Soil Carbon Cycling in a Temperate Forest: Radiocarbon-Based Estimates of Residence Times, Sequestration Rates and Partitioning of Fluxes

• Published in: Biogeochemistry 2000-10, Vol.51 (1), p.33-69
• Main Authors: Gaudinski, Julia B., Trumbore, Susan E., Davidson, Eric A., Zheng, Shuhui
• Format: Article
• Language: English
• Subjects: Carbon; Carbon cycle; Carbon dioxide; Decomposition; Detritus; Earth sciences; Earth, ocean, space; Exact sciences and technology; Forest soils; Geochemistry; Isotope geochemistry; Isotope geochemistry. Geochronology; Leaf litter; Leaves; Microorganisms; Organic matter; Organic soils; Plant litter; Radiocarbon; Reservoirs; Respiration; Settlers; Soil air; Soil and rock geochemistry; Soil depth; Soil ecology; Soil horizons; Soil organic matter; Soil respiration; Soils; Surficial geology; Temperate forests; Turnover time
• ISSN: 0168-2563; 1573-515X
• DOI: 10.1023/a:1006301010014

Temperate forests of North America are thought to be significant sinks of atmospheric CO2. We developed a below-ground carbon (C) budget for well-drained soils in Harvard Forest Massachusetts, an ecosystem that is storing C. Measurements of carbon and radiocarbon (14C) inventory were used to determine the turnover time and maximum rate of CO2 production from heterotrophic respiration of three fractions of soil organic matter (SOM): recognizable litter fragments (L), humified low density material (H), and high density or mineral-associated organic matter (M). Turnover times in all fractions increased with soil depth and were 2-5 years for recognizable leaf litter, 5-10 years for root litter, 40-100+ years for low density humified material and > 100 years for carbon associated with minerals. These turnover times represent the time carbon resides in the plant + soil system, and may underestimate actual decomposition rates if carbon resides for several years in living root, plant or woody material. Soil respiration was partitioned into two components using 14C: recent photosynthate which is metabolized by roots and microorganisms within a year of initial fixation (Recent-C), and C that is respired during microbial decomposition of SOM that resides in the soil for several years or longer (Reservoir-C). For the whole soil, we calculate that decomposition of Reservoir-C contributes approximately 41% of the total annual soil respiration. Of this 41%, recognizable leaf or root detritus accounts for 80% of the flux, and 20% is from the more humified fractions that dominate the soil carbon stocks. Measurements of CO2 and 14CO2 in the soil atmosphere and in total soil respiration were combined with surface CO2 fluxes and a soil gas diffusion model to determine the flux and isotopic signature of C produced as a function of soil depth. 63% of soil respiration takes place in the top 15 cm of the soil (O + A + Ap horizons). The average residence time of Reservoir-C in the plant + soil system is 8±1 years and the average age of carbon in total soil respiration (Recent-C + Reservoir-C) is 4±1 years. The O and A horizons have accumulated 4.4 kgC m-2 above the plow layer since abandonment by settlers in the late-1800's. C pools contributing the most to soil respiration have short enough turnover times that they are likely in steady state. However, most C is stored as humified organic matter within both the O and A horizons and has turnover times from 40 to 100+ years respecti