| Records |
| Author |
Mallick, J.; Singh, C.K.; AlMesfer, M.K.; Kumar, A.; Khan, R.A.; Islam, S.; Rahman, A. |
Title  |
Hydro-geochemical assessment of groundwater quality in Aseer Region, Saudi Arabia |
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Journal Article |
| Year |
2018 |
Publication |
Water |
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10 |
Issue |
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Pages |
1847 |
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CUT @ phaedon.kyriakidis @ Mallick2018 |
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120 |
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Carreira, P. M.; Marques, J. M. |
| Title |
Groundwater Salinity and Environmental Change Over the Last 20,000 Years: Isotopic Evidences in the Lower Sado Aquifer Recharge, Portugal |
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Book Whole |
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2018 |
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Impacts of the Water Resources Variability on Cereal Yields in the Region of Souss-Massa Southern MoroccoErstes |
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Springer |
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THL @ christoph.kuells @ |
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183 |
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Bahir, M.; Ouhamdouch, S.; Carreira, P.M. |
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Geochemical and isotopic approach to decrypt the groundwater salinization origin of coastal aquifers from semi-arid areas (Essaouira basin, Western Morocco) |
Type |
Journal Article |
| Year |
2018 |
Publication |
Environmental Earth Sciences |
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| Volume |
77 |
Issue |
13 |
Pages |
485 |
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| Abstract |
In arid and semi-arid areas, the groundwater is the main source of water supply and agricultural activity. Overexploitation of coastal aquifers and pollution vulnerability are among the main problems related to groundwater resources assessment and management in these zones. In fact, in the last decades, these resources have been threatened by a degradation of their quality and quantity that furthers natural and anthropic effects, such as climate change, seawater intrusion and overexploitation. However, the protection and management of these resources requires knowledge of the origin of their mineralization. In this study, the Essaouira basin is selected as a typical example. Stable isotopes (18O and 2H) together with geochemical data were used to identify the groundwater salinization origin in the coastal aquifers of the Essaouira basin. The results of both the approaches show that the groundwater mineralization is due to: (1) the dissolution of salt minerals, (2) the ion exchange phenomena, (3) seawater intrusion, and (4) sulphate reduction. Also, the recharge is supported by fast infiltration of oceanic precipitation without significant evaporation. |
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1866-6299 |
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THL @ christoph.kuells @ Bahir2018 |
Serial |
177 |
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| Author |
Han, D.; Currell, M.J. |
| Title |
Delineating multiple salinization processes in a coastal plain aquifer, northern China: hydrochemical and isotopic evidence |
Type |
Journal Article |
| Year |
2018 |
Publication |
Hydrology and Earth System Sciences |
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22 |
Issue |
6 |
Pages |
3473-3491 |
| Keywords |
Isotopes, China, multiple salinization |
| Abstract |
Groundwater is an important water resource for agricultural irrigation and urban and industrial utilization in the coastal regions of northern China. In the past 5 decades, coastal groundwater salinization in the Yang–Dai river plain has become increasingly serious under the influence of anthropogenic activities and climatic change. It is pivotal for the scientific management of coastal water resources to accurately understand groundwater salinization processes and their causative factors. Hydrochemical (major ion and trace element) and stable isotopic (δ18O and δ2H) analysis of different water bodies (surface water, groundwater, geothermal water and seawater) were conducted to improve understanding of groundwater salinization processes in the plain's Quaternary aquifer. Saltwater intrusion due to intensive groundwater pumping is a major process, either by vertical infiltration along riverbeds which convey saline surface water inland, and/or direct subsurface lateral inflow. Trends in salinity with depth indicate that the former may be more important than previously assumed. The proportion of seawater in groundwater is estimated to have reached up to 13 % in shallow groundwater of a local well field. End-member mixing calculations also indicate that the geothermal water with high total dissolved solids (up to 10.6 g L−1) with depleted stable isotope compositions and elevated strontium concentrations (> 10 mg L−1) also mixes locally with water in the overlying Quaternary aquifers. This is particularly evident in samples with elevated Sr ∕ Cl ratios (> 0.005 mass ratio). Deterioration of groundwater quality by salinization is also clearly exacerbated by anthropogenic pollution. Nitrate contamination via intrusion of heavily polluted marine water is evident locally (e.g., in the Zaoyuan well field); however, more widespread nitrate contamination due to other local sources such as fertilizers and/or domestic wastewater is evident on the basis of NO3 ∕ Cl ratios. This study provides an example of how multiple geochemical indicators can delineate different salinization processes and guide future water management practices in a densely populated water-stressed coastal region. |
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THL @ christoph.kuells @ hess-22-3473-2018 |
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81 |
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Karami*, S.; Madani, H.; Katibeh, H.; Marj, A.F. |
| Title |
Assessment and modeling of the groundwater hydrogeochemical quality parameters via geostatistical approaches |
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Journal Article |
| Year |
2018 |
Publication |
Appl. Water Sci. |
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8:23 |
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CUT @ phaedon.kyriakidis @ Karami2018 |
Serial |
122 |
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