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Induced polarization applied to landslides. Part 2: Anatomy and water content tomography of a mudflow

Geophysical Journal International - Mon, 06/16/2025 - 00:00
SummaryInduced polarization is a geophysical method that can be applied to determine the water content and CEC (Cation Exchange Capacity) of sediments and rocks. We apply here this technique to image the Harmalière landslide in Isère (East of France). This landslide includes a mudflow of glacio-lacustrine silty clays overlying the Toarcian clayrock formation with local occurrences of compact pebbles from a paleochannel of the Drac river. A petrophysical study is used to characterize the properties of the four main lithofacies occurring in the area with a total of 22 samples. We performed complex conductivity measurements in the frequency range 10 mHz-45 kHz at different salinities (NaCl brines and in situ pore waters). We also measured the porosity and CEC of the samples. We calibrate the relationships between surface conductivity, quadrature conductivity, and normalized chargeability with both the porosity and CEC. The relationship between the formation factor and the porosity conforms to Archie's law with a cementation exponent close to 2.0 ± 0.2. In the field, we performed a time-domain induced polarization survey using a 1.26 km-long cable (including roll along of the electrodes) with an electrode spacing of 20 m. The landslide is imaged down to a depth of 220 m. The inversion of the data (788 electrodes, 15.7 km of profiling, 13 012 apparent resistivity and 5539 apparent chargeability data) is done with the least-square technique penalizing the roughness of the tomograms using Occam inversion. The resulting 3D electrical conductivity and normalized chargeability tomograms are analyzed in conjunction with the petrophysical data to image the extension of the lithofacies at the field scale. Furthermore, the water content and CEC of the formations are imaged. We demonstrate that the compacted pebbles of the Drac paleochannel form both a mechanical and hydraulic barrier that is locally breached by the mudflow before entering the Monteynard-Avignonet Lake. This study demonstrates the ability of induced polarization to finely characterize the anatomy of such landslide and image its water content.

Slab temperature beneath the Tohoku region, Northeast Japan, constrained from surface heat flow and the location of the blueschist-out boundary

Geophysical Journal International - Mon, 06/16/2025 - 00:00
AbstractThis study investigates the following three issues in numerical models of the thermal structure of subduction zones, using the Tohoku region in Northeast Japan as an example: (1) a steady state is often assumed in models, (2) quantitative assessment of the uncertainty in the predicted temperatures is lacking, and (3) surface heat flow has been used to constrain many of the models. I found that, at least under the model setting of this study, a steady state may be safely assumed as long as only surface heat flow within 150 km of the trench is used to constrain the model. I used Bayesian inference to predict the thermal structure, with surface heat flow near the trench and the location of the blueschist-out boundary in the oceanic crust as observational constraints. The depth of slab–mantle kinematic decoupling, effective friction coefficient, and rate of radiogenic heat production in the upper island arc crust were constrained simultaneously to be ∼80–100 km, 0.03–0.08, and 1.5–2.16 μW m−3, respectively, although the decoupling depth is sensitive to the assumed location and temperature of the blueschist-out boundary. The uncertainties in slab temperature reach ∼450 K at depths of <100 km and 100 K for greater depths, which are substantial. To reduce these uncertainties, it is necessary to reduce the uncertainty in the input parameters and obtain additional observational constraints.

Induced polarization applied to landslides. Part 1: Imaging hydraulic barriers

Geophysical Journal International - Mon, 06/16/2025 - 00:00
SummaryWater content and pore fluid pressure increases have been recognized as important drivers of shallow landslides, especially through the role of strong rainfalls promoting gravitational instabilities. Less recognized is the role of vertical hydraulic barriers impeding the flow of ground water at the feet of areas prone to landslides. Induced polarization is a non-intrusive geophysical technique able to image hydraulic properties of the shallow subsurface. Recently developed petrophysical models bridging the gap between hydraulic and electrical properties of soft sediments, soils, and rocks have been developed. Thanks to these relationships, this geophysical method can be used to image the water and clay contents of the formations and their permeability. Therefore, induced polarization can be used to image the occurrence of vertical permeability barriers. We focus our approach on a large landslide that occurred in March 1931 (reactivated in 1971–1972) above Le Châtelard village (Bauges, France). This landslide started inside a kilometer-scale syncline hosting clayey formations and moraines. We performed a 2.2 km profile crossing the syncline and the sliding area including resistivity, induced polarization, and self-potential measurements. In addition, 22 samples were taken from the different formations outcropping at the field site including limestones, sandstones, and clayey formations. The petrophysical investigations are combined with the field data to image the water content and cation exchange capacity as well as their permeability. The dataset shows the existence of a vertical permeability barrier at the bottom of the landslide corresponding to the tight Urgonian limestone formation. We combine the permeability distribution, the resistivity, and self-potential data by forward modeling the groundwater flow and electrokinetic response. We then invert the self-potential measurements to refine the image of the Darcy velocity distribution. The results show a strong upflow of the ground water just above the Manauds canyon where several gravitational instabilities occured in the past.

Carbon dioxide removal methods could worsen marine oxygen loss, study warns

Phys.org: Earth science - Sat, 06/14/2025 - 16:40
Methods to enhance the ocean's uptake of carbon dioxide (CO₂) are being explored to help tackle the climate crisis. However, some of these approaches could significantly exacerbate ocean deoxygenation. Their potential impact on marine oxygen must therefore be systematically considered when assessing their suitability.

How do Propagating Rifts Breach Cratons? Insights from the Northwestern Branch of the East African Rift, Uganda

Geophysical Journal International - Sat, 06/14/2025 - 00:00
SummaryHere, we investigate how continental rifts initiate and propagate across cratons by exploring the crustal structure of northwestern tip of the East African Rift System (EARS), hosting the volcanic-rich Edward-George and non-volcanic Albertine-Rhino rifts, and their termination at the Precambrian Aswa Shear Zone. We conducted a derivative analysis of magnetic data, utilized power spectral analyses, and implemented a two-dimensional (2D) forward modeling of gravity data constrained by the seismic results obtained from the region. A magnetic derivative map indicates that the border faults of the Albertine Rift, at regional-scale, trend parallel to the Mesoproterozoic Madi-Igisi fold belt (MIFB) structures, representing the suture zone between two Archean microcratons. Our results show a pronounced thinned crust (∼24–30 km) beneath the southern segments of the rift zone, particularly the Edward-George rift, the Rwenzori Mountains, and the southern Albertine graben, consistent with previous seismic studies. In general, we observe that: 1) the rift system follows the boundary between a broadly thinner crust (21–41 km) to the southeast in Uganda, and thick crust (34–41 km) to the northwest in Congo, and 2) within the rifts, the crustal thickness along the axes exhibits a strong gradient that attenuates northwards beneath the Albertine-Rhino graben. We supplement the geophysical results with field observations of an exhumed Permian ‘Karoo’ rift (Entebbe Graben) in central Uganda, indicating the possible source of inherited thinner crust to the southeast of the Albertine-Rhino Rift. We propose that the northwestern tip of the EARS exploited a cratonic crustal thickness-gradient, assisted by structural inheritance from crustal metamorphic fabrics, and potentially, thermo-mechanical weakening of the deeper crust by partial melts beneath some of the rift segments.

Fossil corals point to possibly steeper sea level rise under a warming world

Phys.org: Earth science - Fri, 06/13/2025 - 18:00
Coastal planners take heed: Newly uncovered evidence from fossil corals found on an island chain in the Indian Ocean suggests that sea levels could rise even more steeply in our warming world than previously thought.

Ocean acidification may have crossed 'planetary boundary' five years ago

Phys.org: Earth science - Fri, 06/13/2025 - 17:50
A team of planetary scientists, ecologists, and marine biologists affiliated with several institutions in the U.S. and one in the U.K., has found evidence suggesting that parts of the world's oceans have already passed what has come to be known as a planetary boundary.

Increased forest fires due to climate change could alter oceanic CO₂ absorption

Phys.org: Earth science - Fri, 06/13/2025 - 14:57
Forest fires are a fundamental force in Earth's dynamics with a direct impact on human health, food security, and biodiversity. From air quality to landscape configuration and resource availability, the consequences of fire have influenced the development of society throughout history. Their effects on the oceans, though less known, are equally significant.

Fallowed Fields Are Fueling California’s Dust Problem

EOS - Fri, 06/13/2025 - 12:00

California produces more than a third of the vegetables and three quarters of the fruits and nuts in the United States. But water constraints are leaving more and more fields unplanted, or “fallowed,” particularly in the state’s famed farming hub, the Central Valley.

In a study published in Communications Earth and Environment, researchers showed that these fallowed agricultural lands are producing a different problem: dust storms, which can cause road accidents and health problems and can have far-reaching environmental impacts. Using remote sensing methods, the team found that 88% of anthropogenic dust events in the state, such as dust storms, come from fallowed farmland.

California’s frequent droughts could mean a rise in fallowed farmland. In 2014, the state passed the Sustainable Groundwater Management Act (SGMA), a policy aimed at ensuring the sustainability of groundwater resources. A report by the Public Policy Institute of California suggested that to meet the SGMA’s demands, farmers may need to fallow hundreds of thousands of additional acres, potentially worsening dust events.

Tracking Down Agricultural Dust

Dust can come from both natural sources, such as wind blowing across a desert, and anthropogenic sources, such as when transportation, construction, or agricultural activities kick up particles. Previous studies identified agriculture as a significant source of human-generated dust, but study author Adeyemi Adebiyi and his colleagues wanted to narrow down which agricultural practices produced the most.

“If you stop irrigating the land, it becomes dry, and we’re already in a dry climate. It’s easy for it to become a new dust source.”

Fallowed land was a logical culprit. “If you stop irrigating the land, it becomes dry, and we’re already in a dry climate,” said Adebiyi, an atmospheric scientist at the University of California, Merced. “It’s easy for it to become a new dust source.”

The researchers started by pinpointing fallowed land across California between 2008 and 2022 using U.S. Department of Agriculture datasets. The data showed that 77% of the state’s fallowed land was in the Central Valley. 

The team then examined NASA satellite images of atmospheric aerosols, identifying which aerosols were dust particles on the basis of the way they scatter light. When they overlaid the regions that regularly experienced dust events with the agricultural data, they saw that dust events were tightly associated with fallowed fields.

The problem appears to be getting worse. Between 2008 and 2022, both the area of fallowed land and corresponding dust levels have increased: In this period, the amount of dust in the atmosphere over the Central Valley grew by about 36% per decade.

Having grown up in California and spent the first decade of his career studying dust in the Central Valley, Thomas Gill, an Earth scientist at the University of Texas at El Paso who wasn’t involved in the study, has long worried that land use changes could lead to dust issues. “This study by Adebiyi et al., unfortunately, shows that my worries have been coming true,” he said.

“These fallowed land locations are emblematic of the properties you would normally see in a typical desert-type location.”

Daniel Tong, an atmospheric scientist at George Mason University who also wasn’t involved in the study, agreed that the work provides some much-needed conclusive data on the connection between land use and dust levels. “This is a very useful study,” he said.

Adebiyi’s team used additional remote sensing data to determine that compared with nearby nonfallowed land, fallowed fields have lower soil moisture and are about 4.2°C hotter. Combined with a lack of vegetation, these factors work together to make such areas more prone to wind erosion. “These fallowed land locations are emblematic of the properties you would normally see in a typical desert-type location,” Adebiyi said.

Far-Reaching Effects

The dust from fallowed fields has wide-reaching consequences. “California is already the state with the largest number of fatalities caused by dust storms,” said Tong, who authored a 2023 study about windblown dust fatalities in the United States. One concern, he said, is that more dust storms could increase road accidents. Dust also contributes to respiratory problems and cardiovascular disease and carries the Coccidioides fungus, which causes the dangerous infection valley fever. Cases of valley fever increased by 800% in California between 2000 and 2018.

“There’s also been a great population increase in the Central Valley,” Gill said. “So not only do you have more particulate matter, but you have more people living there who are vulnerable to its effects.”

Fallowed fields and the dust they produce may also work counter to the groundwater management goals of the SGMA. The Central Valley dust blows east into the Sierra Nevada Mountains, where it speeds snowmelt, a significant reservoir of water for the state. The researchers also found that the heat concentrated in fallowed fields can spread out to nearby fields, causing surrounding crops to need more water. “It’s a double whammy,” Adebiyi said.

He noted the importance of preventing fields from becoming completely bare while still conserving water. One strategy is to plant native, drought-resistant plants that protect the soil from wind erosion without needing much irrigation.

The researchers are now conducting similar studies on the connection between fallowed lands and dust in other agricultural states, such as Kansas, Montana, and Washington. Their findings suggest that addressing dust problems will become increasingly important nationwide.

“The implications are beyond California,” Adebiyi said. “They’re across the United States.”

—Andrew Chapman (@andrewchapman.bsky.social), Science Writer

Citation: Chapman, A. (2025), Fallowed fields are fueling California’s dust problem, Eos, 106, https://doi.org/10.1029/2025EO250223. Published on 13 June 2025. Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

Study finds airborne particles can reduce cyclone intensity in early stages

Phys.org: Earth science - Fri, 06/13/2025 - 10:21
Aerosols could hold the key to stopping potentially destructive cyclones in their tracks, according to a first-of-its-kind study from The Australian National University (ANU).

Characterization of electrostatic discharge currents in electron-charged polymethyl methacrylate as a proxy for natural compact intracloud discharges

Physical Review E (Plasma physics) - Fri, 06/13/2025 - 10:00

Author(s): Kathryn M. Sturge, Noah Hoppis, Brian L. Beaudoin, Ariana M. Shearin, Ethan T. Basinger, Bryson C. Clifford, Jack R. FitzGibbon, Emily H. Frashure, James E. Krutzler, Abraham A. Levitan, Patrick O'Shea, Holly J. Wilson, and Timothy W. Koeth

Electrostatic discharges occur in numerous media on a range of length scales, from microscopic discharges inside electronic materials to kilometer-long channels in air during natural lightning events. To study the mechanisms and behavior of electrostatic discharges inside materials, we measured the …


[Phys. Rev. E 111, 065207] Published Fri Jun 13, 2025

Highly compressed spin-singlet Be at a million Kelvin

Physical Review E (Plasma physics) - Fri, 06/13/2025 - 10:00

Author(s): M. W. C. Dharma-wardana and Dennis D. Klug

Experiments at the U.S. National Ignition Facility (NIF) [Döppner et al., Nature (London) 618, 270 (2023)] have created highly compressed hot hydrogenlike Be plasmas. Published analyses of the the NIF experiment have used finite-T multiatom density-functional theory with Molecular dynamics, and Pat…


[Phys. Rev. E 111, 065208] Published Fri Jun 13, 2025

Inversion of carbonate-rock properties based on an acoustoelasticity-squirt flow model

Geophysical Journal International - Fri, 06/13/2025 - 00:00
AbstractDeep carbonate reservoirs are characterized by complex stress states and pore structures, and frame compressibility is strongly influenced by differential pressure. We have developed a frequency-dependent acoustoelasticity-squirt flow model based on a threshold pressure to describe the frame compressibility. Based on this model, 3D rock physics templates (RPT) were created and calibrated with laboratory, well log and seismic data from the Longwangmiao Formation in the Gaoshiti-Moxi area, Sichuan Basin, China. The templates are then used to determine the reservoir properties at the well logging and seismic frequencies. The predicted porosity matches well with the actual porosity log curve, and the results are consistent with gas production reports, with high porosity, crack density and threshold pressure (high frame compressibility) indicating high reservoir potential.

NASA sensor on space station eyes contamination off California coast

Phys.org: Earth science - Thu, 06/12/2025 - 20:10
An instrument built at NASA's Jet Propulsion Laboratory to map minerals on Earth is now revealing clues about water quality. A recent study found that EMIT (Earth Surface Mineral Dust Source Investigation) was able to identify signs of sewage in the water at a Southern California beach.

A stress memory effect in olivine at upper mantle pressures and temperatures

Phys.org: Earth science - Thu, 06/12/2025 - 17:30
The Kaiser effect, which is known as a stress memory effect, predicts that seismic events occur only when the previous maximum stress is exceeded. Therefore, the Kaiser effect has been applied for the estimation of the magnitude of "in situ" stress on crustal rocks in the community of geotechnical engineering (including forecasting earthquakes).

Why submarine canyons form in places where the seafloor is particularly steep

Phys.org: Earth science - Thu, 06/12/2025 - 17:06
Geoscientists Professor Anne Bernhardt of Freie Universität Berlin and PD Dr. Wolfgang Schwanghart of the University of Potsdam have uncovered a surprising insight using a global statistical model: The primary factor influencing the formation of submarine canyons is the steepness of the seafloor—not, as commonly assumed, the role of rivers and where they transport sediment into the ocean.

Scientists decode past monsoon instability from paleolake sediments in the Weihe Basin

Phys.org: Earth science - Thu, 06/12/2025 - 16:25
A study published in the Proceedings of the National Academy of Sciences by researchers from the Institute of Earth Environment of the Chinese Academy of Sciences reveals that the East Asian summer monsoon underwent frequent and rapid shifts even during past warm periods that were previously thought to be climatically stable.

How rivers fuel hurricanes—and how that knowledge can improve forecasts

Phys.org: Earth science - Thu, 06/12/2025 - 16:15
As Hurricane Idalia approached Florida's Big Bend in August 2023, warm waters of the Gulf fueled its growth. In less than 24 hours, the storm jumped from a Category 1 to a Category 4 in a phenomenon known as rapid intensification.

New simulations show how much colder European winters would get if AMOC collapses

Phys.org: Earth science - Thu, 06/12/2025 - 16:00
A pair of meteorologists in the Netherlands has used new simulations to show just how cold many of Europe's cities could get if the Atlantic Meridional Overturning Circulation (AMOC) were to collapse due to global warming. In their study, published in the journal Geophysical Research Letters, René van Westen and Michiel Baatsen developed a climate model based on a range of ocean temperature changes that could arise due to global warming.

Coverage Factors Affect Urban CO2 Monitoring from Space

EOS - Thu, 06/12/2025 - 15:35
Editors’ Highlights are summaries of recent papers by AGU’s journal editors. Source: AGU Advances

Carbon dioxide (CO2) is a key driver of global climate change and the ability to monitor human-based emissions of this gas is crucial for quantifying the effectiveness of carbon-reduction policies. In recent years, space-based platforms like the Orbiting Carbon Observatory (OCO-2 and OCO-3) missions have provided atmospheric CO2 observations with near-global coverage and efforts to ingest these data into local, regional, and national carbon accounting methodologies have been successful. However, space-based observations are influenced by physical and environmental factors that affect their coverage.

Roten and Chatterjee [2025] investigate these factors and determine that the time needed to constrain emissions varies among cities within the United States. Key factors that affect these space-based platforms include the type of orbit they are in, the location of clouds in Earth’s atmosphere, and the distribution of atmospheric aerosols. The characteristics of the instruments’ orbits also vary the frequency of urban observations in both space and time. Results show that cities on the west coast are more frequently observed than cities in the northeast. These limitations should be considered when cities are seeking to monitor their emission reduction efforts with space-based technologies.

Predicted mean effective revisit time (τ) values from the Orbiting Carbon Observatory are spatially distributed at a 1km × 1km resolution across CONUS. White points indicate the locations of target cities and their sizes represent the mean CO2 emitted from each city during time interval τ. Much of the west had τ values short enough to facilitate sub-monthly observations; conversely, much of the northeast could not be constrained at such a scale (τ > 30 days). Credit: Roten and Chatterjee [2025], Figure 7

Citation: Roten, D., & Chatterjee, A. (2025). Coverage-limiting factors affecting the monitoring of urban emissions with the orbiting carbon observatory missions. AGU Advances, 6, e2024AV001630. https://doi.org/10.1029/2024AV001630

—Don Wuebbles, Editor, AGU Advances

Text © 2025. The authors. CC BY-NC-ND 3.0
Except where otherwise noted, images are subject to copyright. Any reuse without express permission from the copyright owner is prohibited.

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