groundwater - exam 2 Flashcards

1
Q

what is the most major reservoir of liquid freshwater readily available to humans?

A

groundwater

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2
Q

the dissolving action of groundwater slowly removes soluble rock such as limestone, creating?

A

surface depressions known as sinkholes and subterranean caverns

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3
Q

what is groundwater most used for compared to all other uses combined?

A

irrigation

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4
Q

the upper limit of the zone of saturation is called?

A

the water table

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5
Q

the water table is highly

A

invariable

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6
Q

an important characteristic of the configuration of what varies seasonally and yearly because ether addition of water to the groundwater system is closely related to the quantity, distribution, and timing of precipitation?

A

the water table

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7
Q

the elevation of the water table is mapped and studied in detail by examining?

A

water levels in wells

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8
Q

a stream that gains water from the inflow of groundwater through the steambed?

A

a gaining stream

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9
Q

a stream that loses water to the groundwater system by outflow through the steambed

A

a losing stream

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10
Q

for a losing stream to occur, the water table must sit

A

lower than the surface of the stream

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11
Q

for a gaining stream to occur, the elevation of the water table must be

A

higher than the level of the surface of the stream

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12
Q

the quantity of groundwater that can be stored depends on the ____ of a material

A

porosity

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13
Q

the two factors that strongly influence the rate of groundwater movement and the amount of groundwater that can be stored

A

porosity and permeability

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14
Q

pores must be connected and large enough in a rock to

A

allow water to flow through it

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15
Q

permeability is

A

a materials ability for a liquid to penetrate and transmit through it

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16
Q

the smaller the pores/ porosity of a rock, what is the pace in which the water moves?

A

water is moved slowly

17
Q

the ability of a clay deposit to store water is great because of its high porosity, but its pore spaces are so small that water is unable to move through it. we would refer to clay as

A

impermeable

18
Q

impermeable layers that prevent or hinder the movement of groundwater are referred to as

A

aquitards

19
Q

permeable rock strata or sediments that transmit groundwater freely are referred to as

A

aquifers

20
Q

common examples of aquifers

A

sand and gravels

21
Q

common examples of aquitards

A

clay

22
Q

our modern understanding of groundwater movement comes from the mid nineteenth century by the work of

A

henri darcy

23
Q

the coefficient coined by henri darcy

A

hydraulic conductivity

24
Q

subsurface geology exhibits a complicated arrangement of aquifer units with

A

high hydraulic conductivity

25
Q

subsurface geology exhibits a complicated arrangement of aquitards

A

low hydraulic conductivity

26
Q

the expression of the hydraulic gradient has come to be called

A

darcy’s law

27
Q

the hydraulic gradient is also referred to as

A

the water table slope

28
Q

an aquitard situated above the main water table forms a

A

perched water table

29
Q

this term is applied to any situation in which groundwater under pressure rises above the level of the aquifer

A

artesian

30
Q

when the surface pressure is above the ground and a well is drilled into the aquifer, what is created?

A

a flowing artesian wall

31
Q

the term for when a water table intersects earth’s surface and a natural outflow of groundwater results

A

a spring

32
Q

when groundwater circulates at great depths it can become heated. if this water then rises to the surface, it may emerge as

A

a hot spring

33
Q

intermittent hot springs or fountains in which columns of water are ejected with great force at various intervals

A

geysers

34
Q

the most spectacular results of groundwater intrusion

A

limestone caverns