Lesson 2: Introduction to Soils Flashcards
(35 cards)
soil
“the unconsolidated mineral or organic material on the immediate surface of the earth that serves as a natural medium for the growth of land plants.”
unconsolidated materials
loose materials composed of multiple units (e.g., sand, gravel, etc.) unlike hard, massive materials like rock
soil composition (well-managed)
usually around 50% percent of the soil’s volume is composed of solid particles (i.e. decomposed rocks or sediments), with 1-5% being organic matter
the other 50% is empty space, i.e. “pores” (25% water, 25% air)
organic matter
the live organisms in the soil, and plant, animal, and microbial residues in various stages of decomposition
five soil-forming factors
factors that cause variation in soils in different locations
- Parent material (i.e. starting material for a soil)
- Climate (precipitation, temperature, wind)
- Topography
- Biological organisms
- Time
horizons
In naturally formed soils, distinct layers develop. They may blend together gradually or have abrupt borders between layers, and are identified by letter codes.
A horizon
“topsoil”
The A horizon is usually the surface horizon. This is an area of high biological activity with the greatest organic matter content. It is also a zone of leaching. Most plant roots are found in the A horizon.
B horizon
“subsoil”
This layer usually contains less organic matter than the surface layer but accumulates the dissolved materials leached from the A horizon (clays, iron oxides, aluminum, and dissolved organic compounds). For this reason, the B horizon typically contains more clay than the surface layer.
C horizon
The C horizon contains unconsolidated material that has been minimally affected by the soil forming factors, and may or may not be the same as the parent material from which the soil formed.
landscape soils
“urban” soils
soils that are found in a typical neighborhood community around homes, parks, schools, offices, parking lots, and buildings
In compacted landscape soils, the horizons are scrambled and not defined, organic content is low, and air and water movement is reduced.
texture
the size of the particles that make up the soil (e.g., sand, silt, clay)
sand
the largest particle size and feels gritty
silt
moderate in size with a smooth or floury texture
clay
the smallest sized particle and feels sticky
loam
a soil with a combination of sand, silt, and clay sized particles
soil structure
structure refers to how the various particles of sand, silt, and clay fit together, creating pore spaces of various sizes
aggregates
chemical and biological processes that glue sand, silt, and clay particles together
soil microorganisms including mycorrhizae, earthworms, and plant roots help created aggregates
granular structure
common in the upper layer of undisturbed native soils, rapid drainage
block structure
common in the lower layers undisturbed native soils, rapid to moderate drainage
platy structure
common in soils high in clay, slow to no drainage
peds
describes the soil’s individual aggregates or clods
pore space
controls soil drainage characteristics
large pores
water moves rapidly down through the soil profile, common in sandy soils
pose environmental hazards due to rapid leaching
small pores
water is slow to move or may not move at all, common in compacted soil and soils with greater than 20% clay content
easily waterlog