Source apportionment of the carbonaceous aerosol in Norway – quantitative estimates based on ¹⁴C, thermal-optical and organic tracer analysis

The mixed contribution of fossil-fuel and biomass burning sources has been observed towards carbonaceous species in N-BoB where as S-BoB is more influenced by biomass

global budget, only the fossil fuel burning and atmospheric growth rate terms are based primarily on empirical inputs supporting annual estimates in this carbon budget. The data

For comparison, annual time series of national carbon emissions from fossil fuel combus- tion and cement production for China, Japan and Korea taken from the CDIAC database

HOC: hydrocarbon-like organic carbon; OOC: oxy- genated organic carbon (secondary); COC: cooking organic carbon; BBOC: primary biomass burning organic carbon; OC urb − nf :

Annual mean posterior flux of the individual participat- ing inversions for (a) fossil fuel emission, (b) natural “fossil-fuel- corrected” global total carbon exchange, (c)

In the present study, source apportionment of the ambient summer and winter time particulate carbonaceous matter (PCM) in aerosol particles (PM 1 and PM 10 ) has been.. conducted

tal carbon (EC), organic carbon (OC), water-soluble organic carbon (WSOC), water- soluble inorganic ions (WSII), metal elements, organic compounds and stable carbon isotopic

Temperature profile and carbon evolution thermograms for thermal optical kinetic (TOK) analysis of NIST SRM 1515 (Apple Leaves) [A], SRM 2975 (Forklift Diesel Soot) [D], and the