Introduction to Bridge Engineering - Seismic Consolidation · 01-JFeburary-2016 Lecture # 02 CE-341...

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Engr. Gul-E-Hina Lecturer, Institute of Environmental Engineering & Research (IEER) University of Engineering and Technology, Lahore [email protected] Lecture 4- Environmental Pollution Issues

Transcript of Introduction to Bridge Engineering - Seismic Consolidation · 01-JFeburary-2016 Lecture # 02 CE-341...

Page 1: Introduction to Bridge Engineering - Seismic Consolidation · 01-JFeburary-2016 Lecture # 02 CE-341 –Environmental Engineering-1 Engr. Gul-e-Hina IEER UET Lahore 19 Global Warming

Engr. Gul-E-HinaLecturer,

Institute of Environmental Engineering & Research (IEER)University of Engineering and Technology, Lahore

[email protected]

Lecture 4- Environmental Pollution Issues

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CE-341 – Environmental Engineering-1Lecture # 0201-JFeburary-2016 3Engr. Gul-e-Hina IEER UET Lahore

• pH of pure water is 7

• Rainwater is naturally acidic

because its equilibrium

with carbon dioxide

• So due to the presence of

H2CO3 , the pH of natural

rain is about 5.7

Introduction

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Acid Rain

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• It is defined as precipitation in which has pH < 5.6

• Acid rain or acid snow is a direct result of the

method that the environment clean itself.

• The tiny droplet of water that make up clouds

continuously capture solid particles and gases in the

atmosphere.

• When enough of the tiny cloud droplets clump

together to form a larger water drop it may fall to

the earth as “wet” acid precipitation including rain,

snow , ice , sleet, or fog.

Introduction

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Acid Rain Formation

SOx + H2O H2SO4

NOx + H2O HNO3

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Acid Rain Transport

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• The reactions of sulfur oxide to form sulfuric acid

are quite slow

• Sulfur dioxide may remain airborne for 3-4 days

• As a consequence acid rain derived from sulfur

oxides may travel for hundreds of miles or even a

thousand miles

• Nitrogen oxides may persist for only one half day

and therefore may travel only tens or hundreds of

miles

Acid Rain Transport

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• Once airborne, the sulfur and nitrogen oxides

eventually come down in one form or another.

• Where they come down depends on the height of the

smokestack and the prevailing weather conditions.

• In general, prevailing winds in North America

transport pollutants from west to east or northeast.

Acid Rain Transport

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• The main precursors of acid rain are emissions of

SOx and NOx, are primarily responsible for the

harmful effects on environment.

Sources of SOx:

Anthropogenic (Man made):

• Fuel combustion in power plant

• Exhaust pipes in automobiles

• Industrial emissions(pulp and paper)

• Incineration of refusal waste

• Smelting of sulphur

Causes of Acid Rain

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Natural:

• Volcanic eruptions

• Forest fires

• Out gassings from anaerobic wetlands(decay process)

Sources of NOx:

Anthropogenic:

• Fertilizers

• Fuel burning in automobiles

Natural:

• Terrestrial , tidal, and nutrient- rich oceanic areas

• Decomposition of organic matter

• Sedimentation of rocks

• Lightening strokes

Causes of Acid Rain

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Environmental Effects

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Water and marine life:

• Extinction of fish in lakes

Environmental Effect

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• Vegetation:

Necrosis Epinasty

ChlorosisAbscission

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Human health:

• Respiratory problems

• Failure of Kidney (Norway)

• Irritation to eyes , etc.

Building / Monuments:

• Sandstone, granite- discoloured

• Eroding of building surfaces

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Stone Cancer

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Reduced Fossil fuel Emissions:

• Fuel desulfurization (remove S from fuel)

• Fluidized bed technology (reduce SO2 during

combustion)

• Flue gas desulfurization (remove sulphur gases

using lime slurry in scrubbers)

• Scrubbers can be used to remove NOx from

industrial emissions

• Catalytic converter and lean burn engines (reduce

NOx in motor vehicles)

Control

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Global Warming

“It is the natural or human induced increase in the

average Global Temperature of the atmosphere near

the earth surface or troposphere is known as “Global

Warming”.

Introduction

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Mechanism:

The incoming solar radiations are in the form of:

UV Rays (0.1-0.4 μ), 9 %

Visible Light (0.4-0.7 μ), 45 %

Infrared Rays(0.7-4.0 μ), 46 %

Global Warming

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The “GREEN HOUSE EFFECT”

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The “GREEN HOUSE EFFECT”

1. Incoming Energy

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2. Absorption

The “GREEN HOUSE EFFECT”

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The “GREEN HOUSE EFFECT”

3. Emission

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The “GREEN HOUSE EFFECT”

4. Role of Greenhouse Gases

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The “GREEN HOUSE EFFECT”

5. Human Role

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• Water vapors account for 97 % of greenhouse process

(Their concentration remains almost constant)

• Due to anthropogenic activities, concentration of

• GHGs is increasing, thus resulting in Global Warming.

GHGs contribute 3 %,

CO2, N2O, CH4, CFCs

76 % 6 % 13 % 5 %

Green House Gases(GHG)

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GHGs

1. CO2:

Present Concentration = 397 ppm

Increasing rate = 0.5 % per year

Expected level in 2050 = > 450 ppm

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1. CH4

Present Concentration = 1750 ppb

Increasing rate = 0.5 % per year

GHGs

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1. N2O

Present Concentration = 322 ppb

GHGs

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1. CFCs:

Present Concentration = 532 ppt

GHGs

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GHGs

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GHGs

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Global temperature may rise (1.5 – 5.5 oC) by 2050.

Climatic Change

• A warmer northern hemisphere

• Changes in precipitation patterns

• More droughts, more storms

• More incidents of Malaria

• Extinction of Animal and Plant species

Consequences of Global Warming

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Impact on Crop Yield:

Faster plant growth

Plants prone to pest attack

More fertilizers, pesticides needed.

Global yield of key crops may decrease by 30-70 % by

2050

Rise in Sea level

0.2-2.2 m rise by 2050 (Maldives, Bangkok may be

flooded,Threats to ports)

Consequences of Global Warming

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Impacts on Socio-economics:

Displacement of people

Changes of occupation

Sufferings, Miseries

Consequences of Global Warming

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1. Reduce emissions of GHGs

2. Reduce use of fossil fuels

3. Encourage use of hydal power and solar energy

4. Control gas leaks

5. Employ less fertilizers

6. Stop using CFCs

7. Plant as many trees as possible

Control Strategies

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Ozone

• Ozone is a gas that is naturally present in our atmosphere.

• Each ozone molecule contains three atoms of oxygen and is

denoted chemically as O3

Introduction

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Chemistry of Ozone

UV-B(0.28-0.32um)UV-C(0.1-0.28um)

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• In stratosphere

O2 O+O

O+O2O3

O3O2+O

• UV-A(0.32-0.4um) Not affected by O3, All reaches to

earth

• Ozone Hole: refers to >50% reduction in O3 conc. Over a

particular area

Chemistry of Ozone

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• Significance of UV-B

Damage cells, tissues, DNA

Inhibit photosynthesis, kills phytoplankton

Lower crop and sea food yield

Sunburns, skin cancer

Effects

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Cholofluoro-carbons (CFCs)

Used as : refrigerators, air conditioning, foam production,

solvents, aerosols, insulation material

• CFC-11(CFCl3),CFC-12(CF2Cl2)

• O3 + Cl ClO + O2

• ClO + O3Cl +2O2

Causes of Ozone Depletion

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Ultraviolet rays from Sun

The Ozone layer in stratosphere blocks these harmful UV rays

Chlorofluorocarbons are entering in to atmosphere releasing chlorine. The chlorine than break down the ozone

The chlorine released from CFCs break down the ozone molecule.

chlorine

ozone

More ultraviolet radiations are reaching in to earths surface as there is a whole in ozone layer.

Oxygen

Whole in Ozone layer

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Nitric oxide (NO)

(50-70% ozone depletion)

• N2O +O 2NO

• NO + O2 NO2 + O2

• NO2 + O NO + O2

Causes of Ozone Depletion

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Montreal Protocol (Sept,1982)

CFCs production to stop by 2000

Available CFCs to be recycled

Best alternatives of CFCs:

Butane (C2H10) + Propane (C3H8)

Protection of O3 Layer: