horizons Flashcards
1
Q
soil horizons are…
A
- distinct layers formed by pedogenic processes
- distinct differences in:
- OM
- color
- sand/clay %
- chemical composition
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
3
Q
A horizon
A
- surface mineral horizon, darkened by OM
- may have properties from cultivation
- usually more fertile
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)
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
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
7
Q
R
A
- rock material
- _not_ a horizon
8
Q
L horizon
A
- limnic material, uncommon (but occ. in PacNW)
- lake deposits
- full of diatoms, clay, OM
- @ bottom of wetlands
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
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
11
Q
Ap
A
plowed; structural change
12
Q
subord: t
A
accumulation of silicate clays (Bt)
13
Q
subord: k
A
accum. of carbonate (Bk, Ck)
14
Q
subord: s
A
- illuvial accum. of sesquioxides (Fe/Al)
- orange-reddish color
- (Bs), illuvial
15
Q
subord: h
A
- accum. of humified OM (well decomp’d)
- Bh, Bhs, illuvial