Carbon sequestration by white spruce shelterbelts in Saskatchewan, Canada: 3PG and CBM-CFS3 model simulations

• Published in: Ecological modelling 2016-04, Vol.325, p.35-46
• Main Authors: Amichev, Beyhan Y., Bentham, Murray J., Kurz, Werner A., Laroque, Colin P., Kulshreshtha, Suren, Piwowar, Joseph M., Van Rees, Ken C.J.
• Format: Article
• Language: English
• Subjects: 3PG process-based tree growth model; aboveground biomass; Age; belowground biomass; Biomass; Carbon; carbon sequestration; carbon sinks; Carbon stocks maps; CBM-CFS3 stand-level C simulation model; data collection; ecological function; Ecology; ecosystems; Farmland afforestation; Flux; forests; land use change; Mathematical models; model validation; Picea glauca; Planted windbreaks and shelterbelts; planting; prairies; prediction; Raw materials; shelterbelts; simulation models; soil; soil erosion; tree growth; Trees
• ISSN: 0304-3800; 1872-7026
• DOI: 10.1016/j.ecolmodel.2016.01.003

•There are >60,000km of planted shelterbelts in Saskatchewan, Canada.•Two tree growth and C dynamics models were parameterized for use in shelterbelts.•The effects of tree mortality on C sequestration were greater than tree spacing.•C stocks increased by 106–195Mg Ckm−1 in 60yr due to shelterbelt planting.•C additions totaled 50,440Mg C province-wide in 991km of planted shelterbelts. For more than a century, planted shelterbelts in Saskatchewan, Canada have protected farmyards from the elements, decreased soil erosion, sequestered atmospheric carbon, as well as provided many other ecological functions. It is estimated that there are >60,000km of planted shelterbelts throughout the province, and considerably more in all of the Canadian Prairies. This paper details the overall process of quantifying and mapping the carbon stocks in white spruce (Picea glauca) shelterbelts planted in Saskatchewan. Shelterbelt data collected from field sampling sites, which were identified by a unique site selection approach, were used to parameterize two models for use in shelterbelt systems; an independent data set was used to validate model predictions. Shelterbelt tree growth was modeled with the Physiological Principles in Predicting Growth (3PG) model, and carbon flux and stocks in shelterbelts were modeled with the Carbon Budget Model of the Canadian Forest Sector (CBM-CFS3). Annual total ecosystem carbon (TEC) flux in white spruce shelterbelts increased one order of magnitude, from −0.33 to 4.4Mg Ckm−1yr−1, for age 1–25 years, and reached a peak of 5.5Mg Ckm−1yr−1 (age 39 years). An initial soil carbon loss from the shelterbelt, caused by the land-use change, was offset in full by tree growth by age 17, 18, and 21 years for trees planted at 2.0, 3.5, and 5.0m spacing within a row, respectively. Increase in carbon stocks, after 60 years of growth, was predicted in the litter layer (21.8Mg Ckm−1), belowground biomass (26.1Mg Ckm−1), and aboveground biomass (117.6Mg Ckm−1). Across all the different provincial soils, carbon additions were 106–195Mg Ckm−1 in 60-yr-old white spruce shelterbelts. Cumulatively, accounting for eight decades of white spruce shelterbelt planting and tree growth, carbon additions totaled 50,440Mg C province-wide in 991km of white spruce shelterbelts. The C additions represented 38% of the province-wide TEC stocks, which totaled 131,750Mg C. The cumulative carbon storage in all components of planted white spruce shelterbelts far exceeded the initia