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Changes in Soil Carbon Following Afforestation

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https://www.osti.gov/servlets/purl/1389525/
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Quantifying changes in soil C may be an important consideration under large-scale afforestation or reforestation. We reviewed global data on changes in soil C following afforestation, available from 43 published or unpublished studies, encompassing 204 sites. Data were highly variable, with soil C either increasing or decreasing, particularly in young (&lt;10-y) forest stands. Because studies varied in the number of years since forest establishment and the initial soil C content, we calculated change in soil C as a weighted average (i.e. sum of C change divided by sum of years since forest establishment) relative to the soil C content under previous agricultural systems at &lt;10 cm, &gt;10 cm and &lt;30 cm sampling depths. On average, soil C in the &lt;10 cm (or &lt;30 cm) layers generally decreased by 3.46% y<sup>–1</sup> (or 0.63% y<sup>–1</sup>) relative to the initial soil C content during the first five years of afforestation, followed by a decrease in the rate of decline and eventually recovery to C contents found in agricultural soils at about age 30. In plantations older than 30 years, C content was similar to that under the previous agricultural systems within the surface 10 cm of soil, yet at other sampling depths, soil C had increased by between 0.50 and 0.86% y<sup>–1</sup>. Amounts of C lost or gained by soil are generally small compared with accumulation of C in tree biomass.
提供机构:
Environmental System Science Data Infrastructure for a Virtual Ecosystem; Carbon Dioxide Information Analysis Center (CDIAC), Oak Ridge National Laboratory (ORNL), Oak Ridge, TN (United States)
创建时间:
2012-01-20
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