98%
921
2 minutes
20
We introduce a novel high-precision method for oxygen-isotope analysis of iron (oxyhydr)oxides using high-temperature conversion isotope ratio mass spectrometry (HTC-IRMS). In this approach, a finely ground mixture of iron (oxyhydr)oxide and graphite is heated at 1450 °C in a helium flow environment, converting oxygen to CO gas with nearly 100% yield. Continuous-flow IRMS analysis of the liberated CO yields a precision of ±0.15‰ (1σ, = 28) and shows excellent agreement with (and improved precision over) traditional fluorination methods. This practical and safe technique expands access to oxygen-isotope measurements of iron oxides, thereby enhancing their utility in Earth and environmental sciences.
Download full-text PDF |
Source |
---|---|
http://www.ncbi.nlm.nih.gov/pmc/articles/PMC11983365 | PMC |
http://dx.doi.org/10.1021/acs.analchem.4c04676 | DOI Listing |
Nat Chem
September 2025
Department of Chemistry, University of Wisconsin-Madison, Madison, WI, USA.
Proton transfer plays an important role in both hydrogen and oxygen evolution reactions during electrocatalytic water splitting to produce green hydrogen. However, directly adapting the conventional proton/deuterium kinetic isotope effect to study proton transfer in heterogeneous electrocatalytic processes is challenging. Here we propose using the shift in the Tafel slope between protic and deuteric electrolytes, or the Tafel slope isotope effect, as an effective probe of proton transfer characteristics.
View Article and Find Full Text PDFSci Total Environ
September 2025
Department of Animal Sciences and Aquatic Ecology, Ghent University, Gent, Belgium.
Wetlands play a crucial role in global greenhouse gas (GHG) dynamics, yet their response to climate change is not yet fully understood. Here, we investigate how increasing temperature and oxygen availability interact to regulate wetland GHG emissions through combined analysis of biogeochemical and functional gene measurements. We found distinct temperature-dependent shifts in carbon emission pathways, with CO emissions unexpectedly declining as temperature rose from 15 to 25 °C, while increasing consistently at higher temperatures (25-35 °C), reflecting a transition to more thermally-driven processes.
View Article and Find Full Text PDFJ Environ Manage
September 2025
State Key Laboratory of Water Engineering Ecology and Environment in Arid Area, Inner Mongolia Agricultural University, Hohhot, 010018, China; Inner Mongolia Key Laboratory of Ecohydrology and High Efficient Utilization of Water Resources, Hohhot, 010018, China; Inner Mongolia Section of the Yellow
Large-scale underground coal mining alters regional water cycles, yet the mechanisms governing interactions among water bodies in deep mining areas are poorly understood. For this purpose, by integrating hydrogen and oxygen isotopes, water levels, hydrogeological conditions, and end-member mixing analysis (EMMA), this study systematically analyzed and quantified the circulation and transformation mechanisms among different water bodies influenced by coal mining. Key findings reveal: (1) Mining-induced fractures disrupt the aquitard above the coal seam, establishing a direct hydraulic link between Zhiluo Formation confined groundwater and mine water, with the former contributing 87.
View Article and Find Full Text PDFSci Adv
September 2025
Department of Earth and Planetary Sciences, Stanford University, Stanford, CA, USA.
The Early Paleozoic radiation of diverse animal life is commonly connected to a well-ventilated global ocean. Yet the oxygenation history of Paleozoic deep oceans remains debated. Using thallium (Tl) isotope ratios in deep-marine mudrocks, we reconstruct the history of deep marine oxygenation from ~485 to 380 million years ago.
View Article and Find Full Text PDFYing Yong Sheng Tai Xue Bao
July 2025
School of Geography and Environmental Sciences, Guizhou Normal University, Guiyang 550025, China.
Understanding the stable isotope changes of soil water, hydrogen, and oxygen under different land cover in karst areas is beneficial for revealing the infiltration and transport processes of soil water, as well as the impact of different land cover on hydrological processes, providing theoretical basis for regional water resource utilization and ecological environment construction. We measured hydrogen and oxygen isotope of soil water in 0-50 cm profiles under four different land covers (bare land, cultivated land, grassland, and shrubland) at the Puding Karst Ecological Station in Guizhou Province from May 2021 to April 2022 through regular field sampling and indoor experiments. The stable isotope changes of hydrogen and oxygen in precipitation and soil water at 10, 25, and 45 cm layers under four land covers were compared and analyzed.
View Article and Find Full Text PDF