Integrated Hydrogeological Approach for an Aquifer System and Groundwater Flow, Nukhaib-Km160 Area, Western Iraq
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Abstract The hydraulic characteristics and the hydrogeological conditions of the hydrogeological system at Nukhaib-Km160 were studied within the water-bearing horizons, highlighting the flow system and its effects on the groundwater velocities and its balance (hydraulic gradients and permeability) taking into account the regional situations of structural. Several hydrogeological areas have been selected for future exploitation and development. 3D models and maps of spatial distribution are utilized for interpretation, it is supported by points of hydrogeological controls such as transmissivity and storage coefficients, depth of groundwater, lateral extensions, aquifers thickness, specific capacity, and well productivity. Prediction applications on specific capacities and transmissivity of aquifer and Kimball’s statistical method were used to calculate the ratio of groundwater mixing and recharge from aquifers of Umm Er Dhuma and/or Tayarat Fn. to production wells. The hydrogeological system of the Nukhaib- Km160 region has been categorized into eight major aquifers which include the Mulussa, Mulussa-Ubaid, Muhaywir-Ubaid, Hartha, Muhaywir-Najma, Umm Er Dhuma, Tayarat, and Tayarat- Umm Er Dhuma aquifers. Changes in hydraulic parameters for all aquifers have been examined in order to determine the spatial-hydrologic facts of aquifers, where the traditional TDS distribution, in addition to the hydraulic interpretation, shows the same phenomenon of interconnection and the source of groundwater. According to facts of the hydrogeological, the aquifers of Umm Er Dhuma and Tayrat are important and preferred for the plan of the future of water supply in the Western Desert of Iraq, especially for the increased demand for water resources and the sustainability of the assessment.Depression-focused recharge
Water balance
Groundwater discharge
Groundwater model
Infiltration (HVAC)
Cone of depression
Environmental isotopes
Overexploitation
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Depression-focused recharge
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The present study deals with the problem of evaluation of the recharge mechanism and the characterization of the groundwater flow system in the basement shallow aquifer, which is one of the groundwater resource in the semi-arid South region of Madagascar. Stable isotopes (deuterium and oxygen-18) and tritium are used to achieve with accuracy the hydrogeological and geochemical dynamics study. Chemical analysis is used to provide complementary information to the investigation. A space distribution of tritium concentration and isotopic composition in groundwater shows evidence of two opposite categories of aquifers, which is confirmed by the chemical analysis results and by the geological features of the study site. Some groundwater flow path directions have been identified in the study area thanks to the tritium concentration space distribution and the geological formation. Besides, the groundwater recharge of the shallow aquifers in the South of Madagascar has been characterized by the exponential mixing model.
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Abstract In an aquifer system with complex hydrogeology, mixing of groundwater with different ages could occur associated with various flow pathways. In this study, we applied different groundwater age‐estimation techniques (lumped parameter model and numerical model) to characterize groundwater age distributions and the major pathways of nitrate contamination in the Gosan agricultural field, Jeju Island. According to the lumped parameter model, groundwater age in the study area could be explained by the binary mixing of the young groundwater (4–33 years) and the old water component (>60 years). The complex hydrogeologic regimes and local heterogeneity observed in the study area (multilayered aquifer, well leakage hydraulics) were particularly well reflected in the numerical model. The numerical model predicted that the regional aquifer of Gosan responded to the fertilizer applications more rapidly (mean age: 9.7–22.3 years) than as estimated by other models. Our study results demonstrated that application and comparison of multiple age‐estimation methods can be useful to understand better the flow regimes and the mixing characteristics of groundwater with different ages (pathways), and accordingly, to reduce the risk of improper groundwater management plans arising from the aquifer heterogeneity.
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Environmental isotopes
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Understanding the hydrogeological functioning of aquifers is essential in contexts where water resources are intensively used. Moreover, climate change can have long-term effects on groundwater in terms of availability, residence and transit times. Thus, careful management of groundwater resources require the understanding of the aquifer’s characteristics that can allow then the setting of sustainable yields values in contexts where water is exploited. This understanding requires in particular the estimation of the age of the groundwaters as well as the transfers/transit times within the aquifers. Our study focuses on the Volvic volcanic aquifer (Chaîne des Puys, France), where the question of water use has increasingly raised for several years, given the significant use of drinking water, both for the public drinking water network and bottled water, and the decrease of precipitations (and groundwater recharge) over the watershed due to climate change. Previous studies on Volvic watershed allow defining the overall functioning of the system and comparing withdrawals and recharge on an annual scale, but groundwater ages have been only roughly defined even if they appear as a key point for addressing the question of the resource decrease. We propose then a multi-tracers approach, based on hydrogeological monitoring (hydrodynamical and meteorological data’s), including the estimation of groundwater ages (CFCs, tritium (3H)), major and traces elements chemistry and water stable isotopes (18O/2H) to better characterise this resource decrease and more peculiarly its origin and its impact on the environment that has never been addressed.  The relative fractions of modern and ancient water contributions to the Volvic aquifer will thus be estimated as well as the apparent ages of groundwaters. We highlight here the complementarity of tracers used in the dating of waters, which allows a better definition of recharge sources and flow paths within the aquifer. This will provide key information about the time of the recharge and the time when the decrease began due to increase of abstraction, climate change or a combination of both of these effects.
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The concentrations of chlorofluorocarbons (CFC-11, CFC-12 and CFC-113) and tritium (3H) content in groundwater were used to date groundwater age, delineate groundwater flow systems and estimate flow velocity in the Hohhot basin. The estimated young groundwater age is fallen in the bracket of 21 ~ 50 a and indicates the presence of two different age profiles and flow systems in the shallow groundwater system. Older age waters occur under the topographically low areas, where the aquifer is double-layer aquifer system consisting of shallow unconfined-semi-confined aquifer and deep confined aquifer. This reflects long flow paths associated with regional flow. Groundwater (range from 21 to 34 years) in the north piedmont and east hilly areas, where the aquifer is a single-layer aquifer consisting of alluvial fans, are typically younger than those in the low areas. The combination of CFCs dating with hydrogeological information indicates that both local and regional flow systems are present at the basin. The regional groundwater flow mainly flows from the north and east to the southwest, the local groundwater flow system occurs nearby the Hohhot city. The mean regional groundwater flow velocity of the shallow groundwater is estimated about 0.73 km/a. These findings can aid in refining hydrogeological conceptual model of the study area. Copyright © 2012 John Wiley & Sons, Ltd.
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