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      Greenhouse gas emissions from soils—A review

      , , , ,
      Chemie der Erde - Geochemistry
      Elsevier BV

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          FLUXNET: A New Tool to Study the Temporal and Spatial Variability of Ecosystem–Scale Carbon Dioxide, Water Vapor, and Energy Flux Densities

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            Carbon pools and flux of global forest ecosystems.

            Forest systems cover more than 4.1 x 10(9) hectares of the Earth's land area. Globally, forest vegetation and soils contain about 1146 petagrams of carbon, with approximately 37 percent of this carbon in low-latitude forests, 14 percent in mid-latitudes, and 49 percent at high latitudes. Over two-thirds of the carbon in forest ecosystems is contained in soils and associated peat deposits. In 1990, deforestation in the low latitudes emitted 1.6 +/- 0.4 petagrams of carbon per year, whereas forest area expansion and growth in mid- and high-latitude forest sequestered 0.7 +/- 0.2 petagrams of carbon per year, for a net flux to the atmosphere of 0.9 +/- 0.4 petagrams of carbon per year. Slowing deforestation, combined with an increase in forestation and other management measures to improve forest ecosystem productivity, could conserve or sequester significant quantities of carbon. Future forest carbon cycling trends attributable to losses and regrowth associated with global climate and land-use change are uncertain. Model projections and some results suggest that forests could be carbon sinks or sources in the future.
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              The global carbon dioxide flux in soil respiration and its relationship to vegetation and climate

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                Author and article information

                Journal
                Chemie der Erde - Geochemistry
                Chemie der Erde - Geochemistry
                Elsevier BV
                00092819
                October 2016
                October 2016
                : 76
                : 3
                : 327-352
                Article
                10.1016/j.chemer.2016.04.002
                93b174d1-fa98-46ce-96af-6826c13dc584
                © 2016
                History

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