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      Land-Use Intensity Effects on Soil Organic Carbon Accumulation Rates and Mechanisms

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      Ecosystems
      Springer Nature

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          Most cited references48

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          Aggregate Structure and Carbon, Nitrogen, and Phosphorus in Native and Cultivated Soils1

          E. Elliott (1986)
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            THE TURNOVER OF SOIL ORGANIC MATTER IN SOME OF THE ROTHAMSTED CLASSICAL EXPERIMENTS

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              Greenhouse gases in intensive agriculture: contributions of individual gases to the radiative forcing of the atmosphere

              Agriculture plays a major role in the global fluxes of the greenhouse gases carbon dioxide, nitrous oxide, and methane. From 1991 to 1999, we measured gas fluxes and other sources of global warming potential (GWP) in cropped and nearby unmanaged ecosystems. Net GWP (grams of carbon dioxide equivalents per square meter per year) ranged from 110 in our conventional tillage systems to -211 in early successional communities. None of the annual cropping systems provided net mitigation, although soil carbon accumulation in no-till systems came closest to mitigating all other sources of GWP. In all but one ecosystem, nitrous oxide production was the single greatest source of GWP. In the late successional system, GWP was neutral because of significant methane oxidation. These results suggest additional opportunities for lessening the GWP of agronomic systems.
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                Author and article information

                Journal
                Ecosystems
                Ecosystems
                Springer Nature
                1432-9840
                1435-0629
                May 23 2007
                April 17 2007
                : 10
                : 1
                : 59-74
                Article
                10.1007/s10021-006-9010-y
                242dd859-c091-4d8b-a9af-d60db651c617
                © 2007
                Product
                Self URI (article page): http://link.springer.com/10.1007/s10021-006-9010-y

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