7B Flashcards
It is a product of weathering processes and a medium capable of supporting plant
growth
Soil
Refers to the proportion of particles that fall into each of the three size rangers, namely
clay, silt, and sand
Soil Texture
A semi non-renewable resource since it takes a long time for water and nutrients to
accumulate inside it
soil
Partially decayed organic matter in soil, critical to soil fertility
humus
Is a diagram which helps identify the type of soil based on its composition
Soil Texture Triangle
The mixture of these two soil types makes it ideal for water and air to pass through it due to the big pore spaces.
Sand and Silt
4 Main Characteristics of Soil
- Soil Depth
- Soil Texture
- Soil Structure
- Organic Matter
Thickness of a soil from the surface to a root-limiting layer such as bedrock or seasonal water table
Soil Depth
The relative amount of sand, silt, and clay in each soil. Affects more specific characteristics like porosity, drainage, and permeability
Soil Texture
The shape and size of soil aggregates. Influences the size distribution of pores in
the soil
Soil Structure
Amount of organic matter within a soil. Effects more specific characteristics and is affected by soil management
Organic Matter
The sequence of soil horizons from the surface down to the underlying bedrock
Soil Profile
One of the succession of zones or layers within a soil profile, each with distinct physical, chemical, and biological characteristics
Soil Horizon
Soil Horizon enumerate
- O horizon
- A horizon
- E horizon
- B horizon
- C horizon
- R horizon
contains the accumulation of organic matter
O horizon
typically dark in color because of the humus present
A horizon
a pale layer that is sometimes present in forest areas
E horizon
is brownish or reddish because of the presence of iron hydroxides that have leached from the surface. Also called the “zone of accumulation”
B horizon
is made up of the parent material underneath (bedrock)
in various stages of weathering
C horizon
solid unweathered rock
R horizon
The capacity of a soil to function within ecosystem and land-use boundaries to sustain biological productivity, maintain environmental quality, and promote plant and animal
health
Soil Quantity
Occurs when soil particles are detached, transported, and deposited. Although this may occur naturally, removal of plants and trees from the soil may lead to accelerated erosion
Erosion
The extreme degradation of productive land in arid and semi-arid areas. This can create poor quality vegetation
Desertification
Occurs acidic cations (hydrogen, aluminum, iron and manganese) are concentrated in the soil. The pH decreases and soil becomes more acidic. This is a natural process in weathering. However, the use of certain fertilizers to provide food, like anhydrous ammonia, causes soil to become more acidic much faster
Acidication
Is the buildup of salt on the soil surface. This affects the physical soil quality and hinders the growth of plants
salinazation