The reserves of carbon in peat deposits and peaty and peat bog soils o
f Russia comprise 44.2 Gt C of humic substances (37.3% of the total re
serve of C), 44.7 Gt C (37.8%) of insoluble residue, and 21.1 Gt C (17
.8%) of polysaccharides, The carbon pool of humic acids constitutes 25
.0 Gt and that of fulvic acids reaches 19.1 Gt. Humic acids predominat
e in low-moor peat, whereas fulvic acids predominate in high-moor peat
. Transitional pear deposits contain approximately equal amounts of fu
lvic and humic acids. About 89-91% of the carbon of humic substances i
n different types of peat is represented by heterogeneous complexes of
the first and third fractions.