The piezometric surface is an imaginary surface that represents the total head of groundwater and indicates the level to which water will rise in a well. It is crucial for understanding groundwater flow and pressure distribution in confined aquifers, helping in the design and management of water resources systems.

Piezometric Surface

piezometric surface

total head of groundwater

level to which water will rise in a well

Groundwater flow refers to the movement of water through the subsurface, driven by gravity and pressure differences within aquifers. Understanding groundwater flow is critical for water resource management, pollution control, and predicting the impacts of climate change on water availability.

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