Monterey Herald

‘FOSSIL WATER’ MAY BE VANISHING

New study finds 7 percent of state’s drinking wells are tapping ancient water stores

- By Allison Gasparini newsroom@montereyhe­rald.com

A dinosaur bone. The footprint of a woolly mammoth. An ancient shell imprinted on a rock in your backyard.

These are the images the word “fossil” calls to mind. But, buried deep within the earth, there’s another kind of fossil you might not expect — ancient aquifers, created by rain and snow that fell more than 10,000 years ago. And unless the fossil water stores are better protected, scientists say, they may become a thing of the past.

New research on fossil water from Lawrence Livermore National Laboratory suggests that drinking wells that pump fossil water can’t rely on it being replenishe­d — especially during times of drought.

“It’s just like taking gold out of the ground, out of a moun

tain,” said Menso de Jong, a groundwate­r management consultant at Kear Groundwate­r in Santa Barbara. “The gold is not going to grow back.”

The new Lawrence Livermore study found clear evidence that 7% of the 2,330 California’s drinking wells tested are producing fossil water — and 22 percent of the wells analyzed are pumping mixed-age water containing at least some ancient water. That means that many California­ns are already using fossil water to shower, flush their toilets and irrigate their lawns without knowing it.

On the Central Coast, the Lawrence Livermore research team found fossil water in some of the deeper portions of the Salinas Valley’s aquifer system where the groundwate­r is not now being replenishe­d through Monterey County’s water recy

cling programs.

Scientists say that further mapping out where fossil water is located and pinpointin­g the areas that rely on the ancient resource could help lead to better groundwate­r management and ensure that supplies are sustained to meet future needs.

If managers can determine how much is left, they can then ration it and work on strategies for replenishi­ng the ancient wells.

Excessive agricultur­al and urban water use has depleted many of California’s aquifers, which serve as massive undergroun­d reservoirs. In some areas,

the problem is so severe that the land is subsiding — permanentl­y in some cases.

California’s first- ever groundwate­r protection law, passed by the Legislatur­e in 2014, requires local agencies to make their aquifers “sustainabl­e” by 2042 at the latest. And that has increased the need for further understand­ing and mapping the worlds of trapped water. The new research will help identify where water is being pumped faster than it can be renewed — a critical step toward sustaining water resources to meet future needs.

Fossil water, or “paleowater,” is most commonly defined as water that seeped into the ground during the last Ice Age, when woolly mammoths roamed the earth. The water filled the porous cracks between rocks and grains of sand in a process known as “recharging.”

“Modern” groundwate­r also recharges. But because ancient hydrology was quite different from current conditions — in general, it was a lot cooler and wetter — the paleowater won’t be replenishe­d for hundreds or even thousands of years.

Determinin­g the age of water isn’t easy. The Lawrence Livermore research team, which also included scientists from Cal State East Bay and UC Santa Barbara, tested wells across the state using radioactiv­e isotopes such as tritium.

Though tritium is a naturally occurring element, tritium levels rose in the last century with the advent of nuclear testing. Finding detectable levels of the isotope in water sources indicates to scientists that the water recharged in modern times as opposed to eons ago when levels were much lower.

Paleowater in the Golden State is more likely to be found in the dry south

western part of the Central Valley — between Los Banos and Lemoore — and in Southern California’s deserts in places such as Joshua Tree National Park and Coachella Valley towns like Palm Desert. This is because groundwate­r supplies are often naturally replenishe­d in mountainou­s regions that get a lot of rain. In desert regions, however, the amount of rainfall isn’t enough to replenish the aquifers after the water is pumped to the surface.

Pumping fossil water is hardly new. Arid countries such as Yemen, Jordan and Libya have been using it for years to fill critical needs — but the ancient aquifers are now running frightenin­gly low.

Because fossil water fell from the sky thousands of years ago, there’s a greater risk of depleting the resource, scientists say.

“It’s kind of like a bank account,” said Ate Visser, a research scientist at Lawrence Livermore who co-authored the study on the finite nature of fossil water. “If you start withdrawin­g from your bank account but you have no income, at some point it’s going to run out.”

Knowing how much paleowater is left in a production well is not the only concern scientists have when it comes to the ancient water. A 2017 study published in the journal Nature Geoscience showed that wells that pump fossil water are also at risk for contaminat­ion.

“Even these ancient waters that tend to be tens or hundreds of meters undergroun­d are not safeguarde­d,” said Scott Jasechko, a water scientist at UC Santa Barbara who was the lead author of the contaminat­ion study.

“Just because you drill a deep well into fossil groundwate­r doesn’t mean the quality of that water is going to be pristine,” said

Jasechko, whose study argues that water managers should consider the risk of outside contaminan­ts when ensuring the safety of paleowater.

The slow renewal of groundwate­r could affect whether homes, offices and stores are built in these areas in the future.

Areas that rely on paleowater could face building moratorium­s if the water mining continues, said de Jong, who worked on the Lawrence Livermore study as a graduate student at UC Santa Barbara.

“There are some areas in these desert regions where it is very difficult now to get a permit to either drill a new well or really even to build a new house,” de Jong said.

Finding a way to mimic the natural recharge cycle, he said, might be the only way to stop the fossil water from eventually disappeari­ng.

Visser suggests that California communitie­s consider using treated flood water to replenish groundwate­r resources — an increasing­ly popular idea that is extremely costly and bound to face political opposition.

In addition, communitie­s could prevent depletion of fossil water stores by tapping river water during the rainy season, Visser said.

Ultimately, water managers will need to ensure the water pumped out of California wells is renewed at a sustainabl­e pace. And to do so, scientists say, there must be greater research about the water’s vintage and origins.

According to de Jong, “I don’t think there’s any debate at all that the system that humans have set up in California in the last hundred years will need some alteration­s in order to encourage more groundwate­r recharge.”

 ?? SCOTT SMITH — THE ASSOCIATED PRESS ?? A foreman in 2014works on drilling an 800-foot-deep well at an almond farm in Madera County. During California’s five-year drought, desperate Central Valley farmers were forced to rely more on deeper wells, including some that tapped “fossil water” stores, to irrigate their crops.
SCOTT SMITH — THE ASSOCIATED PRESS A foreman in 2014works on drilling an 800-foot-deep well at an almond farm in Madera County. During California’s five-year drought, desperate Central Valley farmers were forced to rely more on deeper wells, including some that tapped “fossil water” stores, to irrigate their crops.
 ?? KARIS MCFARLANE, LAWRENCE LIVERMORE NATIONAL LABORATORY ?? Ate Visser, a hydrologis­t for the Lawrence Livermore National Laboratory, collects groundwate­r samples in copper tubes for helium isotope analyses. The tests reveal the age of the water.
KARIS MCFARLANE, LAWRENCE LIVERMORE NATIONAL LABORATORY Ate Visser, a hydrologis­t for the Lawrence Livermore National Laboratory, collects groundwate­r samples in copper tubes for helium isotope analyses. The tests reveal the age of the water.

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