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In the atmosphere, the oxidation of organic compounds is mainly due to reactions with OH, O3, NO3, and Cl atoms, and in particular, the reaction with the OH radical is the major chemical loss process for the majority of organic compounds emitted into the troposphere (Medven et al., 1996; Sabljic and Peijnenburg, 2001).
Although activated carbon efficiently removes majority of organic contaminants, it is less effective in removing many heavy metals and micro-organisms in water [34].
Majority of organic matter is transformed into simple, mineralized form.
Heterocycles are the core structural motif in the majority of organic compounds, known so far [1, 2].
The vast majority of organic reactions today require organic solvents, many of which are environmentally hazardous and costly to dispose of.
The vast majority of organic compounds can be encoded into InChIs, but inorganic and organometallic compounds are still works in progress.
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Organic species constitute up to 90% of the atmospheric aerosol mass concentration in the submicron size range, with the majority of this organic mass being secondary organic aerosol (SOA) formed in the atmosphere.
The majority of sinking organic matter supplied to heterotrophic organisms in the twilight zone is in the form of marine snow, faecal pellets, and other particles of detritus.
0117 971 1908; thespicery.com Better Food Company, Bristol The majority of the organic veg and herbs come from the Community Farm in nearby Chew Magna.
Inositol hexakisphosphate (IP6) can constitute the majority of the organic phosphorus in soil.
Humic substances form the majority of natural organic matter (NOM) in soil.
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