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

23
Q

what are heavy soils

A

how hard to get plough through
insulators

24
Q

minerals

A

solid chemical compounds

25
primary rock minerals
silicates
26
valency
fill up from outside shells 2,8,8 shells
27
hydrogen bonds
covalent hydrogen atoms bind to electronegative atoms quite strong
28
silicates
silicon tetrahedrons
29
what type of silicates do soils have
phyllosilicates
30
what are phyllosilicates
2D mineral sheets of tetrahedrons/octrahedrons 3D covalently bonded combos of layers
31
sheet
combinations of planes of atoms (silica in tetrahedral sheet)
32
layer
combinations of sheets (MICA, two silica sheets and alumina sheet)
33
crystal
stacks of layers
34
interlayer space importance
fillied with ions, water, etc. and determines soil properties
35
kaolinite crystal
little interlayer space so little water in
36
muscovite crystal
covalent sandwich bonds potassium ions weak bonds can split sandwiches easily
37
chlorite crystal
strong bonds low interlayer space