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World’s Soil Resources

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Figure 14.7 <strong>Soil</strong> organic carbon change in Canada 201. Source: Clearwater et al., 2015.<br />

14.5.2 | <strong>Soil</strong> organic carbon change<br />

The soil organic carbon (SOC) change indicator used in the national Agri-Environmental Indicators<br />

programme assesses how organic C levels are changing over time in Canadian agricultural soils. The indicator<br />

is based on the method used for the Canadian National Inventory Report (Environment Canada, 2014). The<br />

indicator uses the Century model (NREL, 2007) to predict the rate of change of organic C content in Canada’s<br />

agricultural soils due to the effects of land management change since 1951. These include changes in tillage<br />

and summer fallow frequency, and change between annual crops and perennial hay or pasture. It includes<br />

land use changes such as clearing forests for agriculture or breaking native grass for cropland, but does not<br />

include the loss of C from the above-ground forest biomass.<br />

No changes in SOC were assumed if there were no indicated changes in land use or land management. The<br />

SOC change indicator does not consider soil erosion.<br />

The SOC change indicator results are presented (Figure 14.7) as the percentage of total cropland that falls<br />

into each of five SOC change classes expressed in kilograms per ha per year (kg ha -1 yr -1 ). Negative values<br />

represent a loss of SOC from the soil and positive values represent a gain of SOC.<br />

Status of the <strong>World’s</strong> <strong>Soil</strong> <strong>Resources</strong> | Main Report Regional Assessment of <strong>Soil</strong> Changes<br />

463<br />

in North America

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