Lec 13: Soil water & groundwater III Flashcards

1
Q

What are the 2 regimes of subsurface flow?

A

unsaturated flow (soil water flow)
saturated flow (groundwater flow)

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2
Q

What is saturated flow?

How does its flow velocity compare to that of rivers?

What does its flow velocity depend on?

A

Movement of water through saturated
pores and fractures

Relatively slow (cms to meters/day)
compared to flow of water in rivers

Flow velocity depends upon:
* Slope of the water table
* Permeability of the rock or sediment
in aquifers

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3
Q

Define aquifer

A

A permeable geologic unit that can transmit a significant amount of
water under an ordinary gradient

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4
Q

Define aquiclude

A

A geologic unit which does not transmit a significant quantity of water under
ordinary gradients
Aquiclude = confining bed = confining layer

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5
Q

What determines the type of aquifer?

What are some common types of aquifers?

A

The presence or absence of aquicludes determines the type of aquifer

The most common aquifer types are:
– Unconfined aquifers
– Confined aquifers
– Perched aquifers

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6
Q

Define unconfined water

A

… ground water in an aquifer with a lower barrier to movement caused by the
presence of an aquiclude below; however, there is no upper barrier, which allows
water to fluctuate over distances upwards

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7
Q

When does perched groundwater occur?

A

… occurs when an unconfined water zone sits on top of a clay lens or another quasiimpermeable lens, which separates it from the main aquifer below.

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7
Q

Define confined water

A

… ground water in an aquifer with a lower and upper barrier to movement, as there
is an aquiclude located immediately above and one located immediately below
the aquifer

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8
Q

What is hydraulic conductivity

A

measure of the ease with which water can move through
pore spaces or fractures in aquifers

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9
Q

Define groundwater recharge and discharge

A

Groundwater recharge is any water added to an aquifer, notably through
infiltration and percolation

  • Groundwater discharge is any process that removes water from an aquifer
    system (e.g., natural springs, artificial wells).
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10
Q

The presence and magnitude of subsurface water flow (saturated and unsaturated)
is largely determined by…

A

differences in subsurface water energy

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11
Q

What is hydraulic head a measure of?

what are the two forms of it?

Hydraulic head it sum of …

A

groundwater energy

  • Elevation head (z): Height above a datum
  • Pressure head (hP or ψ): height of water which would create a certain pressure

hydraulic head is total head, it is the sum of elevation and pressure head

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12
Q

What is hydraulic gradient (I)?

Is it negative or positive?

A

Hydraulic gradient: groundwater energy difference between two locations

It is the change in total head over a given distance

Negative, because it is defined from low to high hydraulic head. Groundwater flows in direction of decreasing hydraulic head (from higher to lower hydraulic head)

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13
Q

What does Darcy’s law state?

What is the constant of proportionality that is used?

A

States that the flux of water through a permeable medium is proportional to
pressure differences or energy differences within that medium.

The constant of proportionality that is used is the hydraulic conductivity (K)

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14
Q

What does Darcy velocity describe?

What is the problem with Darcy velocity?

A

The Darcy velocity attempts to describe the average behavior of all water
molecules, in macroscopic terms that are easily measured

Darcy velocity assumes that flow occurs across the entire cross-section,
whereas flow occurs only through interconnected pore channels

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15
Q

How is linear velocity different from darcy velosity?

A

Linear velocity takes into account the tortuous path of water molecules, via an effective porosity value