What is Soil? How is it Formed?

24 Ocak 2026 Çağla Altıntaş 1 görüntülenme
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What is Soil? How is it Formed?

Soil can be defined as the thin layer covering the Earth’s surface and has a vital importance for the survival of living things. This layer is formed as a result of various natural processes and contains minerals, organic matter, water, air, and living organisms. Soil formation is a complex process and occurs through the interaction of various factors. Soil provides the nutrients necessary for the growth and development of plants. Minerals are taken up by plant roots and support their growth. Organic matter improves the structure of the soil, increases the water holding capacity, and increases the fertility of the soil. Water provides for the irrigation of plants and maintains the balance of the soil, while air is important for the respiration of roots and the activities of microorganisms. Consequently, soil is one of the fundamental elements of nature and is vital for the continuation of life. Its formation is a complex process and occurs through the interaction of various factors. Soil enables plants to grow, stores water and nutrients, affects the composition of the atmosphere, and contributes to the preservation of biodiversity.

Soil Formation

Soil is a self-regulating miracle of nature. The formation process is based on the complex interaction of many natural factors over long periods of time. Initially, it begins with the weathering and breaking down of parent rocks by erosion. This process is accelerated by factors such as temperature changes, rain, wind, and plant roots. The minerals and organic matter resulting from weathering form the basic components of the soil. As a result of the activities of plant remains, dead animals, and microorganisms, organic matter accumulates and turns into a stable organic matter called humus. This process affects the color, texture, and nutritional value of the soil. With the accumulation of minerals, a soil profile is formed and different layers become distinct. These layers show the formation of the soil profile and the maturation process of the soil. Consequently, soil formation is a long process and forms a dynamic part of the natural environment.

what is soil

What are the Factors Affecting Soil Formation?

The factors affecting soil formation are as follows:

  • Climate: Climate is one of the most important factors. Temperature and precipitation amount have a great impact on the weathering of parent rocks, chemical reactions, and erosion. Additionally, climatic effects such as sunlight, wind, and glaciers also affect soil formation.

  • Vegetation and Organisms: Plant roots hold and decompose the soil, produce organic matter, and improve the soil structure. Furthermore, microorganisms contribute to the breakdown of organic matter in the soil and the cycling of nutrients.

  • Topography: The shape of the land affects the movement of water and erosion and influences the transport and accumulation of soil. Slopes, valleys, plains, and mountains are factors affecting soil formation.

  • Parent Material: Parent material is the starting material for soil formation. It is formed as a result of the weathering or transport of parent rocks and affects the soil composition.

  • Time: Soil formation is a long process and time is necessary for the maturation of soils. Over time, soil composition and structure change and soils acquire different characteristics.

The interaction of these factors leads to the formation of different soil types and the development of various soil properties. Therefore, it is important to evaluate these factors together to understand soil formation.

what is soil

What are the Soil Types?

Soil types are formed by the interaction of factors such as different climate, vegetation, topography, and parent material. Here are some of the common soil types:

  • Gelisol: These are soils that remain frozen in the Arctic Region.

  • Histosol: These are soils rich in organic matter and are found in swamps and reed beds.

  • Spodosol: These are soils poor in nutrients and are generally seen in mountainous areas.

  • Andisol: These are soils formed on volcanic sand and ashes.

  • Oxisol: These are soils found in tropical regions that are poor in nutrients but rich in oxides.

  • Vertisol: These are soils formed on clayey parent material seen in meadows and steppes.

  • Aridisol: These are soils found in arid regions and are poor in terms of moisture and organic matter. Desert soils are examples of this group.

  • Ultisol: These are soils that are highly weathered in tropical regions due to excessive precipitation and temperature.

  • Mollisol: These are soft and fertile soils and are generally found in herbaceous plant areas in mid-latitudes. These soils, suitable for agriculture, are rich in organic matter and elements.

  • Alfisol: These are soils where clay accumulates on the surface.

  • Inceptisol: These are alluvial soils and are found in areas of delta plains not exposed to flooding.

  • Entisol: These are newly formed soils and occur in areas where erosion and accumulation events take place.

These soil types form in different geographical regions and climatic conditions and play an important role in areas such as plant cultivation, agriculture, and environmental protection.

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