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Our work shows that for the years 1850 to 1990 about 112 PgC were released
to the atmosphere as a result of changes in land use, 85% from forests either
logged or converted to other uses, the rest largely from cultivation of prairie
soils (One Pg [petagram] = one billion metric tonnes = 1000 x one billion kg ).
The total loss of carbon from terrestrial ecosystems was 107 PgC, but about 10
PgC accumulated in wood products (e.g., buildings, furniture, paper, etc.). The
net increment in these wood products is the difference between harvests (about
68 PgC) and oxidation of products (about 58 PgC) over this 140-year period.
Another 15 PgC are estimated to have accumulated in dead plant material left in
forests after harvests.
Conversion
of natural ecosystems to croplands and pastures was responsible for net releases
to the atmosphere of 63 and 10 PgC, respectively. The net effect of logging and
regrowth was to release about 23 PgC. The annual rate at which carbon was
released to the atmosphere generally increased over the period 1850 to 1990 as
rates of deforestation increased [Figure 1]. |