soil and weathering test Flashcards

1
Q

Weathering

A

changes in rock material exposed at surface

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2
Q

mechanical weathering

A

physically changing rock into smaller pieces without changing its composition

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3
Q

Chemical weathering

A

breakdown of rock by changing its chemical composition

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4
Q

types of mechanical weathering

A

exfoliation, ice wedging, biological activity, abrasion

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5
Q

exfoliation

A

process where sheets of rock peel or flake away

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6
Q

ice wedging or Frost wedging

A

occurs when water seeps into rocks in freezes

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7
Q

biological activity

A

The activity of organisms that weather away rock

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8
Q

abrasion

A

collision of rock with one resulting in breaking and wearing away

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9
Q

types of chemical weathering

A

hydrolysis, carbonation, oxidation, acid precipitation, plant acids

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10
Q

hydrolysis

A

change in composition of minerals when they react with water

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11
Q

carbonation

A

when some minerals come in contact with carbonic acid they form a new product

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12
Q

oxidation

A

when metallic elements combine with oxygen – rust is one result of oxidation

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13
Q

acid precipitation

A

reacts with minerals

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14
Q

plant acids

A

plants secrete acids that you rode away the rock

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15
Q

rate of weathering depends on four things

A

Rock composition, and now of exposure, climate, topography

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16
Q

Rock composition

A

igneous and metamorphic rocks don’t weather easily sedimentary rocks do

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17
Q

amount of exposure

A

more exposure receives the faster it will weather

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18
Q

climate

A

slow and very hot/very cold climates but fairly rapid and warm, humid climates

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19
Q

topography

A

elevation or slope of surface where rock is located

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20
Q

regolith

A

A layer of weathered rock fragments that covers much of the earth surface

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21
Q

soil

A

part of the regolith that thatsupports plant growth – complex mixture of minerals, water, gases, and remains of plants and animals

essential to life on earth for growth

except for some steep mountain slopes and extremely cold regions, soil is found almost everywhere on earth surface

22
Q

soil composition has four major components

A

mineral matter, organic matter/humanness, water, air

23
Q

humus

A

dark organic material and remains of animals and plants

24
Q

soil texture

A

Texter refers to the proportions of different particle sizes

25
particle sizes
Sand/large size – silt – Clay/small size – loan/a mixture of all three sizes and best suited for plant life
26
factors in soil formation
Parent material, time, climate, organisms, slope
27
Parent material
source of the mineral matter in soil
28
Time
The longer the soil has been forming the thicker if becomes
29
climate
greatest effect on soil formation and warmer temperatures equals faster soil formation but too hot can slow it down again
30
organisms
furnish organic matter to soil and plants are the main source
31
slope
steep slopes often have poorly developed soil's
32
soil profile
A cross-section in which the layers of the soil in bed rock can be seen each layer is called a horizon
33
in fully developed residue soil…
there are multiple horizons | soil that's formed in place
34
horizons
o horizon/organic, thin, contains humus A horizon/topsoil,mixture of decaying organic matter and small rock particles B horizon/subsoil, contains minerals and Clay C horizon/regolith, partially weathered bed rock bed rock/parent material, solid, on whether to rock that lies beneath regolith
35
tropical( wet and warm ) climate
forms laterites ( thick and infertile soil )
36
dessert/dry climate
form saw whales from mechanical weathering – soil is thin and mostly regolith
37
temperate climates
temps range from cold to warm
38
two types of soil that are found depending on amount of rainfall
pedalfer and pedocal
39
pedalfer
soil form if an area receive 65 cm or more of rain per year found in places east of the Mississippi
40
Pedocal
soil formed of rainfall is less than 65 cm a year
41
soil erosion
erosion is the process by which the products of weathering are transported occurs worldwide slow process New soil forms about as fast as the existing soil erodes
42
agents of erosion
gravity, windy, glaciers, precipitation, ocean waves, currents, streams, groundwater
43
unwise use of the land leads to
climatic conditions upset natural balance
44
deposition
process by which sediment are dropped in a new location – occurs after erosion
45
mass movement
The downward movement of rock, regolith and soil due to gravity
46
mass movement is triggered by (as is all types of soil erosion)
saturated surfaces/excess water , steepness of the slopes, removal of vegetation, earthquake
47
rockfall
The fall of rock from a steep cliff – most rapid
48
landslide
sudden movement of masses of a loose rock and soil down the slope of the hill
49
slump
downhill movement of a large block of soil under the influence of gravity
50
mudflow
The rapid movement of a large mass of mud
51
creep
extremely slow downhill movement of unweathered rock material
52
weathering/erosion of mountains
weathering and erosion wear down rugged peaks to rounded peaks and gentle slopes