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| Mannum Waterfalls in South Australia Photo Credit: © denisbin Creative Commons 2.0 |
A solution to a tricky groundwater riddle from Australia: Researchers at TU Wien have developed numerical models to simulate the movement of fluids in porous materials.
Things are complicated along the Murray–Darling River in southern Australia. Agricultural irrigation washes salt out of the upper soil layers, and this salt eventually ends up in the river. To prevent the river’s salt concentration from rising too much, part of the salty water is diverted into special basins. Some of these basins are designed to let the salty water evaporate, others to slowly release it in a controlled manner in the underground. That keeps salt temporarily out of the river and allows a better management of the river’s water—but increases the salinity in the ground. How can we calculate how this saltwater spreads underground and what its long-term effects will be?
Such questions are extremely difficult to answer, as several physical effects interact in complex ways. At TU Wien, researchers have now developed an efficient computer model that can run on supercomputers to calculate the spreading of fluids in porous materials—allowing the movement of saltwater in the soils, like in the case of the Murray–Darling River, to be predicted much more accurately. The same approach can also be applied to other problems, such as the dispersion of pollutants in groundwater.


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