Lecture6 - Groundwater P = Q + ET + G + S Floridan Aquifer...

Info iconThis preview shows pages 1–19. Sign up to view the full content.

View Full Document Right Arrow Icon
Groundwater P = Q + ET + G + S
Background image of page 1

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Floridan Aquifer Extent
Background image of page 2
Geologic Profiles (Stratigraphy )
Background image of page 3

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Confinement
Background image of page 4
Groundwater and Wetlands
Background image of page 5

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Transmissivit y How much water can be moved horizontally Function of thickness and Ksat Good measure of well productivity Floridan is the most transmissive aquifer in the world
Background image of page 6
Loss of Potential
Background image of page 7

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Background image of page 8
Background image of page 9

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Background image of page 10
Potentiometric Surface Elevation of “free water surface” Where this surface and the ground intersect (and there’s no confinement) water seeps
Background image of page 11

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Background image of page 12
Background image of page 13

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Relevant Questions Where is the water going? Potentiometric (piezometric) surface How much water is moving? How quickly? Potentiometric surface and Darcys Law What level of natural assimilation is occuring? Water quality modeling
Background image of page 14
Gainesville’s Well Field Also Lake City Geol ogy Land use Conserva tion Easemen t
Background image of page 15

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Murphree Wellfield Cone of Depression 1988 (Observed) 2010 (Predicted)
Background image of page 16
How to make a sinkhole Pray for lots o Rain Suck a lot of water
Background image of page 17

Info iconThis preview has intentionally blurred sections. Sign up to view the full version.

View Full DocumentRight Arrow Icon
Drilling and pumping Developed into a hole 300ft deep and 300ft wide Hundreds of sinkholes developed over a period of 6 hours.
Background image of page 18
Image of page 19
This is the end of the preview. Sign up to access the rest of the document.

Page1 / 33

Lecture6 - Groundwater P = Q + ET + G + S Floridan Aquifer...

This preview shows document pages 1 - 19. Sign up to view the full document.

View Full Document Right Arrow Icon
Ask a homework question - tutors are online