Chapter 4 Flashcards

1
Q

What is groundwater?

A

The water found within the pore space of geological materials

  • groundwater does not always follow land surface topography
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2
Q

What is overland flow runoff generation?

A

caused by either infiltration excess or saturation excess

  • when rate of precipitation is greater than infiltration capacity
  • infiltration capacity is determined by soil porperties
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3
Q

What is interflow runoff generation?

A

lateral movement of water in the unsaturated zone, entering streams without having occurred as overland flow

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4
Q

What is groundwater runoff generation?

A
  • in the saturated zone
  • some groundwater flow paths respond to individual rainstorms, while others only respond to climatic changes over the years.
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5
Q

What are gaining rivers and losing rivers?

A
  • gaining rivers receive groundwater discharge from the watershed
  • losing rivers recharge groundwater, since the groundwater table is below the river
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6
Q

What is the vadose zone?

A

Also known as the unsaturated zone

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7
Q

Where can we find groundwater?

A

in soils, rocks, and unconsolidated deposits

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8
Q

What is the difference between macro and micro porosity?

A
  • macropores grain freely by gravity and allow easy movement of air and water.
  • micropores have diameters less than 0.08mm, and suction is required to remove water from micropores.
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9
Q

What is the formula for porosity?

A

porosity = V voids / V total

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10
Q

What is the formula for micro and macro porosity?

A

V pores = V micropores + V macropores

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11
Q

What is permiability?

A

ability to move through a medium (soil/rock)

high porosity does not equal high permeability

clay has high porosity, but low permeability

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12
Q

What are alluvial and aeolian deposits good for?

A

groundwater storage!

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13
Q

What is recharge and discharge?

A

The two ways groundwater can move

  • recharge = percolation: downward migration of water in vadose zone
  • discharge is when groundwater emerges into springs, wetlands, rivers, lakes, oceans
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14
Q

What is an aquifer?

A
  • consists of layers or units of sands, gravels and rocks that contain sufficient saturated and permeable geologic material to yield a useable, sustainable amount of potable groundwater.
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15
Q

What are the two classifications of aquifers?

A
  • consolidated rock - sandstones, limestones, etc. Materials that do not allow groundwater to easily move through.
  • unconsolidated rock - granular materials such as sand and gravel. Generally yields larger amounts of groundwater.
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16
Q

What are aquitards and aquicludes?

A

Confining layers

  • are geological formations that have low permeability and restrict the flow of water.
  • can act as barriers that prevent the movement of water between aquifers or between groundwater and surface water.
17
Q

What is the hydraulic head?

A

The height of water in a column that can be supported by water pressure at a point of measurement.

18
Q

What is hydraulic gradient?

A

The difference in hydrological head over distance

19
Q

What is a piezometer (or pore measure meter)?

A
  • pressure transducers that are installed beneath the ground to measure the sub-surface piezometric level within groundwater level, soil, or rock.
  • they are used to study the effect of water in the pores of soil or rock is to reduce load bearing capacity of soil or rock.