Soils at risk from structural decline and erosion
Soil structural decline through compaction is a threat and ongoing management issue for intensively farmed land under irrigation across the region. Compaction is the result of tillage operations or excessive traffic (animal or vehicular) when soil moisture conditions are less than optimal. Compaction leads to increased bulk density by reducing the volume of air and water in the soil and gives rise to poorer plant growth and root penetration, reduces the ability of water to infiltrate into the soil profile and increases the risk of surface runoff. Structural decline from excessive traffic at elevated soil moisture levels usually occurs during winter and spring in the Cradle Coast region from wet harvesting of crops and on densely stocked intensive grazing enterprises. Structural decline and low levels of ground cover increase the likelihood and severity of soil erosion from rainfall events and irrigation. Poor soil structure reduces water infiltration into the soil profile, with the resultant increase in surface runoff eroding soil particles as water moves downhill. In the absence of ground cover, raindrop impact causes surface sealing of soil also reduces water infiltration leading to increased surface runoff and greater risk of erosion.
outcome
By 2030, 30% of land managers in the region have adopted management practices to manage soil structure and stability and are actively implementing soil loss prevention practices in priority areas for erosion by water (hillslope) and wind (coastal and hinterland), as a result of new CCA projects.
threats
Local threats that can be addressed by NRM actions:
- Soil loss
- Loss of production
- Reduction in economically viable enterprises in the region
- Impacts on water quality, biodiversity and ecosystem function in freshwater and marine ecosystems