4.7 Article

Initial soil conditions outweigh management in a cool-season dairy farm's carbon sequestration potential

Journal

SCIENCE OF THE TOTAL ENVIRONMENT
Volume 809, Issue -, Pages -

Publisher

ELSEVIER
DOI: 10.1016/j.scitotenv.2021.152195

Keywords

Soil carbon; Carbon dioxide; Nitrous oxide; Management intensive grazing; Pasture management

Funding

  1. United States Department of Agriculture National Institute of Food and Agriculture (USDA NIFA) Organic Transitions Program [2015-51106-23967]
  2. USDA Current Research Information System (CRIS) [1915-12630-001-00D]
  3. New Hampshire Innovation Research Center (NHIRC)
  4. NIFA [810510, 2015-51106-23967] Funding Source: Federal RePORTER

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This study examined the potential of Management Intensive Grazing (MIG) pastures in the northeastern United States to store carbon in soils. The findings showed that MIG grazing increased soil carbon content, especially in fields with lower initial soil carbon. Modeled simulations also indicated that soil physio-chemical status had a greater impact on carbon storage than grazing intensity, with continuous grazing leading to a decline in soil carbon.
Pastures and rangelands are a dominant portion of global agricultural land and have the potential to sequester carbon (C) in soils, mitigating climate change. Management intensive grazing (MIG), or high density grazing with rotations through paddocks with long rest periods, has been highlighted as a method of enhancing soil C in pastures by increas-ing forage production. However, few studies have examined the soil C storage potential of pastures under MIG in the northeastern United States, where the dairy industry comprises a large portion of agricultural use and the regional ag-ricultural economy. Here we present a 12-year study conducted in this region using a combination of field data and the denitrification and decomposition (DNDCv9.5) model to analyze changes in soil C and nitrogen (N) over time, and the climate impacts as they relate to soil carbon dioxide (CO2) and nitrous oxide (N2O) fluxes. Field measurements showed: (1) increases in soil C in grazed fields under MIG (P = 0.03) with no significant increase in hayed fields (P = 0.55); and (2) that the change in soil C was negatively correlated to initial soil C content (P = 0.006). Modeled simulations also showed fields that started with relatively less soil Chad significant gains in C over the course of the study, with no significant change in fields with higher initial levels of soil C. Sensitivity analyses showed the physio-chemical status of soils (i.e., soil C and clay content) had greater influence over C storage than the intensity of grazing. More extensive grazing methods showed very little change in soil C storage or CO2 and N2O fluxes with modeled continuous grazing trending towards declines in soil C. Our study highlights the importance of considering both initial system conditions as well as management when analyzing the potential for long-term soil C storage.

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