiente e Ordenamento, Universidade.
WHAT IS MISSING IN THE SOURCE APPORTIONMENT OF PM? Dick Derwent rdscientific, Newbury APRIL Workshop, Imperial College London April 23 rd 2010 This work.
Andrew Rickard, Claire Bloss, Mike Jenkin, Sam Saunders and Mike Pilling Gas phase MCM development University of Leeds Department of Chemistry.
1 00/XXXX © Crown copyright URBAN ATMOSPHERIC CHEMISTRY MODELLING AT THE METEOROLOGICAL OFFICE Dick Derwent Climate Research Urban Air Quality Modelling.
Chapter 12 Organic Chemistry: The Infinite Variety of Carbon Compounds
School of Chemistry Testing and developing aromatic mechanisms against EUPHORE chamber data Mike Pilling, University of Leeds MCM Workshop, Leeds, January18th,
This Week—Tropospheric Chemistry READING: Chapter 11 of text Tropospheric Chemistry Data Set Analysis.
2 nd December 2004 MCM meeting Leeds 1.Aromatic hydrocarbon oxidation 2. Uncertainty analysis Mike Pilling University of Leeds, UK.
Nomenclature or names of compounds Alkanes. Nomenclature or names of compounds Alkanes.
Atmospheric chemistry Day 4 Air pollution Regional ozone formation.
1 1 Model studies of some atmospheric aerosols and comparisons with measurements K. G e o r g i e v I P P – B A S, S o f i a, B u l g a r i a.
QUESTIONS 1.If CO emission to the atmosphere were to double, would you expect CO concentrations to (a) double, (b) less than double, (c) more than double?
Xuexi Tie Xu Tang,Fuhai Geng, and Chunsheng Zhao Shanghai Meteorological Bureau Atmospheric Chemistry Division/NCAR Peking University Understand.
Studying Ozonolysis Reactions of 2-Butenes Using Cavity Ring-down Spectroscopy Liming Wang, Yingdi Liu, Mixtli Campos-Pineda, Chad Priest and Jingsong.
Glyoxal and Methylglyoxal; Chemistry and Their Effects on Secondary Organic Aerosol Dasa Gu Sungyeon Choi.
REACTIVITY SCALES AS COMPARATIVE TOOLS FOR CHEMICAL MECHANISMS: SAPRC-07 vs MCM Dick Derwent rdscientific, Newbury, United Kingdom Presentation to Reactivity.
Center for Environmental Research and Technology University of California, Riverside Bourns College of Engineering Evaluation and Intercomparison of N.
CONTRIBUTION FROM DIFFERENT VOC EMISSION SOURCES TO PHOTOCHEMICAL OZONE FORMATION IN EUROPE Dick Derwent rdscientific This work was supported by the UK.
Review of Biogenic Volatile Organic Compounds and Their Products Brian Lamb (1), Daniel Grosjean (2), Betty K. Pun (3), and Christian Seigneur (3) Biogenic.
Chapter 11 Introduction to Organic Chemistry: Alkanes
Chemical mechanisms within CHIMERE present and future Matthias BEEKMANN.
Functional Groups. Groups of atoms attached to a carbon chain that determine the chemistry of the molecule Usually combinations of C and H Identify and.
Parameterization of Global Monoterpene SOA formation and Water Uptake, Based on a Near-explicit Mechanism Karl Ceulemans – Jean-François Müller – Steven.
Karl Ceulemans– Steven Compernolle – Jean-François Müller
1 The roles of H 2 SO 4 and organic species in the growth of newly formed particles in the rural environment Wu Zhijun Leibniz-Institute for Tropospheric.
Secondary Organic Aerosols
Detection of Nitrooxypolyols in Secondary Organic Aerosol |Formed from the Photooxidation of Conjugated dienes under High- NOx Conditions Kei Sato, Atmospheric.
Organic Chemistry: Functional Groups. Origin of organic compounds Origin of organic compounds Naturally occurring organic compounds are found in plants,
Department of Chemistry CHEM1020 General Chemistry *********************************************** Instructor: Dr. Hong Zhang Foster Hall, Room 221 Tel:
Yunseok Im and Myoseon Jang
Center for Environmental Research and Technology/Environmental Modeling University of California at Riverside Data Needs for Evaluation of Radical and.
METO 621 CHEM Lesson 4. Total Ozone Field March 11, 1990 Nimbus 7 TOMS (Hudson et al., 2003)
Secondary Aerosol Formation from Atmospheric Gas and Particle Phase Reactions of Toluene Department of Environmental Science and Engineering, UNC, Chapel.
Organic chemistry Some last things.. Organic chemistry What are the basics of organic chemistry? Organic molecules contain carbon. Exceptions are carbides,
Ozone Budget From: Jacob. Ozone in the Atmosphere Lifetime: –~1 month –Highly variable – dependent on season, latitude, altitude, etc. Background concentrations:
ATS 621 Fall 2012 Lecture 14. SMOG (Sulfurous vs. Photochemical Pollution) Example: London (also Eastern US) smoke + fog SO 2 + “soot”, sulfuric acid.
Thanks to Colette Heald for many of the slides in this lecture
Department of Environmental Science and Engineering UNC, Chapel Hill
Cl H H C Electrophiles and Nucleophiles
FUNCTIONAL GROUPS.
The science of urban air quality
Alkenes, Alkynes and Functional Groups
Characteristics of Urban Ozone Formation During CAREBEIJING-2007 Experiment Zhen Liu 04/21/09.
Functional Groups Unit 2.
Organic Aerosol is Ubiquitous in the Atmosphere
Functional Groups Unit 3.
Organic Chemistry: Functional Groups
Organic compounds contain carbon..excluding carbonates and oxides
Oxidation of alcohols 1o alcohol aldehyde carboxylic acid
2.1 UNSATURATED HYDROCARBONS
CH 2-3 Survey of other Functional Groups in Organic Compounds
On-going developments of SinG: particles
Pollution Management 5.7 Urban Air Pollution.
UNCERTAINTY ANALYSIS IN OZONE MODELS
Potential Anthropogenic Controls on Biogenic Organic Aerosol
Presentation transcript:

Detailed chemical modelling based on the Master Chemical Mechanism (MCM) Mike Jenkin EMMA Group Department of Environmental Science and Technology

Master Chemical Mechanism Developed by a consortium of groups Imperial College London Leeds Meteorological Office NETCEN (AEA Technology)

MCM: chemical processing of emissions NO X nitrate emissions VOC CH 4 SO 2 CO 2, H 2 O sulphate

MCM: chemical processing of emissions NO X nitrate emissions Oxidant (O 3, NO 2, PAN) VOC CO 2, H 2 O Secondary Organic Aerosol (SOA)

Degradation of CH 4 and 124 non-methane VOC ca. 4,500 chemical species ca. 12,500 chemical reactions Non-methane VOC selected primarily on the basis of UK National Atmospheric Emissions Inventory (NAEI) Provides a reasonable representation of major organic compounds emitted into the boundary layer in UK and other populated regions Master Chemical Mechanism (MCM v3) (

22 alkanes (C 1 -C 12 ) 16 alkenes (C 2 -C 6 ) 2 dienes (C 4 -C 5 ) 2 monoterpenes (C 10 ) 1 alkyne (C 2 ) 18 aromatics (C 6 -C 11 ) 6 aldehydes (C 1 -C 5 ) 10 ketones (C 3 -C 6 ) 17 alcohols (C 1 -C 6 ) 10 ethers (C 2 -C 7 ) 8 esters (C 2 -C 6 ) 3 carboxylic acids (C 1 -C 3 ) 2 other oxygenates (C 3 ) 8 chlorocarbons (C 1 -C 2 ) 125 hydrocarbons, oxygenated and chlorinated VOC representative of a variety of important source sectors e.g. road transport, solvent usage, biogenic VOC degraded in MCM v3 (

Saunders et al., Atmos. Chem. Phys. 3, , 2003 Jenkin et al., Atmos. Chem. Phys. 3, , 2003 MCM scheme writing framework

VOC second generation products first generation products CO 2 OH, O 3, NO 3 OH, O 3, NO 3, h emission

Applications of the MCM Calculation of organic species distribution for comparison with and supplementation of field measurements

alkanes alkenes/dienes aromatics carbonyls ethers esters acids alkynes chlorocarbons Emitted VOCProducts Majority of emitted VOC will be oxidised to: aldehydes (C 1 - C?) ketones (C 3 - C?) nitrates (C 1 - C?) PAN(s) (C 2 - C?) hydroperoxides alcohols esters carboxylic acids percarboxylic acids bi- and multi-functional products (esp. hydroxy- carbonyls and nitrates and dicarbonyls)

Trajectories to Silwood Park, 28 July – 3 August 1999 N 28/7 29/7 30/7 31/7 1/8 2/8 3/8

Ozone at Silwood Park, 28 July – 3 August 1999 (EU PRIME campaign)

Applications of the MCM Assessment of comparative importance of: Free radical sources: O 3 + h Speciated alkenes + O 3 Speciated carbonyls + h HONO + h Free radical sinks: OH + NO 2 HNO 3 HO 2 + HO 2 H 2 O 2 + O 2 RO 2 + NO RONO 2 RO 2 + HO 2 ROOH + O 2 Assessment of oxidant formation associated with different VOCs/VOC source sectors

Reduced mechanism Common Representative Intermediates Mechanism (CRI v1) CRI v1 121 VOC 250 species 570 reactions Jenkin et al., Atmospheric Environment, 36, , 2002

Reduced mechanism Common Representative Intermediates Mechanism (CRI v1) CRI v1 121 VOC 250 species 570 reactions VOCCO 2, H 2 O Jenkin et al., Atmospheric Environment, 36, , 2002

Reduced mechanism Common Representative Intermediates Mechanism (CRI v1) CRI v1 121 VOC 250 species 570 reactions VOCCO 2, H 2 O Jenkin et al., Atmospheric Environment, 36, , 2002 O3O3 O3O3 O3O3 O3O3

CRI vs MCM

dM dlogDa ( gm -3 ) Aerodynamic Diameter (nm) Urban Rural Semi Rural Urban Importance of organics in aerosols (slide from Hugh Coe, UMIST)

VOC second generation products first generation products CO 2 OH, O 3, NO 3 OH, O 3, NO 3, h emission

VOC second generation products first generation products CO 2 first generation products second generation products OH, O 3, NO 3 OH, O 3, NO 3, h emission condensed phase gas phase

monoterpenes second generation products first generation products CO 2 C 5 -C 7 multi- oxygenated species (probably WSOC) OH, O 3, NO 3 OH, O 3, NO 3, h emission condensed phase gas phase

aromatics second generation products first generation products CO 2 OH, O 3, NO 3 OH, O 3, NO 3, h emission condensed phase gas phase (probably WSOC)

X (g) gas phase X (a) Equilibrium partitioning k in k out [X] (a) /[X] (g) = k in [OA]/k out = K p [OA] organic aerosol, OA

European Photoreactor (EUPHORE) Valencia, Spain

Photo-oxidation of -pinene/NO X EU OSOA campaign at EUPHORE