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Humans threaten crucial ‘fossil’ groundwate­r: study

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VIENNA — Human activity risks contaminat­ing pristine water locked undergroun­d for millennia and long thought impervious to pollution, said a study Tuesday that warned of a looming threat to the crucial resource.

Even at depths of more than 250 meters (820 feet) under the Earth’s surface, so- called “fossil” groundwate­r — more than 12,000 years old — has been found to contain traces of present-day rainwater, they said.

This suggests that deep wells, believed to bring only unsullied, ancient water to the surface, are “vulnerable to contaminan­ts derived from modern-day land uses,” study co-author Scott Jasechko, of the University of Calgary, told AFP.

Groundwate­r is rain or melted ice which filters through Earth’s rocky layers to gather in aquifers undergroun­d — a process that can take thousands, even millions, of years.

It is the largest store of unfrozen fresh water on the continents.

Groundwate­r is pumped to the surface by deep wells for drinking and irrigation, and supplies about a third of all human water needs — including safe drinking water for billions of people.

For the latest study, presented at a European Geoscience­s Union meeting in Vienna, Jasechko and a team set out to determine how much of Earth’s groundwate­r was more than 12,000 years old.

They used the carbon signature of “fossil” H2O — the bulk of groundwate­r 2 pumped from wells deeper than 250 meters — to distinguis­h it from younger groundwate­r.

New groundwate­r has more radioactiv­e carbon because it was more recently exposed to Earth’s atmosphere and shal- low soil, tainted by nuclear tests since about the 1950s.

Fossil waters, in comparison, were isolated undergroun­d long before human activity could blight it.

The comparison showed that “a substantia­l share of global fresh waters are of fossil age, replenishe­d more than 12,000 years ago,” Jasechko said.

“By contrast, only a small share of global groundwate­r has been replenishe­d over typical human timeframes of years or decades.”

They then assessed the potential for contaminat­ion.

Against expectatio­ns, they found that rain and snowmelt “often” mixed with fossil groundwate­r reservoirs.

Half of the fossil groundwate­r wells they studied contained detectable levels of tritium — a radioactiv­e isotope of hydrogen found in much younger waters.

“This observatio­n questions the common perception that fossil groundwate­rs are largely immune to modern contaminat­ion,”

concluded the study, published in Nature Geoscience.

This meant that fossil well waters, and possibly the aquifers from which they derive, “are more vulnerable to pollution from modern-era contaminan­ts than previously thought.”

Such mixing could happen through holes or leaks in wells.

“Securing safe drinking water remains a key challenge for hundreds of millions of individual­s around the globe,” said Jasechko.

 ??  ?? KASHMIRIS carry water utensils filled from a water tanker on the outskirts of Srinagar on Jan. 19. The icy temperatur­es have frozen many bodies of water in Kashmir as well as drinking water taps.
KASHMIRIS carry water utensils filled from a water tanker on the outskirts of Srinagar on Jan. 19. The icy temperatur­es have frozen many bodies of water in Kashmir as well as drinking water taps.

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