water and soil resources Flashcards

1
Q

movement of water
around Earth’s surface
and its subsystems.

A

Hydrologic cycle

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2
Q

are the
places where water
resides for varying
amount of time

A

Reservoirs

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3
Q
are the 
processes that allow 
water to move 
between each 
reservoirs and 
subsystems
A

Pathways

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4
Q
is the evaporation 
of water from the leaves and 
stems of plants, which contributes 
about 10% of the water vapor in 
the atmosphere
A

transpiration

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5
Q

average length of
time spent by water molecule in a
reservoir.

A

residence time

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6
Q

is the saltiness of saltwater

A

salinity

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7
Q

a permanent body of ice (largely of

recrystallized snow)

A

glaciers

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8
Q

is a mass of glacial land ice
extending more than 50,000 km2
(covering
most of Greenland and Antarctica

A

Ice sheets

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9
Q

A soil, rock, or sediment that
is frozen for more than two
consecutive years.

A

permafrost

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10
Q

moving body surface water that flows downslope toward sea level because of gravity.

A

stream

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11
Q

stream has clearly-defined passageway

A

channels

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12
Q

is a stream with a considerable volume and a well-defined channel.

A

River

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13
Q

large inland bodies of fresh or saline

water

A

lakes

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14
Q

are small and shallow lakes

A

Ponds

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15
Q

are barriers constructed along

streams to contain the flow of water

A

Dams

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16
Q

Land areas where water covers the

surface for significant periods

A

Wetlands

17
Q

type of wetlands

A

Marsh. swamp and estuary

18
Q
a shallow wetland 
around lakes, 
streams, and 
oceans where 
grasses and reeds 
are the dominant 
vegetation
A

Marsh

19
Q

wetland with lush trees and vegetation found in low-lying areas beside slow-movingrivers.oxygen in the water is typically low and swamp plants and animals are adapted to these low oxygen conditions. Mangrove forests are unique example of swamp ecosystem that tolerates salty condition

A

Swamp

20
Q
partly enclosed 
coastal body of 
water where 
freshwater from 
stream meets the 
saltwater from the 
sea
A

Estuary

21
Q

natural event wherein
an area that is usually
dry is submerged
under water.

A

FLood

22
Q

fresh water found in the rock and soil layers

beneath the surface

A

groundwater

23
Q

Water-bearing rock layers are called

A

aquifers

24
Q

is the total amount of empty pore spaces
in the rock. It determines the amount of
groundwater that an aquifer can hold

A

porosity

25
Q

essential component of the Earth
that enabled life to exist on the
planet and continues to support it

A

soil

26
Q

s the living skin of
Earth which is a result of the
dynamic interaction among the
major subsystems.

A

Pedosphere

27
Q

important in soil formation because its
chemistry and type will determine the
kind of soil that will be formed together
with the effects of the other factors.

A

Parent material

28
Q
temperature, rainfall, and 
moisture affects pattern and 
intensity of soil-forming processes 
(weathering, leaching, 
transportation, and distribution)
A

Climate

29
Q

gradient of the slope affects water

flow and erosion.

A

topography

30
Q

plants, animals, microorganisms, and

humans affect soil formation.

A

Biological factors

31
Q

soil formation is a long and continuous process (hundreds to
thousands years) depending on the climate and environment.

A

Time

32
Q

refers to absolute soil
losses in terms of
topsoil and nutrients.

A

Soil Erosion

33
Q

reduces the amount of air, water, and space

available to roots and soil organisms.

A

Soil compaction

34
Q

characterized by droughts and
arid conditions as a result of
human activities and
exploitation

A

Desertification

35
Q

led to the use of more machinery, deforestation,

and clearing of land for use in cultivation

A

Intensive Agriculture

36
Q

ncreasing population → conversion of land
to urban centers (concrete structures)
• represent a significant loss of soil,
particularly because this loss becomes more
or less permanent as soil is sealed with
concrete

A

Urbanization