horizons Flashcards

1
Q

soil horizons are…

A
  • distinct layers formed by pedogenic processes
  • distinct differences in:
    • OM
    • color
    • sand/clay %
    • chemical composition
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2
Q

O horizon

A
  • OM: but can be different types
  • fresh litter & well-decomp’d humus
  • usually above mineral soil (forest)
  • common and very deep in wetlands
  • seldom found in grasslands
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3
Q

A horizon

A
  • surface mineral horizon, darkened by OM
  • may have properties from cultivation
  • usually more fertile
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4
Q

E horizon

A
  • Eluviated mineral hzn where dominant feature is a LOSS of clay, iron, aluminium, OM, etc
  • loss is due to leaching (causing a gray/white color)
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5
Q

B horizon

A
  • mineral hzn w/ either or both:
    • illuvial increase in clay, Fe, Al, OM… from above (E)
    • substantial alteration of original parent material that eliminated rock structure, forms clay or oxides (giving color)
  • orangish, yellowish, greyish
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6
Q

C horizon

A
  • mineral hzn that has little alteration of original PM
  • lacks properties of AEB hzns
  • lies outside of most biological activity
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7
Q

R

A
  • rock material
  • _not_ a horizon
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8
Q

L horizon

A
  • limnic material, uncommon (but occ. in PacNW)
  • lake deposits
  • full of diatoms, clay, OM
  • @ bottom of wetlands
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9
Q

transition hzns

A
  • transition btwn 2 masters
  • dominant hzn listed first:
    • BC: smooth transition w/ B dominant
    • A/B: interfingered w/ A dominant
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10
Q

subordinate O hzn designations

A
  • Oi: little decomp, OM still recognizable
    • i = fibric
  • Oe: intermediate
    • e = hemic
  • Oa: highly decomp’d, OM not recognizable
    • a = sapric = saprophyte
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11
Q

Ap

A

plowed; structural change

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12
Q

subord: t

A

accumulation of silicate clays (Bt)

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13
Q

subord: k

A

accum. of carbonate (Bk, Ck)

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14
Q

subord: s

A
  • illuvial accum. of sesquioxides (Fe/Al)
  • orange-reddish color
  • (Bs), illuvial
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15
Q

subord: h

A
  • accum. of humified OM (well decomp’d)
  • Bh, Bhs, illuvial
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16
Q

subord: g

A
  • gleying, waterlogging, anaerobic, wet soil
  • loss of O2 makes Fe grey/mottled
  • Bg, Cg
17
Q

subord: w

A
  • some development of color/clumps, but not well developed
  • Bw
  • *** B always gets a subord, so Bw if nothing else is special about it
18
Q

subord: b

A
  • buried
  • Ab (an A under other O, A, & B)
19
Q

subord: o

A
  • accumulation of Fe/Al oxides (Bo) (but not OM)
  • formed in place (not illuvial)
20
Q
A