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There may be emission of methane gases in dams when flooded plants are rotting in the water.
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The optimum case for imaging high-energy (E > 100 MeV) heliospheric protons may be the emission of π0-decay γ-rays following proton collisions with solar wind (SW) ions.
Normally such emission may be an indication of thermal emission by warm dust.
Such a base line may be base year emissions (BYE), like the emissions in the year 1990.
One of possible reasons may be lowered photo emission efficiency in the Interball-2 case.
SPCE is due only to fluorophores near the metal surface and may be regarded as emission from the induced surface plasmons.
Residential wood smoke may be an important emission to control, particularly in the north and eastern regions of Canada.
This technology has the potential to provide what may be called "zero emissions"—in reality, extremely low emissions of the conventional coal pollutants, and as low-as-engineered carbon dioxide emissions.
Though there may be some CO2 emissions during the manufacturing processes these emissions are incredibly small in comparison to the reduction in fossil fuels used.
Air pollutants undergo physical and chemical changes after emission, and our results suggest that primary emissions may be more important than the aged emissions.
In addition, the CO2 emission may be also associated with other volcanic emissions, as it is the case of the radioactive gas radon.
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