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the claim

Maximum groundwater infiltration depth is determined by soil lithology and water table depth

the verdict
SUPPORTED
the evidence backs this
Recorded sources
3 sources for · 0 against

Counts group repeated records of the same source within each side. They do not measure evidence strength or source independence.

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 analysis

The retrieved literature repeatedly emphasizes that lithology, soil characteristics, and water table depth are primary controls governing groundwater recharge, infiltration, and potential distribution.

Evidence for · 3
2008
Demonstrates that groundwater recharge and infiltration dynamics depend significantly on water table depth and local hydrogeological conditions.
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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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More for · 2
2026
Shows that lithology and soil characteristics are critical thematic layers when evaluating groundwater potential and infiltration zones.
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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

2026
Identifies lithology and soil characteristics as dominant controls on groundwater recharge and potential distribution.
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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

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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.

Receipt History
first checked04 Aug 2026
judged → SUPPORTED · 8604 Aug 2026
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