lecture 2 Flashcards

1
Q

What the 3 phases we divide soils into to understand soil properties? List the soils these include.

A
  1. Solid phase: mineral and organic matter
  2. Liquid phase: soil water and soil solution
  3. Gaseous phase: soil has amount and composition
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2
Q

What are the three important aspects of the inorganic solid phase?

A
  1. Particle size distribution
  2. Soil structure
  3. Mineralogy
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3
Q

What are the 4 classes of particle size (in order of biggest to smallest)?

A
  1. Gravel
  2. Sand
  3. Silt
  4. Clay
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4
Q

How do we measure soil texture in the lab?

A

Using Stoke’s law

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5
Q

What are the 5 reasons why soil texture is important?

A
  1. Influences soil infiltration rate, and thus the generation of overland flow and soil erosion
  2. Influences soil permeability and therefore drainage
  3. Controls available water capacity of soil - ability to supply water to plants
  4. Influences soil structure, allowing root growth and aeration
    Provides cation exchange capacity for nutrient supply to plants and buffering against acid rain
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6
Q

Rank the soil tecture class by surface area (smallest to largest):

A
  1. Coarse sand
  2. Fine sand
  3. Silt
  4. Clay
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7
Q

What are the characteristics of soil strucutre?

A
  1. Describes the spatial arrangements of particles to complex aggregates, pores, and channels
  2. Has a major influence on water and air movement as well as root growth
  3. Influences the movement of soil macro and meso fauna
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8
Q

What are the 6 major structural forms in soil?

A
  1. Prismatic
  2. Columnar
  3. Angular blocky
  4. Subangular blocky
  5. Platty
  6. Granular
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9
Q

What are the processes leading to the development of soil structure?

A
  • Expansion/contraction upon wetting and drying
  • Root penetration
  • Earthworms and ingestion/excretion by other soil organisms
  • Input and decomposition of soil organic matter
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10
Q

What are the properties maintaining soil strucuture?

A
  • High organic matter content, especially input of fresh litter - promotes bonding between particles
  • Clay minerals - large, reactive surfaces with positive and negative charges
  • Presence of Fe and Al oxides and hydroxides as cementing agents
  • Si coating on minerals - produces duripans in dry climates
  • CaCO3 deposits - produces caliche in semi-arid soils
  • Presence of flocculating cations (Ca2+ and Mg2+)
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10
Q

What are the processes leading to the destruction of soil structure?

A
  • Loss of soil organic matter, especially fresh inputs
  • Rain-drop impact on bare soils
  • Reduction in root growth, especially in annual crops
  • Trampling by stock and machinery
  • Reduction in soil organisms (e.g. fewer earthworms)
  • Loss of flocculating cations (Ca2+ and Mg2+) and replacement by dispersing cations (Na and K+)
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10
Q

What are the soil structural problems and its associated effects?

A
  • Breakdown of weakened aggregates at soil surface
  • Formation of pan at base of plough depth
  • Compacted subsoil
  • Erosion removes fine particles and o.m.
  • Surface crusting do not infilitrate : water washes away, overflow, reduces seedling emergence
  • Pan layers and compact subsoils impede root growth and water & air movement
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11
Q

What is the difference in soil composition between agricultural top soil by volume and organic soil by volume?

A

Organic soil by volume is mostly composed of water

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11
Q

What is the sweet spot soil texture for agricultural soil?

A

Balance of silt content and some clay

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11
Q

Describe whether sandy, loamy, and clayey soil is low, medium, or high in terms of:
1- water holding capacity
2- Aeration and drainage
3- Organic matter content
4- Decomposition rate
5- Nutrient holding capacity
6- Shrinkage
7- Compaction

A

1- low; medium; high
2- rapid; moderate; slow
3- loa; medium; high
4- fast; moderate; slow
5- small; moderate; high
6- none; small; high
7- resists; moderate; easily

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12
Q
A