Hydraulic Head - Hydraulic Head in Groundwater

Hydraulic Head in Groundwater

Relation between heads for a hydrostatic case and a downward flow case.

The distribution of hydraulic head through an aquifer determines where groundwater will flow. In a hydrostatic example (first figure), where the hydraulic head is constant, there is no flow. However, if there is a difference in hydraulic head from the top to bottom due to draining from the bottom (second figure), the water will flow downward, due to the difference in head, also called the hydraulic gradient.

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