Greenhouse gas overview
Greenhouse gases are atmospheric gas that is trapping the heat in the atmosphere and warming the planet. It creates greenhouse effect and climate change. The Kyoto protocol lists 6 categories of GHG emission: carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), and sulphurhexafluoride (SF6).
Carbon dioxide CO2
Carbon dioxide is the highest
concentration among other GHGs. It is a major contributor to the climate
change. In 1990, the concentration is almost 60 percent of the total greenhouse
effect. In 2013, it is 82 percent of all GHG emissions from human activities.
(USEPA 2015). CO2 is produced by burning fossil fuels (coal, natural
gas and oil) for energy and transportation.
Figure 2 Electricity: Pounds of
CO2/kWh
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The
chart in Figure 2 above shows that coal fuel creates 6.39 Pounds of CO2 when creates one
kilowatts per hours while natural gas produce 1.21 and other fuel sources
generate 3.47 pounds of CO2 kWh.
Transportation:
Gasoline and diesel use in transportation are second largest source of CO2
emission. It is accounting for 31 percent of total US CO2 emission
and 26 percent of total GHG emission in US.
Figure 3 Transportation: Pounds of
CO2/gallon
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Industry:
Combustion of fossil fuels for many industrial processes is about 15 percent of
total US CO2 emission and 12 percent of total GHG emission in US.
There are other processes that also produce CO2 emissions such as
production of chemicals, production of metals or cement by chemical reactions.
Methane CH4
Nature and human are both sources
to provide methane emissions. The main natural sources are from wetlands and
ocean. The human sources are from landfills, farming, production,
transportation and use of fossil fuels. It creates the majority of CH4
emission, 64 percent of the total comparing to 36 percent of CH4
emission from natural sources.
Waste and landfills:
Methane is produced by the decomposition of organic waste in landfill sites.
The decomposition rate is depended on the waste types. Kitchen garbage such as
food, fruit, and vegetable decompose quickly. Newspaper, grass, leaves, and
wood take more time to decompose. Plastics do not decompose for long period of
time. Garbage and solid waste come to landfill and bury layer by layer. New
garbage is pilled over the old garbage. The organic waste gets trapped in no
oxygen condition (anaerobic condition) which is good condition for microbes to
break down the waste to produce methane. Landfill gas is generated for 20-30
years after the landfill is closed. With the new regulations and policies,
waste disposal is recycled, incineration before sending to landfill. Therefore,
waste sends to landfill also declining. In addition, landfill gas can be
collected and used for other energy purposes. Burning methane can generate
electricity and reduce the emission release into the air. In the beginning, the
recovery rate of the gas life cycle is minimal and higher in the middle and end
stage of the landfill. Maximum efficiency for landfill gas is 55 percent - 60
percent of methane. (Cora, 2009)
Besides, wastewater is also produce
methane emissions. During the process of wastewater treatment, the organic material
in wastewater decays in anaerobic condition as in landfills and produce
methane. (El-Fadel & Massoud, 2001)
Farming:
CH4 from agricultural emission is about one third to two third in
the countries. Main source are from manure storage and cattle digestion
process. The ratio of ruminants and manure is 8 to 1.5 worldwide. Methane
emission in ruminant fermentation is from 3 to 8 percent of the cattle intake.
Manure is stored and managed in holding storage produced CH4 (USEPA,
2015). Another big source of methane emission that releases to atmosphere is
rice field. It releases between fifty to one hundred million tones of methane a
year. The warm and waterlogged soil of rice field is ideal condition for
creating methane. Methane produced by oxidized by methanotrophs in the shallow
water and majority released into the atmosphere. Emission from rice field can
be various during a year (Van Groenigen, 2013)
Nitrous Oxide (N2O)
With the potential of 296 times of
carbon dioxide (CO2) that creates global warming, N2O is
considered as one of the powerful greenhouse gas. Major sources, which
contribute to the N2O creation, are fossil fuel combustion, biomass
burning, livestock management, and through the practice of soil cultivation and
its usage of profitable and organic fertilizers.
Agriculture:
Emission has been decreased due to reduced fertilizers’ applications. In US,
there was a decrease of 2.5 percent from 1990 to 2010 in N2O which
total to 304,082 thousand metric tons of CO2 equivalent. Agriculture
accounts for 58.6 percent of the total. In European countries, N-ferteilization
rates between 50 kg/ha in Southern European countries to 195 kg in Netherlands.
(Gielen & Kram, 1998) (http://wdi.worldbank.org/table/3.9)
Figure
4
N-fertilization and Emissions by Europe Countries
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Figure 4 includes two charts: N-fertilization and Emissions. The charts show that Ireland took lead in N-fertilization by 199 kg per hectare, followed by Belgium, 123, and Germany, 104. The country that emitted most CO2 equivalent per hectare, followed by Belgium. France emitted the least, 0.55.
Transportation:
N2O emisison is created by NOx in exhaust gases conversion in
automobiles, trucks and heavy equipments, etc.
Hydrofluorocarbons (HFCs)
HFCs are commonly used as refrigerants
and propellants in aerosols. The HFCs are not considered as significantly
contribute to the depletion of the stratospheric ozone layer, but they are
powerful greenhouse gases with global warming potentials ranging from 140
(HFC-152a) to 11,700 (HFC-23) (Gielen & Kram, 1998)
Perfluorocarbons (PFCs)
Although PFCs constitutes less than 0.25
percent of greenhouse gasses emissions, they play an important role global
climate change. With up to 9,500 times
of CO2, PFCs are exceptionally efficient at trapping heat. The
aluminum smelters/production is largest factor of PFC emission. Even with
economic incentives to reduce PFCs, the aluminum sector accounts for 60 to 70
percent of total emission in 2005.
Sulfur hexafluoride (SF6)
Sulfur
hexafluoride, SF6, is an insulating component that is used in
electrical convertors. It can and is
often use as an inert blanket. It is an unnaturally produced gas. Waste
management and leakages from old equipment cause emissions. SF6 leaves a trace of gas that
helps determine air movement or ventilations rates in buildings. Waste
management and leakages from old equipment cause emissions. Due to the unique
nature of SF6, the property is hard to neither replicate nor using
another material to substitute. Emission’s potential of reduction is 20 percent
to 40 percent with an estimated cost ranges from 0 to 25 ECU/t CO2 equivalent.
The use of SF6
in magnesium and aluminum casting has been favored in the automotive industry.
Comparing to other metals, SF6 provides a weight advantage. The transportation
section accounts for less than 5 percent of SF6 emission. However,
it is forecasted an increase of 2 to 4 times in usage in the next decade. Through
enhanced methods for recovery, emission can be reduced. In 1995, the semiconductor industry used some
of SF6 as solvent, which less than 5 Mt CO2 equivalent. There is a anticipatable of rapid growth in
this sector as well. Some SF6 can be use for different applications
such as tires for cars, sporting shoes etc. Either declining in SF6
usage or suggested alternative elements for SF6 has been mentioned.
(Gielen & Kram, 1998)
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