lecture 6 Flashcards

Soils

1
Q

2 concept of soil?

A

Pedological concept and Edaphological concept

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2
Q

A natural body differentiated into horizon of mineral and organic constituent, consolidated of variable depth. Differs from the parent material below in morphology, physical properties and constitution

A

Pedological concept

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3
Q

A natural body, synthesized in profile form from a variable mixture of broken and weathered minerals and decaying organic matters, which covers the earth in a thin layer and which supplies when containing the proper amounts of air and water, mechanical support and in part sustenance for plants

A

Edaphological concept

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4
Q

Functions of soils

A

media for plant growth
modify the atmosphere through emission and absorption of gases
Habitat for animals that live in the soil
process recycled nutrients

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5
Q

Mineral horizon, finer textured, usually clayey with blocky structure
zone of maximum illuviation (movement of materials - Clay and AI oxides into the horizon

A

B horizon

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6
Q

Reffered to as the parent material, blocky to primatic structure, hard and sometime brittle but can still be dug by digging tools

A

C HORIZON

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7
Q

d

A

dense unconsolidated materials/physical root rstric

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7
Q

co

A

coprogenous earth

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7
Q

i

A

Organic matter, slightly decomposed

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7
Q

j

A

Jarosite

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7
Q

jj

A

Cryoturbation

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8
Q

k

A

accumulation of carbonates

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9
Q

kk

A

engulfment of horizon by secondary carbonates

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10
Q

m

A

cementation or induration

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11
Q

ma

A

marl

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12
Q

n

A

accumulation of sodium

13
Q

o

A

accumulation of Fe and AI oxides

14
Q

P

A

plowing

15
Q

q

A

accumulation of silica

16
Q

r

A

weathered os soft bedrock

17
Q

solum

A

horizon a and b

18
Q

regolith

A

horizon a, e, b and c

19
Q

0 to 20 cm depth (plow layer)

A

top soil

20
Q

soil beneath the topsoil (below20 cm depth)

A

subsoil

21
Q

how soil formed

A

addition, transformation, transfer, losses

22
Q

factors of soil formation

A

Climate, Organisms, Relief, Parent material and Time

23
Q

Temperature and rainfall are the most critical both affect the rate of soil processes weathering and decomposition, also impacts the type of vegetation in area

A

climate

24
Q

includes plants and animals from micro to macro: Grassland vs. forest vegetation, alter physical properties of soil like pore spaces

A

organism

25
Q

Includes elevation, slope, aspect or exposure, affects stability of land surface for other soil-forming factors and processes to initiate and continue soil formationm

A

relief

26
Q

has a great influence on the resulting property of the soil

A

Parent material

26
Q

Types of parent material

A

A. Sedentary
Rocks - Igneous/ Sedimentary/ Metamorphic
B. Transported
Gravity - Colluvium
Water - Alluvium (river),
Ice - Glacial
Wind

27
Q

determines the duration the parent material was subjected to the other soil-forming factors, the longer the time, under stable conditions, the more developed and old the soil,

A

time

28
Q
A