“…With AMS, the measurement of 14C in various chemical fractions of interest is also possible. The method has been used to determine the fossil contribution to "organic" (i.e., volatile or oxidizable) and "elemental" (nonvolatile or nonoxidizable) carbon in atmospheric particles (9, 10), to atmospheric GH4 and CO (8,25), and to low-polarity organic compounds (LPCs) extracted from aerosols (9).…”