Flinders PhD graduate Tom Anderson led a study of Scott Creek, a high rainfall area, that shows the combination of time and volume of water flow has resulted in salt regression through it being flushed from the water table.
He believes the methodology could have wide application across Australia — especially in areas where streams and rivers have been affected by high salinity.
Dryland salinity occurs after deep-rooted native vegetation, mainly gum trees, has been cleared and replaced with short-rooted agricultural crops, which allows more rainfall to infiltrate into groundwater and subsequently raise the water table.
Historical salts built up over thousands of years can therefore discharge into surface water, but a finite mass of historical salts mean that streams become less saline as salt is eventually flushed from the system.
In the case of Scott Creek, a return to salt equilibrium is happening faster than expected — within about 300 years of the area being deforested — noting that continued rainfall and drainage are key factors to ensure continued change.
Mr Anderson said the results came as a surprise, emerging as an important side-project into his examination of salinity trends.
Now, he believes this new way of assessing existing high-resolution data will reveal fresh insights for a range of waterways in different locations across Australia.
‘‘Now it’s time to go into other areas to apply the same testing methodology — in areas of lower rainfall, and subject to more extreme salinity damage,’’ Mr Anderson said.
‘‘Fortunately, for the interest of future studies, many rivers throughout South Australia and around the world contain such data.’’
Theories of reaching a new salt equilibrium have been explored by scientists since the 1970s, but this is the first study to reveal a statistically significant trend that shows a stream returning to a new salt equilibrium.
A 28-year record of flow and salinity in Scott Creek between 1989 and 2016 was analysed, based on monthly data, finding that about three times more salt was leaving the catchment when salt deposited in rainfall was compared to salt exported from Scott Creek.
During the time period investigated, salt load exported to surface water decreased by an average 6.4 tonnes annually due to catchment freshening.
The stream could reach a new and lower salinity level by 2090 if this trend continues at a constant rate.
Mr Anderson said evidence of a catchment returning to the original salinity levels before European settlement was ‘‘exciting news’’ for farmers, as areas continued to face salinity issues.
