Carbon transfer from 14C‐labelled needles to mineral soil, and 14C‐CO2 production, in a young Pinus radiata Don stand

In forest ecosystems, few data are available on transfer rates of litterfall carbon (C) to mineral soil. Such data are, nevertheless, needed for predicting the effects of forest land-use change and management on soil C stocks. We here report the transfer of C from Pinus radiata litter to mineral soil over 117 weeks, using 14C-labelled needles mixed with unlabelled needles in lysimeters placed on the forest floor of a 5-year-old P. radiata stand. Mean annual temperature was about 12.9 degrees C and mean annual rainfall about 995 mm; the soil was a well-drained silt loam. Measurements were made at 39, 78 and 117 weeks of 14C in residual litter and in 10-mm increments of mineral soil to 50 mm depth and 25-mm increments from 50 to 100 mm depth. Measurements were also made of 14C-CO2 production, at frequent intervals over the first 5 weeks and then less frequently. Recovery of 14C in litter and mineral soil ranged from 51 to 66% at the different exposure times. Cumulative respired 14C-CO2, expressed as a percentage of the initially added 14C, increased from 16 to 19% after exposure times of 39 and 117 weeks, respectively. Total recovery of the added 14C did not differ significantly (P > 0.12) with time over the three measurement periods, with means ranging from 68 to 84%. Apparent losses of 14C were associated with large replicate variability, with coefficients of variation ranging from 20 to 31%, and with some disturbance of litter in the lysimeters by birds. We estimate that 1.0-2.2% of the litter 14C was transferred annually to 10-100-mm depth of mineral soil. On the basis of microbial biomass-14C measurements, this transferred C contained proportionately more microbial (labile) C than did the older total C in mineral soil. Results therefore are consistent with other studies on forests with well-developed organic horizons indicating that C in humified organic matter, rather than in newly fallen litter, is the main above-ground source for transfer of C to the mineral soil.