Lecture 2: Soil habitat Flashcards

1
Q

Soil formation (Dokuchaev equation)

A

soil=f(cl,o,r,p,t,…)tr
climate, organisms, parent material, relief, relative time

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2
Q

What is pedogenesis

A

exposed rock formes soil

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3
Q

what is weathering

A

degradation of material by chemical/physical processes accelerated by orgniams

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4
Q

newly developed soil layer

A

lithosol/entisol/rudisol

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5
Q

Over time formation of forst soil

A

colonisation of thin litter layer by lichens, mosses, liverworts
lithosol formed with shrubs increasing litter layer and weathering
deciduous forests alter parent material

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6
Q

rock cycle

A

magma forms igneous rock through crystallisation
exposed to weathering
form sedimentary rocks via erosion
heat and pressure make metamorphic rocks

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7
Q

igenous rocks

A

granite, basalt, gabbro

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8
Q

sedimentary rocks

A

limestone, sandstone, shale

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9
Q

metamorphic rocks

A

marble, slate, quartzite

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10
Q

weathering rind

A

biological processes occurring here with mycorrhizae helping

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11
Q

Soil horizons

A

litter
organic (O)
surface (A)
subsoil (B)
substratum (C)
bedrock (R)

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12
Q

what is O horizon

A

organic material with lots of humus

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13
Q

what is A horizon

A

OM accumulates and leaches

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14
Q

what is B horizon

A

deposited minerals and metal salts with less OM

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15
Q

what is C horizon

A

partly weathered parent material

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16
Q

what is R horizon

A

un-weathered parent material

17
Q

soil composition

A

mostly mineral matter
water
air
less than 5% OM

18
Q

mineral basis of soils

A

clay (smallest particles)
silt
sand
gravel (largest particles)

19
Q

soil textural classes

A

form a triangle of clay, silt, sand %

20
Q

why is soil texture important

A

helps define suitability for agriculture

21
Q

what is clay-rich soil good for

A

water and nutrient retention

22
Q

what are sandy soils good for

A

drainage

23
Q

what are heavy soils

A

how hard to get plough through
insulators

24
Q

minerals

A

solid chemical compounds

25
Q

primary rock minerals

A

silicates

26
Q

valency

A

fill up from outside shells
2,8,8 shells

27
Q

hydrogen bonds

A

covalent hydrogen atoms bind to electronegative atoms
quite strong

28
Q

silicates

A

silicon tetrahedrons

29
Q

what type of silicates do soils have

A

phyllosilicates

30
Q

what are phyllosilicates

A

2D mineral sheets of tetrahedrons/octrahedrons
3D covalently bonded combos of layers

31
Q

sheet

A

combinations of planes of atoms (silica in tetrahedral sheet)

32
Q

layer

A

combinations of sheets (MICA, two silica sheets and alumina sheet)

33
Q

crystal

A

stacks of layers

34
Q

interlayer space importance

A

fillied with ions, water, etc. and determines soil properties

35
Q

kaolinite crystal

A

little interlayer space so little water in

36
Q

muscovite crystal

A

covalent sandwich bonds
potassium ions weak bonds
can split sandwiches easily

37
Q

chlorite crystal

A

strong bonds
low interlayer space