Soil is a complex, dynamic, and vital natural resource that supports the growth of plants and is essential for the survival of all living organisms. It is a mixture of organic matter, minerals, gases, liquids, and countless organisms that together support life on Earth.
Soil is composed of mineral particles, organic matter, water, and air. The mineral particles are classified based on their size into sand, silt, and clay. The relative proportions of these particles determine the soil's texture.
Soil is formed through the weathering of rocks, organic matter decomposition, and the activity of living organisms. The process of soil formation, known as pedogenesis, involves physical, chemical, and biological processes that transform parent material into soil over time.
Due to its crucial role in supporting life, it is essential to conserve and protect soil from degradation. Soil conservation practices include erosion control, agroforestry, crop rotation, and the use of cover crops to maintain soil fertility and structure.
Understanding the properties and functions of soil is essential for agricultural practices, environmental conservation, and the sustainability of ecosystems.
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