What is soil?
The soil is defined as the upper layer of earth composed of a mixture of organic remains, clay, and rock materials on which plants grow. It is also regarded as one of the major natural resources. Soil supports plant life and growth.
There are three stages of soil:
• Solid soil
• Soil with air in the pores
• Soil with water in the pores
There are various types of soil that undergo diverse environmental pressures. Soil is mainly classified by its texture, proportions, and different forms of organic and mineral compositions.
Types of Soil:
Soil is classified into four types:
• Sandy soil.
• Silt Soil.
• Clay Soil.
• Loamy Soil.
Sandy Soil:
The first type of soil is sand. It consists of small particles of weathered rock. Sandy soils are one of the poorest types of soil for growing plants because it has very low nutrients and poor water holding capacity, which makes it hard for the plant’s roots to absorb water. This type of soil is very good for the drainage system. Sandy soil is usually formed by the breakdown or fragmentation of rocks like granite, limestone, and quartz.
Silty Soil:
Silt is known to have much smaller particles compared to sandy soil and is made up of rock and other mineral particles, which are smaller than sand and larger than clay. It is the smooth and fine quality of the soil that holds water better than sand. Â Silt is easily transported by moving currents and it is mainly found near the river, lake, and other water bodies. The silt soil is more fertile compared to the other three types of soil. Therefore, it is also used in agricultural practices to improve soil fertility.
Clay Soil:
Clay is the smallest particle amongst the other two types of soil. The particles in this soil are tightly packed together with each other with very little or no airspace. This soil has very good water storage qualities and makes it hard for moisture and air to penetrate into it. It is very sticky to the touch when wet, but smooth when dried. Â Clay is the densest and heaviest type of soil that does not drain well or provide space for plant roots to flourish.
Loamy Soil:
Loam is the fourth type of soil. It is a combination of sand, silt, and clay such that the beneficial properties from each are included. For instance, it has the ability to retain moisture and nutrients; hence, it is more suitable for farming. This soil is also referred to as agricultural soil as it includes an equilibrium of all three types of soil materials being sandy, clay, and silt and it also happens to have humus. Â Apart from these, it also has higher calcium and pH levels because of its inorganic origins.
Overview of Soil:
The ground on which we walk is never quite the same; it keeps on changing. Sometimes, it is made up of millions of tiny sand granules, and other times; it is a hard, rocky surface. Other places have the ground covered with moss and grass. When humans came along, the landscape slowly changed with the introduction of roads and rails.
1. The classifications of soil.
Soil can be classified into three primary types based on its texture – sand, silt, and clay. However, the percentage of these can vary, resulting in more compound types of soil such as loamy sand, sandy clay, silty clay, etc.
2. The characteristics of sandy soil.
Sandy soil essentially consists of small particles formed by weathering rocks. It is also very low in nutrients and poor in holding water, which makes it one of the poorest types of soil for agriculture.
3. The significant features of silty soil.
Silt has smaller particles compared to sand. It is also made up of rock and other mineral particles. Furthermore, its fine quality holds water better than sand. Due to the above-mentioned features, it is also beneficial for agriculture.
4. The characteristic of clay soil.
Clay contains the smallest particles amongst the other two types of soil. Particles are so densely packed that there is very little or no airspace. Consequently, this property effectively retains water. However, it also becomes hard for moisture and air to penetrate into it, thereby impeding the growth of plants.
