Changes in global groundwater organic carbon driven by climate change and urbanization

Climate change and urbanization can increase pressures on groundwater resources, but little is known about how groundwater quality will change. Here, we use a global synthesis ( n  = 9,404) to reveal the drivers of dissolved organic carbon (DOC), which is an important component of water chemistry an...

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Veröffentlicht in:Nature communications 2020-03, Vol.11 (1), p.1279-10, Article 1279
Hauptverfasser: McDonough, Liza K., Santos, Isaac R., Andersen, Martin S., O’Carroll, Denis M., Rutlidge, Helen, Meredith, Karina, Oudone, Phetdala, Bridgeman, John, Gooddy, Daren C., Sorensen, James P. R., Lapworth, Dan J., MacDonald, Alan M., Ward, Jade, Baker, Andy
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Sprache:eng
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Zusammenfassung:Climate change and urbanization can increase pressures on groundwater resources, but little is known about how groundwater quality will change. Here, we use a global synthesis ( n  = 9,404) to reveal the drivers of dissolved organic carbon (DOC), which is an important component of water chemistry and substrate for microorganisms that control biogeochemical reactions. Dissolved inorganic chemistry, local climate and land use explained ~ 31% of observed variability in groundwater DOC, whilst aquifer age explained an additional 16%. We identify a 19% increase in DOC associated with urban land cover. We predict major groundwater DOC increases following changes in precipitation and temperature in key areas relying on groundwater. Climate change and conversion of natural or agricultural areas to urban areas will decrease groundwater quality and increase water treatment costs, compounding existing constraints on groundwater resources. Groundwater is Earth’s largest source of freshwater, but the cost and ease with which it is turned to drinking water is dependent on the concentration of organic carbon. Here the authors show that climate change and urbanization will likely elevate future levels of groundwater dissolved organic carbon across the globe.
ISSN:2041-1723
2041-1723
DOI:10.1038/s41467-020-14946-1