Soil Flashcards
(35 cards)
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
ideal soil for agriculture use since it provides good aeration and drainage properties of large particles with nutrient nutrition and water holding abilities of clay particle
Loam
is the superficial or topmost layer of the soil that is primarily composed of decaying organic matter, living organism, and fresh soil. The color of the topmost layer is normally either brown or black due to its organic composition. It is the layer that hosts most of the roots of small vegetation cover like grass and contains about 20% of organic matter
O-Horizon
is the second layer of the soil. It is referred to as the top-soil. It is composed of highly decaying organic matter and minerals, and its color ranges from gray to brown. It is the layer that hosts many plants and supports many agricultural and grassland areas. Thus, seed germination and the growth of plant roots take place in this soil layer. It is distinguishable by the different soil types including loam, clay, sand, and silt. It is also the soil layer that is most vulnerable to water and wind erosion
A-horizon
This is the third and the thinnest soil layer, and it is lighter in color compared to the A-Horizon. It is termed as the eluviation layer due to the leaching of minerals. As a result, this layer is depleted of aluminum, clay, organic compounds, and other soluble elements. It is mainly made up of silt and sand after losing most of its minerals as they drip down through the soil
E-horizon
is the fourth layer and is also referred to as the sub-soil. It is mainly made up of large rocks, clay, and bedrock. The color of the sub-soil is lighter than the layers above it and ranges from rust to tan. It is also composed of minerals and little organic matter. The sub-soil accumulates a lot of clay, aluminum, iron, and organic compounds from the layers above it from the dripping down of mineralized water through a process known as illuviation. Hence, it is sometimes called the illuviation zone. It is the layer where the roots of big trees en
B-horizon
This is the fifth layer of the soil and it also known as the regolith. Plant roots do not go through this layer and it has very little organic matter. The color of the_ is gray and is made up of fragmented pieces of bedrock. Also, it has compacted sediment and cemented geological material. Very little activity is present in this layer but there may be instance of additions or losses of minerals and other soluble compounds.
C-Horizon
The_ is the sixth and final layer of the soil. It is also known as the bedrock. The materials here are mainly solid un weathered rock that are cemented and compacted by the weight of the overlying layers. The color of this layer is gray with several hard rocks. This layer is beyond 50 meters from the top-soil. Some of the rocks found here include granite, limestone, and basalt
R-Horizon
describes the relative amounts of differently sized soil particles
Soil texture
Soil properties are used to classify different soil
These properties include soil texture, color, chemistry, pore space, and fertility