Groundwater Flashcards

1
Q

Estimated that there is 3000x more water stored as groundwater in the upper 800m of

A

the continental crust than water found in ALL the rivers and streams

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2
Q

Groundwater is our most important:

A

source of freshwater

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3
Q

About 30% of the Canadian pop depends on:

A

groundwater

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4
Q

Groundwater is present where:

A

the crust has pores (like sand) or fractures (breaks in rocks)

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5
Q

What is the water table?

A

The level below which the ground is saturated with water, fills all pore spaces, fluctuates with flooding, etc.

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6
Q

What is the capillary fringe?

A

the boundary zone b/w unsaturated and saturated zones

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7
Q

Water Table rises and falls with:

A

The seasons, and is not flat. Has muted topography.

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8
Q

Porosity

A
  • Pores are open spaces within any sediment or rock
  • The total volume of open space is term porosity
  • Geologic materials exhibit a wide range of porosities (i.e crystal size)
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9
Q

Two categories of porosity:

A

primary and secondary

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10
Q

Primary porosity

A

originally formed with the material, ie voids in sediment, vesicles in basalt

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11
Q

Secondary porosity

A

develops later = fracturing, faulting, dissolution

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12
Q

Permeability

A
  • The ease of water flow due to pore interconnectedness
  • Highly permeable material allows water to flow readily
  • Water cannot flow through impermeable material
  • Many large and straight flow paths enhance permeability
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13
Q

Aquifer

A

a body of rock or unconsolidated sediment through which groundwater can flow, transmits water easily

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14
Q

Aquitard

A

impermeable or low permeability sediment or rock that hinders water flow

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15
Q

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

A

Travels longer distance, works its way far down and recharging is slower rate

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16
Q

Unconfined vs Confined Aquifers

A
  • Unconfined: an aquifer that intersects the surface, in contact with the atmosphere, easily contaminated
  • Confined: an aquifer beneath an aquitard, isolated from the surface, less susceptible to pollution
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17
Q

Hydraulic Gradient

A
  • Hydraulic gradient is the slope of the water table
    = (h1 - h2)/L
  • basically rise over run for water table
  • Steeper slope means faster water table flows
18
Q

Darcy’s Law

A

V = K(dh/dL) or K(h1-h2)/L
V is groundwater flow velocity
K is the coefficient of permeability
(h1-h2)/L or (dh/dL) = hydraulic gradient

19
Q

Most water wells are drilled with

A

truck-mounted drill rigs

20
Q

Groundwater is fed by

A

snowmelt and rainfall in recharge areas

21
Q

In some situations, groundwater contributes to the base flow of a stream. In others:

A

streams contribute to the groundwater

22
Q

Gaining stream:

A

water table is above base flow so gains water

23
Q

Losing stream (connected):

A

water table is below, but connected to stream, loses water to ground

24
Q

Losing stream (disconnected):

A

water table is super far below stream, loses water

25
Q

Groundwater can maintain a 3D surface because:

A

pore water moves super slow = topography

26
Q

Wetlands are critically important for:

A

storage of both surface and groundwater

27
Q

Groundwater moves in response to

A

gravity and hydraulic pressure (pressure from behind)

28
Q

Aquiclude

A

aquitard = impermeable layer

29
Q

Confined or artesian aquifer

A

contained between 2 aquicludes

30
Q

Potentiometric surface

A

an imaginary plane where a given reservoir of fluid will “equalize out to” if allowed to flow, based on hydraulic principles.

31
Q

Potentiometric surface vs water table:

A

the difference between the naturally occurring surface of the water in a groundwater aquifer and the surface of the water in a monitoring well in a confined aquifer.

32
Q

Groundwater is vulnerable to many different sources of

A

pollution

33
Q

Any other fluid released into the ground will

A

try to do as water does

34
Q

Groundwater contains a wide range of dissolved

A

ions, most at levels that are higher than in surface water

35
Q

Hard water

A
  • Water with high levels of calcium or magnesium
  • often leaves coatings of white precipitates on plumbing fixtures
  • related to the history of where the water has flowed in sediments
36
Q

Saltwater Intrusion

A
  • Well creates a cone of depression and used so much of freshwater so now where saltwater flows in, near the coast
37
Q

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

A

Dig well further inland, limit water use

38
Q

An improperly functioning septic tank can be a source of

A

groundwater contamination

39
Q

Springs (where the water table intersects with topography) exist where

A

groundwater naturally comes to the surface

40
Q

Karst topography

A

A landscape that is characterized by numerous caves, sinkholes, fissures, and underground streams

  • usually forms in regions of plentiful rainfall where bedrock consists of carbonate-rich rock that is easily dissolved
  • i.e hydrothermal activity like geysers, hot springs, fumaroles