Salinity refers to the concentration of dissolved salts in water or soil. Salt is a natural part of the environment and comes from several sources, including:
- Geological processes, such as the weathering of rocks and soils. Some rocks naturally contain salt, and as they weather over time, they release salt into the surrounding environment.
- Rainfall and runoff, which dissolve salt particles, making them mobile. This allows salt to be carried to new locations, including waterways and other parts of our landscapes.
- Wind can transport salinity through dust storms, spreading salt over long distances. Coastal winds can also carry salt particles inland, depositing new salt into areas far from the coast.
- Evaporation, which draws salt up from water tables, leaving it closer to the soil surface. This process can concentrate salts in the root zones of plants or in water bodies, where it has a greater impact on the surrounding ecosystem.
The balance between salt and water is delicate, with changes in one often impacting the other.
Irrigation, which increases the amount of water input into the landscape. Excess water can cause groundwater levels to rise, bringing mobile salts closer to the ground surface and concentrating them. The water used in irrigation may also have a high salt content, further increasing salinity in the area.
Land clearing, which disturbs natural water flows and accelerates salt accumulation. Clearing deep-rooted plants, whether perennial pastures or trees, can have an immediate impact on the water table, as there are no longer deep roots to absorb water and keep the water table down. This leads to higher water tables and increased salt levels closer to the soil surface.
Resources:
Dryland salinity – causes and impacts