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CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as...

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CHAPTER 20: GROUNDWATER
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Page 1: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

CHAPTER 20:GROUNDWATER

Page 2: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater

• It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental crust than the water found in all the world’s rivers and streams. (United States Geological Survey )

Page 3: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater

• Groundwater is our most important source of fresh water.

• About 30% of the population of Canada depends on groundwater.

Page 4: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater is present where the material of the crust has pores or fractures

Page 5: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

There Are Several Types of Earthquake Hazards

What’s the term used to describe the boundary zone between the unsaturated and saturated zones?

Page 6: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

The Water Table rises and falls with the seasons

Page 7: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Most water wells are drilled with truck-mounted drill rigs

Page 8: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater is fed by snowmelt and rainfallin recharge areas

Page 9: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Streams

• In some situations groundwater contributes to the base flow of a stream. In others, streams contribute to the groundwater.

What is the difference between a connected losing stream and a disconnected one?

Page 10: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Wetlands

• Wetlands are critically important for storage of both surface and groundwater

Page 11: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Hydraulic Pressure

• Groundwater moves in response to gravity and hydraulic pressure

Page 12: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Aquifer

• An aquifer is body of rock or unconsolidated sediment through which groundwater can flow

Why should deep groundwater take many times longer to reach the discharge area than shallow groundwater?

Page 13: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Permeability and porosity

Of the following pairs of situations, which should have the greater permeability and why: (a) versus (b), (a) versus (c), (a) versus (d), (e) versus (f)?

Page 14: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Hydraulic Gradient

• In this situation the hydraulic gradient is the slope of the water table.

Page 15: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Darcy’s Law

Page 16: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Porous Materials and Fractured Rocks Hold Groundwater

Porous Materials

Fractured Rocks

Page 17: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Aquifer Terminology

What is the difference between the water table and the potentiometric surface?

Page 18: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater is vulnerable to many different sources of pollution

Groundwater Animation

Page 19: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Hard Water

• Groundwater contains a wide range of dissolved ions, most at levels that are higher than in surface water.

• Water with high levels of calcium or magnesium is known as hard water and often leaves coatings of white mineral precipitates on plumbing fixtures.

Apart from Ca and Mg, what are some common dissolved ions in groundwater?

Page 20: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Saltwater Intrusion

What can people living near to the coast do to reduce the likelihood of saltwater intrusion?

Page 21: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

An improperly functioning septic field can be a source of groundwater contamination.

Page 22: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Contaminant plumes

• Common human activities contaminate groundwater

Page 23: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Salt Contamination

• It is common to combat icy conditions by spreading salt on roads and highways.

• This results in salty runoff that percolates into the unsaturated zone.

Page 24: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Landfills, pesticides and undergroundfuel storage tanks

Page 25: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

It is estimated that there are >10 million underground storage tanks buried in the United States and that 70%

of them leak.

Page 26: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Monitoring wells

How many abandoned gas stations—surrounded by chain-link fencing—can you find in your region?

Page 27: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Are there examples of some of these types of contamination in your region?

Page 28: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater contamination in Canada’s far north

Who is responsible for cleaning up contamination at DEW-line sites like Cape Dyer?

Page 29: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater remediation includes several types of treatments

• Air sparging• Extraction wells• Recirculation wells• Aquifer fracturing• Injection wells

Page 30: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Groundwater remediation includes several types of treatments

• Permeable reactive barriers• Bioremediation• Phytoremediation• Thermal or electrical treatments

Page 31: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Hydrological Regions of Canada

From: Natural Resources Canada. 2007. Groundwater Mapping Program. Hydrogeological Regions.

Page 32: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Springs exist where groundwater naturally comes to surface.

Page 33: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Spring water has deposited tufa (calcium carbonate) over this outcrop at Johnston Canyon in the Alberta Rockies

Page 34: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Karst topography is also a product of groundwater

What type of rock is found in karst regions, and what

property of that rock facilitates the development of karst?

Page 35: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

As is hydrothermal activity.

Geyser Fumarole Hot Spring

Page 36: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

Speleothems

Page 37: CHAPTER 20: GROUNDWATER. Groundwater It is estimated that there is 3000 times more water stored as groundwater in the upper 800 meters of continental.

COPYRIGHT

Copyright © 2014 John Wiley & Sons Canada, Ltd. All rights reserved. Reproduction or translation of this work beyond that permitted by Access Copyright (The Canadian Copyright Licensing Agency) is unlawful. Requests for further information should be addressed to the Permissions Department, John Wiley & Sons Canada, Ltd. The purchaser may make back-up copies for his or her own use only and not for distribution or resale. The author and the publisher assume no responsibility for errors, omissions, or damages caused by the use of these programs or from the use of the information contained herein.


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