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Carbon and Land Use Change
Using Forests to Sequester Carbon
Missing Carbon Sink
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].
Graph - CO2 release
Figure 1
For the decade of the 1980s the net release of carbon from changes in land use averaged 1.6±0.7 PgC/yr. In 1980 the net flux of 1.4 PgC from changes in land use was the difference between a release of 3.9 PgC from oxidation of dead vegetation, soil organic matter, and wood products and an uptake by regrowing ecosystems of about 2.5 PgC/yr).
For the decade of the 1980s, the global carbon cycle can be summarized as follows (units are PgC):
Atmospheric increase = Emissions from fossil fuels + Net emissions from changes in land use - Oceanic uptake - Missing carbon sink
3.3(±0.2) 5.5(±0.5) 1.6(±0.7) 2.0(±0.8) 1.8(±1.2)

For additional information on the "Missing carbon sink", see Missing Carbon.
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