J. Magid et al., SIZE-DENSITY FRACTIONATION FOR IN-SITU MEASUREMENTS OF RAPE STRAW DECOMPOSITION - AN ALTERNATIVE TO THE LITTERBAG APPROACH, Soil biology & biochemistry, 29(7), 1997, pp. 1125-1133
Decomposition rates have been elucidated by litterbag studies or in so
me instances by field-scale CO2 flux monitoring, but some deficiencies
are apparent in these methods. In a randomized block experiment with
additions of 0, 4 or 8 t of straw material the particulate organic mat
ter (POM > 100 mu m) was monitored for 20 months. During the first 4 m
onths the POM in the amended treatments decreased quite rapidly, and m
ore slowly during the remaining 16 months. By separating the total POM
into light (rho < 1.4 g cm(-3)) and heavy (rho > 1.4 g cm(-3)) fracti
ons, further resolution of the residue decomposition was possible. The
heavy fraction C was completely unaffected by the application of resi
dues, and apparently consisted mainly of ''native'' organic matter wit
h a low rate of decay. The differences in POM between treatments could
be attributed completely to differences in the light POM fraction. An
alysis of lignin and cellulose in light fractions from the 8 t treatme
nt showed that cellulose was preferentially utilized in the early stag
es of decomposition. The analysis also indicated that the initial lign
in concentration was high in the light fraction (20%) compared with th
at of the rape straw (15%). Thus the ''native'' light fraction must ha
ve been rich in lignin, which may explain the slower rate of decay of
light fraction in the unammended treatment. The estimates of decomposi
tion from POM were in qualitative agreement with estimates of decompos
ition based on field scale CO2 fluxes, but indicated a considerably hi
gher turnover in the initial phase of decomposition. This is of specia
l interest, since it has been recognized that the static chamber metho
d for estimating field scale CO2 fluxes underestimates high rates of C
O2 evolution, and thus the study of POM may be complementary to this a
pproach. Furthermore, it seems the study of POM may be an alternative
to the litterbag method in some instances. In contrast to the litterba
g method, POM fractionation approach allows the added residue to be co
mpletely exposed to the soil environment, and thus to the full range o
f faunal and other soil interactions. (C) 1997 Elsevier Science Ltd.