Unit 5.1: soils Flashcards

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1
Q

what is biogeography?

A

study of geography of life and how it changes through space and time.

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2
Q

what is the biosphere?

A

the focus of biogeography. between the lithosphere and the atmosphere.

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3
Q

what is the biosphere divided in?

A
  1. soil material that is used by flora

2. the distribution of flora and fauna

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4
Q

what is pedogenesis?

A

the process of soil formation: weathering of rocks, activities of organisms, movement of rainwater, time.

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5
Q

what is pedology?

A

study of the origin, classification, distribution, and description of soil

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6
Q

what is soil?

A

uppermost portion of regolith and has been modified by organisms. also influenced by atmosphere, hydrosphere, and lithosphere.

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7
Q

what are two characteristics of soil?

A
  • forms slowly and is easily destroyed.

- most of life on Earth depends on it

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8
Q

what is bedrock?

A

rock that is structurally part of and connected to earths crust. no weathering or erosion

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9
Q

what is regolith?

A

loose earth material that covers bedrock

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10
Q

what is soil composed of?

A
  1. Minerals: inorganic material from rock; supply nutrients to green plants (sand, silt, clay)
  2. organic material: paint and animal matter; releases nutrients into the soil or combines with mineral particles.
  3. water
  4. air
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11
Q

what are horizons?

A

horizontal zones in the soil column with various characteristics

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12
Q

what are the various horizons?

A

O horizon: (Humus) organic horizon, topmost layer composed mostly of organic matter

A horizon: (topsoil) rich in organic material; where most plants roots are, dark in colour

E horizon: (transition) lighter in colour and formed from elevation and leaching

B horizon: (subsoil) formed by illuviation or deposition of leached material

C horizon: (weathered bedrock) no or limited amount of organic material; lower boundary of true soil

R horizon: (solid bedrock) mostly solid, unweathered bedrock

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13
Q

what is elevation?

A

water carries soil particles and weathered material down the soil column

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14
Q

what is leaching?

A

movement of dissolved material downward by rainwater

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15
Q

what is illuviation?

A

deposition of weathered material deeper in soil

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16
Q

soil horizons can be defined by what characteristics?

A
  1. soil texture
  2. soil structure
  3. soil colour
17
Q

how does soil texture affect soil horizons?

A

the size of particles in soil affect the permeability of water. there’s clay (

18
Q

what is loam?

A

soil that contains 20% clay, 40% silt, 40% sand, and lots of organic material

19
Q

in terms of soil structure, what are the 4 basic structures of the grain?

A
  • Platy structure: layered soil particles that look like flakes stacked horizontally.
  • prismatic structure: soil particles arranged in columns giving soil vertical strength.
  • blocky structure: irregularly shaped soil particles
  • spheroidal structure: soil parts are very small and nearly round in shape
20
Q

what do various soil colours mean?

A
  • dark brown/ black: high presence of organic matter (in temperate grasslands)
  • red: indicates strong chemical weathering, iron and oxidation (tropical rainforest)
  • grey: indicates heavy leaching (boreal forest)
21
Q

where does soil develop fastest?

A

where chemical weathering predominates.

22
Q

what factors control the rate of soil formation?

A
  • parent material: the original bedrock that the soil is formed from. hard material will take longer to develop
  • climate: temperature and precipitaiton controls amount of weathering and the breaking down of bedrock and regolith into soil particles.
  • topography: slope of bedrock or environment will affect the soil formation. a steep slope will typically not have thick soil layer due to mass movement.
  • plants and animals: flora & fauna will not affect uptake of material in the soil, but will add to organic material as they die.
  • time: soil particles require a long time to form
23
Q

what factors of soil formation are active and what are passive?

A

active; climate and plants/animals because they supply energy

passive: parent material, topography, and time because they receive energy..