the “master” horizons o a e b c r organic horizon on the soil surface surface horizon high in...

Post on 21-Dec-2015

249 Views

Category:

Documents

0 Downloads

Preview:

Click to see full reader

TRANSCRIPT

The “Master” horizons

• O

• A

• E

• B

• C

• R

organic horizon on the soil surface

surface horizon high in organic matter, but composed of mineral soil – eluviation zone

subsurf. horizon light in color due to leaching – eluviation zone

subsurf horizon, from soil forming processes – illuviation zone

least weathered (and deepest) of all the soil horizons – from R or transported inbedrock

Subscripts: Processes occurring in these Horizons

O horizon

• Oi

• Oe

• Oa

A horizon

• Ap

• Ab

identifiable (recognizable) materialIntermediate

highly decomposed (almost all gone)

plowed surface

buried surface

More Subscripts

B horizons

• t

• g

• k

• s

• h

• w

• o

clay

“gleying” (very wet)

carbonates (dry regions)

“histic” humus (high organic content)

sesquioxides (iron, aluminum, red/yellow)

“cambic” – weakly altered by removal & chem rx, no illuviation

“oxic” highly wx’d, tropical soils (Fe, Al oxides, red)

Last One (whew) and Rules• C horizon

– r (weathered bedrock)– k (carbonates)– u (transported-in PM: unweathered)– ox (transported-in PM: weathered (“oxidized”)

• Subscript Rules– rarely use more than three– t (almost) always first

Examples: Btg, Cr, Bw, Ap, . . .

Types of Parent Material - Mode of transport

Type of P.M. Mode of transport Degree of sorting by size

Glacial till

Alluvium

Colluvium

Loess

Lacustrine

Residuum

Ice Low (all sizes)

Stream/river High (coarse dropped 1st)

Gravity Low

Ice + wind High (silt only)

Water (lakes) High

None NA

Effect of Parent Material on Soil Formation – Transported PM

Eolian sand

40cm

A

C 1m

Mixed alluvium

A

C

Bw

Effect of Parent Material on Soil Formation - Residuum

1.5m

Residual shale

A

AB

C

Bt1

Bt2

Granite

40cm

A

Bw

C

Influence of climate on soil pH

High (basic)

Low (acidic)

Why?

• Base cations soluble• Water = biomass (acids)

Influence of climate on Soil Organic Matter

Cold = low inputs

Hot= rapid losses

Influence of climate on Clay Formation

So where find the soil with more clay, Alabama, or Nevada?

Influence of climate on Carbonate Layer Depth

i.e., near surface

Depth

top related