Backtracking Core: Earth’s Inner Dynamics Unveiled

Backtracking Core : Earth's Inner Dynamics Unveiled


June 18, 2024
Above: Banner Illustration by Edward Sotelo, courtesy of the University of Southern California.

For the past two decades, the movement of this solid yet searing hot metal sphere, suspended in the liquid outer core, has been studied closely and debated by the scientific community

For the past two decades, the movement of this solid yet searing hot metal sphere, suspended in the liquid outer core, has been studied closely and debated by the scientific community. Past research has shown that the inner core has been rotating slightly faster than the planet’s surface.

But a different picture is emerging under a study led by the University of Southern California and published this week in Nature. The research team, which includes U geology professor Keith Koper, verified with new evidence—built on analyses of seismographic data—that the inner core’s rotation began to ease and synced with Earth’s spin about 14 years ago.

Keith Koper, University of Utah

The inner core is a solid sphere composed of iron and nickel, surrounded by the liquid iron outer core. Roughly the size of Pluto at 2,442 kilometers in diameter, it accounts for only 1% of Earth’s mass, yet it influences the magnetic field enveloping the planet and the length of the day. But the core’s location, more than 3,000 miles below Earth’s surface, presents a challenge to researchers since it can’t be visited or viewed.

Past research into the inner core’s movement has relied on data from repeating earthquakes, which occur in the same location to produce identical seismograms. Differences in the time it takes for the waves to pass through Earth indicate how the core’s position changed during the period between two repeater quakes.

In the latest study, researchers analyzed seismic data associated with 121 earthquakes that occurred in the South Atlantic between 1991 and 2023.

“The inner core is just sitting in this fluid outer core, so it’s decoupled a little bit from the rest of the planet. It’s rotating at a different rate,” Koper said. “The angular momentum has to be conserved, so if it’s rotating differently, then that could affect the rotation observed at Earth’s surface. One of the big ideas in this paper is we have basically a new model or new observations about how the inner core is rotating slightly differently than the rest of the planet.”

Read the full article by Brian Maffly in @TheU.

The College of Science Welcomes New Faculty Fellows

THE COLLEGE OF SCIENCE WELCOMES NEW FACULTY FELLOWS


June 6, 2024
Above:  Crocker Science Center

Geologist and mathematician to serve during the coming academic year.

The College of Science welcomes Associate Professor Lauren Birgenheier and Professor Akil Narayan as its inaugural class of Faculty Fellows. By working closely with colleagues on key projects, the new Fellows Program is designed to develop emerging academic leaders who are interested in learning more about college administration.

Lauren Birgenheier

Birgenheier is a sedimentary geologist and geochemist. Her research studies fluvial, shallow marine and lacustrine systems, shedding light on the processes that shaped our planet's past with a view toward implications for energy development, critical mineral exploration, carbon storage and paleoclimate reconstruction. Previously, Birgenheier served as Director of Graduate Studies and Associate Chair for the Department of Geology & Geophysics.

Akil Narayan

Narayan is an applied mathematician specializing in numerical analysis. As a member of the University of Utah's Scientific Computing and Imaging (SCI) Institute, his broad research agenda at the forefront of computational innovation includes machine learning, model reduction and uncertainty quantification, among others. Narayan has previously held many departmental and university roles, including serving on an Academic Senate subcommittee and as a member of the Executive Committee of the Department of Mathematics.

"Lauren and Akil are exceptional scholars and leaders," said Dean Peter Trapa. "Their diverse expertise, coupled with their commitment to excellence, will be put to good use in these new Faculty Fellow roles.  I look forward to working with them both."

 

 

 

How Earth’s oceans were oxygenated

How Earth's oceans were oxygenated


June 12, 2024

 

New research led by U geochemist uses thallium isotopes to track the rise and fall of free oxygen on Earth 2.5 billion years ago, the process that enabled life as we know it.

About 2.5 billion years ago, free oxygen, or O2, first started to accumulate to meaningful levels in Earth’s atmosphere, setting the stage for the rise of complex life on our evolving planet.

Scientists refers to this phenomenon as the Great Oxidation Event, or GOE for short. But the initial accumulation of O2 on Earth was not nearly as straightforward as that moniker suggests, according to new research led by a University of Utah geochemist.

Chadlin Ostrander

This “event” lasted at least 200 million years. And tracking the accumulation of O2 in the oceans has been very difficult until now, said Chadlin Ostrander, an assistant professor in the Department of Geology & Geophysics.

“Emerging data suggest that the initial rise of O2 in Earth’s atmosphere was dynamic, unfolding in fits-and-starts until perhaps 2.2. billion years ago,” said Ostrander, lead author on the study published June 12 in the journal Nature. “Our data validate this hypothesis, even going one step further by extending these dynamics to the ocean.”

His international research team, which is supported by the NASA Exobiology program, focused on marine shales from South Africa’s Transvaal Supergroup, yielding insights into the dynamics of ocean oxygenation during this crucial period in Earth’s history. By analyzing stable thallium (Tl) isotope ratios and redox-sensitive elements, they uncovered evidence of fluctuations in marine O2 levels that coincided with changes in atmospheric oxygen.

These findings help advance the understanding of the complex processes that shaped Earth’s O2 levels during a critical period in the planet’s history that paved the way for the evolution of life as we know it.

“We really don’t know what was going on in the oceans, where Earth’s earliest lifeforms likely originated and evolved,” said Ostrander, who joined the U faculty last year from the Woods Hole Oceanographic Institution in Massachusetts. “So knowing the O2 content of the oceans and how that evolved with time is probably more important for early life than the atmosphere.”

Read the full article by Brian Maffly in @TheU. Read a repost of it in SciTechDaily.

Kip Solomon announced as interim chair, Geology & Geophysics

Kip Solomon tapped as Interim Chair


June 7, 2024
Above: Kip Solomon

 

D. Kip Solomon has been selected as the new interim chair of the Department of Geology and Geophysics at the University of Utah.

Solomon in Greenland to measure fresh water aquifer below deep ice in 2016.

Solomon holds the Frank Brown Presidential Chair in the department and will replace William Johnson as department chair beginning July 1, 2024.

Johnson served as department chair beginning April 2022. “I’m satisfied to have spurred new infrastructure (SIRFER and clean room), new faculty and two new positions in play, as well as salary transparency and staff domain clarity,” says Johnson of his term. “Kip will be a steady lead as the above changes settle and as additional institutional changes occur.”

Solomon has a PhD in Earth Sciences from the University of Waterloo and BS and MS degrees from the U’s Department of Geology and Geophysics. He joined the department in 1993 and served as chair from 2009-2013.

His research includes the use of environmental tracers to evaluate groundwater flow and solute transport processes in local-to regional-scale aquifers. He has developed the use of dissolved gases including helium-3, CFCs and SF6 to evaluate groundwater travel times, location and rates of recharge, and the sustainability of groundwater resources. He constructed and operates one of only a few labs in the world that measures noble gases in groundwater. His research results have been documented in more than 120 journal articles, book chapters, and technical reports.

Solomon will also receive the 2024 O.E Meinzer Annual Award by the Geological Society of America in September.

“Geology and Geophysics is a great department and has been strengthened considerably by the hard work and dedication of previous chairs Thure Cerling and Bill Johnson,” said Solomon. “With new hires and academic programs, the future looks very bright.”

By Ashley Herman

Breakthrough in Geothermal Energy at Utah FORGE

Breakthrough in Geothermal Energy
at Utah FORGE


June 3, 2024
Above: The Utah FORGE site near Milford, Utah. PHOTO CREDIT: ERIC LARSON, FLASH POINT SLC.

In $218 million DOE-funded research project, University of Utah scientists aim to make enhanced geothermal a key part of world's energy portfolio.

A major University of Utah-led geothermal research project, funded by the U.S. Department of Energy (DOE), achieved a critical breakthrough in April after hydraulically stimulating and circulating water through heated rock formations a mile and a half beneath its drill site in the Utah desert and bringing hot water to the surface. The test results are seen as an important step forward in the search for new ways to use Earth’s subsurface heat to produce hot water for generating emissions-free electricity. The successful well stimulations and a nine-hour circulation test were the fruits of years of planning and data analysis at the Utah FORGE facility near Milford, 175 miles southwest of Salt Lake City.

More than two-thirds of the water that was injected underground and pushed through the fractured formation—acquiring heat on the way—was extracted from a second well, offering proof that enhanced geothermal systems (EGS) technology could be viable, according to John McLennan, a co-principal investigator on the project formally known as the Utah Frontier Observatory for Research in Geothermal Energy, or Utah FORGE.

“Nine hours is enough to prove that you have a connection and that you’re producing heat,” said McLennan, a U professor of chemical engineering. “It really is a Eureka moment. It’s been 60 years coming, and so this actually is significant.”

Kris Pankow, associate director of the U of U Seismograph Stations

Utah FORGE is a $218 million research project, involving numerous institutions and industry partners, funded by a DOE grant to the U’s Energy & Geoscience Institute. The project aims to develop and de-risk new geothermal technologies that could potentially be deployed all over the world, not just where conventional geothermal plants are sited.

For this recent test, FORGE personnel and industry specialists directionally drilled two boreholes—one for injecting water underground and the other for extracting it. The injection well is 10,897 feet long and drops to a depth of 8,559 feet below the surface. “We speculate, and we’ll see this in the 30-day test, that as we fill the fracture system back up, this number is going to get to where I’m suspecting it’s 85 to 90% efficiency,” McLennan said.

Equally promising was the absence of any noticeable ground shaking associated with the stimulations and circulation test. U seismologists led by geology professor Kris Pankow, associate director of the U of U Seismograph Stations, are overseeing an extensive network of seismometers to document ground movement associated with the project.

Discover more about this Breakthrough by visiting the full article by Brian Maffly at @The U.

Tapping coal mines for rare-earth materials

Tapping coal mines for rare-earth materials


May 23, 2024
Above: Michael Vanden Berg, a geologist with the Utah Geological Survey, examines a coal outcrop near Utah's old Star Point mine. Credit: Lauren Birgenheier

 

In a groundbreaking study led by the University of Utah, researchers have discovered elevated concentrations of rare earth elements (REEs) in active coal mines rimming the Uinta coal belt of Colorado and Utah.

This finding suggests that these mines, traditionally known for their coal production, could potentially serve as secondary sources for critical minerals essential for renewable energy and high-tech applications. "The model is if you're already moving rock, could you move a little more rock for resources towards energy transition? " Lauren Birgenheier, an associate professor of geology and geophysics, explains, In those areas, we're finding that the rare earth elements are concentrated in fine-grain shale units, the muddy shales that are above and below the coal seams."

Lauren Birgenheier

This research was conducted in partnership with the Utah Geological Survey and Colorado Geological Survey as part of the Department of Energy-funded Carbon Ore, Rare Earth and Critical Minerals project, or CORE-CM. The new findings will form the basis for a grant request of an additional $9.4 million in federal funding to continue the research.

"When we talk about them as 'critical minerals,' a lot of the criticality is related to the supply chain and the processing," said Michael Free, a professor metallurgical engineering and the principal investigator on the DOE grant. "This project is designed around looking at some alternative unconventional domestic sources for these materials."

The U-led study was published last month in the journal Frontiers in Earth Science. Team members included graduate students Haley Coe, the lead author, and Diego Fernandez, a research professor who runs the lab that tested samples.

“The goal of this phase-one project was to collect additional data to try and understand whether this was something worth pursuing in the West,” said study co-author Michael Vanden Berg, Energy and Minerals Program Manager at the Utah Geological Survey. “Is there rare earth element enrichment in these rocks that could provide some kind of byproduct or value added to the coal mining industry?”

Haley Coe, U geology graduate student, inspects drilling cores. Photo Credit: Lauren Birgenheier.

“The coal itself is not enriched in rare earth elements,” Vanden Berg said. “There's not going to be a byproduct from mining the coal, but for a company mining the coal seam, could they take a couple feet of the floor at the same time? Could they take a couple feet of the ceiling? Could there be potential there? That's the direction that the data led us.”

To gather samples, the team worked directly with mine operators and examined coal seam outcrops and processing waste piles. In some cases, they analyzed drilling cores, both archived cores and recently drilled ones at the mines. The team entered Utah mines to collect rock samples from the underground ramps that connect coal seams.

The study targeted the coal-producing region stretching from Utah’s Wasatch Plateau east across the Book Cliffs deep into Colorado. Researchers analyzed 3,500 samples from 10 mines, four mine waste piles, seven stratigraphically complete cores, and even some coal ash piles near power plants.

The study included Utah’s active Skyline, Gentry, Emery and Sufco mines, recently-idled Dugout and Lila Canyon mines in the Book Cliffs, and the historic Star Point and Beaver Creek No. 8 mines. The Colorado mines studied were the Deserado and West Elk.

Discover more about this groundbreaking research by visiting the full article by Brian Maffly at @The U.

Read more about this story at KUER.

Toxic Thalium: Humans changing the chemistry of the Baltic Sea

changing chemistry of the Baltic Sea


May 6, 2024

Above: Assistant Professor of Geology & Geophysics Chad Ostrander stands in front of the Elisabeth Mann Borgese research vessel.

Human activities account for a substantial amount — anywhere from 20% to more than 60% — of toxic thallium that has entered the Baltic Sea over the past 80 years, according to new research by scientists affiliated with the Woods Hole Oceanographic Institution (WHOI) and other institutions.

Chad Ostrander, lead author of the study, preparing a short sediment core collected from the East Gotland Basin during the investigation. - Credit: Colleen Hansel, ©Woods Hole Oceanographic Institution

Currently, the amount of thallium (element symbol TI), which is considered the most toxic metal for mammals, remains low in Baltic seawater. However, the research, using stable isotope analysis, suggests that the amount of thallium could increase due to further anthropogenic, or human induced, activities, or due to natural or human re-oxygenation of the Baltic that could make the sea less sulfide rich. Much of the thallium in the Baltic Sea, the largest human-induced hypoxic area on Earth, accumulates in the sediment thanks to abundant sulfide minerals.

“Anthropogenic activities release considerable amounts of toxic thallium annually. This study evidences an increase in the amount of thallium delivered by anthropogenic sources to the Baltic Sea since approximately 1947,” according to the journal article, “Anthropogenic forcing of the Baltic Sea thallium cycle,” published in Environmental Science & Technology.

“Humans are releasing a lot of thallium into the Baltic Sea, and people should be made aware of that. If this continues — or if we further change the chemistry of the Baltic Sea in the future or if it naturally changes — then more thallium could accumulate. That would be of concern because of its toxicity,” said Chadlin Ostrander lead author of the article which he conducted as a postdoctoral investigator in WHOI’s Department of Marine Chemistry and Geochemistry. Currently, he is an assistant professor in the Department of Geology & Geophysics at the University of Utah.

For the study, the researchers set out to better understand how thallium and its two stable isotopes 203Tl and 205Tl are cycled in the Baltic Sea. To discern modern thallium cycling, concentration and isotope ratio data were collected from seawater and shallow sediment core samples. To reconstruct thallium cycling further back in time, the researchers supplemented their short core samples with a longer sediment core that had been collected earlier near one of the deepest parts of the sea. They found Baltic seawater to be considerably more enriched in Tl than predicted. This enrichment started around 1940 to 1947 according to the longer sediment core.

Read the full press release from Woods Hole Oceanographic Institution here.

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Outstanding Undergrad Research Awards 2024

Outstanding Undergrad Research Awards 2024


April, 2024
Above: Student recipients at the 2024 OUR Awards Ceremony

The University of Utah is one of the top research academic institutions in the Intermountain West, and it’s thanks in major part to the U’s undergraduate student researchers and the faculty who advise and mentor them.

Some of the university’s up-and-coming researchers and mentors were honored at the 2024 Office of Undergraduate Research (OUR) Awards, held virtually on April 1.

Every year, OUR recognizes one undergraduate student researcher from each college/school with the Outstanding Undergraduate Researcher Award, according to the office’s website. Partnering colleges and schools are responsible for selecting the awardee.

This year, 18 undergraduate researchers were honored with the Outstanding Undergraduate Researcher Award, two of them from the College of Science / College of Mines & Earth Sciences:

Autumn Hartley (Mentor: Professor Sarah Lambart)

Dua Azhar (Mentor: Professor Sophie Caron)

Autumn Hartley

Autumn Hartley (she/they) is also a College of Science ambassador and has a passion for science and learning as geology and geophysics major. Originally from Midway, Utah, she moved to Salt Lake City when she started school at the U where she became involved in many different organizations including oSTEM, which connects LGBTQ+ students in STEM. Outside of academia, she loves all things artistic. “I’m a writer, graphic designer, and a character designer when I’m not in the lab!” she says.

Dua Azhar

Born and raised a Utahn in Draper, Dua Azhar (she/her) is an honors physics student with a biomedical emphasis. During her undergraduate years here at the U, she says, “I intend to tie my education and research together towards an MD/PhD, in order to specialize in neurology.” Along with the sciences, she love the arts, especially film and photography. “So if you don’t see me in the lab, you’ll most likely see me making something with a camera!”

Opening remarks at the event were made by Associate Dean Annie Fukushima, followed by Provost Mitzi Montoya and VP Research Erin Rothwell. They were followed by the presentation of Undergraduate Research Scholarship recipients which included the 2023 – 2024 recipients of the Francis Family Fund Scholarships, Dee Scholarship, and Parent Fund Scholarship.

The Monson Essay Prize winner, Pablo Cruz-Ayala, was then acknowledged followed by the 18 OUR & Research Mentor Awards by college.

At the ceremony event, award recipients were able to thank their mentors, family and others for their support.

More information and criteria for both awards can be found on the OUR’s website Watch video of OUR awards 2024 program below:

Cool Science: Monitoring earthquakes in Utah

Cool science: Monitoring Earthquakes in Utah


April 22, 2024

Above: Keith Koper, director of the University of Utah Seismograph Stations, looks at quake evidence. Credit: Remi Barron, University of Utah

It’s easy to forget that the Wasatch back is very near an active fault. Earthquakes are continually happening around us, maybe not close enough to always feel, but they are happening.

Monitoring these continual motions and shifts are the University of Utah Seismograph Stations. These stations, situated throughout Utah and surrounding states, pick up and report on regional earthquakes. With this data, scientists at the university are able to develop a better understanding of earthquakes in our area. This can then help reduce the risk from earthquakes in Utah thanks to their research, education, and public service.

Director Keith Koper shares more about the Seismograph Stations and the important work they are doing in this interview on KCPW's Cool Science Radio.

More information can be found at https://quake.utah.edu

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Placing geology at the foundation of essential discoveries

Placing geology at foundation of essential discoveries


March 29, 2024 | Carleton College

by Daniel Myer 

Above: Professor Bereket Haileab leads a geology field trip in 2023.

Bereket Haileab, MS'88, PHD'95, chair and professor of geology at Carleton College, is a researcher and teacher animated by his passion for geology.

Bereket Haileab

Haileab has been a cornerstone of geology at Carleton College, a small, private liberal arts college in the historic river town of Northfield, Minnesota, since he joined the faculty in 1993. Through his research over the years, he has also helped rejuvenate the study of the guiding principles behind his discipline, and connected that work with the larger Northfield and Carleton communities. His experiences, ranging from studying Rice County’s hydrology to helping chart the founding story of the entire human species, have revealed the role geology plays in multiple major disciplines. Today, he teaches these lessons to new generations of students, and shows that the College’s geology department is a true testament to the quality of a Carleton education.

At first, Haileab’s work had a utilitarian angle. After his undergraduate education at the University of Addis Ababa in Ethiopia, he had the opportunity to study for his PhD with well-known geochemists at the University of Utah. “There,” Haileab said, “I got the skills to do chemical analysis, interpret the results, and write about it.”

These experiences solidified his background in geochemistry, petrology, and mineralogy, which Haileab used to become an exploration geologist with the Geological Survey of Ethiopia. In his role, Haileab surveyed regions of western Ethiopia to find new gold deposits. Although he found the chance to apply his skills in chemical analysis fulfilling, he was interested in getting more involved with the interdisciplinary field of paleoanthropology — the study of human evolution through fossils, cultural artifacts, and more — which his graduate school experiences had introduced him to.

“When I came to Utah, I went to the field every summer and met many [experts in paleoanthropology] there and in meetings,” Haileab said. “My research was used in every place.”

Those who study the origin of the human species, like paleoanthropologists, depend on extensive geological research. With a lot of their modern work based on the fossils of early people or closely related species, scholars and scientists also need those fossils’ detailed geological contexts, including the current state and geologic history of their dig sites. After all, Haileab said, “you don’t find fossils floating by themselves.”

In 1985, Haileab joined a University of Utah research group working in Kenya, where just one year prior, the “Turkana Boy,” a Homo ergaster, was discovered. Haileab’s group needed to map the surrounding Turkana Basin in order to refine the dating process that allowed geologists and paleoanthropologists to prove that the Turkana Boy was 1.6 million years old. Haileab’s research, however, expanded far beyond one basin.

“We found that the volcanic ash from Turkana, to the sediments of the Red Sea cores, to the sediments in the Gulf of Aden, all the way south to Lake Albert in Uganda, to Ethiopia… was all formed originally [in the Turkana Basin], which makes it the most important point,” Haileab said. “For most of the fossiliferous [fossil rich] sediments, we could correlate all of the sedimentary basins and all of the findings temporally.”

Read the entire article at Carleton News.

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