Soil physical properties Flashcards

1
Q

sand group

A

loamy sand, loamy fine sand

  • at least 70% sand
  • <15% clay
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2
Q

clay group

A

sandy clay, silty clay

- at least 30% clay

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3
Q

loam group

A
  • even mixture of sand, silt and clay

- best combination for physical (a chemical) properties

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4
Q

Sand group advantages

A
  • good drainage
  • easy cultivation
  • quick to warm up in the spring
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5
Q

Sand group problems

A
  • poor water retention for plant use
  • poor nutrient supply
  • poor ability to hold applied nutrients
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6
Q

Clay group advantages

A
  • good nutrient supply & retention

- medium water retention for plant use

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7
Q

Clay group problems

A
  • poor drainage
  • cultivation restricted to a narrow range of water content and has high power requirement
  • easily puddled when wet
  • slow to warm up in he spring
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8
Q

Loam group advantages

A
  • well drained
  • good water retention for plant use
  • good nutrient supply
  • easy to cultivate over a wide range of water content
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9
Q

Loam group problems

A

some are structurally weak and prone to erosion

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10
Q

soil structure determines

A
  • size
  • shape
  • distribution of pores both within and between the aggregates
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11
Q

soil structure develop through

A
  • natural processes during soil formation, often by management
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12
Q

soil strucure influences

A
  • water movement
  • aeration
  • heat supply
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13
Q

soils structure types

A
  • plate like (platey)
  • prism like (prismatic & columnar)
  • block like (blocky & subangular blocky)
  • spheroidal (granular & crumb)
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14
Q

pores are need for …

A
  • water storage
  • drainage
  • oxygen entry
  • carbon dioxide removal
  • root penetration
  • mechanical strength
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15
Q

Processes involved in the development of soil structure

A

development of cracks and channels along planes of weakness through:

  • shrinkage and swelling, caused by drying/wetting and freezing/thawing cycles during soil formation
  • root and soil animal actions
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16
Q

microbial activity during soil structure development

A

formation of humus during the break down of plant and animal residues

17
Q

Micro-aggregate

A
  • <250um
  • flocculation of clay particles to form domains
  • interactions between organic matter and clay domains
18
Q

Macro-aggregate

A
  • > 250um
  • coalescence of micro-aggragates
  • forces exploiting planes of weakness
19
Q

transmission pores (macro)

A

> 50um

  • drainage
  • root penetration
  • gas movement
20
Q

storage pores (micro)

A
  • 50-0.5um

- water available for plant growth

21
Q

residual pores (micro)

A
  • <0.5um
  • water not available to plants
  • controls mechanical strength of soils
22
Q

Porosity =

A

1 - (bulk density/particle density)

23
Q

Bulk density

A

mass of solid soil particles in a unit volume of field soil

- soils + pore space occupied by air and water

24
Q

Particle density

A

mass of soil soil particles in a unit volume of those solid particles

25
Q

unstable soil structure

A
  • soils that lose structure easily when rain falls on the surface or water is help up in the soil
  • soils dominated with single particle size class
  • repeated or poorly timed cultivation
26
Q

consequences of unstable soil structure

A
  • surface capping
  • slaked and puddled structure
  • under-consolidation
  • compaction and erosion