Soils Exam 1 Flashcards
(40 cards)
Pedon
A 1X1X1.5 M DEEP UNIT OF SOILIS REFFERED AS A PEDON.
Regolith
Volume of soil between surface and bedrock
Soil functions
- Supports plant life in our biosphere
- Harbors thousands of types of saprophytes (organisms that eat or decompose dead organisms)
- Serves as foundations for homes, industries and highways
- Absorbs harmful contaminants from surface h20
- Filters pathogens/parasites from waste water
Four ways soils support plant life
- Anchor plant roots
- Supply water for plan roots
- Supply air for plant roots
- Furnish roots for plant growth
- Release water with low levels of nutrients
Types of rocks
- Igneous Rocks
- metamorphic rocks
- Sedimentary rocks
Rocks
Collection of minerals
Hydrologic Cycle
Breaks rocks to form soils
Rock + Rain=
The current landscape+soil
Five hills lope position
Summit Shoulder Back slope Foot slope Toe slope
Soil forming processes
- Losses(erosion)
- Additions(deposition)
- Translocation
- Transformation
Soil forming factors
- Parent material
- Topography
- Climate
- Time
- Organisms
Different types of parent materials
- Alluvium-water-river-flood plains
- Colluvium-gravity-foot slope
- Lacustrine-water-lakes-dried up lake beds
- Aeolian-wind-wind blown deposits
- Marine-ocean-exposed ocean deposits
- Glacial till-retreating glaciers-broad glacial plains
- Glacial outwash-melt water from glaciers-areas with in glacial areas
Soil Horizons
- surface
- topsoil
- subsoil
- substratum
- bed rock
Texture
Soils containing large amounts of sand exhibit little plasticity and cannot retain large amounts of water or nutrients. They have large voids (macropores) that readily transport water and air.
Mineral fraction of soils
Sand Silt Clay
Diameter of particles
0.05-2 mm 0.002-0.05 mm <0.002 mm
Soil Color
Useful tool for providing information about other soil properties Organic matter content Soil minerals Seasonal high water tables
Structure
The arrangement of primary soil particles into compound particles or aggregates. The type and grade of structure plays an important role in the movement of water within soils.
Minerals particles having an average diameter>2mmare termed gravel..
and are not used to calculate soil texture
NOT TRUE ABOUT TEXTURAL CLASSES
They are closely related to its color
There are 11
They are related to structure
Dull-gray coloration of an iron-rich mineral soil profile, particularly with increasing depth, indicates
saturation or seasonal water table
The hue of a soil is considered non-existent, and denoted as N, when the:
Chroma is 0
Soil color can be highly indicative of:
- OM content, parent material, and/or degree of seasonal saturation (drainage)
B) Sand content, parent material, and/or calcium content
C) Soil fertility (namely base saturation)
D) OM content and nematode infestation
E) Horizon depth and load-bearing capacity
F) Sand content and shrink-swell characteristics
Redox depletions, localized pockets of soil where anaerobic conditions persist, take on a ‘gley’ color in which chroma is low (less than or equal to 2) and value is typically:
greater than or equal to 4
Which type of soil structure is common in soil horizons dominated by shrinking-swelling clays?
Wedge