Water Resources Flashcards

1
Q

The ease with which fluids pass through a rock is determined by the rock’s

A

Permeability

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2
Q

Which of the following would probably have the highest porosity?

A

Sandstone

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3
Q

Most of the water in the hydrosphere is found in

A

The oceans

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4
Q

The vadose zone is also known as the

A

Unsaturated Zone

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5
Q

The water table

A

Is the top of the zone of saturation

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6
Q

When the groundwater leaves the aquifer via escaping the surface in a spring or flowing into a stream it results in

A

Discharge

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7
Q

To be useful as a source of water, a rock must be

A

Both porous and permeable

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8
Q

Artesian conditions require

A

A confined aquifer

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9
Q

If the water were unconfined, the height to which the water’s pressure would raise the surface is called as the _______ surface

A

Potentiometric

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10
Q

Groundwater flow is best explained by

A

Darcy’s Law

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11
Q

Hard water is

A

Water containing high levels of dissolved calcium and magnesium

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12
Q

Limitations on the use of surface water as a water source include

A

All choices correct- Look up

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13
Q

The largest reservoir of unfrozen freshwater is

A

Groundwater

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14
Q

Around an actively pumped well in an unconfined aquifer, a ____________ may develop in the water table

A

Cone of Depression

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15
Q

Possible consequences of excessive groundwater withdrawal include

A

Surface Subsidence

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16
Q

Recharge of groundwater

A

Varies according to the geology and climate of the region and so groundwater may have been underground a few years (Karst regions) to 10,000 years or more (southwestern USA).

17
Q

Most of the water consumed in the United States is consumed by

A

Agricultural Activities

18
Q

A problem associated with aquifers in coastal regions is

A

Saltwater Intrusion

19
Q

The quality of water can be measured using which of the following ways:

A

All- look up

20
Q

Along its length, the Colorado River

A

Is greatly reduced in volume by heavy use and evaporation loss from reservoirs

21
Q

What is groundwater?

A

Typically not “underground lakes and streams” but occurs in tiny pore spaces. In sediment or sedimentary rocks, adjacent grains do not fit together, so there is PORE SPACE between the grains where groundwater can be stored. All types of rocks have FRACTURES that provide openings in which groundwater can accumulate. If the fractures are connected, the water can flow. Some rocks (like limestone) get eroded by water, forming CAVES that can be filled with water.

22
Q

What controls how water flows through rocks?

A
  1. Porosity
  2. Permeability
  3. Hydraulic Conductivity
23
Q

Porosity

A

Volume percentage of rock that consists of voids or openings. Porosity is a measure of the rock’s ability to hold water. It is the proportion of the volume of rock that is open space. PRIMARY is during rock formation and SECONDARY is after rock forms (joints, dissolution, fractures)

24
Q

Permeability

A

Capacity of a rock to transmit fluid through pore space and fractures. Rocks that allow water to flow easily are referred to as permeable, while those that do NOT are referred to as impermeable. It really is the ability of a fluid to move through a rock or sediment… proportional to the void spaces, conduits like number, size, straightness, and also measured in terms of water velocity.

25
Q

Hydraulic Conductivity

A

The ease with which a material will transmit a fluid. Takes into consideration properties of the material (permeability) and the fluid (density and viscosity)

26
Q

How do permeability and porosity relate to groundwater?

A

Confined and unconfined aquifers.

27
Q

Acquifer

A

Large body of permeable, saturated material through which groundwater can flow

28
Q

How and where does groundwater flow?

A
  1. Water table has the same general shape as the overlying land surface
  2. The water table is deeper under mountains, so the slope is subdued here
  3. Groundwater flows downslope
  4. Where groundwater intersects the land surface, lakes, rivers, or wetlands may occur.
29
Q

What controls the rate of groundwater flow?

A
  1. Permeability
    - The rate of flow is strongly controlled by the permeability of a rock type. Flow is fastest in highly permeable cavernous limestone.
    - Flow is moderately fast in a porous conglomerate or well-sorted sandstone.
    - Flow is slower in shale, which has small pores, and in a granite with poorly connected fractures.
  2. Hydraulic Gradient
    - To a lesser degree, the rate of flow is controller by the steepness of the water table.
30
Q

Potentiometric Surface

A

Heigh to which the water’s pressure would raise the water if the water were confined

31
Q

How do we mine groundwater?

A

Qanats used for past 3000 years. They are a water management system used to provide a reliable supply of water to human settlements in hot, arid, and semi-arid climates.

32
Q

Using ground water, what do you want?

A

Good Supply– adequate volume, as pure as possible

At low cost – for drilling, pumping, treat, transporting

33
Q

What happens when we OVER mine groundwater?

A
  1. Cone of depression: mining groundwater can lower the surrounding water table
  2. Land subsidence: groundwater depletion
  3. Saltwater intrusion
34
Q

Where does your water come from?

A
  1. Kaw river treatment plant

2. Clinton reservoir water treatment plant

35
Q

As water travels over land surface, it dissolves natural occurring minerals and can pick up substances?

A

viruses and metals, salts, pesticides and herbicides, organic chemicals from industrial or petroleum use.