Soils of BC Flashcards

1
Q

What are the 4 main factors that influence soil formation?

A

Climate, Biota, Parent Material, Topography

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2
Q

What physical component of soil is the most important component affecting plant growth?

A

Organic content

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3
Q

What are the two most active processes in soil formation?

A

Biota and Climate

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4
Q

What are the different levels of the Canadian soil hierarchy?

A
Order
Great Group
Sub Group
Family
Series
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5
Q

What does Order Describe?

A

Largest and most broad descriptor. Organizes soils based on properties that reflect the predominant soil processes.

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6
Q

What does Great Group describe?

A

Properties that modify the strongest soil forming process of the order. ex humus accumulation in chernozems make it black, brown, or dark grey

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7
Q

What does Sub Group describe?

A

Describes how a subgroup may be transitioning into another subgroup. Ex Gleyed brown chernozemic.

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8
Q

What does Family Describe?

A

A group of soil that are similar in mineralogy, texture, genetic material, soil climate

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9
Q

What does Series describe?

A

Subdivision of family where horizons depth, colour, texture and structure fall within a narrow range similarity.

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10
Q

Describe the Brunisolic order.

A

• Result of minor modification of parent material
• poorly developed soil horizons
◦ caused by long cold winters in north and high altitudes or lack of
moisture in interior BC
• in drier landscapes than Podzols
• the “young” soils – young parent material
• thick reddish-brown Bm horizon
• 2 main types

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11
Q

Describe the Chernozemic order.

A

What: Grassland vegetation. A lot of organic matter.

Where: Found in arid to sub arid. Low rainfall, high summer temps, high evaporationtraspiration rates. South and west facing slopes.

Dominant Process: accumulates organic matter. as topsoil.

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12
Q

Describe the Cryosolic order

A

What: Contain permafrost close (within 2 m) to the surface.

Where: North east BC in the dry peatlands, High mountains. North facing slopes.

Dominant process: permafrost formation, cold temperatures, causing organic accumulation.

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13
Q

Describe the Gleysolic order.

A

• Characteristic of poorly drained areas
• saturated for extended periods so reducing conditions present
◦ less mineral and OM transformation in soils
• fine-grained parent materials such as clayey till and glaciolacustrine deposits

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14
Q

Describe the Luvisolic order.

A
  • Associated with forest vegetation, parent materials that are base-saturated and fine-grained with moderate precipitation
  • characterized by leaching and accumulation of clay in Bt horizon
  • interior plateaus of BC and foothills of rocky mountains - peace river region.
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15
Q

Describe the Organic Order

A

• Develop in wettest parts of the landscape; saturated for most of the year
• composed mainly of OM – in situ accumulation – not modification of parent
material
• found in wetlands across the province
• several different types based on OM composistion

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16
Q

Describe the Podzolic order

A

• Cool, humid climates beneath coniferous forests
• widespread along BC coast & throughout mountains (except at lowest elev.)
• high acidity and profile development (caused by lots of leaching)
• tend to develop on volcanic ash
Ferro-humic podzols = display red horizon where Fe, Al and OM have accumulated
- found on western slopes of coast and insular mountains

17
Q

Describe the Regosolic Order

A

• Little soil development – little to no B horizon
• on high mountains and steep slopes where soil development doesn’t really
happen much
• lithic soil is when you have bare rock… so basically not soil

18
Q

Describe the Solonetzic order

A
  • Have significant Na and/or Mg salt accumulations
  • scattered across interior region
  • moderately common on sedimentary rocks with high salt content