CHAPTER 7 Flashcards

(31 cards)

1
Q

It is the pores of soil contain both water and air in varying amounts; the water in the upper layers of this zone is called soil moisture.

A

Zone of aeration

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2
Q

It is the pores of the soils or rock are filled with water; the water in this zone is called groundwater.

A

Zone of saturation

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3
Q

It is a geologic formation which contains water and transmits it at a rate sufficient to be economically developed for pumping.

A

Aquifer

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4
Q

It is a geologic formation containing water but transmits it at a rate insufficient to be economically developed for pumping.

A

Aquiclude

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5
Q

It has a water table serving as the upper surface of the zone of saturation.

A

Unconfined / water table aquifer

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6
Q

One where the groundwater is confined by a relatively impermeable layer.

A

Confined or artesian aquifer

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7
Q

It is the upper confining layer is leaky or semi-permeable.

A

Semi-confined or leaky aquifer

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8
Q

Its lower limit is relatively impermeable layer while its upper surface is a free water surface on water table.

A

Perched Aquifer

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9
Q

4 types of aquifer:

A
  • Unconfined / Water table aquifer
  • Confined or artesian aquifer
  • Semi-confined or leaky aquifer
  • Perched Aquifer
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10
Q

6 properties of aquifer:

A
  • Porosity
  • Specific yield
  • Specific retention
  • Aquifer conductivity or permeable
  • Transmissibility
  • Storage coefficient
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11
Q

It is the capacity of formation to contain water.

A

Porosity

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12
Q

It is the water that can be extracted by gravity flow; measure of the volume of water yield per unit soil volume.

A

Specific yield

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13
Q

It is the water retained by the soil formation against force of gravity.

A

Specific retention

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14
Q

It is the measure of the ease with which an aquifer will transmit water; influenced by both the properties of water and aquifer materials.

A

Aquifer conductivity or permeable

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15
Q

It is the measure of the potential discharge of well penetrating an aquifer, its magnitude is an indication of the economic value of an aquifer as a source of water supply.

A

Transmissibility

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16
Q

It is the water yielding capacity of confined aquifer.

A

Storage coefficient

17
Q

5 threats to groundwater:

A
  • Quantity
  • Overdraft
  • Drawdown
  • Subsidence
  • Quality
18
Q

It is an increased quantity of groundwater is being withdrawn to meet the demands of a growing population.

19
Q

Typical threats that is associated with QUANTITY.

A
  • Overdraft
  • Drawndown
  • Subsidence
20
Q

It occurs when groundwater is removed faster that recharge can replace it.

21
Q

TRUE OR FALSE:

Overdraft can result a permanent loss of a portion of its storage capacity.

22
Q

TRUE OR FALSE:

Overdraft can result a change that can cause water of unusable quality to contaminate good water.

23
Q

It differs significantly from overdraft.

24
Q

It results in a temporarily lowered water table generally caused by pumping.

25
It results from overpumping.
Subsidence
26
As the water table declines, water pressure is reduced.
Subsidence
27
This causes fine particles that help water to become compacted. In addition, to permanently reducing storage capacity, the land above the aquifer can sink from a few inches to several feet causing a sinkhole. This can damage property and fields.
Subsidence
28
It is inorganic compounds, pathogens, and organic compound can harm water quality, affecting the health of humans, fish and wildlife. Scientists continually learn more about contaminants, their sources and prevention practices.
Quality
29
2 Potential sources of contamination / pollution:
- Point sources - Non-point sources
30
It is widespread, seemingly insignificant amounts of pollutants which, cumulatively, threaten water quality and natural systems.
Point sources
31
It can easily identified because the usually come out of a pipe.
Non-point sources