Soil formation

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Last updated 12:26 AM on 6/3/26
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104 Terms

1
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what are the organic soil horizons

L - fresh litter, F - partly decomposed litter, H - well decomposed litter, O - organic horizon containing humus in a damp environment

2
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what are the mineral horizons

A - surface/topsoil,

E- elluviated subsurface, less organic matter, paler colour,

B - subsurface, no rock, illuviation/accumulation,

C - partialy weathered parent material,

R - Rock

3
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what are the 3 soil formation models

Environmental product, soil material flux, dynamic rate model

4
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What is pedology?
The study of soils in their natural environment, including formation, classification, and distribution.
5
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What are the five soil forming factors in CLORPT?
Climate, Organisms, Relief, Parent material, Time.
6
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Which soil forming factor controls weathering and leaching most strongly?
Climate.
7
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What does parent material influence in soils?
Texture, fertility, mineralogy, and weathering rate.
8
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What is a pedon?
The smallest 3D unit that represents a soil.
9
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What is a polypedon?
A group of similar pedons forming a soil unit.
10
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What is the solum?
The weathered and biologically active part of soil including A, E, and B horizons.
11
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What is found in the O horizon?
Organic litter and decomposing material.
12
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What characterises the A horizon?
Mineral soil mixed with organic matter.
13
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What characterises the E horizon?
A pale eluviated horizon depleted in clay, Fe, and Al.
14
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What occurs in the B horizon?
Accumulation (illuviation) of clay, Fe, Al, or organic matter.
15
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What is the C horizon?
Partially weathered parent material.
16
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What is the R horizon?
Unweathered bedrock.
17
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What is eluviation?
The removal of material from an upper horizon.
18
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What is illuviation?
The accumulation of material in a lower horizon.
19
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What process creates an E horizon?
Eluviation.
20
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What is hydrolysis?
A chemical weathering reaction where water breaks down minerals to form clays.
21
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Give an example of hydrolysis.
Feldspar weathering to kaolinite clay.
22
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What is oxidation in soils?
Loss of electrons, commonly Fe²⁺ becoming Fe³⁺.
23
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What colours are associated with oxidation?
Red, yellow, and brown colours.
24
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What is reduction?
Gain of electrons under anaerobic conditions.
25
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What soil conditions favour reduction?
Waterlogged or anaerobic conditions.
26
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What is topdown pedogenesis?
Soil development downward from the surface.
27
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What is upbuilding pedogenesis?
Soil development through addition of new material at the surface.
28
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What is developmental upbuilding?
Thin additions incorporated into the existing soil.
29
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What is retardant upbuilding?
Large additions bury old soils and slow development.
30
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What is the environmental product model?
A model where soil is the product of interacting environmental factors.
31
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What is the dynamic-rate model?
A model recognising soils change progressively or regressively through time.
32
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What is a progressive soil pathway?
Increasing soil development over time.
33
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What is a regressive soil pathway?
Soil simplification caused by erosion or disturbance.
34
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What are additions in soil systems?
Inputs such as organic matter, dust, or volcanic ash.
35
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What are removals in soil systems?
Losses through erosion or leaching.
36
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What are transformations in soil systems?
Changes such as weathering or decomposition.
37
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What are translocations in soil systems?
Movement of material within the soil profile.
38
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How does relief affect soil depth?
Steep slopes generally have shallower soils.
39
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How do organisms influence soil acidity?
Some vegetation, especially conifers, produces acidic litter.
40
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Why are volcanic ash soils often fertile?
They contain reactive minerals and good structure.
41
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How long can soil formation take?
Thousands to tens of thousands of years.
42
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What happens to soils as they age?
They become more weathered and more strongly leached.
43
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44
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What does NZSC stand for?
New Zealand Soil Classification.
45
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What is the purpose of NZSC?
To classify and predict the behaviour of NZ soils.
46
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List the hierarchy of NZSC.
Order, Group, Subgroup, Family, Sibling.
47
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What is a diagnostic horizon?
A horizon used for soil classification.
48
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What does a Bt horizon indicate?
Clay accumulation.
49
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What does a Bh horizon indicate?
Humus accumulation.
50
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What does a Bs horizon indicate?
Fe and Al accumulation.
51
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What does a Bg horizon indicate?
Gleying/reducing conditions.
52
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What is a lithologic discontinuity?
A boundary between different parent materials.
53
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How are lithologic discontinuities shown?
Using prefixes such as 2Bw or 2Cu.
54
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What are Allophanic soils associated with?
Volcanic ash and allophane minerals.
55
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Name key features of Allophanic soils.
Low bulk density, high P retention, excellent structure.
56
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What are Gley soils?
Soils affected by prolonged saturation and reducing conditions.
57
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What are Podzol soils?
Strongly leached acidic soils with E and Bh/Bs horizons.
58
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What are Granular soils?
Strongly weathered clay-rich soils with granular structure.
59
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What does ā€œOrthicā€ mean in NZSC?
Typical or common expression of a soil.
60
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What does ā€œTypicā€ mean in NZSC?
Default subgroup lacking special features.
61
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What are soil families based on?
Texture, permeability, mineralogy, and profile material.
62
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What are soil siblings used for?
Detailed land management distinctions.
63
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What properties define siblings?
Depth, drainage, texture, stoniness, and functional horizons.
64
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What are functional horizons used for?
Predicting soil behaviour such as drainage and rooting.
65
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What is the main clay mineral in allophanic soils?
Allophane.
66
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What is the Horotiu soil?
A Typic Orthic Allophanic Soil.
67
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What are characteristics of Horotiu soil?
Well drained, volcanic ash derived, highly productive.
68
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What is Te Kowhai soil?
A Typic Orthic Gley Soil.
69
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What are features of Te Kowhai soil?
Grey colours, poor drainage, reducing conditions.
70
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Why are diagnostic horizons important?
They indicate pedogenic processes and aid classification.
71
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What is the benefit of NZSC?
It reflects NZ-specific soil conditions and processes.
72
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Why are soil siblings useful?
They help guide land use and management decisions.
73
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74
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What is leaching?
The downward movement of dissolved ions through soil.
75
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Which ions are commonly leached?
Ca²⁺, Mg²⁺, Na⁺, and K⁺.
76
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What causes increasing soil acidity during leaching?
Loss of base cations and replacement by H⁺ and Al³⁺.
77
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What is ionic potential?
Ionic charge divided by ionic radius.
78
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Which ions are most easily leached?
Ions with low ionic potential.
79
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Name two easily leached ions.
K⁺ and Na⁺.
80
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Name two less mobile ions.
Fe³⁺ and Al³⁺.
81
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What is base cycling?
Nutrient recycling through vegetation and litter decomposition.
82
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Which vegetation type promotes strongest base cycling?
Grasslands.
83
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Which vegetation type promotes strong acidification?
Coniferous forests.
84
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What is podzolisation?
Movement of Fe, Al, and organic matter downward under strong leaching.
85
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What horizon is characteristic of podzolisation?
E horizon.
86
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What does ā€œPodzolā€ mean?
ā€œAshes underneath.ā€
87
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What horizons define Podzol soils?
Bh and/or Bs horizons.
88
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What is a Bh horizon?
A humus-rich illuvial horizon.
89
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What is a Bs horizon?
A horizon enriched in Fe and Al oxides.
90
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What conditions favour podzolisation?
Acidic, humid, free-draining conditions.
91
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What vegetation commonly promotes podzolisation?
Conifers and kauri.
92
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What is allophane?
A nanocrystalline aluminosilicate mineral.
93
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What is ferrihydrite?
An Fe oxide mineral.
94
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What is gibbsite?
An aluminium hydroxide mineral.
95
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What causes the pale colour of E horizons?
Strong eluviation of Fe, Al, and OM.
96
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What is a humus pan?
A cemented Bh horizon.
97
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What is ortstein?
A cemented Bs horizon.
98
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Why are podzol boundaries often sharp?
Limited biological mixing due to acidity.
99
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What type of parent material commonly develops podzols?
Sandy or coarse-textured parent material.
100
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What process often accompanies podzolisation?
Argillisation.