Lab 6 Flashcards

(19 cards)

1
Q

What is groundwater

A

Groundwater is water found filling pore spaces beneath the earth’s surface in a zone called the zone of saturation

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2
Q

what is the difference between the zone of saturation and unsaturated zone

A

the zone of saturation has all the pore space filled with water. The unsaturated Zone has some combination of water and air, or only air

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3
Q

What can make up the zone of saturation

A

the zone of saturation may be loose soil and debris, or may be rock that has some pore space to it (that is open spaces)

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4
Q

What is the porosity

A

the ratio of open spaces to solid material is called porosity, expressed as a percentage

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5
Q

What is Permeability

A

If the pores are not connected, the water cannot move and so the material would be considered impermeable. The better the spaces connect, the more easily the water can move through the material, and this can be measured and is called permeability.

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6
Q

What is an aquifer

A

an Aquifer is a body of rock or sediments that is capable of both storing (porosity) and transmitting (permeability) water

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7
Q

What is an unconfined aquifer

A

an aquifer that has no confining layer between it and the land surface

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8
Q

what is the water table

A

the top of the zone of saturation in an unconfined aquifer

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9
Q

What is a confined aquifer

A

a confined aquifer is an aquifer that is blocked from the surface by an impermeable layer. Can develop higher pressures than is found in the groundwater above them.

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10
Q

What is the potentiometric surface

A

The theoretical water table for an unconfined aquifer. The imaginary level the water would rise to if it could due to higher pressure in unconfined aquifers

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11
Q

What is an artesian aquifer

A

A confined aquifer is sometimes called an artesian aquifer because if it contains enough pressure that a well drilled into it will send water above ground level, it creates an artesian well, a well that flows under its own pressure (no pumping required)

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12
Q

What is a piezometer

A

a well drilled to simply determine the level of the groundwater, without pumping or injecting water.

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13
Q

How can we draw the water table

A

By connecting water levels in piezometers and other known points of a water table (river, lake, non-pumping well)

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14
Q

What is a potential gradient or hydraulic gradient

A

Often the water table is not flat, because water is being added to a system in one area and removed from another area. the inclined surface is called the potential gradient or hydraulic gradient. Can allow us to determine the direction of flow in a system

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15
Q

What is a hydraulic head

A

Measuring the difference in elevation of the water table in different locations can give us the difference in water pressure between these locations which is called the hydraulic head. It is effectively how hard the water is being “pushed” by gravity from high areas to low areas.

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16
Q

How can we determine the rate at which water in an aquifer should flow

A

By combining the hydraulic head with the conductivity of the aquifer (conductivity is largely based on permeability)

17
Q

What is a cone of depression

A

When we pump from a water well faster than the water can be replenished, the water. level in the surrounding aquifer drops more and more as you approach the well, causing what is called a cone of depression

18
Q

How do plant leaves and twigs become diamond

A

Energy derived from sunlight is used to fix carbon, nitrogen, and other nutrients to form organic matter (plants and twigs) by photosynthesis
Burial of plant and other organic matter in stagnant or low-oxygen aquatic environments forms peat
Continued compaction and heat of burial drive off most of the volatile elements and water, leaving a compact material (coal) that is high in carbon
Further metamorphisms recrystallizes the carbon into the mineral graphite
Extremely high pressures found only in the earth’s mantle change the carbon atoms again into an even more stable crystalline form, diamond

19
Q

What minerals might be added to a shale in order of metamorphic grade

A

Chlorite, Muscovite Mica, Biotite Mica, Garnet, Staurolite, Sillimanite.
Quartz and Feldspars are present throughout metamorphism