Factors of Soil Formation Flashcards

(37 cards)

1
Q

What are PM weathering rates determined by?

A

Mineralogy, hardness, porosity, surface area(faster) or finer grains(water retention)

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2
Q

Solum

A

These are the surface and subsoil layers that have undergone same soil-forming conditions

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3
Q

Example of soil created by PM…

A

Quartz sand doesn’t create clay soils due to no Al

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4
Q

PM soil formation with igneous rocks…

A

Form abundant clay minerals with high fertility due to cations and building block

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5
Q

Example of materials determining weathering rates…

A

Granite contains mostly quartz and K feldspars, less quartz and more Na and Ca feldspars are mafic

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6
Q

What do sedimentary rocks depend on?

A

Formation fpressure, composiion of original deposit, sandstone orignates from sand-size sediment

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7
Q

Why are transported soils more productive?

A

Higher porosity

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8
Q

How does wind sort particles?

A

Drops largest particles newar source, carrying smaller larger distances

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9
Q

Loess

A

Terrestrial clastic sediment composed predominantly of silt-size particles formed by accumulation of wind-blown dust

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10
Q

Ice/Water particle distribution…

A

Glacial till and glaciations

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11
Q

Colluvium

A

This is soil and debris that accumulate at the base of a slope by mass wasting or sheet erosion

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12
Q

Climate variability in soil formation….

A

Precipitation/temperature most important, varying depending on elevation/latitude, yearly also

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13
Q

Cool humid climate soil characteristicis…

A

High OM accumulation, weathering products removal and dominant acidification

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14
Q

Arid-semiarid climate soil characteristics…

A

Evapotranspiration exceeds precipitation, OM accumulates more slowly, with rapid soluble salt and carbonate accumulation

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15
Q

What is regional climate characterised by?

A

Mean annual temperature and precipitation

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16
Q

Results of poor drainage or high water table?

A

Dominant redox reactions and gleying

17
Q

Temperature influence on sois…

A

Increases clay formation, clay type then influenced by climate: smectite found in drier climates than kaolinite

18
Q

Example of topgoraphy improtance?

A

Slope length and angle determine effective precipitation

19
Q

How slope influences soil?

A

Soil development(pedon thickness and horizon differentation) decreases with slope with increasing erosion

20
Q

How do slopes differ per hemisphere?

A

NH north faceing slopes colder due to less incident solar radiation

21
Q

How do plants add OM?

A

Root exudates, ell death with root growth and death/degradation

22
Q

How does OM influence soil formation?

A

Produce compounds that chelate cations and humus production

23
Q

How does canopy interception influence soils?

A

Rainfall assimialtes dissolved ions in crown drip, reacting with soil solid phase differently than pure water

24
Q

Hans Jenny equation?

A

S = f(Pm, C, R, B, T)

25
Example of climate and time syngerism...
Calcaerous rock with moderate rainfall may have increased OM early, approaching equilibrium in few decades, whilst calcite and lcay take longer for steady levels for vegeatation
26
Hydrolysis
H+ in H2O replacement, like clay mineral feldspar releasing K and adding H, accelearting weathering
27
What can released K ion replaced by H+ do?
Form new complexes, cationic exhcnage, plant use, soil leeching
28
What does hyrdolysis increase with?
OM decomposition, nutrient uptake, nitrification and S oxidation, as pH lowers with increasing H+
29
How does hydration differ from hyrdolysis?
Water does not dissociate, expanding minerals and increasing weathering susceptibility
30
Where are redox reactions most important?
Fe2 oxidation to Fe3 which strains crystals and accelerates weathering rate
31
How do redox reactions influence solubility?
Some cations more mobile when reduced than when oxidised
32
What are the two horizon groups?
Master Horizons - AOEBCR Transitional Horizons
33
A Horizon
Surface layer with high bio-activity thus high humus accumulation, mineral weathering, soluble product leaching and eluviation
34
Eluviation
This is the sideways or downards movement of dissolved or suspended material within soil caused by rainfall
35
O Horizon
Predominanntly organic matter
36
E Horizons
Eluviation influenced by organic acid from A/O horizons combination with leaching waters that weather/translocate silicate clays, fe and al, leaving residual material
37