Lesson 1: Introduction to Soils Flashcards
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