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Potential sources of present-day recharge to theSaq-Ram Sandstones include: Runoff from the Basement in the south- west directly passing over outcrops of the permeable sandstones. Infiltration of runoff through wadi beds. Infiltration of rain falling directly on the sandstones, sand dunes or through overlying soils. Infiltration of excess irrigation water (locally, mainly in outcrop areas).
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