Exam 1 Flashcards

(55 cards)

1
Q

Factors of soil formation

A

time, topography, parent material, climate and organisms

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2
Q

soil formation main processes

A

addition and losses, transformation, translocation

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3
Q

additions and losses

A

inputs water and organic matter and there are losses through weathering.
- change the soil overtime

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4
Q

transformation

A

weathering and decomposition change the nature of the soil

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5
Q

translocation

A

movement of material creates zones of depletion and enrichment, this creates vertical heterogeneity

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6
Q

O-Horizon

A

organic, decomposition, typically at the soil surface

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7
Q

A-Horizon

A

top mineral, organic matter accumulates and it is darkened by organic matter

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8
Q

E-Horizon

A

Lighter colored than A, Clay and organic matter have been leached , eluviation below A and O

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9
Q

B-Horizon

A

Where clay and organic matter from A and E accumulate, illuviation occurs

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10
Q

C-Horizon

A

Parent material, unconsolidated material below A and B

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11
Q

eluviation

A

removal, leaching

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12
Q

illuviation

A

accumulation

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13
Q

g

A

strong gleying - molting

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14
Q

h

A

illuvial accumulation of organic matter

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15
Q

k

A

accumulation of carbonates

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16
Q

n

A

accumulation of sodium

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17
Q

s

A

illuvial organic matter and iron, aluminum oxides

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18
Q

t

A

accumulation of silicate clays

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19
Q

o

A

accumulation of iron and aluminum oxides

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20
Q

p

A

plowing or other disturbances

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21
Q

glacial till

A

sediment deposited by a glacier

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22
Q

alluvium

A

transported by water (streams)

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23
Q

colluvium

24
Q

aeolian/loess

A

transported by wind/wind blown dust

25
tephra
transported by volcanic eruption
26
lacustrine/marine
formed at bottoms of lakes, carried to oceans by rivers and streams
27
residual
formed in place - none
28
physical weathering
change in size of the rocks and minerals by atmospheric agents without chemical alteration
29
physical weathering examples
freezing/thawing, grinding and abrasion
30
chemical weathering
change in the chemical nature of the rocks/minerals by atmospheric agents
31
chemical reaction - hydrolysis
splitting H2O
32
chemical reaction - hydration
addition of intact water molecule
33
chemical reaction - carbonation
reaction with CO2 and H2Co3 solubilizing minerals
34
chemical reaction - oxidation
electron loss
35
reduction
electron gain
36
dissolution
water as a solvent, hydration cations and anions
37
Alfisols
argillic, natric and kandic horizon that has a high to medium base saturation
38
Alfisols
alf
39
andisols
from volcanic ejecta, dominated by allophane and al-humic complexes
40
andisols
and
41
aridisols
dry soil, ochric epipedon that is sometimes argillic or natric
42
aridisols
id
43
entisols
little profile development, ochric epipedon common
44
entisols
ent
45
gelisols
permafrost often with cryoturbation (frost churning)
46
gelisols
el
47
histosols
peat or bog >20% organic matter
48
histosols
ist
49
inceptisols
ept
50
inceptisols
embryonic soils with few diagnostic features, ochric/umbric epipedon, cambric horizon
51
mollisols
mollic epipedon, high base saturation, dark soils, argillic/natric horizons
52
mollisols
oll
53
oxisols
oxic horizon, no argillic horizon highly weathered
54
oxisols
ox
55