Articles tagged with Isotope Fractionation
Researchers used a quantum device to simulate a vibrating molecule, tracking how energy moves within it. They found that vibrations can actively steer energy flow in unexpected ways, speeding up transfer and opening new pathways.
Researchers from the University of Göttingen have identified oxygen isotopes in 'cherts' as indicators of heat flow on early Earth. The study reveals that cherts record paleo-heat flow on the Shatsky Rise oceanic plateau, providing insights into the conditions on the Earth's surface up to 3.5 billion years ago.
The DS method demonstrates superior precision in measuring inter-mineral isotope fractionation, improving temperature determination results. The SSB method achieves sufficient precision but struggles with concentration matching, leading to potential discrepancies in δ26Mg data.
Researchers investigate microbial reduction of vanadate to detoxify the environment. Electron transfer pathways, including extracellular and intracellular processes, are identified as crucial for vanadium detoxification. Vanadium isotope fractionation also follows a Rayleigh model, with lighter isotopes reacting preferentially.
Researchers discovered a stable lithium isotope fractionation mechanism in Qinghai Lake, indicating minimal Li cycling. The lake's Li reserves are expected to increase over time, providing insights into paleoclimate history.
Researchers at Columbia University have developed a novel technique for isolating isotopes, which are crucial for energy, medicine, and scientific research. The new method is more effective, cheaper, and easier to scale than current state-of-the-art techniques.
A new study published in the Proceedings of the National Academy of Sciences confirms that the Megalodon shark was warm-blooded, with a body temperature estimated at around 27°C. This discovery provides empirical evidence for the extinct species' internal heat production, shedding light on its biology and ecological role.
Researchers have discovered that primitive meteorites contain a different mix of potassium isotopes than those found in other, more-chemically processed meteorites. This suggests that the Solar System was formed from a 'poorly mixed cake batter' of materials, with some planets receiving a unique blend of elements from distant sources.
Researchers analyzed ancient zeolite specimens to discover that some prefer lighter isotopes, while others prefer heavier ones. This finding could help quantify temperatures in geologic systems and mitigate human-caused climate change.
A new study incorporated water vapor isotope compositions into a general circulation model to improve forecast accuracy by several percentage points. The Isotope-incorporated Global Spectral Model (IsoGSM) demonstrated improved modeling of air temperature and specific humidity.
Researchers recreated high-pressure conditions to study iron isotope fractionation, shedding light on Earth's core composition and planetary history. The study identified potential light elements in the core, including oxygen, silicon, and sulfur, and provides a new understanding of the planet's geochemical evolution.
Researchers propose alternative explanation for anomalous sulfur isotope composition in ancient rocks, suggesting early oxygen-rich atmosphere may have been present. Laboratory experiments show that organic material and thermal sulfate reduction can produce similar isotopic signatures.
Researchers have found a new class of isotope fractionation effects that violate the simple rule of mass dependency. The discovery was made in an effort to explain anomalous excesses of oxygen-17 in atmospheric CO, which has been observed at various air monitoring stations.