SR24185Salinity in Calcarosols occurs through the presence of sodium, chloride, bicarbonate and sulfate ions, is caused by sodicity, and leads to decreased osmotic potential



Salinity occurs in alkaline sodic soils in Australia, but its effect in Western Australia is poorly understood. We determined the cause of salinity, the ions responsible, and their potential significance as constraints to crop growth on sodic soils. Our paper suggests that crop growth in affected landscapes is likely to be constrained by salinity with the adverse effects being more severe in dry than wet seasons.
SR24185 Abstract | SR24185 Full Text | SR24185PDF (2.1 MB) | SR24185Supplementary Material (1.8 MB) Open Access Article