Page1 / 8

Lecture_27_Groundwater_Notes - Groundwater Lecture Notes...

This preview shows document pages 1 - 4. Sign up to view the full document.

View Full Document Right Arrow Icon
Lecture_27_Groundwater_Notes

Lecture_27_Groundwater_Notes - Groundwater Lecture Notes...

Info iconThis preview shows pages 1–4. Sign up to view the full content.

View Full Document Right Arrow Icon
1 Groundwater Lecture Notes What is Groundwater? Groundwater is water that: lies beneath the earth’s surface occupies the space between grains in sediments and sedimentary rocks fills fractures and voids in igneous, sedimentary, and metamorphic rocks Porosity = a measurement of a rock’s or sediment’s ability to store water Permeability = a measure of a rock’s or sediment’s ability to transmit water The Water Table There are 3 major “zones” that describe the distribution of water in the earth’s subsurface (see Fig. 11.1) Vadose Zone: unsaturated, relatively dry material Capillary Fringe: moist (but not saturated) material in between the vadose zone and the saturated zone Saturated Zone: saturated material in which all pores/ fractures are filled with water The top of the saturated zone is called the “Water Table”. A “Perched Water Table” occurs where saturated materials are separated from the main water table by an unsaturated zone (Fig. 11.2) The Movement of Groundwater Most groundwate moves relatively slowly through earth materials Clay rich soils cm-m/yr Sandy soils 10’s-100s m/yr Rock Fractures up to km/day In porous media (e.g. soils), groundwater moves down the slope of the water table Hydraulic Head Hydraulic head = elevation of water + pressure on water Hydraulic Gradient Hydraulic Gradient = change in head from a to b / distance from a to b. HG = head / distance = h/L
Background image of page 1

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

View Full DocumentRight Arrow Icon
2 Rules of Groundwater Flow Groundwater flows from regions of high head to regions of low head Groundwater flows from regions of high fluid potential to regions of low fluid potential Water table Water table A B L h
Background image of page 2
3 Groundwater Flow Velocity Flow velocity depends on: Hydraulic gradient ( h / L) Permeability (K) Porosity (n) Velocity = (K / n)( h / L) This equation essentially shows that groundwater will flow faster where the
Background image of page 3

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

View Full DocumentRight Arrow Icon
Image of page 4
This is the end of the preview. Sign up to access the rest of the document.
Ask a homework question - tutors are online