Maximum groundwater infiltration depth is determined by soil lithology and water table depth
Is it true that maximum groundwater infiltration depth is determined by soil lithology and water table depth?
Yes. Maximum groundwater infiltration depth is strongly controlled by subsurface lithology and the depth to the water table, as confirmed by hydrological and multi-criteria spatial analyses.
Verdict: SUPPORTED · 3 sources for, 0 against · Last checked
The retrieved literature repeatedly emphasizes that lithology, soil characteristics, and water table depth are primary controls governing groundwater recharge, infiltration, and potential distribution.
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Smerdon, B. D., Mendoza, C. A., & Devito, K. J. (2008). Influence of subhumid climate and water table depth on groundwater recharge in shallow outwash aquifers. doi.org. https://doi.org/10.1029/2007wr005950
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H, E. (2026). Integrating remote sensing and multi-criteria decision analysis for groundwater zoning in the Eastern Desert of Egypt.. doi.org. https://doi.org/10.1038/s41598-026-55824-y
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M, S., SA, K., T, S., A, S., D, A., A, G., A, A., & A, A. (2026). Enhancing groundwater recharge mapping in arid regions with geospatial multi-criteria analysis in the Eastern desert of Egypt.. doi.org. https://doi.org/10.1038/s41598-026-39134-x
What does the evidence say?
The retrieved literature repeatedly emphasizes that lithology, soil characteristics, and water table depth are primary controls governing groundwater recharge, infiltration, and potential distribution.
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