Litter input, litter decomposition and the evolution of carbon dioxide in a beech woodland?Wytham woods, Oxford

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Abstract
Tree litter fall was measured from May 1969 to April 1973 and varied between 205 and 388 g m-2a-1. Peak standing crops of the ground flora were determined between September 1969 and October 1972 and fell in the range 17.3 to 20.9 g m-2 a-1. Litter losses due to wind action had a net value of 8 g m-2 a-1 and the mean above ground litter input to the soil was 235 g m-2 a-1. Between February 1971 and January 1973 above ground litter loss due to decomposition was calculated from litter standing crop depletions and litter turnover times. It was estimated to be 235.8 g m-2 a-1. Steady state conditions were thus assumed for this woodland. The contribution to litter from dying roots was estimated at 92 g m-2 a-1 and hence the total input of dead organic matter to the site was 327 g m-2 a-1. Soil metabolism, measured as carbon dioxide evolution, showed a significant correlation with temperature and during 1973–1974 had a dry matter equivalent of 342 g m-2 a-1. The difference between the above ground litter input (235 g m-2 a-1) and the dry matter equivalent of soil metabolism (342 g m-2 a -1) was attributed to the decomposition of root litter, root respiration and the respiratory activity of fungal mycorrhizae. Total organic matter decomposition accounted for 95% of total soil metabolism whilst the contributions by root and mycorrhizal respiration approximated 4 and 1%, respectively.