Ri. Barbosa et Pm. Fearnside, PASTURE BURNING IN AMAZONIA - DYNAMICS OF RESIDUAL BIOMASS AND THE STORAGE AND RELEASE OF ABOVEGROUND CARBON, JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 101(D20), 1996, pp. 25847-25857
Aboveground biomass in cattle pasture converted from tropical dense fo
rest was studied both before and after reburning in Brazilian Amazonia
. In a 7-year-old pasture studied in Apiau, Roraima, the aboveground d
ry weight of biomass (live plus dead) exposed to burning consisted of
96.3 t ha(-1) of original forest remains, 6.2 t ha(-1) of secondary su
ccessional vegetation (woody invaders in the pasture), and 8.0 t ha(-1
) of pasture grass (carbon contents 48.2%, 45.4%, and 42.2%, respectiv
ely). In terms of carbon, burning efficiencies for these three categor
ies were 13.2%, 66.7% and 94.6%, respectively. Net charcoal formation
was 0.35 t C ha(-1) or 0.63% of the carbon exposed to the reburn, whil
e the total accumulated since conversion (including the initial burn)
is estimated at 2.3 t ha(-1) (1.82% of the predeforestation abovegroun
d biomass carbon stock). The dynamics of the original forest remains w
ere represented in simulations that included parameters such as charco
al formation, burning efficiency and carbon concentration in different
biomass components. Releases from initial burning of the cleared fore
st (44.0 t C ha(-1)) plus releases over the course of the succeeding d
ecade through combustion (12.5 t C ha(-1)) and decay (51.5 t C ha(-1))
total 92% of the original forest biomass carbon (126 t C ha(-1)). Of
biomass carbon remaining after the initial burn (84.3 t C ha(-1)), 76.
0% is released: 61.1% through decay and 14.9% through combustion in re
burns, while 1.2% is net conversion to charcoal in the reburns. These
results indicate an amount of charcoal accumulation that is smaller th
an some carbon calculations have assumed, therefore suggesting a great
er impact on global warming from conversion of forest to pasture.