GROUNDWATER FLOWS TO WELLS Flashcards

1
Q

maximum rate of pumpage that can be allowed while ensuring that water-level declines are kept with acceptable limits.

A

Groundwater yield

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2
Q

maximum pumping rate that can be supplied by a well without lowering the water level in the well below the pump intake

A

Well yield

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3
Q

maximum rate of withdrawal that can be sustained by an aquifer without causing an unacceptable decline in the hydraulic head in the aquifer

A

Aquifer yield

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4
Q

maximum rate of withdrawal that can be sustained by the complete hydrogeologic system in a groundwater basin without causing unacceptable declines in hydraulic head in the system or causing unacceptable changes to any other component of the hydrologic cycle in the basin.

A

Basin yield

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5
Q

is the artificial application of water to soil or land to assist in the growth of crops and vegetation, typically to supplement insufficient rainfall and ensure optimal agricultural productivity.

A

Irrigation

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6
Q

is the process of removing or lowering the water table in soil or construction areas through pumping or other techniques, typically to create a dry and stable environment for construction, mining, or excavation activities.

A

Dewatering

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7
Q

a model refers to the process of defining and assigning specific values to the parameters within a mathematical or computational model.

A

Parameterizing

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8
Q

who said that groundwater science is like trying to read a textbook with a hole punch…”

A

D. Irvine

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9
Q

K and transmissivity properties can be determined from single well tests

A

At least one pumping well…

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10
Q

To determine storage properties

A

At least one observation well

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11
Q

Better estimates of storage and transmissivity

Boundaries

Anisotropy

A

Multiple observation wells

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12
Q

-record the pump rate and know the location of the pumping
well, and observation wells

A

From the test

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13
Q

Solved transient flow (accounting for storage) to a well in an infinitely extending aquifer

A

Theis Solution

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14
Q

affects the slope of the time drawdown curve

A

Transmissivity

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15
Q

Higher transmissivity,

A

lower slope

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16
Q

Higher transmissivity requires a __________ to move the same Q

A

lower gradient

17
Q

affects the lag time for drawdown to commence

A

Storativity

18
Q

Higher storativity,

A

longer lag time

19
Q

means that more water is available in storage, which buffers drawdown (initially)

A

Higher storage

20
Q

What properties affect drawdown in an unconfined aquifer?

A

Storativity

Horizontal conductivity

Vertical conductivity

Specific yield

21
Q

three phases of unconfined drawdown

A

neuman solution

22
Q

drawdown is controlled by the specific yield of the aquifer called

A

the concept of delayed yield

23
Q

refers to the decline of water level of well due to pumping

A

draw down

24
Q

it refers to the vertical distance from the ground surface to the water level in a well, borehole, or piezometer

A

Depth to Water

25
Q

true of false: drawdown is always reported as a positive number

A

true

26
Q

is a property of an aquifer that describes its ability to transmit water

A

Hydraulic conductivity (k)

27
Q

Generally performed in piezometers

Can’t perform pump tests

Have a significant response to a small stress

A

slug test

28
Q

a confined aquifer is bounded on one side by a straight line impermeable boundary

A

bounded aquifer