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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
refutedsupported
the weight of evidence
3 sources for · 0 against

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.

Evidence for · 3
Influence of subhumid climate and water table depth on groundwater recharge in shallow outwash aquifers
2008 · cited by 59
Demonstrates that groundwater recharge and infiltration dynamics depend significantly on water table depth and local hydrogeological conditions.
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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.

More for · 2
Integrating remote sensing and multi-criteria decision analysis for groundwater zoning in the Eastern Desert of Egypt.
2026 · cited by 0
Shows that lithology and soil characteristics are critical thematic layers when evaluating groundwater potential and infiltration zones.
Enhancing groundwater recharge mapping in arid regions with geospatial multi-criteria analysis in the Eastern desert of Egypt.
2026 · cited by 0
Identifies lithology and soil characteristics as dominant controls on groundwater recharge and potential distribution.
The paper trail · every fact has a biography
first checked04 Aug 2026
judged → SUPPORTED · 8604 Aug 2026
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