Abstract
AbstractRemoval of biomass for bioenergy production may decrease soil organic carbon. While perennials or cover‐cropped grains often have greater root production than annual grain crops, they variably impact soil carbon and underlying mechanisms remain unclear. We used high‐frequency measurements of soil respiration and natural abundance carbon stable isotopes to differentiate respiration sources, pool sizes, and decomposition rate constants during a 10 month incubation of soils collected to 1 m depth from a 10 year old field experiment in Iowa, United States. Conversion of corn–soybean rotations to reconstructed prairies or addition of a rye cover crop to continuous corn significantly altered respiration sources and dynamics of fast‐ and slow‐cycling carbon (turnover times of weeks to months–years, respectively), but had little effect on bulk soil carbon and several extractable pools (except in fertilized prairie). Both unfertilized and fertilized prairies increased slow‐cycling carbon pools relative to annual crops, but only in 0–25 cm soil. Compared with fertilized prairie, the unfertilized prairie significantly increased decomposition rates of fast‐ and slow‐cycling carbon pools in 0–25 cm soil, likely explaining the lack of significant bulk soil carbon accrual despite twofold greater root production. Carbon derived from C4 plants decomposed faster than C3‐derived carbon across all depths and cropping systems and contributions of C3‐carbon to respiration increased with depth. Respiration of cover crop‐derived carbon was greatest in 0–25 cm soil but comprised >25% of respiration below 25 cm, implying a disproportionate impact of the cover crop on deep soil metabolism. However, the cover crop also increased the decomposition rates of fast‐ and slow‐cycling carbon pools and decreased their pool sizes across all depths relative to corn without a cover crop. Despite their notable environmental benefits, neither unfertilized perennials nor cover crops necessarily promote rapid soil carbon sequestration relative to conventional annual bioenergy systems because of concomitant increases in decomposition.
Highlights
Potential environmental benefits of bioenergy cropping systems substantially depend on their impacts to soil biogeochemical processes, those related to soil organic carbon (SOC) accumulation and retention of nutrients (Lemus & Lal, 2005; Robertson et al, 2017)
We hypothesized that (a) soil CO2 fluxes and δ13C values vary among cropping systems even when C pools are indistinguishable; (b) prairie vegetation and a rye cover crop grown with continuous corn increase the size of fast‐ and slow‐ cycling SOC pools relative to annual crops in surface and subsurface soil; (c) C4‐C derived from corn and warm‐season prairie grasses dominates C pools and respiration among all treatments and depths
Soils from the bioenergy cropping systems examined here had few measurable differences in concentrations of total SOC and C released in several extraction solutions, even when sampled after 10 growing seasons (Tables 1 and 2)
Summary
Potential environmental benefits of bioenergy cropping systems substantially depend on their impacts to soil biogeochemical processes, those related to soil organic carbon (SOC) accumulation and retention of nutrients (Lemus & Lal, 2005; Robertson et al, 2017). The objectives of this study were to: (a) explore the impacts of diversified cropping systems on soil CO2 fluxes and their δ13C values, as compared with continuous corn and corn/soybean rotations; (b) characterize the sizes and turnover rates of fast‐ (days–months) and slow‐ (years–decades) cycling soil C pools under different cropping systems and at different depths; (c) determine the relative contributions of different C inputs (e.g., C4 vs C3) as sources of soil respiration among cropping systems. We hypothesized that (a) soil CO2 fluxes and δ13C values vary among cropping systems even when C pools are indistinguishable; (b) prairie vegetation (perennial grasses/forbs) and a rye cover crop grown with continuous corn increase the size of fast‐ and slow‐ cycling SOC pools relative to annual crops in surface and subsurface soil; (c) C4‐C derived from corn and warm‐season prairie grasses dominates C pools and respiration among all treatments and depths
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