Environmental Data Analysis BC ENV 3017
Atmospheric Particulates
Particulate matter in urban centers
-
aerosol = a colloid in which small solid or liquid particles are suspended
in a gas
-
colloid = a mixture in which one substance is divided into minute particles
(called colloidal particles) and dispersed throughout a second substance
-
Total Suspended Particulates (TSP), partical size 0.01 - 10mm
-
PM10 = mass of particulate matter <= 10mm;
-
these particles enter lungs
-
in NYC data indicate that PM10 = 0.5 * TSP
-
PM2.5 = mass of particulate matter <= 2.5mm
-
these particles enter the smallest spaces in the lungs
-
typical spectrum of particles (Fig)
Health effects
-
how much air do you breathe per day?
-
intake of particles by average person.
-
Asthma & particulates
-
NYC has seen a 34% increase in asthma since 1984 - why?
-
hypothesized causes
-
indoor air
-
increased tightness of modern buildings & windows
-
molds, dandruffs (cockroach, rat, pet, human), rat & mice feces, pet
hair, pollen
-
outdoor air
-
increase in fine particulates (10mm vs 2.5mm)
-
the NRC estimates
that each year about 64,000 people die prematurely from cardiopulmonary
causes linked to particulate air pollution
-
Premature mortality due to particulate Air pollution in New York (Tab)
-
current EPA standards:
(NAAQS)
-
PM2.5: annual mean concentrations < 15 µg/m3
, and 24-hour average concentrations < 65 µg/m3
-
PM10: annual mean concentrations < 50 µg/m3
, and 24-hour average concentrations < 150 µg/m3
(99 percentile form)
-
these standards will not take immediate effect, there is an implementation
timetable for these standards
Trends
Particle sizes and composition
-
idealized particle distributions. By size,
numeric peak size range < surface area peak size range < total volume
peak size range
-
particles >= 10mm settle from the atmosphere
by sedimentation
-
particles > 0.01 and < 1mm are affected by
coagulation (gather together) and condensation
-
composition of particles reflect
their source; i.e. crustal material (dust from rocks) vs. acid aerosols
and metals from energy use
-
anthropogenic sources vary but are usually dominated by fossil fuels (Fig)
-
burning fossil fuel is the source of most of the organics, most of the
sulphate (SO4) via SO2 oxidation, most of NOx
, certain metals
-
there are also natural sources of sulfate, such as volcanoes,
DMS (dimethyl sufide) from oceans and estuaries
-
amount of PM produced decreases from coal/diesel to gasoline to natural
gas
-
old incinerators were also a major source
-
worst offenders are the small inefficient apartment building incinerators
=> black cloud of smoke
-
modern high tech incinerators can be built with very low particulate outputs
-
Formations of strong acids via homogenous reactions.
Processes controling PM concentrations
-
transport effects
-
low pollution expected during passage of cold fronts, low pressure systems,
and during the initial stages of a typical high pressure system, winds
from NW or NE
-
moderate pollution expected on 2nd or 3rd day into new air mass after SW
or W air flow established
-
high pollution expected on backside of a high pressure system (SW or W
winds)
-
very high pollution, same as above but generally associated with slow moving
systems
-
effect of mixing heights (Fig).
-
degree days (heating) for a month are defined as the sum of (65F - T) for
the days of one month; the mixing height during the winter is larger than
during the summer
-
weekly cycle (fig)
-
diurnal variation of aerosol concentration, traffic and power production
in New York City (Fig)
Resources