Perspective - Journal of Agricultural Science and Botany (2023) Volume 7, Issue 2

From rocks to rich soil: The processes and phases of soil formation.

Ingrid Hung^*

Department of Crop Production Ecology, Swedish University of Agricultural Sciences (SLU), Uppsala, Sweden.

*Corresponding Author:

Ingrid Hung
Department of Crop Production Ecology
Swedish University of Agricultural Sciences (SLU)
Uppsala, Sweden.
E-mail: hung.ingrid@slu.se

Received: 24-Feb-2023, Manuscript No. AAASCB-23-90639; Editor assigned: 25-Feb-2023, PreQC No. AAASCB-23-90639(PQ); Reviewed: 10-Mar-2023, QC No. AAASCB-23-90639; Revised: 05-Apr-2023, Manuscript No. AAASCB-23-90639(R); Published: 12-Apr-2023, DOI: 10.35841/2591-7366-7.2.173

Citation: Hung I. From rocks to rich soil: The processes and phases of soil formation. J Agric Sci Bot. 2023;7(2):173

Abstract

Soil formation is a complex and dynamic process that occurs over a long period of time. It is the result of a combination of physical, chemical, and biological processes that transform rock and mineral materials into the fertile and nutrient-rich soil that supports plant growth and sustains life on Earth. Understanding the processes and factors that contribute to soil formation is essential for farmers, gardeners, and land managers to optimize soil fertility and productivity

Keywords

Soil, Rocks, Minerals, Nutrient.

Introduction

Soil formation begins with the weathering of rocks and minerals. Weathering is the process by which rocks and minerals are broken down into smaller particles by physical, chemical, and biological means. Physical weathering occurs when rocks and minerals are exposed to environmental factors such as wind, water, and temperature fluctuations, which cause them to crack and break apart. Chemical weathering occurs when rocks and minerals react with water and atmospheric gases, such as oxygen and carbon dioxide, to form new compounds that are more easily broken down. Biological weathering occurs when plants and animals break down rocks and minerals through their physical and chemical processes [1].

As rocks and minerals weather, they begin to break down into smaller particles, creating a layer of loose material known as regolith. Regolith is the foundation upon which soil formation occurs. Over time, regolith becomes mixed with organic matter from plants and animals, which begins to decompose and create humus, a dark, nutrient-rich material that provides the foundation for soil fertility [2].

The next stage of soil formation is the accumulation of clay, silt, and sand particles in the regolith. These particles are carried by wind, water, and gravity and deposited on the surface of the regolith. The size and composition of these particles determine the texture of the soil, which in turn affects the soil's water-holding capacity, nutrient retention, and aeration [3].

The accumulation of organic matter and the deposition of mineral particles in the regolith are not enough to create a mature soil. Soil development requires the interplay of several factors, including climate, topography, parent material, organisms, and time. These factors influence the chemical and physical processes that take place in the soil, leading to the formation of distinct soil horizons.

Climate is one of the most important factors affecting soil formation. Temperature and precipitation determine the rate at which weathering occurs, the amount of organic matter that accumulates, and the types of plants and animals that can survive in the soil. In regions with high rainfall and warm temperatures, for example, soil development is rapid, leading to the formation of thick, nutrient-rich soils. In contrast, arid and cold regions may have thin and nutrient-poor soils due to slow soil formation rates [4].

Topography also plays an important role in soil formation. The slope of the land affects the rate at which water moves through the soil and the depth of soil horizons. Steep slopes may result in erosion and the loss of topsoil, while flat terrain may result in waterlogged soils with poor aeration. Parent material is the rock or mineral material from which the soil develops. The chemical and physical properties of the parent material influence the properties of the soil. For example, soils formed from granite or basalt are typically rich in nutrients, while soils formed from sandstone or shale may be nutrient-poor [5].

Conclusion

Organisms also play a critical role in soil formation. Plants and animals contribute organic matter to the soil, which provides nutrients and improves soil structure. Microorganisms, such as bacteria and fungi, break down organic matter and release nutrients, making them available to plants. Soil animals, such as earthworms, burrow through the soil, improving aeration and water infiltration.

References

1. Chen JM. Carbon neutrality: toward a sustainable future. Innov. 2021;2(3).

Google Scholar, Cross Ref

2. Liu L, Basso B. Impacts of climate variability and adaptation strategies on crop yields and soil organic carbon in the US Midwest. PloS one. 2020;15(1):0225433.

Indexed at, Google Scholar, Cross Ref

3. Kurganova IN, Telesnina VM, Lopes de Gerenyu VO, et al. The dynamics of carbon pools and biological activity of retic albic podzols in southern taiga during the postagrogenic evolution. Eurasian Soil Sci. 2021;54(3):337-51.

Indexed at, Google Scholar, Cross Ref

4. Baldocchi DD. Assessing the eddy covariance technique for evaluating carbon dioxide exchange rates of ecosystems: past, present and future. Glob Change Biol. 2003;9(4):479-92.

Indexed at, Google Scholar, Cross Ref

5. Rawls WJ, Pachepsky YA, Ritchie JC, et al. Effect of soil organic carbon on soil water retention. Geoderma. 2003;116(1-2):61-76.

Indexed at, Google Scholar, Cross Ref