Soils at risk from biological and carbon decline
Tasmanian agricultural systems have relatively high organic carbon content (significantly greater than most of those on mainland Australia) due to climatic and soil influences (lower mean annual temperature and higher precipitation in Tasmania result in less oxidation of soil organic matter). Soil organic carbon
relates directly to productivity in agricultural soils. The relationship is a function of the organic carbon content in soil improving water holding capacity and nutrient availability, in addition to improving conditions for soil biological activity. Declining soil carbon levels across farmland of the Cradle Coast region are an issue for numerous aspects of soil health and farm productivity. Well-structured soils provide habitat for necessary organisms within the soil profile, with natural senescence of such soil organisms contributing to soil carbon stocks. Soil carbon itself has beneficial properties for soil structure, chemistry and microbiology, and soil carbon levels will reach a state of effective equilibrium based on land use and rainfall or irrigation. Excessive use of inputs, inadequate rest periods between intensive cropping or removal of carbon stocks at rates higher than biological processes can replace them, can lead to declining biological activity and the carbon that this activity facilitates the accumulation of.
outcome
By 2030, 30% of land managers in the region have adopted management practices to improve levels of soil organic carbon and biological activity.
threats
Local threats that can be addressed by NRM actions:
- Loss of natural capital
- Loss of production
- Reduction in economically viable enterprises in the region