Increased ionic strength of soil solutions due to dissolution of gypsum may also increase adsorption of phosphate ions and organic matter to soil particles.
These multiple modes of action can partially address both hydrological and chemical factors influencing nutrient losses. Gypsum application has been reported to at least halve phosphorus losses in some conditions but results have varied between experiments.
Variability may be partly due to experimental design (insufficient time for gypsum to take effect in the soil, or high simulated rainfall conditions) but could also be related to soil type and existing exchangeable calcium level in the soil.
An understanding of the causes of variability will assist in the choice of target areas for optimal economic use of gypsum to reduce phosphorus losses.
Surface runoff of nitrogen, organic matter and soil particulates, as well as drainage losses of of nutrients in organic form can also be reduced with gypsum.
The reduction in losses of organic forms of nutrients may be particularly important for mitigating effluent application losses.
Reducing nutrient loss
Gypsum is calcium sulfate (CaSO4.2H2O) and provides a readily available source of calcium and sulfate ions due to its partial solubility. It has been used for decades as a soil conditioner and fertiliser (Shainberg et al., 1989) but it is in comparatively recent years that gypsum's ability to reduce nutrient losses has been researched.
Soil structural improvement resulting from gypsum application can include reduced surface crusting and sealing, improved water infiltration (reducing potential for runoff), soil aggregation, drainage and aeration with subsequent benefits for plant growth.
Benefits to plant growth, including root condition, may also result from the calcium and sulphur nutrition provided by gypsum. In the case of sodium build up which can result from some effluent types (dairy factory effluent in particular), there is a clear benefit in assisting the leaching of sodium, benefiting soil structure particularly where there is dispersive clay.