Water as a Resource Flashcards

1
Q

NASA’s motto in the hunt for extraterrestrial life: “follow the water”

A
  • Perfect solvent

- Water flows -> provides a way to transfer substances between cells and environment

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2
Q

Where is the water?

A

Total water on Earth = 100%

  • Oceans and salt lakes: 97.41%
  • Ice and snow: 1.984%
  • Groundwater: 0.592%
  • Lakes and rivers: 0.0071%
  • Soils, wetlands, and biota: 0.0059%
  • Atmospheric water: 0.001%

Lots of water BUT only a tiny fraction by volume of the world’s water supply is available for human use

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3
Q

Storage of Freshwater (2.5% of total)

A
  • Ice caps and glaciers: 68.6% (not readily available)
  • Groundwater: 30%
  • Rivers and lakes: 1.4%
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4
Q

Freshwater is not distributed equally on the surface, resulting in:

A

deserts, rainforests, and glaciers…

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5
Q

Lakes hold less than 0.4% of the world’s freshwater

A
  • 80% of the water stored in lakes worldwide is held in <40 large lakes.
  • They are only important as local sources of water
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6
Q

Rivers hold about 1% of the world’s freshwater

A

Rivers supply abundant water to cities:

  • Hydroelectric power generation
  • Household use
  • Industrial use
  • Agriculture
  • Etc.
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7
Q

In Canada, most of our water use is for:

A

power generation and industrial purposes

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8
Q

Of the 38 billion m3 of water withdrawn in 2013, ~90% was returned to the

A

rivers and lakes of origin, 3.6billion m3 were consumed (consumed water cannot be used again immediately)

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9
Q

Power generation uses ~27bil m3 of water;

A

2% is consumed

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10
Q

Agriculture uses ~2bil m3 of water; 80-90% is consumed

A

Worldwide, agriculture extracts >6.4 trillion litres of water per day (82% for irrigation)

  • This is suspected to increase to 56.4 trillion litres of water per day by 2050, BEYOND dependable flow of the world’s rivers
  • Water availability is expected to limit pop growth in the 21st century
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11
Q

In many areas, consumption exceeds local surface water supplies, so water must be imported or mined.

A
  • It is estimated that 3000x more water is stored as groundwater in the upper 800m of the continental crust than water found in all the world’s rivers and streams
  • About 30% of the population of Canada depends on groundwater
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12
Q

Hydrogeologists

A

Groundwater geologists that specialize in distribution, circulation, and contamination of groundwater

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13
Q

Misconception is that groundwater exists in vast, underground rivers and lakes

A

This is generally not true, except in karsted carbonate rocks

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14
Q

Where is groundwater stored and how does it move?

A

Most groundwater is stored in pore spaces and fractures in rocks

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15
Q

Outcrops

A

Areas of exposed rock that provide a glimpse of subsurface conditions that we can’t see otherwise. Fractures and pore spaces can be microscopic to macroscopic

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16
Q

Porosity

A

Volume of empty space/total volume of rock (expressed as percent or fraction of 1)

  • Shales can have higher porosity than sandstones, but the pore size is very small
  • Primary porosity in limestones and other crystalline rocks may be very low, but secondary porosity (e.g vugs or fractures) may be high
17
Q

Permeability

A

A measure of the ability of a rock or sediment to transmit fluid. Related to the size and interconnectedness of pores or fractures

18
Q

The permeability of a medium is related to the porosity, but also to

A

the shapes of the pores in the medium and their level of connectedness.

High porosity, from high to low permeability: gravel, sand, silt, clay

19
Q

High permeability allows for lots of drainage, whereas low permeability

A

minimizes drainage

20
Q

Water that doesn’t run off enters porous rock through:

A

Infiltration.

- Fractured and porous rocks can store water

21
Q

If these rocks are permeable, they can also transmit water.

A
  • Infiltrating water tends to percolate downwards (gravity)
  • The pores fill with water until it is saturated
  • The top of the saturated zone is called the water table
  • Above the water table in the unsaturated zone, pores may contain a mix of water and air
22
Q

The shape of the water table mimics topography, but is subdued

A

The water table can move up and down with precipitation/drought withdrawal

23
Q

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

A

In others, streams contribute to the groundwater

- If an area is dry, the water table may be far below the stream (disconnected losing stream)

24
Q

Types of Streams

A
Gaining stream: base of stream is in the water table and gains base flow of water
Losing stream (connected): base of stream touches the water table but loses base flow
Losing stream (disconnected): base of stream does not touch the water table, losing base flow to ground and infiltrates down to water water
25
Q

Wetlands often occur where

A

The water table intersects the land surface

26
Q

Springs generally form where

A

The water table intersects a slope

27
Q

Aquifer

A

Saturated rock that contains and transmits “significant” quantities of water
- Depends on usage

28
Q

Unconfined aquifer

A

Recharged by water seeping directly from the ground above

- The level of the water can change over time

29
Q

Confined aquifer

A

Fully saturated and bound by ~impermeable layers above and below the aquifer

30
Q

How does water get into confined aquifers?

A

Recharge from other places

31
Q

What are some groundwater issues we are facing?

A

Contamination:
Acid mine drainage:
- acidic solution gets into surface water: harms terrestrial, vegetation, and aquatic systems, and weathering increases.
- Acidic solution gets into groundwater: difficult to recharge or fix once contaminated