MR 1 Study Guide - Soil Physical Properties Flashcards

1
Q

What are the main soil particle sizes and their size ranges?

A

Sand, silt, and clay

Sand is 0.05-2 mm
Silt is 0.002-0.05 mm
Clay is <0.002 mm

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2
Q

What is soil texture?

A

The relative proportion of particle sizes in a soil

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3
Q

What is soil structure?

A

Defines how soil mineral particles (sand, silt and clay) are bound together and arranged in the three dimensional space

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4
Q

What is the textural class of a soil with 20% clay, 40% silt, 40% sand?

A

Loam

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5
Q

Which soil texture has larger total soil pore space (or pore volume), a sandy or a clayey soil? Why?

A

A clayey soil because it has many more pores despite them being small

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6
Q

Which soil texture has larger surface area, a sandy or a clayey soil? Why?

A

Clayey soil because it has more particles, resulting in more surface area

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7
Q

What soil texture results in a larger amount of plant available water? Sand, sandy loam, loam, clay loam or clay?

A

Loam, but clay and sandy loam are second best

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8
Q

What is granular soil structure and where it is most typically found within the soil profile?

A

A healthy soil texture found at the top of the soil profile

Aggregates less than 0.5 cm diameter

Particles held together by organic substances

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9
Q

Describe platy soil structure

A

Thin, flat horizontal plates formed by compaction

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10
Q

Describe wedge soil structure

A

Elongated shape; polished surface (slickensides)
Caused by the shrink-swell process

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11
Q

Describe blocky soil structure

What horizons is it commonly found in?

A

Irregular blocks
1.5-5.0 cm in diameter
Particles held together by clay
Commonly found in B horizons (also A and C)

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12
Q

Describe prismatic soil structure

A

Vertical columns
Particles cemented by shrink/swell (smectitic) clay

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13
Q

Describe columnar soil structure

A

Vertical columns with rounded tops
Found in soils of arid climates with high content of salts

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14
Q

Describe structureless soil structure

A

Have no observable aggregation or structural units

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15
Q

Soil bulk density

A

The mass per unit volume of dry soil, including pore space

(dry meaning no water)

Soil bulk density = weight oven dry soil (g)/total volume soil (cm3)

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16
Q

Typical soil bulk density

A

Mineral soils: 1-1.8 g/cm^3 or g cm^-3
Organic soils: 0.5 g /cm^3 or g cm^-3

17
Q

Soil porosity

A

The percentage of the soil volume that is pore space

Soil porosity (%) = [volume of soil pores (cm^3)/soil volume (cm^3)] x 100

or

[1-(Bulk density/particle density)] x 100

18
Q

How does soil structure drive infiltration and permeability?

A

Depending on structure, soil can have good or poor infiltration/permeability

19
Q

Which soil structure will have higher infiltration rates: Granular or platy? Why?

A

Granular because there’s a lot more pore space and it hasn’t been compacted

20
Q

What causes soil compaction? How can you determine an issue of soil compaction?

A

Mostly related to ‘traffic’, which can be many things

21
Q

How does compaction affect soil bulk density and porosity?

A

Increases soil bulk density but decreases porosity