Groundwater Flashcards

1
Q

This is a major source of water, major component of the hydrologic cycle, and is mostly hidden from view

A

Groundwater

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2
Q

What percent of the world’s water is groundwater?

A

0.6%

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3
Q

What percent of the world’s freshwater is groundwater?

A

12%

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4
Q

What are two sources of groundwater?

A
  1. Precipitation that infiltrates the ground; 2. Surface water that infiltrates or is connected to water table
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5
Q

How many major aquifers are in Oklahoma?

A

23

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6
Q

80% of groundwater withdrawals are for this

A

Irrigation

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7
Q

How many groundwater permits are there?

A

> 9,500

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8
Q

What are six things that influence infiltration?

A
  1. Climate; 2. Slope; 3. Soil/rock type; 4. Vegetation; 5. Land use; 6. Degree of saturation
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9
Q

This is the percentage of a material’s total volume that is pore space

A

Porosity

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10
Q

What is the equation for porosity?

A

Porosity = pore volume/total volume x 100

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11
Q

What are two ways water can get through bedrock?

A
  1. Bedrock fractures; 2. Slightly acidic water dissolves other substances
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12
Q

What are two particle qualities that affect porosity?

A

Shape and sorting

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13
Q

Porosity is highest when these are equal in size

A

Sediment clasts

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14
Q

Which has higher porosity: well-sorted or poorly-sorted sediment?

A

Well-sorted

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15
Q

What particle shape results in higher porosity: rounded or angular?

A

Rounded particles

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16
Q

Does porosity depend on particle size?

A

No

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17
Q

This is a material’s ability to allow fluids to pass through

A

Permeability

18
Q

What are three factors that affect permeability?

A
  1. Porosity; 2. Pore size; 3. Pore interconnection
19
Q

This is a permeable layer beneath the surface that transports groundwater easily

20
Q

This is an impermeable layer that prevents groundwater movement

A

Aquiclude/aquitard

21
Q

What materials are aquifers typically composed of?

A

Well-sorted and well-rounded sands and gravels

22
Q

What materials are aquicludes/aquitards typically composed of?

A

Shales and clays

23
Q

What are the two types of aquifer?

A

Confined and unconfined

24
Q

This type of aquifer is completely filled with water under pressure and is separated from the surface by an impermeable layer (aquitard)

A

Confined aquifer

25
Are confined aquifers recharged slowly or rapidly?
Slowly recharged
26
This type of aquifer has a water table and is only partly filled with water
Unconfined aquifer
27
Are unconfined aquifers recharged slowly or rapidly?
Rapidly recharged
28
Water infiltrates the ground through this sediment zone, where pore space is mostly filled with air
Zone of aeration
29
This is the boundary between the zone of aeration and saturation where water can seep upwards through capillary action
Capillary fringe
30
Water collects in this sediment zone, where all available pore space is filled with water
Zone of saturation
31
This can become dissolved in groundwater from the atmosphere to make it acidic
Carbon dioxide
32
When carbon dioxide dissolves in water, it forms this acid
Carbonic acid
33
This is a common sedimentary rock composed of calcite (CaCO3) that is easily dissolved in carbonic acid
Limestone
34
This topography forms where limestone bedrock dissolves both at the surface and in underlying cave networks
Karst topography
35
These form where groundwater seeps through pores and cracks and reaches soluble materials like limestone
Caves
36
These are surface streams that flow underground into caves
Disappearing streams
37
What are four ways groundwater has been over-exploited/contaminated?
1. Lowering the water table (cones of depression); 2. Saltwater intrusion; 3. Land subsidence; 4. Groundwater pollution
38
This occurs when groundwater use exceeds the amount of recharge in an aquifer
Groundwater overdraft
39
This occurs when overuse of wells depletes groundwater and lowers the water table in the vicinity
Cone of depression
40
This occurs mostly in coastal communities when excessive pumping draws saltwater into wells
Saltwater intrusion
41
This occurs when groundwater removal causes poorly consolidated sediments to become compacted
Land subsidence