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Listen to native speakers pronounce “water table” in real conversational contexts with synchronized timestamps and subtitles.
Deeper down, groundwater completely fills a material’s pores.This point marks the water table — the boundary where water-saturated ground begins.Water tables rise and fall for all sorts of reasons: the slope of the land, the amount of rainfall or snowmelt, the porosity and permeability of the rock, and even how the land is used.
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