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University of Utah Reveals Freshwater Reservoir Beneath Great Salt Lake

· Confirmed

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In Short: Researchers from the University of Utah have discovered a vast reservoir of freshwater beneath the Great Salt Lake, according to a new study published in Attheu.

Great Salt Lake by Sentinel-2
Photo: Copernicus Sentinel-2, ESA / Wikimedia Commons (CC BY-SA 3.0 igo)

Researchers from the University of Utah have discovered a vast reservoir of freshwater beneath the Great Salt Lake, according to a new study published in Attheu. The study used airborne electromagnetic (AEM) surveys to map the freshwater reservoir beneath the lake’s hypersaline surface.

The analysis shows that freshwater saturates the sediments beneath the lake to depths of 3 to 4 kilometers, or about 10,000 to 13,000 feet. This discovery was made possible by measuring electrical resistivity to a depth of about 100 meters via airborne electromagnetic surveys, which helped distinguish freshwater from brine.

The Great Salt Lake has been experiencing declining water levels since 1986, dropping by about 22 feet. This has exposed 800 square miles of lake playa, which has become a major source of dust pollution in Utah’s population centers.

The helicopter-borne geophysical survey was conducted last year after U scientists documented freshwater welling up under pressure at several spots on the lake’s exposed playa in Farmington Bay, manifesting as strange phragmites-choked mounds.

The unexpected part of this discovery was not the salt lens near the surface across the playa, but the fact that the freshwater extends so far into the interior of the lake and possibly under the entire lake, according to Bill Johnson, a UT hydrologist and coauthor of the study.

The study demonstrated for the first time the ability of AEM methods to detect freshwater underneath the thin layer of conductive salt water at the surface of the Great Salt Lake. The team also characterized the spatial extent of the freshwater reservoir beneath Farmington Bay and studied the potential depth of freshwater-saturated sediments by delineating the basement structure.

The data showed a continuous freshwater reservoir layer stretching from about 330 feet down to 2.5 miles. This discovery could have practical applications, such as using the freshwater to wet dust hotspots and douse them without perturbing the freshwater system too much.

Researchers from the US analyzed a 120-meter sediment core taken from the lake bed, dating its layers by the radioactive decay of the minerals it carried. This analysis revealed that for most of the past 240,000 years, the lake stayed about the same size but briefly grew 10 times larger on two separate occasions.

Suspicions of the subterranean freshwater reservoir first arose with the sudden appearance of strange reed-covered islands, each 50 to 100 meters in diameter, in the dried-out lakebed.

The unexpected part of this discovery was that the freshwater underneath the salt lens extends so far into the interior of the lake and possibly under the entire lake, according to Johnson. This finding could reshape our understanding of subsurface water flow in the region.

...Suspicions of the subterranean freshwater reservoir first arose with the sudden appearance of strange reed-covered islands, each 50 to 100 meters (164 to 328 feet) in diameter, in the dried-out lakebed.

Researchers from the US analyzed a 120-meter (394-foot) sediment core taken from the lake bed, dating its layers by the radioactive decay of the minerals it carried, which revealed the lake had dried up approximately 5,000 years ago.

What this adds

The study adds to the understanding of the Great Salt Lake's subsurface water dynamics, potentially offering solutions to dust pollution issues. The dynamic nature of red blood cells, as revealed in a separate study published in Blood, underscores the adaptability of biological systems to changing environmental conditions.

Background

Researchers from the University of Utah have discovered a significant body of freshwater hidden beneath the Great Salt Lake playa, a finding that could reshape our understanding of subsurface water flow in the region.

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