Soils Flashcards

1
Q

What factors control soil formation?

A

Parent material, time, climate, biota, topography

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2
Q

Why is soil important?

A

Soil is an important interface between all spheres on earth (lithosphere, biosphere, mesosphere, atmosphere, hydrosphere)

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3
Q

Soil texture is comprised of what 3 things?

A

Sand, silt and clay

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4
Q

What size is a coarse fragment?

A

Greater than 2 mm

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5
Q

Gravels, cobbles and stones are called what?

A

Coarse fragments

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6
Q

Name 4 properties of Sand

A

Feels gritty, excellent air supply to roots, large pores allow water to move quickly, generally resistant to compaction

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7
Q

Name 4 properties of Silt

A

feels slippery or floury, small pores for increased water retention, easily compacted, less air supply than sand

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8
Q

Name 4 properties of Clay

A

feels sticky, tiny pores hold water, compacts easily, air supply is restricted

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9
Q

Name 4 properties of Organic Matter or Humus

A

feels slippery, holds water and nutrients, generally broken down into LFH layers and into Mor, Moder and Mull, cannot hand texture

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10
Q

What contributes to soil structure?

A

texture, organic and mineral composition, water content, soil organisms, biological processes (e.g. root growth)

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11
Q

Soil particles aggregate to form what?

A

a Ped

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12
Q

What are the six types of soil structure?

A

Granular, Blocky, Columnar (or Prismatic), Platy, Single-Grained, Massive

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13
Q

What system is used to determine the color of soil samples?

A

Munsell Color System

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14
Q

Name the 10 soil orders in Canada

A

Brunisol, Cryosol, Chernozemic, Gleysolic,

Luvisolic, Organic, Podzolic, Regosolic, Solonetzic, Vertisolic

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15
Q

Name the taxa used to classify soils (broad to narrow)

A

Order, Great Group, Sub Group, Family, Series

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16
Q

What does CSSC stand for?

A

Canadian System of Soil Classification

17
Q

Name the 4 soil formation processes

A

1) Additions - the addition of organic material (i.e., addition of dead root mass in grassland ecosystems).
2) Transfers - the downward movement of soluble material in water (i.e., redistribution of calcium carbonate in a soil profile). Note that while the distribution of material with depth has changed, the material has not been completely lost from the soil.
3) Transformations - the weathering of primary minerals to secondary minerals, or the decomposition of organic matter.
4) Removals - the complete loss of material from the soil profile (i.e., the loss of calcium carbonate in a soil forming in a humid environment).

18
Q

Chernozemic soils are typically found in what types of environments?

A

Grasslands

19
Q

The youngest soils are found in what soil order?

A

Regosol

20
Q

This soil occurs in a wide variety of climatic and vegetative conditions and has brownish Bm or Btj horizons

A

Brunisol

21
Q

This soil is typically associated with coniferous forests

A

Podzol

22
Q

Name the soil where the dominant process is the eluviation of clay from the Ae horizon and its deposition in the Bt horizon

A

Luvisolic

23
Q

Which soil has a saline C horizon?

A

Solonetzic

24
Q

This soil is characterized by the shrinking and swelling of clays

A

Vertisolic

25
Q

Soil found in areas of temporary or permanent water saturation. Low chroma, prominent mottling, or both.

A

Gleysolic

26
Q

Soils that have accumulated organic materials in water-saturated conditions

A

Organic

27
Q

Name the Organic Horizons

A

O, L, F, H

28
Q

Permafrost soil found in arctic or sub-arctic conditions

A

Cryosol

29
Q

Name the 3 broad categories of Humus forms

A

Mor, Moder, Mull

30
Q

List some human activities (other than agriculture and forestry) that can have a direct impact on soil formation.

A

Road building, excavation, construction of various buildings, and mining.

31
Q

Why are A horizons more common in grassland soils than forest soils?

A

In grasslands, most of the organic matter is added directly to the mineral soil through dead roots and a significant amount of biomass is found underground. In forested ecosystems, above-ground biomass is much larger than below ground, while organic material is added to the surface of the soil where it tends to decompose before it is incorporated into the soil.

32
Q

How deep would the layer of topsoil on a hilltop be as compared to a valley below?

A

Soil at the top of a hill would be much thinner than in a valley because sediments move down slope.

33
Q

If all four processes are active in all soils, why aren’t all soils alike?

A

All four processes can and do occur at the same time in any given soil. It is the balance of these processes that determines the type of soil that forms. The balance of the four processes is controlled by the five soil-forming factors.

34
Q

The Ae horizons are more commonly present in soils that are under a vegetative cover of trees, rather than grasses. Can you think of why this might be?

A

Grasses tend to grow more quickly than trees in the spring and soak up more of the snow melt and early rainfall. Hence, more leaching takes place in soils under a vegetative cover of trees than grasses leading to formation of an Ae horizon.

35
Q

What is the difference between eluviation and illuviation?

A

Eluviation is the process by which clay is removed and illuviation is the process by which clay is deposited. Distinct eluvial and illuvial horizons may develop over time as water moves clay particles through the profile. The upper Ae (eluvial) horizon is depleted of clay and the lower Bt (illuvial) horizon is enriched with clay. Therefore, we can say that the eluviation of clay from the surface horizon created an Ae horizon, a horizon which is depleted of clay.

36
Q

What does the lower case “g” indicate about a horizon?

A

The “g” describes a horizon is gleyed or mottled and is usually characterized by grey colouring. This indicates the soil is permanently or periodically under intense anearobic conditions.

37
Q

List the Mineral Horizons

A

A, B, C