摘要

The debate remains unresolved about soil erosion substantially offsetting fossil fuel emissions and acting as an important source or sink of CO2. There is little historical land use and management context to this debate, which is central to Australia%26apos;s recent past of European settlement, agricultural expansion and agriculturally-induced soil erosion. We use %26quot;catchment%26quot; scale (similar to 25 km(2)) estimates of Cs-137-derived net (1950s-1990) soil redistribution of all processes (wind, water and tillage) to calculate the net soil organic carbon (SOC) redistribution across Australia. We approximate the selective removal of SOC at net eroding locations and SOC enrichment of transported sediment and net depositional locations. We map net (1950s-1990) SOC redistribution across Australia and estimate erosion by all processes to be similar to 4 Tg SOC yr(-1), which represents a loss of similar to 2% of the total carbon stock (0-10 cm) of Australia. Assuming this net SOC loss is mineralised, the flux (similar to 15 Tg CO2-equivalents yr(-1)) represents an omitted 12% of CO2-equivalent emissions from all carbon pools in Australia. Although a small source of uncertainty in the Australian carbon budget, the mass flux interacts with energy and water fluxes, and its omission from land surface models likely creates more uncertainty than has been previously recognised.

  • 出版日期2014