Soil Flashcards

(33 cards)

1
Q

bedrock:

A

rock thats structurally apart of/connected to earths crust

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2
Q

regolith:

A

any loose fragmented earth material that covers bedrock

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3
Q

what is soil?

A
  • the upper most material of terrestrial environments.
  • provides chem and phys needs of plant life (including water)
  • contains minerals (from rocks) and organic matter
  • soil isnt just dirt (the solid factor)
  • it contains gas and liquid components too
  • soil atmosphere contains O2 and other gases from air, and CO2 and methane from the soil.
  • soil water contains dissolved substances such as nutrient’s for the plants
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4
Q

how does soil form? (soil formation aka pedogenesis)

A

5 factors !
1) parent material
2) climate
3) organisms
4) relief
5) time

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5
Q

1) parent material (underlying rock)

A

The nature of the parent mat. will influence the composition of the soil made from it

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6
Q

2) relief (topography)

A

slope of the environment and its aspects whether it faces N, S, E, W

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7
Q

3) climate

A
  • measure of temperature and precipitation
  • precipitation influences downward movement of mat.
  • temp influences decomposition
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8
Q

4) organisms

A

Biological activity of plants, animals, and microbes (bacteria and fungi) is essential for good soil development

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9
Q

5) time

A

properties of soil develop over time in centuries

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10
Q

S.P - colour

A
  • colour of soil changes with depth in its profile
  • colour can come from the parent material or processes of the location
  • munsell soil colour chart
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11
Q

S.P - texture

A
  • based on the particles of sand, silt, and/or clay present in the sample
  • clay > silt > sand. clay retains the most water
  • determines different factors (e.g ability to retain water and how much gases in it)
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12
Q

S.P - structure

A
  • refers to the way particles are grouped together into soil masses called PEDS
  • shape and size of peds influences movement of water + air
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13
Q

S.P - minerals

A

parent material

primary minerals

secondary minerals (changes from primary)

  • Clay minerals are the most important secondary bcus they hold plant nutrients
    through chemical interactions.
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14
Q

S.P - chemistry

A
  • pH of soil, how acidic/basic it is
  • primary nutrients: nitrogen, phosphorus, potassium
  • pH affects nutrients availability for plants (e.g farmers alter the soil pH to suite their needs)
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15
Q

S.P - moisture

A
  • water comes from precipitation.
  • some water flows over surface, some infiltrates the soil
  • water leaves soil through evaporation, transpiration, and leaching (aka percolation)
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16
Q

soil horizon:

A

distinct layers that are different in phys or chem composition, organic content, or structure

  • we follow the canadian system of soil classification CSSC for naming horizons
17
Q

soil horizon

A
  • Horizons develop from the removal or accumulation of chemical compounds, usually by water movement
  • Horizons are separated into organic and mineral groups
18
Q

soil profile: soil pedon: polypedon:

A

the full set of horizions in a location down to its parent material.

a small division of soil column in an area showcasing these properties

area of the same type of soil type, made of many pedons

19
Q

Organic Horizons

A
  • top most layer of the soil profile
  • O horizon
  • formed from material that accumulates from plants and animals (organic material)
    -humus.
20
Q

Mineral Horizons

A
  • A, B, C horizons
  • the roots of plants penetrate and influence A + B horizons.
21
Q

A Horizon

A

Mineral soil at surface where mixed with organic humus
- mineral and humus

22
Q

B Horizon

A

where drained/filtered materials accumulate
- high concentrations of clay located here

23
Q

C Horizon

A
  • weathered rock
  • little to no organic material
  • partially altered parent material
  • above bedrock
24
Q

Ah + Ae Horizons (Mineral horizons)

A
  • Ah, darked coloured organic rich layer where biological activity occurs
  • Ae, light coloured portion where downward eluviation (transport) has removed clay, o.g matter, iron, and aluminum compounds.
  • common subdivision of the uppermost mineral layer
25
soil forming (4) processes
1) enrichment: Addition of (mineral or organic) material to the soil. 2) removal: removal of material (erosion or leaching) from the soil. 3) transformation: chemical change of material within soil. Humification is the decomposition of organic matter to produce humus 4) translocation: The movement of materials upward or downward in the soil profile - Eluviation – downward movement of fine materials (like clays, metal oxides) - Illuviation – accumulation of these fine materials (usually in B horizon)
26
are all soil profiles the same everywhere?
no. Not every soil profile will have all the horizons and subhorizons described. This is due to locations.
27
how many soil classifications are in Canada?
10 soil orders
28
Chernozemic Order
Soil of Canada’s agricultural bread basket; the Prairies Have thick, dark A horizons, rich in organic matter Roots of grasses provide material for decomposition
29
Luvisolic Order
One of 3 forest soil types “The ground under your feet”; the mixed wood plains of Southern Ontario are underlain by luvisols Soils often rich in clays because of geology
30
Podzolic Order
Forest soil associated with coniferous (i.e. needle-bearing) trees Moist, cool climate rapidly breaks down organic matter Percolation of water moves minerals, giving strong Ae horizon
31
Brunisolic Order
Forest soil of cooler, drier locations Associated with sandy, glacial deposits Tend to be somewhat acidic Thick, brown horizon, not as well developed as the podzols (no distinct Ae)
32
Organic Order
Called histosols in other countries Accumulation of organic matter (peat) in water-logged soils Large amount of organic matter (high in carbon) means organic soils are of great interest to climate science!
33
Unclassified areas
Not all of Canada has abundant soils Glacial ice and exposed bedrock occur in many locations across Canada This includes portions of central Ontario dominated by exposed Canadian Shield bedrock