Factors controlling groundwater hydrogeochemistry in the area west of Tahta, Sohag, Upper Egypt
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Sixteen groundwater samples were collected from the area west of Tahta, Sohag, Egypt.

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Piper diagram showed the predominance of Na–Cl type (75%) in groundwater.

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Dissolution and ion exchange reactions are the main source of ions in the aquifer.

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Anthropogenic inputs due to using fertilizers impact the new reclaimed areas.

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The R-mode factor analysis helped in recognizing the main inputs in the aquifer.

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