1. Groundwater

2. Groundwater
Water underground is not in underground lakes and rivers but stored in pore and fractures

3. Source of groundwater is infiltration of rain or surface water

4. Water table
Is the top of the zone of saturation where the water pressure is equal to atmospheric.
Because of this equal pressure if a hole Is dug water will flow freely into that hole up to the top of the water table.
water at the water table will flow freely into a well up to the height of the water table.

5. Below the water table all pore spaces are filled with water Saturated
Zone
© 2005 Pearson Prentice Hall

6. Unsaturated zone
Above the water table, water in the unsaturated zone is under negative pressure (less than atmospheric)
Water in this zone will not flow freely into a well.
This zone can contain air

7. Above the water table water does not fill most of the pore spaces
Unsaturated
Zone
Above the water table water does not fill
most of the pore spaces
Saturated
Zone
© 2005 Pearson Prentice Hall

8. Water Table Unsaturated Zone Saturated Zone Soil-water Zone
Capillary fringe
Saturated
Zone
© 2005 Pearson Prentice Hall

9. Water table changes seasonally and daily
Dry Period
Wet Period

10. Level of water in lakes and rivers is often the level of the surrounding water table

11. Unconfined aquifer Water table Confined aquifer Potentiometric surface
1207
Confined aquifer
Potentiometric surface

12. Groundwater Recharge Confined aquifer –
Recharge only at the limited outcrop area
Unconfined aquifer –recharge everywhere the aquifer occurs

13. Gravity controls groundwater flow.
Groundwater flows from high head to low head.

14. Flow can be complex.

15. What is a water well?
Hole drilled and lined with PVC or stainless steel pipe.
Bottom 1 to 2 feet of the pipe is slotted for the water to flow in.

16. Hydraulic Head (h) The level that water rises in a well.
In an unconfined aquifer it is the elevation of the water table.

17. Mapping an aquifer Elevations of the Water Table (head) at each well
Map of Water Table Surface – from contours of water level elevation (head)
© 2005 Pearson Prentice Hall

18. Direction of groundwater flow
is perpendicular to the head (groundwater elevation) contours
© 2005 Pearson Prentice Hall

19. Velocity of Groundwater Flow
Average linear groundwater velocity
vx = K (dh/dl) q

20. Velocity of Groundwater Flow
Average linear groundwater velocity
vx = K (dh/dl) q
K = hydraulic conductivity
q = porosity
dh/dl = hydraulic gradient- change in head with distance. Calculated from the hydrologic map.

21. The greater the hydraulic gradient (dh/dl) the faster the groundwater velocity.
Slow
Fast

22. Confining
layers

23. How long does it take a contaminant to travel.
Travel time T = vx L
vx = average linear velocity (previous slide)
L = distance of flow path

24. Importance of Groundwater
Nearly 50% of the population of the US uses groundwater for its drinking water supply.
30 % of stream flow in the US is derived from groundwater discharging to the stream.
Many aquifers are being mined
(that is withdrawal is greater than natural recharge)
Reduced rainfall from global warming is predicted to increase the need for groundwater.

25. Groundwater Pollution
Any degradation of water quality as measured by biological, chemical or physical criteria
with respect to health or ecology
A pollutant is any substance in which an identifiable excess is known to be harmful to a desirable living organisms.

26. Examples of Groundwater pollutants

27. LNAPL (Light Non-Aqueous Phase Liquid)
Non-aqueous phase is organic liquid instead of water.
Common LNAPL – gasoline
LNAPL floats on water at the top of the water table
Smears across the zone of water table fluctuation.

28. LUST (Leaky Underground Storage Tanks) usually LNAPL – gasoline or other fuel

29. DNAPL (Dense Non-Aqueous Phase Liquid)
Sinks in water to the bottom of the aquifer
Common DNAPL is dry-cleaning solvents

30. Modern Municipal Landfills
Landfills are lined with clay or plastic.
A network of drains collects the leachate and pumps it to the surface for treatment.
Monitor wells installed around the landfill to monitor groundwater quality and to detect leakage.
Old landfills are serious pollution problem

31. Salt Water Intrusion Seawater Drinking water 35,000 mg/L NaCL

32. Salt water intrusion at Long Island New York

33. Road Salt

34. Septic-tank sewage disposal
Used in areas lacking sewage treatment plants for household waste
30% of households in U.S. use septic tanks.
Must remove bacteria, organic compounds and
                                                                                                             From Thurston County (Washington State) Public Health & Social Services Department web page on Inspecting Your Septic Tank.

35. How Septic tank systems work
Sewage flows to underground septic tank where solids drop to the bottom and bacteria breaks it down.
The liquid leaks into the drain field and seeps into the soil zone where it is purified by bacterial activity in the soil.
From Thurston County (Washington State) Public Health & Social Services Department web page on Inspecting Your Septic Tank.

37. Failure of septic system can occur because of
Poor soil drainage
Times of high water table
Sewage will poor onto surface and into shallow soil zone if system fails.
Can infiltrate into the groundwater and contaminate the aquifer
Contaminants released
Nutrients (nitrates/phosphates), metals, synthetic organic compounds, virus and bacteria.

38. Groundwater remediation
Many methods – these are just a few
Sediment removal and treatment
Pump and treat
Vapor extraction
Enhanced Bioremediation

39. Pump and Treat Old preferred remediation method, now seldom used.
It is slow, taking decades to centuries to remove contamination and often fails to remove all contamination
Some contaminants stick to soil and rock (they are adsorbed) and they cannot easily be removed (desorbed).
Non-Aqueous Phase Liquids NAPLs cannot be removed.
It is very costly.
From Environment Protection Agency

40. Vapor Extraction Used to remove volatile organic compounds

41. Enhanced Bioremediation
Bacteria living in the aquifer degrade toxic contaminants into less toxic compounds.
Growth of the natural bacteria is stimulated by injecting nutrients and/or carbon compounds needed by the bacteria into the aquifer.
The bacteria break down contaminants such as trichloroethylene TCE into non-toxic compounds such as carbon dioxide

42. Who owns the Groundwater?
English Rule (Absolute Ownership)
Water can be pumped at will by landowner independent of effect on other users of the aquifer
American Rule (Reasonable Use) – applied in areas were water supplies are limited
Applied in much of the western U.S.
Limits water use to what is reasonable and beneficial (hard to determine)
Argue over what is beneficial use
Is supplying water to a river more important than to crops?
Safe yield calculated and used to regulate aquifers.

43. Texas groundwater law “Law of the biggest pump”
Based on the English rule - a landowner has a right to take for use or sale all the water that he can capture from below his land
Once pumped, groundwater may be used or sold as private property
Creation of groundwater conservation districts is the only way to limit use.

44.                                                      
(Texas Groundwater Use,

45. Well head protection of aquifer recharge zones

46. Federal regulations protecting groundwater quality

47. Federal “Superfund” legislation
The Comprehensive Environmental Response, Compensation, and Liability Act (CERCLA), 1980, commonly known as Superfund,
This law created a tax on the chemical and petroleum industries to be used to clean up releases of hazardous substances that may endanger public health or the environment.

48. Superfund National Priorities List Sites

49. RCRA Resource Conservation and Recovery Act.
It controls all solid waste disposal and encourages recycling and alternative energy sources.

50. New American Recovery and Reinvestment Act of 2009
$600 million to EPA to clean up land contaminated by hazardous wastes.
Part of Federal stimulus funding program to create jobs.