Carbon in the atmosphere comes mainly from fossil fuel
combustion (emissions of approximately 5 billion metric tons/yr) and
deforestation (loss of stored carbon in biomass) (emissions of about 1-2
billion metric tons/yr) (Schneider, 1989). Carbon in trees comes from
atmospheric carbon dioxide (a very minor portion may come from other chemicals
containing carbon [e.g., carbon monoxide], but many of these chemicals convert
to carbon dioxide through time).
Sea level rise under
warming is inevitable
• Long time scales
of thermal expansion & ice sheet response to warming imply that
stabilisation of GHG concentrations at or above present levels will not
stabilise sea level for many centuries
Northeast, maple-beech-birch
forests
25 year old forest: 12,000 lbs of carbon / 25 = 480 lbs of C per acre per year x 44/12 =1,760 lbs of CO2 per acre per year
120 year old forest: 128,000 lbs of carbon / 120 = 1,066 lbs of C per year per acre x 44/12 =3,909 lbs of CO2 per acre per year
Tree density varies, and we used an average of 700 trees per acre (this number was taken from DOE's "Sector-Specific Issues and Reporting Methodologies Supporting the General Guidelines for the Voluntary Reporting of Greenhouse Gases under Sections 1605(b) of the Energy Policy Act of 1992")
25 year old forest: 1,760 lbs of CO2 per acre per year / 700 trees =
average of 2.52 lbs of CO2 per tree per year (rounded to 3 lbs)
120 year old forest: 3,909 lbs of CO2 per year per acre =
average of 5.58 lbs of CO2 per tree per year
Northeast, white and red pine forests
25 year old forest: 67,000 lbs of carbon / 25 = 2,680 lbs of C per acre per year x 44/12 = 9,826 lbs of CO2 per acre per year / 700 =
average of 14 lbs of CO2 per year per tree (rounded to 15 lbs)
120 year old forest: 246,000 lbs of carbon / 120 = 2,050 lbs of C per acre per year x 44/12 = 7,516 lbs of CO2 per acre per year / 700 = average of 11.7 lbs of CO2 per year per tree .
25 year old forest: 12,000 lbs of carbon / 25 = 480 lbs of C per acre per year x 44/12 =1,760 lbs of CO2 per acre per year
120 year old forest: 128,000 lbs of carbon / 120 = 1,066 lbs of C per year per acre x 44/12 =3,909 lbs of CO2 per acre per year
Tree density varies, and we used an average of 700 trees per acre (this number was taken from DOE's "Sector-Specific Issues and Reporting Methodologies Supporting the General Guidelines for the Voluntary Reporting of Greenhouse Gases under Sections 1605(b) of the Energy Policy Act of 1992")
25 year old forest: 1,760 lbs of CO2 per acre per year / 700 trees =
average of 2.52 lbs of CO2 per tree per year (rounded to 3 lbs)
120 year old forest: 3,909 lbs of CO2 per year per acre =
average of 5.58 lbs of CO2 per tree per year
Northeast, white and red pine forests
25 year old forest: 67,000 lbs of carbon / 25 = 2,680 lbs of C per acre per year x 44/12 = 9,826 lbs of CO2 per acre per year / 700 =
average of 14 lbs of CO2 per year per tree (rounded to 15 lbs)
120 year old forest: 246,000 lbs of carbon / 120 = 2,050 lbs of C per acre per year x 44/12 = 7,516 lbs of CO2 per acre per year / 700 = average of 11.7 lbs of CO2 per year per tree .
The amount of
carbon sequestered by vegetation depends upon a number of factors including the
age of the trees, their growth rate, local climatic conditions and soil
conditions. Additionally, the carbon intake may be altered over time as
temperatures and carbon dioxide concentrations in the atmosphere change with
global warming. While greater concentrations of carbon dioxide may increase the
growth of trees, greater cloud cover can reduce light and thus limit growth.
Additionally, photosynthesis is reduced when temperatures are above optimal
levels (Clark, 2003; Brown, 2000; Osborne, 2005).
One of the
largest challenges that arise with carbon sequestration is measurement. The
carbon cycle in trees is complex. During the day, plants synthesize carbon
dioxide yet at night and under stress situations (e.g. drought and heat) the
process reverses and plants respire CO2. Furthermore, the carbon cycle is
altered by seasonal changes in temperature and precipitation (Hadley, 2002).
Clearly,
land use management and reforestation projects are vitally important to protect
and restore watersheds, ensure clean drinking water and protect biodiversity.
Yet we feel that such projects should be implemented to secure exactly those
benefits and not to achieve carbon sequestration.
one acre of tree cover in Brooklyn gives off an approximate
net amount of 2.8 t O2/yr (this estimate does not include tree decomposition).
a) The average density in a forest stand is around 480
tree/ac (e.g., Raile and Leatherberry, 1988). Average tree density within tree
covered urban areas is approximately 204 trees/ ac of tree cover. This estimate
is based on field data from 7 cities (Dwyer et al., in review). In the Chicago
area (Cook and DuPage Counties), 77% of the trees were less than 6 in. dbh.
(Nowak, 1994a).
b) The average annual oxygen consumption for a person at rest
at 20 degrees C and 760 mm Hg (standard pressure) is between 355 lbs/yr and 444
lbs/yr (average = 400 lbs O2/ yr). This is a conservative estimate as exercise
will increase oxygen consumption.
Estimated
annual average net oxygen production for Brooklyn trees is (for various dbh
classes):
DBH
Class (in)
|
Oxygen
produced (lbs/yr)
|
0-3
|
6
|
9-12
|
49
|
18-21
|
115
|
27-30
|
148
|
39+
|
247
|
1. One acre of trees would produce enough oxygen for 14
people.
There are many sources of oxygen and plenty of oxygen in the
atmosphere, but trees do contribute oxygen to the atmosphere. "We have a
large number of serious ecological problems, but suffocation from lack of
oxygen is not one of them (Broeker 1970, SCEP 1970). The oxygen content of the
atmosphere remains essentially constant, with the oxygen consumed by all
animals, bacteria, and respiration processes roughly balanced by the oxygen
released by land and sea plants during photosynthesis.
The present atmospheric oxygen content seems not to have
changed since 1910 (SCEP 1970). Furthermore, because air is about 20 percent
oxygen, the total supply is immense (Broeker 1970)" (Miller,1979). Waters
of the world are the main oxygen generators of the biosphere; their algae are
estimated to replace about 90% of all oxygen used (Encyclopedia Brittannica, 1994).
Also, most of the oxygen produced by trees will be consumed when the tree dies
and decomposes.
a) This answer depends on tree density per acre, diameter
structure, species composition, and growth rates. Estimates from Chicago are
2.7 t C/ac of tree cover/yr (Nowak 1994b); the Chicago area: 2.2 t C/ac of tree
cover/yr (Nowak, 1994b); and in Brooklyn, NY: 1.0 t C/ac of tree cover/yr
(Nowak et al., in review). These are gross carbon sequestration estimates and
do not account for carbon emitted due to decomposition. The Chicago estimates
are likely liberal as they do not account for tree condition or stand structure
effects on growth. Gross carbon sequestration estimates for individual trees in
Brooklyn, by various diameter classes are (Nowak et al., in review):
Gross
carbon sequestration estimates for individual trees in Brooklyn, by various
diameter classes are (Nowak et al., in review):
DBH
Class (in)
|
Carbon
Sequestration (lbs/yr)
|
0-3
|
2
|
9-12
|
19
|
18-21
|
43
|
27-30
|
55
|
39+
|
93
|
b) Estimate of carbon emitted per vehicle mile is
approximately 0.24 lb C/mi (see Nowak, 1993 for calculation and references) but
is as high as 0.29 lb C/mi if carbon produced from transportation and fuel
processing is included. Thus, a car driven 26,000 miles will emit 6,240 lbs C
(22,880 lbs CO2) or 7,540 lbs C (27,647 lbs CO2) if the
whole fuel process is included. Thus, one acre of tree cover in Brooklyn can
compensate for automobile fuel use equivalent to driving a car between 7,200
and 8,700 miles, depending on which estimate you choose to use. However, when
the tree dies, most, if not all, of the carbon stored will eventually be
released back to the atmosphere and form CO2. Thus, the CO2
gains made by trees are sustained as long as the forest structure is sustained.
Also, the gains made are only good for the first generation of trees, unless
the carbon is prevented from decomposing. If first generation decomposes, the
second generation of trees will only compensate for the loss of the first
generation (Nowak et al., in preparation).
Trees
remove several tons/day of O3, CO2, SO2, NO2,
PM10. How many trees does it take to remove so many tons of one
element?
We
are currently completing a comparison of pollution removal by trees in 50
cities across the United States. Pollution removal varies based on meteorology,
amount of tree and shrub cover (acres), pollution concentration, and length of
growing season. Pollution removal (ozone, particulate matter, sulfur dioxide,
nitrogen dioxide, and carbon monoxide) by trees and shrubs in Chicago in 1994
was estimated at 651 tons (rates varied for each pollutant) (Nowak, 1994c). In
Brooklyn,1994 pollution removal (same 5 pollutants) by trees and shrubs was
estimated at 287 tons (Nowak et al., in review). Average individual tree
pollution removal estimates for Brooklyn by various diameter classes are:
DBH
Class (in)
|
Pollution
Removal (lbs/yr)
|
0-3
|
0.07
|
9-12
|
0.8
|
18-21
|
2.2
|
27-30
|
2.0
|
39+
|
5.3
|
Differences
in removal rates per tree by diameter classes are due to differences in the
average amount of healthy leaf area per tree among the diameter classes.
Where
did the info come from on trees reducing urban temps & the 2% increase in
electricity consumption for every 1 deg.?
"For
U.S. cities with populations larger than 100,000, peak utility loads will
increase 1.5 to 2 percent for every 1 degree F increase in temperature" is
from page 16 of Akbari et al. (1992). On page 18 it reports "the nation-wide
response of peak-cooling electricity load to temperature in the United States
could range from 0.5 to 3 percent for each 1 degree F rise in
temperature." It appears that these figures may come from Linder and
Inglis (1989). It is important to note that these data are for peak loads.
However, from a graph on page 20, it appears that annual energy use could
increase between 0.25% and 3% (average of approx. 1.1%) per degree F rise in
temperature, depending on city location.
How
much carbon does a tree store in its wood? Is it based on size ?
One
half of a tree's dry weight is carbon (see Nowak, 1994b for various citations).
Thus carbon storage is directly related to size (i.e., bigger trees have more
carbon stored). Annual carbon sequestration (the amount of carbon removed from
the atmosphere each year) is related to tree size and growth rates (large trees
with fast growth rates will remove more carbon annually than small trees with
slow growth rates).
How
is the value derived from the in leaf pollution removal (Dave Nowak's
research)?
Values
are derived based on median environmental externality values for the United
States for each pollutant from Murray et al. (1994) (Nowak et al, 1998).
Environmental impacts or damage caused by pollutant emissions are one type of
environmental externality. Externalities include benefits and costs resulting
as an unintended byproduct of economic activity that accrue to someone other
than the parties involved in the activity. Externality values attempt to
account for
the
cost to society due to the pollutant emission, and are usually given in $/ton.
There are various limitations with certain approaches to obtaining externality
values, but externality values are one of the most reasonable approaches to
valuing the functions of urban forests, particularly if the externality value
is directly derived from the societal costs of the pollutant emitted into the
atmosphere (e.g., human health, materials damage, etc.).
10
|
Nitrogen
dioxide (NO2) General Area, µg/m3
|
200
|
-
|
80
|
40
|
-
Jacob & Hochheiser Modified
Method
-
Chemiluminescences
|
Nitrogen
dioxide (NO2) Sensitive Area(2), µg/m3
|
-
|
-
|
-
|
30
(3-month Avg)
|
||
11
|
Ozone
(O3), µg/m3
|
180
|
90
|
-
|
-
|
- UV
Photometric technology
-
Chemiluminescences
|
12
|
Particulate
matter (PM10), µg/m3
|
-
|
-
|
100
|
60
|
-
Approved Particle size cutoff sampler
-Gravimetric
analysis
|
Particulate
matter (PM2.5), µg/m3
|
-
|
-
|
60
|
40
|
||
13
|
BSF/TSF
(benzene/toluene soluble fraction), µg/m3
|
-
|
-
|
20
|
-
|
ASTM
D4600-87,1990
|
14
|
Sulphur
dioxide (SO2) General Area, µg/m3
|
260
|
-
|
80
|
50
|
-
Improved West and Geake
- Ultraviolet Fluorescence |
Sulphur
dioxide (SO2) Sensitive Area (2), µg/m3
|
|
|
|
20
(3-month Avg)
|
||
15
|
Ammonia
(NH3), µg/m3
|
-
|
-
|
400
|
100
|
-Chemiluminescence
-
Indophenol- blue method
|
(1)
Whenever measurement of vapour mercury cannot be done, standard for particulate
mercury only is applicable
(2)
For sensitive area, more stringent standards will be applicable for NO2
and SO2; standards for other parameters remain unchanged Notes:
Notes:
(a)
Annual Arithmetic mean of minimum 104 measurements taken twice a week 24
hourly at a uniform interval should not exceed the annual standard.
(b)
1-hour/24-hourl/8-hourl values should be met 98% of the time in a year.
However, 2% of the time, it may exceed but not on two consecutive days.
No comments:
Post a Comment