Soil Flashcards
an essential component on Earth that enabled life to exist on the planet and continues to support.
Soil
The term pedosphere is derived from the Greek words “” which means soil and “”which means sphere
Pedon and sfaira
Soil is composed of
Soil is generally composed of 45% mineral ( gravel, sand. silt and clay), 25% air, 25% water and 5% organic matter ( humus, roots, dead and decaying organisms). These components reflect the processes hat formed the so
Is a loose mixture of rock fragments, organic matter, water, and air – that portion of the regolith ( rhegos=blanket, lithos = stone) that support the growth of vegetation
Soil
First step of soil formation
Weathering of parent rock into smaller pieces
What causes soil to form?
- Rock is broken down by weathering and plant root growth to form sediment
- Some microorganisms, such as bacteria and fungi, decompose the remains of plants and animals
What factors determine how long it takes for soils to form?
These factors include parent material, time, climate, plants and animals, and topography
The source of the weathered mineral matter from which soil develops. The rate of weathering depends on the structure of the rock and minerals that make up the rock. When the parent material is bedrock, the soils are termed residual so
Parent material
By contrast, those developed on unconsolidated sediment are called
transported soil
an important component of every geological processes and soil is no exception. The longer a soil has been forming, the thicker it becomes and the less it resembles the parent materia
Time
Soil usually develops more quickly in warm, wet areas than in cold, dry areas. The most influential factor in soil formation. Variations in temperature and precipitation determine whether mechanical or chemical weathering prevails
Climate
The biosphere plays a vital role in soil formation. The types and abundance of organisms present have a strong influence on the physical and chemical properties of soil. Without a lot of_, soil tends to develop slowly
plants and animals
The lay of the land can vary greatly over short distances. Such variations can lead to the development of a variety of localized soil types.
Topography
Defined as the relative proportion of the particle sizes in the soil – sand, silt and clay.
- Clay ( <0.002 mm) – smallest particle
- Silt ( 0.002 – 0.005 mm)
- Sand – ( 0.005 – 2.00 mm
Soil Texture
Particles larger than coarse grained sand are called_ if they are > 75.00mm
gravel and rock