0
What else can I help you with?
How does the nature of illuviation determines the characteristics of pedalfer?
Illuviation refers to the process where materials such as clays, organic matter, and other dissolved substances accumulate in the B horizon of the soil profile. In pedalfer soils, the accumulation of illuviated materials leads to the development of specific characteristics such as a dark color, high clay content, and enriched fertility due to the concentration of minerals and organic matter.
How was ice found?
it was found by people it was found by people
Is zinc found with copper?
Zinc is found with copper and is also found with gold and nickel.
What 2 places is ozone found?
The ozone is found in atmosphere. It is also found in troposphere.
Where proteins are found?
proteins are found in meat.
What is pedalfer?
Pedalfer is defined as a formative element in the United States Alfisols soil taxonomic system. Pedalfer is composed of iron oxides and aluminum.
Pedalfer soils would most likely be found?
Pedalfer soils are typically found in regions with moderate to high precipitation levels and cool temperatures, such as in the eastern United States. They are characterized by their high iron and aluminum content and are usually fertile for agriculture when properly managed.
What climates are usually associated pedalfer pedocal laterite?
Pedalfer is associated with a moist climate, Pedocal with a dry climate and laterite with a wet climate.
What soil has the characteristic of the humid eastern US?
Pedalfer
What is A soil that is characteristic of the humid eastern US?
pedalfer----novanet
What is a soil that is a characteristic of the humid eastern US?
pedalfer----novanet
What is an pedalfer?
Soil that is characterized by an abundance of aluminum and iron oxides. Pedalfers are common in humid regions and are deposited in the B horizon of ABC soils, through leaching
In what areas can you find pedalfer soil?
Pedalfer soil is typically found in humid temperate regions, particularly in areas with deciduous forests. It is characterized by a significant accumulation of aluminum and iron oxides, leading to a clay-rich, fertile soil profile. Common locations include parts of the eastern United States, southeastern Canada, and some regions of Europe and Asia where precipitation is moderate. These soils are often associated with landscapes that experience significant weathering and leaching processes.
What factor accounts for most of the differences between three common types of soil pedal fer pedocaland laterite?
Climate is the factor that accounts for most of the differences between pedocal, pedalfer, and laterite soils. Pedocal soils are found in arid or semi-arid climates, pedalfer soils are typical in humid climates with high rainfall, and laterite soils develop in humid tropical climates with intense weathering. These climate conditions influence the processes of soil formation and the dominant minerals present in each soil type.
What describes a characteristic process in the formation of a pedalfer soil?
Pedalfer soil formation involves the accumulation of iron and aluminum oxides in the B horizon, which is enriched in clay minerals. This process occurs in humid climates where organic matter decomposition and leaching of soluble minerals is common. The resulting soil is typically red or brown in color and has good fertility.
How does the nature of illuviation determines the characteristics of pedalfer?
Illuviation refers to the process where materials such as clays, organic matter, and other dissolved substances accumulate in the B horizon of the soil profile. In pedalfer soils, the accumulation of illuviated materials leads to the development of specific characteristics such as a dark color, high clay content, and enriched fertility due to the concentration of minerals and organic matter.
What factor accounts for most of the differences between three common types of soil pedalfer pedoc and laterite?
The main factor that accounts for the differences between pedalfer, pedoc, and laterite soils is their composition and formation processes. Pedalfers are rich in iron and aluminum, forming in humid, temperate regions with well-drained soil. Pedocs are characterized by their calcareous content and form in semi-arid to arid regions. Laterite soils are highly weathered and rich in iron and aluminum oxides, forming in tropical regions with high rainfall and intense weathering.
