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Envi Sci 114 4

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PLANTS & OZONE
humans: exposure usually = response

plants: exposure may not = response
depends on environmental
conditions being right





OZONE CONTACT WITH LEAVES
uptake via stomata
contact with mesophyll cells

reaction with waxes & cuticle on epidermis

polarity may increase
surface more hydrophobic
cations & other solutes may leak








OZONE IN THE SUBSTOMATAL CAVITY
ozone reacts with moist surfaces of
mesophyll cells

reactive oxygen (Ro) species form
highly reactive and cause oxidative injury

ozone cannot be measured inside the leaf
ozone leaves no break-down products








DETOXIFICATION
excess oxidative capacity dissipated
in a controlled manner

examples of antioxidants
reductants ascorbate
enzymes superoxide
constitutive dismutase
induced

present or produced proportionally to
amount of ozone entering











OZONE INJURY INCIDENCE
occurs in mid-late
summer
occurs on older
lower leaves
occurs on upper
leaf surfaces
injured areas do not
cross leaf veins








ACUTE OZONE INJURY
cell membranes break down
cell contents leak, cells die necrosis

mesophyll cells affected first

then palisade parenchyma cells

phenolic pigments may accumulate in
palisade parenchyma cells









CHRONIC OZONE INJURY
low concentrations on a long-term basis

chloroplasts affected - chlorosis

premature leaf fall & senescence

anthocyanin pigments - bronzing







PLANT GROWTH EFFECTS
photosynthesis affected
changes in allocation patterns
accelerated senescence
reduced flowering and yields
reduced secondary (radial) growth
reduced root systems
reduced mycorrhizal formation
increased incidence of diseases
and insects









BIOINDICATORS
Useful to evaluate relative air quality for ozone


sentinels reliable
special care
non-native

detectors respond when conditions
are right
ecologically relevant










PARTICLE SIZE
trimodal distribution
fine particles:
nuclei mode condensation of vapors
accumulation mode grow in size

coarse particles:
from abrasion






PARTICLE SIZE
.001 - 500 microns

molecular clusters to visible particles

suspended droplets or particles are
called aerosols






Natural sources of particles
natural sources
pollen
fungal spores
salt spray
soil from wind erosion
volcanoes
biological decomposition
trees terpenes








Human sources of particles
human activity
soot from combustion diesel exhaust
fly ash from combustion
iron oxide steel mills
metallic vapors smelting
power plants
fecal dust megaplex areas
stone dust rock crushing
catalytic convertors sulfate aerosol









Particle Size and Behavior
• Size determines effects of gravity
• Nuclei mode particles behave as gases
o Subject to Brownian motion
o Low settling velocities, travel distances
• Capable of coagulation and enlargement
o The process is called “scavenging”
o Fine particles do not become course particles!
• Course particles are affected by gravity








Particle Classes and Sources
⬢ Based on origin and formation
⬢ Primary
o Produced by chemical and physical
processes emitted as is
⬢ Do not change much in air
⬢ Rock crushing, grain milling
⬢ Secondary
o Natural sources
⬢ Volcanoes, terpenes from trees,
biological decomposition
o Anthropogenic sources
⬢ Combustion
o Over 50 % of ambient aerosol secondary
sources is from natural sources














Secondary Aerosols from Anthropogenic Sources
⬢ The most common secondary aerosols from anthropogenic emissions
⬢ Sulfate and nitrate aerosol from SO2 and NO2 from combustion
⬢ Involved in visibility reduction
⬢ Involved in acidic decomposition




Some Changes in Particles in the Troposphere
⬢ Grow in size
o Collide and adhere (coagulate)
⬢ Adsorb gaseous molecules on surfaces
⬢ Change electrical charge
⬢ Undergo deliquescence(liquefy)
⬢ Are removed by deposition depending on size






Aerosol Generation
⬢ Fume aerosols
o Combustion and condensation

⬢ Dust aerosols
o Fragmentation of matter

⬢ Mist aerosols
o Atomization of liquids

⬢ Smoke
o Gases, particles, droplets











Particulate Air Pollution and Human Health
⬢ Its all about transfer of oxygen from lungs to blood and/or transfer of toxicants from surfaces of respired particles to blood
⬢ Reduced lung capacity
⬢ Toxins transferred to other organs



The Human Respiratory System
⬢ Air is inhaled via nose (or mouth)
⬢ Passes through nasopharyngeal system
o The upper airway
⬢ Passes through tracheobronchial system
⬢ Ends up in pulmonary system
⬢ Air is exhaled






The Respiratory Tract
⬢ The nasopharyngeal system
⬢ Nasal passages
o Course hairs, cilia, mucus
⬢ Nasopharynx
o Cilia, hairs
⬢ Oropharynx
o Cilia, mucus







Innate Defense Mechanisms
⬢ Nasal Region
o Hairs, cilia, mucus
⬢ Sneeze Reflex
o Upper airway
⬢ Cough Reflex
o Upper part of bronchial tree






The Respiratory System
⬢ The pulmonary system
⬢ Terminal or respiratory bronchioles
o Cilia and mucus
⬢ Alveolar Ducts
o Mucus
⬢ Alveoli
o Mucus, phagocytes(eat bacteria and small
particles, Pacman)








Alveoli
⬢ Transfer of oxygen and or toxicants from air or particles to red blood cells
⬢ Tiny sac-like structures attached to bronchioles
⬢ Capillaries surround alveoli
⬢ Transfer through alveolar membrane to capillaries
⬢ 3 million/person





Direct Irritant Effect
⬢ Sulfate aerosol can become sulfuric acid aerosol on contact with water vapor or moist cell surfaces
⬢ This can lead to irritation of the respiratory system
⬢ More serious when combined with ozone and high temperatures



Respiratory Deposition and Retention
⬢ Particles must penetrate respiratory defense mechanisms
⬢ Particles larger than 10 microns are not retained
⬢ Inhalable : smaller than 10 microns are deposited in the upper respiratory system
⬢ Removable anything larger than 2.5 microns are removed from the upper respiratory system




Effects of Adsorbed Substances from Pm 2.5 particles
⬢ Damage to organs distant from lungs
⬢ Concentrations of adsorbed substances increase with decreasing particle size due to increased surface area
⬢ PAHs
⬢ Metals
o Pb, Cd Zn, Hg





Lead
⬢ Ubiquitous (its everywhere)
⬢ Inhalation of particulate Pb
⬢ Enters blood from alveoli
⬢ Deposited in bone, excreted, or causes problems
⬢ Ingestion of lead paint particles
⬢ Absorbed by blood from intestines






Symptoms of Lead
⬢ Chronic anemia
o Pb inhibits enzymes in hemoglobin synthesis
⬢ Acute (a lot of lead)
o Kidney damage
o Brain damage
⬢ Cross-placental transfer
o Mentally-retarded children





URBAN ADVANTAGES
population in small dense areas
jobs
essential services available
cultural opportunities




URBAN DISADVANTAGES
crowding
slums
pollution
poverty
health effects





MODIFICATIONS CAUSE CHANGES
Natural vegetation removed and replaced with
paved surfaces and high density buildings

This affects:
absorption of solar radiation
storage of heat
surface & air temperatures
water absorption & evaporation
turbulence & wind – “urban canyons”









URBAN CANYONS
Streets with rows of high buildings on both sides - like the canyon of a river

Building heights and orientation of the
canyon determines incoming solar radiation,
heat retention, and wind speed

Views of the sky may be obscured







HUMAN ACTIVITIES CAUSE CHANGES
High energy demands by residents:
heating
cooling
appliances, computers
transportation
dining, entertainment






URBAN HEAT ISLAND (UHI)
A metropolitan area which is significantly
warmer than its surroundings

This effect is greatest at night



“On hot summer days, urban air can be
2-10F hotter than the surrounding
countryside”*

* US EPA












HOW UHI FORM
“Heat islands form as vegetation is replaced by asphalt and concrete for roads, concrete and stone for buildings and other structures
needed to accommodate growing populations”

US EPA




SOLAR RADIATION IS ABSORBED
Paved surfaces and buildings absorb and hold solar radiation, rather than reflecting it

This causes surface temperatures and overall
ambient temperatures to rise




NATURAL COOLING DECREASED
The process of water evaporation provides
cooling of ambient air

evaporation from soil: non-paved areas

evapotranspiration from vegetation: well-
watered plants







ANTHROPOGENIC HEAT INPUT
air conditioning in summer
refrigeration
heating in winter
public transport
private cars
factories






UHIs & RAINFALL
Rainfall is usually higher in urban areas

Monthly rainfall can be as much as 28%
higher 20-40 miles downwind of a city




VEGETATION AND UHIs
Vegetation can mitigate UHIs

Directly
by shading heat absorbing surfaces

Indirectly
by evapotranspirational cooling







TREES & GREEN SPACES
Evapotranspiration in tree crowns
cools the air

Air moving through the tree moves the cooler air into the non-tree area

Large numbers of trees can reduce
local air temperatures by 1-5 F







USING VEGETATION TO REDUCE URBAN HEAT
Plant trees to shade roofs and south-, east-,
and west-facing walls

Use trees to shade roads & parking lots

Green roofs reduce heat in buildings

Parks & greenspace cool off neighborhoods








WATER IN THE CITY
The amount of rainfall in urban areas is usually higher than in surrounding non-urban areas

Evapotranspiration is much lower

Surface run-off is greater

Water storage is lower







WHY RAINFALL IS HIGHER
Mainly due to short but intensive rainfall events

Air pollution results in small particles that serve as condensation nuclei for raindrops

UHIs favor cloud formation

Low wind speeds favor high relative humidity







AIR POLLUTION IN URBAN AREAS
Combustion of fuels for transportation and energy generation

Gasoline & diesel oil for transportation
nitrogen oxides
small hydrocarbons (VOCs)
carbon monoxide
photochemical oxidants
ozone
nitrogen dioxide









SOILS IN URBAN AREAS
Most urban soils are either highly disturbed
or man-made soils

The ideal soil, as described in textbooks,
is difficult if not impossible to find in urban areas

Urban soils provide extreme and often severe conditions for plant growth







CHARACTERISTICS OF URBAN SOILS
great verical and horizontal variability
compressed structure leading to compaction
surface crusts on bare soils – hydrophobic
modified pH, usually elevated
restricted water drainage and aeration
interrupted nutrient cycling
restricted microbial activity
presence of pollutants & other materials
modified soil temperatures









EFFECTS OF COMPACTION

normal water and gas movement impaired

this creates conditions that are either:

excessively wet or
excessively dry







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