When floodwaters recede, where do they go?
The groundwater superhighway in the Sydney Basin transports water at a rate of up to 3 metres per day. Credit: Mather et al.
University of Sydney researchers have 聽a groundwater 鈥榮uperhighway鈥� along Australia鈥檚 east coast. Stretching from Canberra to Brisbane, the flow of water connects aquifers (underground layers of water-bearing permeable rock) that stretch for thousands of kilometres.
In the case of the recent ongoing floods 鈥� among the largest on record 鈥� these aquifers store a significant amount of floodwater 鈥� up to 20 percent of it. Floodwaters seep through rock layers into groundwater aquifers via stream beds and soil.
The study鈥檚 lead author, Dr聽Ben Mather聽from the聽School of Geosciences, said the aquifers are especially useful during drought conditions. 鈥淪urface and groundwater sources are connected. Groundwater acts as a buffer during flood and drought, by either soaking up or providing water supplies as the situation demands.鈥�
During flooding or bushfires, groundwater can also be a source of safe drinking water as overhead rock and soil layers filter contaminated surface water.
How fast is a drop of water?
Built from sediment from the Permian (around 300 to 250 million years ago) and Triassic (around 250 to 50 million years ago) geological periods, the superhighway transports groundwater from the Great Dividing Range into Sydney Harbour and off the continental shelf. On average, it takes a droplet of water 300 to 1,000 years to travel from its source to coastal aquifers.
Groundwater extraction threatens water security
The study, published in Nature鈥檚 Scientific Reports, also examined the impact of pumping (using groundwater for productive activities) on water reserves and conditions. 鈥淕rowing human reliance on surface water for urban use and groundwater for agriculture and mining are changing our naturally interconnected water system,鈥� Dr Mather said. 鈥淲e are now seeing widespread and long-lasting effects from the last 20 years of groundwater pumping.鈥�
Since the year 2000, groundwater pumping has resulted in a seven-metre drop in aquifers across eastern Australia, and up to 17 metres in agricultural regions. This leads to increased pressure on surface water supplies. It can also increase water salinity during drought conditions; as groundwater levels drop and stop naturally replenishing rivers, water evaporation leaves salt behind, with negative implications for rural and urban water users.
Declaration: This study was supported by the Office of the Chief Scientist and Engineer, NSW Department of Industry, and the AuScope Simulation, Analysis & Modelling node funded by the Australian Government, through the National Collaborative Research Infrastructure Strategy, NCRIS.
Hero image:聽Brisbane flood, the Centenary suburbs, 2011. Tatters via Flickr.聽