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- W97048148 abstract "We initiated a field experiment in July of 1991 to determine the response of a deciduous forest to elevated soil temperatures. From July 1991 through June 1992, CO[sub 2] fluxes from control, disturbance control, and heated plots were 711, 791, and 1113 g C/m[sup 2]*yr, respectively. Over the period from July to November 1991, CO[sub 2] fluxes increased 47% due to warming. However, during the same period in 1992, CO[sub 2] fluxes increased only 9% due to warming. These results suggest that heating may have significantly reduced the amount of labile carbon in the soils of the heated plots. Heating also increased CH[sub 4] uptake by 0.21 9 C/m[sup 2]*yr and doubled net N mineralization rates. Unlike CO[sub 2] emissions, the changes in CH[sub 4] uptake and net N mineralization persisted throughout the first year of the experiment." @default.
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- W97048148 date "1993-06-01" @default.
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- W97048148 title "Trace gas fluxes and nitrogen availability in a deciduous forest after one year of elevated soil temperatures" @default.
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