Laterite soil is rich in Iron & Alumunium .
It is found on mountaneous region of south India in Kerala , Tamilnadu & Karnataka .
Heavy rains wash away soluble salts of Sodium , Magnesium , Calcium etc leaving behind insoluble salts of Iron & Alumunium .
Laterite soil is good for TEA,COFFEE,COCONUT & CASHEW NUT.
Riverine alluvium Terai soils Lateritic soils Red-yellow loams Red sandy soils
J. A. Prescott has written: 'Laterite and lateritic soils' -- subject(s): Soils, Laterite, Analysis
Alluvial soils, Piedmont soils, Hill soils , Lateritic soils
The Indian Ocean basin consists of various types of soil depending on the geographical location. Common soil types include alluvial, red, lateritic, and volcanic soils. These soils vary in composition and fertility, influencing the flora and fauna in the region.
Bauxite is typically found in tropical or subtropical regions where there is significant weathering of aluminum-rich rocks. It is commonly found in soils with a high content of aluminum minerals, such as laterite soils. These soils are typically acidic and well-drained, allowing for the accumulation of bauxite deposits.
Laterite soils are known as leached soils because they are heavily weathered and have lost most of their soluble nutrients and minerals due to the leaching process. Continuous rainfall leaches out the nutrients, leaving behind a soil that is nutrient-poor and acidic.
Lateritic soil is typically red or orange in color due to the high iron oxide content.
In Alabama, you can find a variety of soils such as sandy soils, clay soils, loamy soils, and peaty soils. The dominant soil types in the state include Ultisols, Alfisols, and Inceptisols. These soils vary in their characteristics and suitability for different types of crops or land uses.
Soils are classified based on factors such as texture, color, structure, and composition. These characteristics help categorize soils into different types such as sandy, loamy, clayey, and peaty soils. This classification system is used to determine the potential uses and management practices for different soil types.
Soils vary in terms of texture (sand, silt, clay), structure (how particles are arranged), composition (organic matter, minerals), pH level, fertility (nutrient content), and drainage capabilities. These variations influence the suitability of soils for different types of plants and specific land uses.
Ahmad Gharib has written: 'Geochemistry of some trace elements in nickeliferous lateritic profiles'
Unproductive soils refer to soils that have poor fertility, low organic matter content, and limited ability to support plant growth. These soils may lack essential nutrients, have a high acidity or alkalinity, or be compacted, restricting root growth and water infiltration. Improving soil health through proper management practices can help make unproductive soils more productive for agriculture or other uses.