Groundwater. Water on Earth Artesian and Non-flowing (pumping) Wells.

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Presentation transcript:

Groundwater

Water on Earth

Artesian and Non-flowing (pumping) Wells

Saturated and Unsaturated Zones

Gaining and Losing Streams

Darcy’s law THIS IS EASY!!!!! Discharge/Flow = (Hydraulic Conductivity x Area) x (Hydraulic Gradient) Hydraulic Conductivity x Area This is the ease at which fluids flow through the material. Coarser material is easiest Finer material is harder Hydraulic Gradient This is the pressure pushing the water The more pressure the steeper the surface the faster the flow.

Hydraulic Conductivity x Area “The ease at which fluids flow through the material” Coarser material is easiest Finer material is harder

Groundwater Flows From High to Low Areas (Hydraulic Gradient)

Hydraulic Gradient

Groundwater Flowlines

Darcy’s law THIS IS EASY!!!!! Discharge/Flow = (Hydraulic Conductivity x Area) x (Hydraulic Gradient) Hydraulic Conductivity x Area This is the ease at which fluids flow through the material. Coarser material is easiest Finer material is harder Hydraulic Gradient This is the pressure pushing the water The more pressure the steeper the surface the faster the flow.

Springs and Perched Water Tables

Spring-Arizona’s Marble Canyon

Hot Springs and Geysers

Geysers How They Work

Groundwater and Caves

Groundwater Withdrawal

Heavy Pumping of Groundwater

Groundwater Contamination