Groundwater Flashcards

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1
Q

what is ground water

A

water that infiltrates into the ground

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2
Q

how is water available to us?

A

Most fresh water on Earth tied up in glacial water

Most fresh water comes from groundwater aquifers
- Underground layers of permeable soil, sediment or rock that host extractable groundwater

Most fresh water used for irrigation (in agriculture), less for residential use

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3
Q

what is the zone of aeration

A

pores contain water + air

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4
Q

what is the of saturation

A

pores contain water only

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5
Q

where is the water table located?

A

top of zone of saturation

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6
Q

where does groundwater occur?

A

in the zone of saturation (below water table)

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7
Q

storage capacity of an aquifer is controlled by what?

A

by porosity (spaces in material)

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8
Q

what is the ability to flow

A

permeability (interconnectedness of pores)

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9
Q

what is a runoff of water

A

runoff occurs when there is more water than land can absorb

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10
Q

What is the groundwater relationship with surface water

A

Addition to water from runoff, streams can also receive water from groundwater sources

This is why river level can remain high long after an event of heavy rainfall (takes time for groundwater to reach the river)

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11
Q

what is the flow behaviour of groundwater

A

Water flows very slowly downslope in generally predictable pattern (provided that the characteristics of the material is fairly uniform)

Water table contours represent line of equal elevation above sea level

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12
Q

what are the two main types of aquifers

A

Unconfined aquifer
Confined aquifer

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13
Q

what is a unconfined aquifer?

A

an aquifer that receives water directly from the land surface above

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14
Q

what is a confined aquifer

A

an aquifer that is overlain by a layer of relatively impermeable material (commonly clay or clay-rich rock) that limits groundwater movement in or out the aquifer

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15
Q

what is an aquitard

A

An impermeable unit of material

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16
Q

what are the important feature of aquifer

A

Flow direction

Recharge area

Aquifers (confined, unconfined)

Aquitards

Perched water table

Additional features:

Influent stream (loses water to groundwater system)

Effluent stream (gains water from groundwater system)

The buildup of water over a local aquitard produces a spring

17
Q

What type of system “pumps themselves” and why?

A

Artesian Systems

Artesian systems “pump” themselves” due to water table in recharge area being at a higher elevation than land surface above a well in confined aquifer in a lower-lying area (creates “hydraulic head”)

18
Q

what is a artesian system

A

The higher the water level, the higher the water pressure

The downward “push” of the water (hydraulic head) helps the delivery of water through pipes to homes

19
Q

What are the groundwater consequences when water exceeds recharge

A

Local drawdown of water table

Formation of cone of depression

Cone of depression expands laterally as more water is withdrawn

20
Q

what is consequences of water overdraft

A

Agricultural demand (irrigation)

Output&raquo_space; input

Regional drawdown of water table

Shrinking water supplies

Consequences:

Compaction

Permanent lowering of permeability

Subsidence (sinking of land)

21
Q

What are the consequences of withdrawal of groundwater

A

Increased flood hazards, more runoff due to decreased permeability, greater concentration of pollutants in wetlands

In coastal areas, excessive groundwater withdrawal (from freshwater lens) can lead to an inflow of salt water (from the sea)

22
Q

what is a septic tank sewage disposal

A

Contaminated water slowly infiltrates into soil, organic contaminants naturally broken down by bacteria in soil

Under normal conditions, “beneficial” bacteria naturally occurring in the soil dominate over potentially harmful bacterial strains

23
Q

what are the effects on permeability on groundwater flow?

A

Contaminated water may be “purified” by beneficial microbes as the groundwater is flowing relatively slowly through moderately permeable sandstone

Highly permeable limestone (w/ large holes dissolved in the rock) allows groundwater to move too quickly to allow beneficial microbes to “purify” the water of contaminants

24
Q

How do we avoid polluting drinking water sources?

A

We can predict effects of water table drawdown + the migration of the septic plume
- Excessive pumping can alter direction of groundwater flow

Groundwater moves through high permeability materials faster than less permeable materials
- Less time for microbes to filter out contaminants

25
Q

what is Karst

A

Dissolution of carbonate sedimentary rocks by groundwater produces a distinctive type of land topography called karst

Characterized by underground drainage systems (dissolved by groundwater) with caves/caverns + sinkholes (produced when caves collapse)

26
Q

when do sinkholes form

A

Form when the “roofs” of caves collapse

Collapse events often spectacular

Common in temperate to tropical regions underlain by carbonate rocks