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Nitrogen (N) stored in deep profiles is important in assessing regional and/or global N stocks and nitrate leaching risk to groundwater. The Chinese Loess Plateau, which is characterized by significantly thick loess deposits, potentially stores immense stocks of mineral N, posing future threats to groundwater quality. In order to determine the vertical distributions of nitrate and ammonium content in the region, as well as to characterize the potential accumulation of nitrate in the deep loess profile, we study loess samples collected at five sites (Yangling, Changwu, Fuxian, An'sai and Shenmu) through a 50 to 200m loess profile. The estimated storage of mineral N varied significantly among the five sites, ranging from 0.46 to 2.43×10kgNha. Ammonium exhibited fluctuations and dominated mineral N stocks within the whole profile at the sites, except for the upper 20-30m at Yangling and Changwu. Measured nitrate content in the entire profile at Fuxian, An'sai and Shenmu is low, but significant accumulations were observed to 30-50m depth at the other two sites. Analysis of δN and δO of nitrate indicates different causes for accumulated nitrate at these two sites. Mineralization and nitrification of manure and organic N respectively contribute nitrate to the 0-12 and 12-30m profile at Changwu; while nitrification of NH fertilizer, NO fertilizer and nitrification of organic N control the nitrate distribution in the 0-3, 3-7 and 7-10m layer at Yangling, respectively. Furthermore, our analysis illustrates the low denitrification potential in the lower part of the vadose zone. The accumulated nitrate introduced by human activities is thus mainly distributed in the upper vadose zone (above 30m), indicating, currently, a low nitrate leaching risk to groundwater due to a high storage capacity of the thick vadose zone in the region.
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http://dx.doi.org/10.1016/j.scitotenv.2018.03.249 | DOI Listing |
J 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 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
College of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi, 712100, China. Electronic address:
Groundwater plays a pivotal role in mediating nitrogen transfer to aquatic ecosystems, particularly in arid regions. Water scarcity, coupled with intensive agricultural activities, has placed the groundwater systems under significant pressure from non-point source pollution, underscoring the need for targeted investigation. Focusing on the Chinese Loess Plateau (CLP), we combined dual-isotope analysis (δN-NO, δO-NO) with water isotopes (δD-HO, δO-HO) and implemented a dual-framework approach to investigate nitrate dynamics.
View Article and Find Full Text PDFLangmuir
August 2025
Department of Chemistry, Umeå University, Umeå SE-901 87, Sweden.
The geochemical behaviors of phosphate-containing species at mineral surfaces are of fundamental importance for controlling phosphorus (P) mobility, fate, and bioavailability. Understanding these interfacial behaviors in water-unsaturated environments, where minerals are covered by thin water films, is of special importance in the context of soil vadose zone geochemistry. This study resolved the transformation of pyrophosphate to orthophosphate within the confines of nanometer-thick water films condensed on nanosized birnessite (MnO).
View Article and Find Full Text PDFJ Contam Hydrol
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:
Understanding selenium (Se) distribution mechanisms in groundwater from farmlands is crucial for ensuring water resource safety. In this study, the distribution patterns and sources of Se in the groundwater of Bawuer, Daxing, and Xinglonggang farmlands within the Naoli River Basin (Sanjiang Plain, Northeast China) were analyzed through comprehensive analyses of 154 groundwater samples and 200 soil/sediment samples from boreholes in the farmlands. Isotopic data of δD and δO demonstrated that precipitation and river recharge are the primary sources of groundwater.
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