Genetically, most saline groundwater bodies are to one of the following categories:
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Main class of origin |
Genetic category or salinization mechanism |
Typical environment at the time of origin |
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A0 Marine origin |
A1. Connate saline water |
Coastal zone (off-shore) |
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A2. Intruded by marine transgression |
Coastal zone (off-shore) |
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A3. Intruded by recent incidental flooding by the sea |
Coastal zone (on-shore) |
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A4. Laterally intruded sea water |
Coastal zone (on-shore) |
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A5. Intruded sea water sprays (aerosols) |
Coastal zone (on-shore) |
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A6. Mixture of A2 (marine transgression) and A3 (recent incidental flooding by sea) |
Coastal zone (on and off-shore) |
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A7. Mixture of A1 (connate water), A2 (marine transgression) and A3 (recent incidental flooding by sea) |
Coastal zone (on and off-shore) |
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B0 Terrestrial origin - natural |
B1. Produced by evaporation (concentration) |
Shallow water-table zones in arid climates |
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B2. Produced by dissolution of subsurface salts |
Zones of salt tectonics or regional halite or other dissolvable formations |
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B3. Produced by salt filtering membrane effects |
At depth in thick sedimentary basins containing semi-permeable layers |
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B4. Emanated juvenile water and other products of igneous activity |
Regions of igneous activity |
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B5. Mixture of B1 (evaporation) and B2 (dissolution) |
Shallow water-table zones in arid climates and aquifers containing dissolvable formations |
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C0 Terrestrial origin - anthropogenic |
C1. Produced by irrigation (input of concentrated residual water) |
Arid and semi-arid zones; shallow depths |
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C2. Anthropogenically polluted groundwater |
Anywhere on earth, particularly in modern consumptive societies |
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D0 Mixed origin |
D0 Saline groundwater produced by mixing an A-, B- or C-class mineralized groundwater with fresh water or with another type of saline groundwater. |
Anywhere on earth; hydraulic gradients facilitate the mixing processes |