Melissa Fraser Image
Melissa’s research aims to understand the causes of structural decline occurring in saline Vertosols as they become sodic through the combined effects of declining rainfall and artificial drainage. Her research was motivated by the concern of land owners on this soil type in the Upper South East of South Australia. Reductions in watertable levels have occurred, along with a steady decline in annual rainfall, throughout this region since the early 1990s.
Lowering of the watertable has facilitated the leaching of salts from the uppermost horizons of the soil profile with the consequent development of sodicity (ESP >30% in most cases). It is hypothesised that the location, geographic extent and severity of sodicity are a result of a seasonally variable saline watertable, landform, variability in soil type and properties of soil horizons.
Melissa’s research falls into the CRC’s Program 2 research area.
For more information, email Melissa.