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Carbon pool size and stability are affected by trees and grassland cover types within agroforestry systems of western Canada
- Baah-Acheamfour, Mark, Chang, Scott X., Carlyle, Cameron N., Bork, Edward W.
- Agriculture, ecosystems & environment 2015 v.213 pp. 105-113
- Picea, Populus, agricultural land, carbon sequestration, carbon sinks, climate, climate change, grasslands, land cover, land use, mineral soils, nitrogen, shelterbelts, silvopastoral systems, soil organic carbon, surface storage, trees, ultrasonics, Alberta
- Agroforestry systems are common land uses across Canada and could play a substantial role in sequestering carbon (C) as part of efforts to combat climate change. We studied the impact of component land cover types (forested vs. adjacent herbland) in three agroforestry systems (hedgerow, shelterbelt and silvopasture) on organic C and nitrogen (N) distribution in three density fractions of soils at the 0–10 and 10–30cm layers. The study evaluated 36 sites (12 hedgerows, 12 shelterbelts and 12 silvopastures) in central Alberta, Canada, distributed along a soil/climate gradient of increasing moisture availability. At the 0–10cm layer, soil organic C (SOC) stock in the bulk soil was significantly greater in the silvopasture system (101) than in either the hedgerow (77) or shelterbelt system (67Mg Cha−1). Soil organic C stock in both soil layers (0–10 and 10–30cm) was also significantly greater in the forested land cover (89 and 119Mg Cha−1, respectively) than in adjacent herblands (76 and 77Mg Cha−1). Across all sites, 31.5, 29.1, and 35.5% of SOC was found in the light fraction (<1.6gcm−3), occluded fraction (ultrasonic dispersion at 360W for 5min, <1.6gcm−3), and heavy fraction (>1.6gcm−3) of soils, respectively. The largest pool of SOC in the more labile light fraction of the 0–10cm layer was in the silvopasture system (50Mg Cha−1), whereas the smallest labile light fraction component of SOC was in the shelterbelt system (17Mg Cha−1). The largest pool of SOC in the more stable heavy fraction of both the 0–10 and 10–30cm depth classes was in the shelterbelt (33 and 35Mg Cha−1, respectively), while the least SOC was in the silvopasture system (26 and 20Mg Cha−1, respectively). We conclude that the presence of Populus based silvopasture system can increase C storage in surface mineral soils, and that the establishment of Picea based shelterbelts in an otherwise annually cropped agricultural landscape enhances the size of the stable SOC pool.