What Is Soil (original) (raw)

Last Updated : 23 Jul, 2025

**Soil is the loose material that covers the Earth's surface in most parts of the world. It gives plants the nutrients they need to grow and plants give people and animals food to live. Soil also provides building materials, homes for animals, and things we use every day. More than just dirt, soil is a valuable natural resource that serves as the basis for life as we know it on Earth. Rocks, decaying plants and animals, air, and water all makeup soil. By the process of weathering big rocks break down into smaller and smaller pieces eventually, becoming part of soil.

Table of Content

What is Soil?

Soil is the **top layer of the earth's crust composed of mineral particles, organic matter, water, and air. It's a living, dynamic **ecosystem that supports plant life and plays a vital role in the environment. Soil is formed when rocks break down into tiny pieces due to repeated drying, heating, and cooing by sun, wind, and rain, This process is called **weathering.

Soil

Water seeps through the fractures in the rocks during the rainy season. This water freezes in the cold and creates pressure, which causes rocks to shatter. This reduces the already tiny rock fragments into even **smaller fragments known as pebbles. Eventually, the stones crumble into small soil particles. When the soil is contaminated with humus (dead and decayed small animals and plants) it is good for the growth of the plants. There are three main layers of soil- **topsoil, subsoil, and bedrock. The topsoil layer is best for plant growth while the subsoil has very little humus and is orange. Bedrock is quite deep inside the earth.

Composition of Soil

The composition of soil is mentioned below:

Inorganic Components of Soil

They are derived from rocks and minerals. 50% of the total mass of the soil is inorganic minerals. The inorganic components are important as:

Organic Components of Soil

The percentage of organic matter in the soil is <5%.

Water and Air in the soil

Mineral soil consists of 20-30% of water and only half of it is available to plants.

Formation of Soil

Soil formation is the most complicated and slow process. It will take several years that is 100 to 1,000 years the conversion of parent material into soil known as soil formation. This process was carried out by the following factors:

Factors of Soil Formation Condition
Weathering It is the breakdown and decomposition of rocks and minerals by factors including air and water.
Translocation It is the movement of material in solution or suspension from one horizon to another is referred to as translocation.
Transformation It is a process of changing the soil by microorganisms.
Leaching It is the loss of soil particles when rain exceeds its normal point.

Factors Influencing Soil Formation

Various factors influence soil formation like:

Characteristics of Soil

Some of the important characteristics of soil are mentioned below:

Types of Soil

Soil can be categorized into three primary types based on particle size.

Types-of-Soil

Importance of Soil

Soil is important because of the following reasons:

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