ENAC-SSIE Laboratoire de Pollution de l'Air. O 2 + h →O + O O + O 2 + M→O 3 + M In the stratosphere (U.V. radiation): NO 2 + h →NO + O O + O 2 + M→O 3.

Slides:



Advertisements
Similar presentations
Atmospheric chemistry
Advertisements

5-2. OZONE LAYER Formation of Ozone Layer  Ozone layer: A part of stratosphere (ca. 20km high) in which ozone concentration is relatively high.
Air Pollution-Tropospheric Ozone. Good Ozone and Bad Ozone Stratospheric ozone protect lives on Earth from harmful effects of UV radiation. Tropospheric.
Chemistry in the Atmosphere Chapter 17 Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
1/03/09 De 89 à 98. 1/03/09 De 89 à 98 1/03/09 De 89 à 98.
ENAC-SSIE Laboratoire de Pollution de l'Air The energy Consumption is a Consequence of the Industrial Development
ENAC-SSIE Laboratoire de Pollution de l'Air Bogotá air quality Colombia, 2003.
ENAC-SSIE Laboratoire de Pollution de l'Air Model Strategies Simplify the equations Find an analytical solution Keep the equations Simplify the resolution.
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.
METO 637 Lesson 14. Photochemical chain initiation In the troposphere several species are present that absorb solar ultraviolet radiation and can initiate.
1 Air Pollution and Atmospheric Chemistry Sasha Madronich Atmospheric Chemistry Division National Center for Atmospheric Research Boulder, Colorado USA.
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.
This Week—Tropospheric Chemistry READING: Chapter 11 of text Tropospheric Chemistry Data Set Analysis.
ENAC-SSIE Laboratoire de Pollution de l'Air The Atmospheric Layers.
OZONE ATMOSPHERIC POLLUTION Ozone in urban smog J (Hans) van Leeuwen.
Atmospheric chemistry Day 4 Air pollution Regional ozone formation.
Environmental Chemistry Chapter 3: The Detailed Chemistry of the Atmosphere Copyright © 2007 DBS.
Typical mixing ratios for some compounds of environmental importance.
Introduction to Photochemistry Marin Robinson Department of Chemistry Northern Arizona University.
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?
5.7 URBAN AIR POLLUTION. Beijing, China Tropospheric ozone  Tropospheric ozone (ground level ozone) = bad ozone (not protective) as a result of human.
Midterm Matters any appeals regarding the test must be communicated to Dr. Gentleman by THURSDAY, NOVEMEBER 4 Next week: Lab.
OZONE ONE KIND OF AIR POLLUTION. A photochemical reaction  Sunlight + a chemical = different chemicals  Not all kinds of light  Only shorter wavelengths.
Urban Air Pollution Public and Environmental Health Concerns –Elevated levels of toxic compounds Regional and Global Impacts –Background Chemistry and.
1 Chemistry in the Atmosphere Chapter 17 Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display.
TROPOSPHERIC OZONE AND OXIDANT CHEMISTRY Troposphere Stratosphere: 90% of total The many faces of atmospheric ozone: In stratosphere: UV shield In middle/upper.
Air Quality 101 Rice Air Curriculum Teacher Training.
Practice Exam. 1. (10 pts) The figure on the left illustrates the challenges to an environmental chemist. (a) Using acid rain as your illustration, discuss.
Photochemical Smog Lecture-2.
Department of Chemistry CHEM1020 General Chemistry *********************************************** Instructor: Dr. Hong Zhang Foster Hall, Room 221 Tel:
History of Ozone Discovered in 1840 by Christian Friedrich Schönbein. In the 1920’s Gordon Dobson made the first O 3 column measurements. 1 DU = 1x10 -3.
Slap it! Survive the 5. What is HNO 3 Nitric Acid Rain.
METO 621 CHEM Lesson 4. Total Ozone Field March 11, 1990 Nimbus 7 TOMS (Hudson et al., 2003)
Environmental chemistry E. 10 smog. smog State the source of primary pollutants and the conditions necessary for the formation of photochemical smog.
Layers of the Atmosphere Layer NameAltitude (km) Temperature change with altitude.
南京菩提小组义务献血记实 时近年关, 2012 年 1 月 12 日上午,较平时冷 清的江苏省血液中心采血处忽然热闹起来, 原来是南京菩提小组的道友们集中在此集体 义务献血。
Workshop on Air Quality Data Analysis and Interpretation Role of Hydrocarbon Oxidation in Ozone Formation.
。 33 投资环境 3 开阔视野 提升竞争力 。 3 嘉峪关市概况 。 3 。 3 嘉峪关是一座新兴的工业旅游城市,因关得名,因企设市,是长城文化与丝路文化交 汇点,是全国唯一一座以长城关隘命名的城市。嘉峪关关城位于祁连山、黑山之间。 1965 年建市,下辖雄关区、镜铁区、长城区, 全市总面积 2935.
Ozone Budget From: Jacob. Ozone in the Atmosphere Lifetime: –~1 month –Highly variable – dependent on season, latitude, altitude, etc. Background concentrations:
Biogeochemical Rx in Troposphere Trace biogenic gases (NO, NO 2, N 2 O, CH 4, SO 2 ) more Rx than major constituents (N 2, O 2, Ar) NITROGEN & SULFUR Ozone.
Ch. 18 Air Pollution.
EPA Air Policy Priorities
Air Pollution.
Climate and Pollution Jeopardy
Why is it so important to life on earth?
Workshop on Air Quality Data Analysis and Interpretation
SMOG by Emre YAZICIOĞLU 1140 , 12 / C.
Environmental chemistry
Hard Facts What do you need to memorize in order to get a 5 on the AP Environmental Science Exam?
What is INSOLATION? A Science Sisters Production 2017.
Chemistry in the Atmosphere
Gases in the Atmosphere absorb Radiation
APES Test Review.
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. 4 ways the atmosphere affects.
Ozone.
Greenhouse effect.
Earth’s Changing Atmosphere
We have atmosphere because gravity pulls gas molecules “down”.
Concept mapping.
Troposphere The Air We Breath.
FOLDABLES, FLASH CARDS, OR PAPER PENCIL LIST
OZONE PRODUCTION IN TROPOSPHERE
Tropospheric Ozone System
Climate Change.
The Atmosphere.
Chemistry in the Atmosphere
Characteristics of the Atmosphere
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. Atmosphere affects light in.
The Earth’s Atmosphere
Characteristics of the Atmosphere
Presentation transcript:

ENAC-SSIE Laboratoire de Pollution de l'Air

O 2 + h →O + O O + O 2 + M→O 3 + M In the stratosphere (U.V. radiation): NO 2 + h →NO + O O + O 2 + M→O 3 + M In the troposphere (visible radiation): Ozone Formation NO 2 + O 2 + h ↔NO + O 3

ENAC-SSIE Laboratoire de Pollution de l'Air

Hydrocarbons C H CC C H H H H H H H H H C H H H H C H C C C H H H H H H H Methane Alcane Alcene Aromatic C C H H H H H H C C C C

ENAC-SSIE Laboratoire de Pollution de l'Air

NO 2 + O 2 + h ↔NO + O 3 OH + RH + O 2 → H 2 O + RO 2 RO 2 + NO→ NO 2 + RHO + HO 2 HO 2 + NO→ NO 2 + OH OH + NO 2 → HNO 3 Ozone Formation Photochemical equilibrium Competition

ENAC-SSIE Laboratoire de Pollution de l'Air