Presentation is loading. Please wait.

Presentation is loading. Please wait.

Chapter 8 Air Pollution & Energy Use Lecture 13. Properties and Motion of the Atmosphere Air Pollutants and Sources –Acid rain –Particulates –Aerosols.

Similar presentations


Presentation on theme: "Chapter 8 Air Pollution & Energy Use Lecture 13. Properties and Motion of the Atmosphere Air Pollutants and Sources –Acid rain –Particulates –Aerosols."— Presentation transcript:

1 Chapter 8 Air Pollution & Energy Use Lecture 13

2 Properties and Motion of the Atmosphere Air Pollutants and Sources –Acid rain –Particulates –Aerosols –VOCs –Indoor Air Pollution –Air Quality Standards –Automobile Emissions –Emission Control Devices

3 The Ocean That We Live In We live in an ocean of air 20 miles deep Air pressure exerted on us is 14.7 psia (100,000 Pa) at sea level As a comparison, air pressure at the top of Mt. Everest is ~5 psia at a height of 29,035 ft Measured with a Barometer at 76 cm of Mercury at sea level Measured with Water column Barometer at 39.959 feet

4 Table 8-1, p. 244

5 Effects of Atmospheric Pressure

6 Mercury Barometer

7 Aneroid barometers More info: http://www.bom.gov.au/info/aneroid/aneroid.shtmlhttp://www.bom.gov.au/info/aneroid/aneroid.shtml

8 Buoyancy Forces Archimedes’ Principle – the buoyant force on an object is equal to the weight of the fluid displaced by that object –Allows concrete and steel battleships to float –Balloons to float

9 Fig. 8-3, p. 247

10 What are we measuring here? Body density = W/[(W - WW)/c.f. - LV] –W: weight in air (kg) –WW: weight in water (kg) –c.f.: water correction factor (equal to 1 at 39.2 o F because one gram of water occupies exactly one cm 3 at this temperature, equal to.997 at 76-78 o F) –LV: residual lung volume (liters)

11 Air Currents & Temperature Inversions Air rises from the surface as bubbles of hot air called “Thermals” Thermals continue to rise and cool until their temperature matches the temperature at that level When the thermal temperature reaches an equilibrium temperature level, it stops vertical motion and creates an “inversion layer ”. Rising air reaches an overriding layer of warmer air Air Temp decreases ~3.5 o F/1000 ft.

12 Fig. 8-4, p. 248

13 Houston, TX Lochcarron, Scotland

14

15 Definition and history of acid rain How acid rain is formed –Industries –Natural processes The effects of acid rain Ways to reduce acid rain

16 Definition of Acid Rain Any type of precipitation with a pH that is unusually low (acidic) –pH = 7 is neutral (not acid or base) Natural dissociation of CO 2 gives rain a pH = 5.6 –In areas with natural sources of acidity the rain has acidity between 4.5 < pH < 5.6 Generally any precipitation with pH < 5 is considered “acid rain” Acid rain can be in the form of snow, dew, or dry particles

17 pH Scale acid rain affects aquatic life and reproductive ability

18 History of Acid Rain In 1852 Robert Angus Smith in Manchester, England found the relationship between acid rain and atmospheric pollution –Manchester was an ‘industrial revolution’ city –He used the term “acid rain” in 1872 Acid rain began to be widely researched in and after the late 1960’s –Harold Harvey researched a “dead” lake in Canada Dead = fish used to live there and no longer do –In 1990’s the New York Times reported on a forest in New Hampshire that was greatly affected by acid rain

19 p. 263 Effect on forests

20 How Acid Rain is Formed Industries burn fuels that contain sulfur (e.g., coal; oil and natural gas to a lesser extent) The sulfur forms SO 2 (sulfur dioxide) when it burns In the atmosphere the SO 2 first reacts to form SO 3 (sulfur trioxide) and reacts with water to form H 2 SO 4 (sulfuric acid) The sulfuric acid comes down with rain and affects buildings, forests, rivers, and lakes

21 Human Caused SO x Emissions Most SO x is caused from coal since it has much more sulfur in it compared to gasoline Since 2006 China is largest contributor, 25.49 million tons

22 How Acid Rain is Formed Sulfur has the biggest effect but nitrogen can also make acid rain Monatomic nitrogen (N) can come from: –Fuel (such as coal) –Air; dissociation of diatomic nitrogen (N 2 ) used in burning coal, gasoline, or natural gas Nitrogen forms NO x (nitrogen oxides) –Transportation is largest contributor of NO x In the atmosphere NO x reacts to form HNO 3 (nitric acid) Nitric acid has the same effects as sulfuric acid

23

24 Human Caused NO x Emissions Transportation has greater effect on NO x than SO x –Nitrogen comes from air –Transportation has fewer devices to clean up NO x ( because devices are large & heavy)

25 How Acid Rain is Formed from Natural Processes Biggest natural source of acid rain is from emissions from volcanoes that contain sulfur –3% - 20% Carbon Dioxide –46% - 87% Sulfur Dioxide Other areas of geothermal activity (besides volcanoes) also have sulfur, such as Yellowstone Some wetlands have a source of sulfur

26 Natural Sources: hydrogen sulfide (H 2 S) carbon disulfide (CS 2 ) carbonyl sulfide (COS) methyl mercaptan (CH 3 SH) dimethyl sulfide (DMS) (CH 3 SCH 3 ) dimethyl disulfide (DMDS) (CH 3 SSCH 3 )

27

28

29 The Effects of Acid Rain Rivers and Lakes Forests Visibility Manmade Outdoor Objects –Buildings, monuments, cars People’s health

30 The Effects of Polluted Air – Acid Rain Being One Part of This Greater medical costs Greater food costs Decrease in visual appearances


Download ppt "Chapter 8 Air Pollution & Energy Use Lecture 13. Properties and Motion of the Atmosphere Air Pollutants and Sources –Acid rain –Particulates –Aerosols."

Similar presentations


Ads by Google