No abstract

Plant allocation patterns may affect soil C and N storage due to differences in litter quality and the depth of plant C and N inputs into the soil. We studied the dynamics of dual-labeled ( 13 C/ 15 N) Pinus ponderosa needles and fine roots placed at two soil depths (O and A horizon) in a temperate conifer forest soil during 2 y. Input of C as fine roots resulted in much more C retained in soil (70.5 ± 2.2% of applied) compared with needle C (42.9 ± 1.3% of applied) after 1.5 y. Needles showed faster mass loss, rates of soil 13 CO 2 efflux, and more 15 N immobilized into microbial biomass than did fine roots. The larger proportion of labile C compounds initially present in needles (17% more needle C was water soluble than in fine roots) likely contributed to its shorter C residence time and greater degree of transformation in the soil. A double exponential decay function best described the rate of 13 C loss, with a smaller initial pulse of C loss from fine roots (S 1 k 1 ) and a slower decay rate of the recalcitrant C pool for fine roots (0.03 y À1 ) compared with (0.19 y À1 ) for needles. Soil 13 C respiration, representing heterotrophic respiration of litter C, was much more seasonal from the O horizon than from the A. However, offsetting seasonal patterns in 13 C dynamics in the O horizon resulted in no net effect of soil depth on total 13 C retention in the soil after 1.5 y for either litter. Almost 90% of applied litter N was retained in the soil after 1.5 y, independent of litter quality or soil depth. Very small amounts of 13 C or 15 N (<3% of applied) moved to the horizon above or below the placement depth (i.e., O to A or A to O). Our results suggest that plant allocation belowground to fine roots results in more C retained and less N mineralized compared with allocation aboveground to needles, primarily due to litter quality differences.Abbreviations: CFE -chloroform fumigation extraction; DED -double exponential decay; IRMS -isotope ratio mass spectrometer; SED -single exponential decay; SOM -soil organic matter