Soil properties Flashcards

(62 cards)

1
Q

What direct effect does color have on behavior or use of soil?

A

Soil warming in spring (the darker the soil the faster it warms)

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2
Q

Importance of soil color

A

Provides valuable clues to the nature of other soil properties (as well as classification)

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3
Q

Hue

A

Designates the color (number on top of page)

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4
Q

Value

A

designates the lightness of color (number on side of page)

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5
Q

Chroma

A

Distinguishes pure hue from a gray shade (number on bottom of page)

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6
Q

Main factors influence on soil color

A
  1. Water content
  2. Organic matter
  3. Oxidation state of iron and manganese/Magnisum
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7
Q

Black - Dark Brown (10Yr 2/1)

A

High organic matter

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8
Q

Reds and yellows

A

Ferric Iron (Fe^3+) oxides and hydroxides

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9
Q

Hematite

A

red (intense weathering) (5R 3/6)

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10
Q

Goethite

A

Yellowish brown (10YR 8/6)

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11
Q

Limonite

A

Yellow (humid environments)

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12
Q

Ferrihydrite

A

dark red (2.5 YR 3/6)

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13
Q

Gray and Bluish

A

Reduced iron compounds and poorly drained soils

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14
Q

Black (10YR 2/1) (Little Organic material)

A

Manganese Oxides

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15
Q

Greenish

A

Glauconite

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16
Q

White/Gray (10YR 6/1)

A

Quartz and silicate minterals

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17
Q

Whites (10YR 8/2)

A

Carbonate accumulation calcites, and soluble salts

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18
Q

How does chemical reduction affect soil color and under what conditions does it occur?

A

ferric iron oxides to mobile ferrous iron

results in gray colored soils

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19
Q

Why is texture considered a “basic soil property”?

A

does not change

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20
Q

Relationship between particle size and surface area

A

Larger particle = lower surface area

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21
Q

What does soil surface area influence in the soil?

A

Water holding capacity, chemical reactions, soil cohesion, cation exchange capacity, ability to support microorganisms

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22
Q

Teton dam

A

Failure to pay attention to soil properties. Seepage of water into an area with poor sealing like sand or silt.

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23
Q

Aggregates

A

Sand, silt, and clay particles when they are not independent of each other

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24
Q

Microaggreates

A

Comprised of smaller particles (2-250 micrometers)

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25
Macroaggregates
larger (.25-5mm) comprised of microaggregates
26
Peds
Large-scale structure evident when observing soil profile
27
Granular
-spherical aggregates -loosely packed together -typically high in organic matter -very porous -often observed in A horizons -susceptible to rapid changes
28
Blocky
-irregular and cubelike -molded by shape of surrounding blocks -common in B horizon in humid regions (angular and sub angular)
29
prismlike
-pillarlike -up to 150mm -swelling clays -b horizon -arid regions (columnar and prismatic)
30
platy
-thin sheets -caused by soil forming process or PM -compaction -lower porosity
31
Block density
mass of a unit volume of dry soil
32
factors that affect bulk density
-texture -Organic matter -type of material -compaction
33
What bulk density inhibits root growth
above 1.6 g/cm^3
34
Equation for bulk density
Db= mass soil/bulk soil volume
35
What typically has the greatest bulk density?
Sand
36
Least amount of bulk density
clay
37
Particle density
Mass per unit volume of soil solids
38
Factors that affect particle density
-type of mineral present -organic matter content
39
Average particle density in mineral soils
2.65
40
Exceptions for average particle density
soils with high O.M Very sandy or clayey soils
41
Particle density equation
Dp= mass soil/volume of soil solids
42
Benefits of tillage
-break large clods into aggregates -incorporate organic material -kills weeds
43
disadvantages of tillage
-accelerate decomposition of OM -compaction
44
Plow pans
Dense zones immediately below plow layer (increases bulk density and restricts root growth)
45
Ways to reduce compaction
-decrease tillage -use wider wheels -minimize operations on wet soils - use rotations with deep-rooting crops
46
Porosity
the total volume percentage of the bulk density that is not occupied by soil particles (air and water and plant)
47
pore space equation
% pore space= 100- (Db/Dp * 100)
48
Macropores
-Allow rapid movement of water/air into or through soil -large enough to accommodate plant roots and small organisms
49
micropores
-do not allow air movement -usually filled with water in field soils -water movement through micropores is slow -some pores are too small for bacteria
50
when is pore size more important than total pore volume
soil drainage and aeration
51
effect of cultivation on pore space
reduces pore space and pore size
52
Soil aggregates
many soil particles held in a single mass or cluster, such as a clod, crumb, block or prism
53
Primary mechanism of soil particles being held together
held together by clay or organic matter
54
psuedosand
clay and iron oxides held together forming a stable aggregate
55
What if a more weakly charged ion such as sodium (Na+ or K+) is present with few divalent or trivalent ions?
-clays will not stick together -not good for plant production -common in arid regions
56
Earthworms form _____ after ingesting soils
casts
57
what form sticky networks to bind particles together?
Plant root hairs and fungal hyphae
58
Microorganisms create
organic glues
59
Soil tilth
the physical condition of soil in relation to plant growth
60
Soil tilth is influenced by
- aggregate formation and stability -bulk density and pore space -soil moisture -soil texture
61
Soil crusting
develop when sealed over soil surface dries out after rainfall or irrigation
62
proctor test
simple way to evaluate how compact you can get a soil and what content you want