Ch 9 Flashcards

1
Q

Outgassing:

A

Water deep in the interior of the earth (below crust), are released in the form of gas (vapors)

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
2
Q

Eustasy:

A

global sea level caused by changes in the volume of water in the oceans

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
3
Q

In a globe, where is mostly water and where is mostly land

A

Land is mostly found in the northern hemisphere, water in the southern hemisphere

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
4
Q

The hydrological cycle

A

Vast currents of water, water vapor, ice, and associated energy

3 components:

1- atmosphere

2- surface

3- subsurface

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
5
Q

What happens in
the atmosphere part?

A

Evaporation + transpiration = evapotranspiration

transpiration: when plants release water to the atmosphere through small openings called stomata in their leaves, which is another way water moves into the atmosphere from land environments including water moving from the soil into plant roots and passing through their leaves to the air

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
6
Q

What happens in the surface?

A

Interception

stemflow

through fall

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
7
Q

what happens in the subsurface?

A

infiltration

Overland flow

surface run off

percolation

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
8
Q

Infiltration:

A

Water get soaked by the soil

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
9
Q

What happens if the ground surface is permeable?

A

then it won’t soak up the water

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
10
Q

surface run off:

A

Same as overland flow

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
11
Q

Overland flow

A

Surplus of water on surface so it causes a runoff in an area

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
12
Q

Percolation:

A

the movement of water through rocks and soil, filtering downwards after it has infiltrated the ground

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
13
Q

Soil-moisture zone

A

area where most of the water is stored in the soil, and roots have access to it

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
14
Q

Zone of saturation

A

When soil is fully saturated, extra water moves downward as gravitational water into deeper groundwater, filling all spaces in the soil

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
15
Q

Base flow

A

when water table reaches a stream, groundwater flows into the stream

How well did you know this?
1
Not at all
2
3
4
5
Perfectly
16
Q

describe the water budget:

A

measures the input of precipitation and its outputs like evapotranspiration, evaporation, and transpiration from plants, and surface runoffs, and moisture in the soil moisture zone.

income = precipitation

expenditure = run off, evaporation, transpiration

savings account = soil moisture storage

17
Q

Rain gauge:

A

measures the amount of precipitation, its like a big cup that collects all of it

18
Q

Potential evapotranspiration:

A

the amount of water that would evaporate and transpire if there was always enough water available

19
Q

Actual evapotranspiration:

A

the water deficit, the subtraction of the water deficit by the (PE)

20
Q

3 categories of water:

A

gravitational: drains downwards after filling the soil pore spaces

hygroscopic and capillary:
Both remain in the soil but ONLY capillary is accessible to plants image below

21
Q

Why is hygroscopic water not accessible to plants?

A

it is a thin molecule layer tightly bound to each soil particle by the hydrogen bonding of water molecules

22
Q

Wilting point of a plant:

A

when soil moisture only contains inaccessible water, so plants wilt and die

23
Q

Capillary water:

A

valid for plants

24
Q

Gravitational water:

A

un valid for plants as it percolates deep to the groundwater zone

25
Q

Soil moisture utilization:

(desperation)

A

When plants use any moisture they can get from the soil to survive

26
Q

Meteorological drought:

A

defined by the degree of dryness. This definition is region-specific, since it relates to atmospheric conditions that differ from area to area.

27
Q

Agricultural drought:

A

occurs from shortages of precipitation and soil moisture affect crop yields.

28
Q

Hydrological drought:

A

The effects of precipitation shortages (both rain and snow) on water supply, such as when streamflow decreases, reservoir levels drop, mountain snowpack declines, and groundwater mining increases.

29
Q

socioeconomic drought:

A

when reduced water supply causes the demand for goods or services to exceed the supply, such as when hydroelectric power production declines with reservoir depletion.

30
Q

Effects of climate change:

A

Lake levels are rising due to glaciers being melted at a rapid late, also causing freshwater to mix with saline water lower overall salinity in the ocean.

31
Q

Hydropower:

A

electricity generated using the power of moving water

32
Q

Wetland:

A

an area that is permanently or seasonally saturated with water and characterized by vegetation adapted to glycolic soils

Water found in wet lands is all freshwater

33
Q

Where is groundwater found?

A

Beneath the surface that is beyond soil root zone

34
Q

Zone of aeration:

A

a zone above the water table that has air in its pore spaces which may or may not have water

35
Q

Zone of saturation:

(opposite of aeration)

A

a zone above the water table that has water filled in all its pores

36
Q

Water table

A

the upper surface of groundwater, it’s the contact point between the zone of aeration and the zone of saturation

37
Q

Aquifer:

A

subsurface layer of permeable rock or unconsolidated materials (silt, sand, or gravels) through which groundwater can flow in amounts adequate for wells and springs

38
Q

Unconfined:

A

permeable layer above allowing water to pass through and an impermeable layer below

39
Q

Confined:

A

Bounded above and below with permeable layers of rock or unconsolidated materials