L13 - Soil forming processes Flashcards

1
Q

When is soil formation fastest?

A

Warm, rainy summers in sedimentary rocks

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2
Q

Where is soil formation slowest?

A

Arid, cold climates in igneous and metamorphic rocks

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3
Q

Main soil forming processes?

A
  1. Additions
  2. Losses
  3. Transformations
  4. Transfers
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4
Q

Name a rock with a low albedo and high albedo?

A

Basalt has a low albedo, low heat capacity and low thermal conductivity (surface temp very high). Chalk has a high albedo, high heat capacity and high thermal conductivity (more temperature distribution)

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5
Q

Unloading

A

Breaking up when erosion removes the pressure on underlying rocks

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6
Q

Thermal weathering (thermoclasty)

A

results from low and high variable thermal conductivity of minerals and rocks

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7
Q

Gelifraction (freeze-thaw)

A

occurs when water in rock pores, joints and cracks freezes, expands by 9% and thus breaks rock.

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8
Q

What is the loss of solutes and suspended material related to?

A

Precipitation frequency, intensity and surplus

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9
Q

Leaching

A

organic and inorganic solutes are transported by percolating water

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10
Q

Where does CO2 in soil come from?

A

respiration

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11
Q

Where do H+ ions in soil come from?

A

Leaching from humus (organic acids) and cation exchange

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12
Q

Hydrolysis

A

when acid rain reacts with rock-forming minerals such as feldspar to produce clay and salts which are removed in solution

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13
Q

Weathering index

A

comparison between a chemical compound or mineral that is relatively stable with one that is readily removed by weathering

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14
Q

What is the main source of electrons in soil?

A

Organic material

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15
Q

Gley soils

A

caused by seasonal dynamics in soil water saturation. These soils have mottles (irregular arrangement of spots or patches of colour - cutans) from movement of iron and manganese by redox processes.

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16
Q

What are some chelating agents?

A

Polyphenolics (occur in plants and leach from leaves) and humic and fulvic acids (leach from litter)

17
Q

Podzolization

A

occurs in temperate climates which are warm enough to support vegetation growth, but cold enough to limit rapid decomposition. There must also be high levels of rainfall. In this way, clay minerals are dissolved and transported down the soil profile through leaching and cheluviation, and OM builds up to create acidic conditions.

18
Q

Why is the E horizon bleached in podzols?

A

Due to organic acids e.g. carbonic, lactic and fulvic.

19
Q

Mechanical sieve effect

A

depends on size of transported material and pore sizes in deep soil. Chemical changes lead to lower solubility or suspension (peptisation) with precipitation as a result - increased pH