Soils NR 200 - Modesto Junior College

Document technical information

Format ppt
Size 1.3 MB
First found May 22, 2018

Document content analysis

Category Also themed
Language
English
Type
not defined
Concepts
no text concepts found

Persons

Organizations

Places

Transcript

Soils NR 200
Unit 2
Formation of Soils
From Parent Materials
SOIL FORMING FACTORS
A. Parent Material origins
1) Igneous rock – ¼ of the earth’s surface
solidification of molten rock
a) Granite - intrusive
i. Quartz – weathers to form sand
ii. Feldspar biotite – form clays
b) Basalt - extrusive
2) Sedimentary Rocks – a great majority of the
earth’s surface, readily breaks down into soil.
Consolidation by silicates and carbonates
cementing together.
a) Limestone - organic marine animal
formation
b) Sandstone
3) Metamorphic – rock that is heated under
pressure and changes-generally resists weathering.
a) Marble
b) Slate
c) Gneiss
d) Talc- which is ground into powder.
e) Graphite- used in pencils and lubricants.
f) Serpentinite
14- Rocky Mountain
region all rock types
15- Mostly igneous rocks
loess in river basins
16- Great Basin gravels,
sands alluvial fans
igneous and sedimentary
rocks
18. Sierra and
Cascade mountains –
Igneous
19. Mostly
Sedimentary
20. Glacial sediments
21. Great Valley –
alluvial fans
B. Climate
1) Heat
2) Water
3) Freezing
C. Biota (Living Organisms)
1) Plants
* Accumulation can form peat bogs, Moss
Peat, Herbaceous peat, Woody peat and
sedimentary peat
2) Micro-organisms
* Animals turning the soil - pedoturbation
3) Macro-organisms
How organic
mater is formed
and the
accumulation of
the material to
form peat bogs.
D. Topography
1) Moving soil by water and gravity
2) Low – accumulate salts, if saturated then reduced
om degradation
3) Steep areas are never allowed to develop the soil
profile as the unconsolidated material leaves the
site.
E. Time - allowing for the other factors to affect
the soil.
Soil transportation modes.
If not transported, Residual
a) Glacial Ice - Moraine
b) Wind – Eolian
c) Water –
Stream –Alluvial
Lake - Lacustrine
Oceans - Marine
d) Gravity – Colluvium
A qualifier thapto- indicates the presence of a buried soil or
a buried horizon. This would be the case if a soil has a
surface mantel of new material that is 50 cm thick or more.
The surface mantel is named in the normal way (e.g. as a
Regosol, Andosol or Arenosol) and the buried soil would be
classified with a prefix qualifier `thapto-`.
If the surface mantle is less than 50 cm thick, it is ignored
in the soil name but the soil may be marked on the soil
map by a phase indicator.
2) Soil Formation processes
a)Transformations
i) The physical and chemical changes that
occur in the soil
- Degradation of minerals while forming
silicate clays
- Degradation of OM and formation of
humus and organic acids
- Also the changing of aggregates
b) Translocations
i) Movement of materials by water downward when in
abundance and upwards when the absence of surface
water.
c) Additions
i) OM
ii) Fine particles wind deposition
d) Loss
i) Leaching
ii) Erosion
iii) OM
3) Soil Profile
a) O- organic layer
i) How is this formed??
ii) Sub classes i and a
b) A- topsoil – the most productive soil
i) With the addition of the acids from the higher
organic material leaching of the easily soluble
compounds calcium, calcite and gypsum will move
down into the lower horizons of the profile as far as
the water penetration will carry them.
ii) p -
c) E – an area where the greatest eluvation (removal of
clay, iron and OM) occurs, resistant materials such as
quartz, sand and silts remain usually light in color.
d) B – sub soil or zone of accumulation, illuviation usual location of hardpan
i) Where clay and/or silt concentration will increase
from transformation of particles weathering and
moving down.
ii) m - cemented zone usually silicates or calcium
iii) g - strong gleying
e) C – Parent material
but broken down but not
subject to the soil
forming properties as the
above solum (A&B) and
not massive in structure
as R
f) R- Rock
The subscript notes for each horizon and their meaning.
×

Report this document