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Sediment accumulation from upland agricultural erosion provided a source of P along drainageways, where shallow, reductive groundwater increased P solubility.
EC of groundwater increased towards the east following the general groundwater flow direction.
This scenario may account for the decrease in infiltration to groundwater, increased surface runoff and decline in baseflow observed in the current study.
The production of groundwater increased dramatically over the last 20 years, to make up for the shortfall of surface water supply and also to meet a rise in demand, particularly in the Urban Grouping of Tlemcen.
Although the concentration of Cl− in borehole groundwater increased with depth, that in the groundwater seepages were higher than in boreholes at the same depth (−300 m) (Table 1).
They include acid drainage induced by the sudden rapid exposure and subsequent oxidation of formerly buried materials, the introduction of metals into surface-water and groundwater, increased erosion, sulfur-gas emissions, and air pollution caused by the production of particulates during processing, transport, and support activities.
Similar(53)
High concentration of bi-carbonates in groundwater increases the precipitation of calcium and magnesium as carbonates.
The transport of pathogens from surface water to groundwater increases the vulnerability of groundwater (Jin and Flury [2002]).
The hydrostatic pressure in the groundwater increases with depth, creating a large horizontal pressure gradient, driving water into the pipe.
But as water has been drawn at a higher rate than natural replenishment, seawater from the Mediterranean has infilitrated the groundwater, increasing salinity to unsafe levels.
More specifically, Pisinaras (2016) investigated potential climate change effects in an aquifer located in northeastern Greece and the results indicated a significant decrease in groundwater level, as a result of decreased groundwater recharge and increased groundwater abstractions for irrigation.
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