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Trees may survive prolonged droughts by shifting water uptake to reliable water sources, but it is unknown if the dominant mechanism involves activating existing roots or growing new roots during drought, or some combination of the two. To gain mechanistic insights on this unknown, a dynamic root-hydraulic modeling framework was developed that set up a feedback between hydraulic controls over carbon allocation and the role of root growth on soil-plant hydraulics. The new model was tested using a 5 yr drought/heat field experiment on an established piñon-juniper stand with root access to bedrock groundwater. Owing to the high carbon cost per unit root area, modeled trees initialized without adequate bedrock groundwater access experienced potentially lethal declines in water potential, while all of the experimental trees maintained nonlethal water potentials. Simulated trees were unable to grow roots rapidly enough to mediate the hydraulic stress, particularly during warm droughts. Alternatively, modeled trees initiated with root access to bedrock groundwater matched the hydraulics of the experimental trees by increasing their water uptake from bedrock groundwater when soil layers dried out. Therefore, the modeling framework identified a critical mechanism for drought response that required trees to shift water uptake among existing roots rather than growing new roots.
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http://dx.doi.org/10.1111/nph.16043 | DOI Listing |
F1000Res
September 2025
Department of Biotechnology, Faculty of Life and Allied Health Sciences, M.S. Ramaiah University of Applied Sciences, Bengaluru, Karnataka, 560054, India.
Background: Chintamani village, Chikkaballapura district, Karnataka, India was found to possess high aquifer uranium concentrations. Geologically, Chintamani village is located on bedrock that is rich in elements like potassium (K) that naturally contain high levels of radioactive elements, such as uranium and thorium, due to the presence of alkali-feldspar granites and gneisses. Aquifer depletion has caused the concentration of these elements in groundwater to increase over time, posing a potential health hazard to the residents of Chintamani village.
View Article and Find Full Text PDFSci Rep
September 2025
Department of Microbial Interactions, Institute of Microbiology, Friedrich Schiller University (FSU), Jena, Germany.
Subsurface habitats, found under various geological conditions, exhibit diverse microbial communities. The vadose zone, a previously unexplored subsurface compartment, connects the surface to phreatic groundwater. Drilling into the subsurface allows access to these habitats for microbial diversity study.
View Article and Find Full Text PDFEnviron Pollut
August 2025
School of Water Resources and Environment, Key Laboratory of Groundwater Conservation of MWR, and State Key Laboratory of Geomicrobiology and Environmental Changes, China University of Geosciences (Beijing), Beijing, 100083, PR China. Electronic address:
Different hydrodynamic sedimentary conditions may cause significant differences in the enrichment behavior of selenium (Se) in soils with the same provenance. To elucidate basin-scale Se enrichment mechanisms, adjacent Songhua River (alluvial) and Naoli River (lacustrine) Basins with the same bedrocks but differing sedimentary environments were investigated, and 5369 topsoils (0-20 cm depth) and 1380 subsoils (at 1.5 m depth) were collected and analyzed.
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July 2025
Department of Earth Sciences, The University of Hong Kong, Pokfulam Road, Hong Kong, Hong Kong.
Determining the current presence of liquid water on Mars has important hydrological, geological, and astrobiological implications. Recurring slope lineae (RSL), as features presently developing on Mars, have been suggested to result from transient flows of liquid water or dry particles. This study presents a time-series analysis of RSL in Palikir and Raga craters on Mars, using datasets collected during Mars years (MY) 32 to 36.
View Article and Find Full Text PDFHuan Jing Ke Xue
June 2025
Center for Hydrogeology and Environmental Geology, China Geological Survey, Tianjin 300304, China.
To study the hydrochemical characteristics and controlling factors of groundwater from the quaternary aquifer, basalt aquifer, and other bedrock aquifer in the Angulinao Basin, 175 water samples from groundwater, surface water, and rain were collected. Comprehensive methods such as mathematical statistics, Piper trilinear diagram, Gibbs plot, ion ratio, and factor analysis were used to analyze and explore the hydrochemical characteristics and controlling factors of the groundwater in the study area. The results showed that the groundwater was characterized by a generally low alkalinity, with average TDS values of the three types of groundwater, from highest to lowest, shown as follows: 929.
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