Exam 3 Flashcards

1
Q

How does climate influence soil formation?

A

Precipitation and temperature determine the intensity/nature of weathering

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2
Q

What are the types of weathering?

A

Physical, chemical, biological

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3
Q

What is effective precipitation?

A

Precipitation that penetrates to lower levels of soil profile. Carries solutes down horizon

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4
Q

How does effective precipitation influence soil formation?

A

A lack of water can keep elements in place to carry out/limit weathering. Higher eff/prec means higher weathering

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5
Q

How does temperature impact soil formation?

A

Warm + wet conditions= increase weathering, leaching, plant growth => carbon sequestration

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6
Q

What do organisms influence in soil formation?

A

Influences organic matter accumulation, weathering, and profile mixing

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7
Q

How do animals impact soil formation?

A

Animals create pores, mix layers, consume OM, and influence nutrient levels of soils

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8
Q

How does aspect of a slop affect soil formation?

A

Affects weathering, S-facing slopes have less water and less OM

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9
Q

How does relief and topography affect soil formation?

A

Different vegetation types inhabit different locations on the slope (grasses, confiders, deciduous) and have different soil effects

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10
Q

Where do you find residual material?

A

Upper slopes

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11
Q

Where would you find the colluvium soil? How is it characterized?

A

Lower slopes. Chunky and not well sorted

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12
Q

What is a floodplain?

A

A part of a river valley that is inundated during floods

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13
Q

What are the 3 types of alluvian stream deposits?

A

Floodplains, alluvial fans, deltas

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14
Q

Soil factor =

A

Climate, orgaisms, relief/topography, parent material, time

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15
Q

5 types of physical weathering

A

Temperature, water, ice, wind, biota

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16
Q

Define exfoliation

A

Peeling of outer layers because of difference in temp inside vs outside the rock. Expansion + contraction => stress => exfoliation

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17
Q

What are the 6 taxonomic categories of soils?

A

Order, suborder, great group, subgroup, family, series

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18
Q

How are orders defined?

A

Based off morphology

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19
Q

How are suborders defined?

A

Based on genetic similarities

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20
Q

How are great groups defined?

A

Diagnostic horizons and levels of certain chemicals

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21
Q

How are subgroups defined?

A

By a typic member and other members that have characteristics not shared with the typic member

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22
Q

How are families defined?

A

By properties like pH, texture, minerals, soil temp/depth

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23
Q

How are series defined?

A

Slight differences in texture or surface later. Very closely related soils

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24
Q

Which taxonomic group has the most detail?

A

Series

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25
Q

Which taxonic group has the least detail

A

Order

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26
Q

Which taxonomic group covers the most area?

27
Q

Which taxonomic group covers the least area?

28
Q

What is soil texture?

A

Proportion of sand/silt/clay
Size/distribution of soil particles

29
Q

Why is soil texture useful?

A

Helps infer plant growth and suitability
Does not change easily

30
Q

How does particle size relate to water movement speed and retention?

A

Increased size = more surface area; high water speed less retention

31
Q

Describe sand

A

Gritty, visible to naked eye, round or angular

32
Q

How does sand correspond to plant growth?

A

Low nutrients available to plants
Large pore space, well drained
Loose soil
Infertile and drought prone

33
Q

Describe permeability and infiltration rates for sand

A

Low permeability and high infiltration

34
Q

Describe silt

A

Smaller than sand, similar shape/comp, silky texture, low plasticity

35
Q

How does silt relate to plant growth?

A

Large surface area = nutrient availability
Better water retention

36
Q

What is piping and where does it occur?

A

Water process that washes away silt and develops macropores in subsurface

37
Q

Difference between adsorption and absorption

A

Ad: molecules adhere (sand)
Ab: molecules drawn into (clay

38
Q

What are clay particles? What are their traits

A

Colloids; do not readily settle out of water, shaped like flakes

39
Q

Define gravity water, available water, hydroscopic water

A

Gravity water: moves fast through soil, cannot be used by plants => high in sand
Available water: available for plants
Hydroscopic water: tightly adhered water, unavailble to plants => high in clay

40
Q

List textures in order of water availability

A

Silt loam is high H2O availability
Sand is low availability
Clay is low availability

41
Q

Define biogeochemical weathering

A

When primary materials are converted into insoluble or soluble forms

42
Q

What are the 6 types of biogeochemical weathering?

A

Hydration, hydrolysis, dissolution, acid rxns, redox, complexation

43
Q

Define hydration

A

Intact water molecules bind to mineral

44
Q

Define hydrolysis

A

Molecules split, hydrogen replaces cation from mineral

45
Q

Define dissolution

A

Minerals dissolved by hydrating cations and anions until they are dissociated and surrounded by water

46
Q

Difference between oxidation and reduction

A

Oxidation is loss of electron, reduction is gain

47
Q

Define acid reactions

A

Weathering accelerated by acids, increading hydrogren activity in water

48
Q

Define redox

A

Minerals containing iron, manganese, sulfur exposed to air and gain/lose electrons

49
Q

Define complexation

A

Organix reactions between different acids produce acid complexes and speed chemical rxns

50
Q

What are the 4 soil forming processes

A

Transformation, translocation, additions, losses

51
Q

Define transformation

A

Rock weathering and decomposition destroy some soil component and create others

52
Q

Define translocation

A

In/organic materials move out/up/down profile

53
Q

What are the 6 soil horizons?

A

Organic, A(topsoil), Eluviation, B(subsoil), C(parent), R(bedrock)

54
Q

Define the O horizon

A

Organic material above mineral soil

55
Q

Define A horizon

A

Topsoil- mix of mineral and OM

56
Q

Define E horizon

A

Eluviation- light colored, water facilitated loss of material that leaves behind materials

57
Q

Define B horizon

A

Subsoil - deposited minerals/salts, alteration to parent

58
Q

Define C horizon

A

Parent rock - conconsolidated mineral horizon with no other horizon traits, retain parental structure

59
Q

Define R horizon

A

Bedrock - continuous, consolidated rock without weathering

60
Q

How are forest O horizons differentiated?

A

Litter, fermented, and humic based on level of decomposition

61
Q

What are the 3 O subordinate horizons?

A

Oi, Oe, Oa

62
Q

What is the Oi horizon?

A

Fibric, slightly recognizable OM

63
Q

What is the Oe horizon?

A

Hemic, fine fragments, slight decomp, partially recognizable material

64
Q

What is the Oa horizon?

A

sapric, high decomp, not recognizable material