Organic matter in Urbic Anthrosols often contains chemically and biological
ly inert organic carbon. This material, called black carbon (BC), originate
s from municipal wastes, coal-mine deposits and/or fly ash. This black carb
on needs to be differentiated from the other soil organic substances becaus
e of its very different physical and chemical nature. In this paper, we pro
pose a new method for determining BC, integrated into the humic fractionati
on procedure. The remaining organic carbon in the soil residue left after l
ipid extraction, alkaline extraction [0.5 M sodium hydroxide (NaOH)], and f
urther oxidation with 30% hydrogen peroxide (H2O2) is defined as inert orga
nic carbon or BC. The common fractions of soil organic matter, such as lipi
ds, fulvic and humic acids, and humins are thus supplemented with a new fra
ction, BC. According to our results by C-13-NMR spectroscopy, this fraction
consists mainly of polyaromatic hydrocarbons with few functional groups.