Agricultural systems are leaky and losses of phosphorus, nitrogen, organic matter and suspended solids can impact on water quality.
While direct contamination of surface water can be prevented by avoiding livestock access and effluent discharge, it is less straightforward to prevent losses over and through soil that can eventually reach waterways.
These less direct losses are affected by complex hydrological and chemical factors.
Gypsum has long been used as a soil conditioner and fertiliser but it is only recently that gypsum's potential for reducing agricultural emissions to waterways has been researched.
Gypsum (CaSO4.2H2O) can improve soil aggregation through calcium-induced flocculation of particles and sulfate-induced leaching of excess sodium.
Such effects can reduce surface runoff volume by improving water infiltration into soil.
Improved stability of aggregates reduces the potential loss of soil particles to waterways both over and through soil.
The calcium ions can also increase precipitation of phosphate ions either directly as calcium phosphate or indirectly by increasing availability of aluminium ions.