Guidance for the Integrated Use of Hydrological, …
Stable isotopes provide a useful tool to assess water sources as well as mixing fractions in mine-related environments. For …
Stable isotopes provide a useful tool to assess water sources as well as mixing fractions in mine-related environments. For …
The research results may provide scientific guidance for the rational development and utilization of water resources in coal mining subsidence areas, enrich the study of the hydrological cycle in the area, and are of great significance for the protection of the local water balance and water environment.
Bojar et al. (2020a) combined stable isotopes, and major anion and cation distributions in spring and borehole water with field-derived geological information. The investigated area belongs to a region with high continentality index, Mehedinți County, Romania. The siliciclastic aquifer is situated in Quaternary deposits of the Moesian unit.
This paper summarizes international state-of-the-art applications and opportunities for employing and deploying hydrological, geochemical, and isotopic tools in an integrated manner for investigations of mining operations. It is intended to aid formulation of more integrated approaches for evaluating the overall sustainability of …
Together with MTT, Fyw is a highly reliable variable applied to hydrological assessment in heterogeneous, anthropogenic …
Meanwhile, the water stable isotopes (δ 2 H, δ18 O) in J 2 z and J 2 y groundwater show obviously consistent depletion in June 2018 (e.g., borehole J17 and SK16).
Here, we constrained a Bayesian mixing model with stable isotope data (2018–2019) in rainfall (N = 704), spring water (N = 96), and surface water (N = 94) with seasonal isotope sampling (wet and ...
Stable isotopes of oxygen and hydrogen (δ 18 O and δ 2 H) in waters are effective tracers for identifying stream water sources, hydrologic flowpaths and understanding hydrological processes across a range of spatial and temporal scales (McGuire and McDonnell, 2006, Klaus and McDonnell, 2013, Jasechko et al., 2016).
To effectively restore the groundwater environment of the Shiping Mine (SPM) area, which is contaminated by acid mine drainage (AMD), a hydrogeochemical conceptual model was constructed based on groundwater chemistry and environmental stable isotopes. The contribution rate of various pollution sources in the groundwater …
Coal mining may cause considerable environmental problems (Gomo and Vermeulen 2014) including the excessive decline in the elevation of the water table, the drying up of springs near mine sites, the reduction of river levels, and the contamination of groundwater and nearby surface water bodies (Howladar et al. 2017).Consequently, coal …
Spatiotemporal variations in soil water content (SWC) and soil water stable isotopic compositions (SWSIC; 2 H/ 1 H (δD) and 18 O/ 16 O (δ 18 O)) provide critical information on elucidating land surface processes across scales. Meanwhile, little is known about the spatiotemporal characteristics of SWSIC and its driving factors. Therefore, it's …
Abstract. Measurement and modeling of the stable isotope signature of water in continental runoff provides unique information for large scale hydrological process studies and global water budget assessment. This chapter presents theory and case studies that illustrate isotopic signals relevant to understanding large scale hydrological …
central, eastern, and western areas of the basin from July, 2017 to July, 2018 for stable isotope tests; whereas, three of these samples were also used for hydrochemical tests. The samples were filtered through 0.45 μm membranes on Fig. 2 Hydrogeological cross-section (along line A–A′ in Fig. 1) of the study area
Future studies, ideally using multi-isotope approaches combined with element isotope mass balances and modeling/assessment of potential post-release fractionation, are expected to confirm the promise offered by stable isotope systems in source identification as well as to provide more precise and accurate estimates of the fate of …
Stable isotopes in water of oxygen (16 O and 18 O) and hydrogen (1 H and 2 H) are typically inert and conservative in mixing relationships and used as a tracer to investigate hydrogeological and hydrological processes including groundwater recharge and groundwater–surface-water interaction [14,15].Accordingly, the deuterium excess (D ex) …
Hydrogen and oxygen stable isotopes (2 H/ 1 H and 18 O/ 16 O), as components of water molecules, are a particular category of environmental tracer. Variations in isotopic abundances can be used to infer water environmental processes such as recharge, flow path, discharge and evaporation ( Chang et al., 2020, Hu et al., 2020, Liu et al., 2022 ...
Lithium and Boron isotope are number of the "non-traditional stable isotopes", which have become one of the most popular fields and frontiers of isotope geochemistry in recent years (He et al., 2020). large mass differences between Li isotopes and B isotopes lead to large isotope fractionation during geological processes …
Here, we explore and evaluate the feasibility of using the stable isotopes of oxygen and hydrogen (18 O, 2 H) to track hydrological processes at an operating oil …
The slope and intercept of LMWL are smaller than those of GMWL (Global Meteoric Water Line: δD = 8δ 18 O + 10), indicating the aridity of the plain area (Craig, 1961). The stable isotopes values of snowmelt water in the mountainous areas are from −84.18 to −37.00 ‰ for δD and from −11.90 to −7.10 ‰ for δ 18 O with the average ...
Combining unmanned aerial vehicle-based remote sensing and stable water isotope analysis to monitor treatment peatlands of mining areas May 2019 Ecological Engineering 133(1):137-147
This CRP aims to improve the capability and expertise among Member States for the use of environmental isotope techniques to assess hydrological …
The existing studies on water age in alpine catchment focused on investigating the impacts of topography, vegetation, and snow on water age using short-term isotope data, and did not consider the effects of glacier and permafrost changes on hydrological processes (Ceperley et al., 2020, Song et al., 2017, Yang et al., 2021).
The karst water resources in the Fengfeng mining area are an important water supply source in the region. In recent years, due to the influence of external environment changes, the hydrochemical environment of karst groundwater has changed. In order to scientifically understand karst groundwater and rationally develop …
Stable and radioisotopes isotopes of water in and around mine complexes can be used to help fingerprint and trace the origin, age, flow, transport and all the complex hydrological phenomena involving water availability and quality. ... for the use of environmental isotope techniques to assess hydrological processes in mining areas …
Hydrogen and oxygen stable isotope tracing technique is adopted in this study, to analyze the composing characteristics, circulation process and recharge sources of mid-layer groundwater in Waibei ...
Fraction of young water (Fyw) and mean transit time (MTT, ̅) calculated from water isotope profiles are valuable information for catchment hydrological assessment, especially in an ...
Therefore analysis of stable water isotopes is a powerful tool for studying complex contaminant behavior and interactions in mining-influenced environments (Larkins et al., 2018), as well as water flow paths and preferential flow areas in wetlands (e.g., Carrer et al., 2015, Palmer et al., 2015, Ronkanen and Kløve, 2008, Sun et al., 2016).
However, there is less research on hydrological process based on δD-H 2 O and δ 18 O-H 2 O. Hydrochemical and isotopic composition of river water, reservoir water, shallow groundwater (water level between 0 and 30 m), deep groundwater (water level≥50 m) and precipitation in mining area of Fenhe River Basin are analyzed in this study.
In this paper, descriptive statistical method, stable isotope measurements and Piper trilinear diagram are employed to analyze the interaction among river water, groundwater …
Abstract. The oxygen and hydrogen isotopic compositions (δ 18 O and δ 2 H) were measured on river water and precipitation collected from four sub-catchments …
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