My Vision
to Soil Fertility
Introduction to soil fertility:
Soil fertility is defined as “the function of the soil to act as a mediator of nutrients, water, and air for plants and edaphon (soil life). Soil fertility is the result of physical, chemical, and biological processes.
However, soil fertility has ancient origins and has been steadily used over centuries to refer to soil's capability to support plant production in agricultural contexts. Historically, the most common use of soil fertility has focused on provisioning mineral nutrients for plant growth.
Therefore, an emphasis on fertilizer-based nutrient amendment has continued despite the well-understood contributions of soil organisms to nutrient availability and soil physical conditions for plant growth. Here, my understanding is to explore the separation of biological, chemical, and physical soil fertility to clarify the unique contributions and interactions among these components of soil fertility. It is necessary to ensure that the contributions of soil organisms are considered within a soil fertility framework and not overshadowed by a focus solely on plant production responses to the chemical fertility of the soil. A further contribution of this conceptual model is that it provides insights into the interacting mechanisms that control soil fertility. Because biological processes have the potential to contribute significantly to chemical and physical processes that influence soil fertility. Likely we need to know that soil biological processes drive the transformation of carbon and nutrient cycling, improve soil structure, and regulate pests and diseases.
However, fertilizers have been the traditional tool to overcome soil fertility depletion, and fertilizer use is responsible for a large part of the food production increases worldwide, including in the commercial farm sector. Fertilizer use is viewed as a recurring cost of production that must be paid for by the increased crop yields farmers obtain. Attempts to introduce this approach to smallholder farming have failed, even with input subsidies and credit schemes. However, current thinking on natural resource management leads us to propose an alternative approach for situations where the traditional one has not worked.
Understanding the factors influencing soil fertility:
Understanding the factors influencing soil fertility and adopting responsible land management practices is essential for maintaining healthy soils that can support plant growth and contribute to a sustainable and thriving ecosystem. I can summarize the key aspects of soil fertility:
1. Nutrient Content: Soil fertility is heavily dependent on the availability of essential nutrients, primarily nitrogen (N), phosphorus (P), and potassium (K), often referred to as NPK. These nutrients are vital for plant growth and development. Other micronutrients like iron, zinc, and manganese also play essential roles.
2. Organic Matter: Organic matter in the form of decomposed plant and animal material, known as humus, greatly enhances soil fertility. It improves soil structure, water-holding capacity, and nutrient-holding capacity. Additionally, organic matter provides a food source for beneficial microorganisms in the soil.
3. Soil pH: Soil pH measures the acidity or alkalinity of the soil and significantly affects nutrient availability. Most plants thrive in soils with a pH range of 6 to 7. Soils that are too acidic or alkaline can limit nutrient uptake by plants.
4. Texture and Structure: Soil texture refers to the relative proportions of sand, silt, and clay particles in the soil. Soil structure relates to how these particles are arranged. A well-balanced soil with a good structure allows for proper root growth, aeration, and water drainage, which are essential for plant health.
Aggregates form when soil organisms reproduce, hunt, graze, and produce waste. The largest ones are called macroaggregates. These range from 0.25 to 2 millimeters in diameter, and they are made up of microaggregates, which are tiny clusters of particles cemented by chemical and physical bonds and are less than 250 μm (0.25 millimeters ) in diameter.
The size and composition of mineral particles in the soil is a significant factor that largely determines whether the soil will form clumps or aggregates. The composition of sand, silt, or clay also plays an important role in structure development. Primary particles are bound together with glues and slimes in the form of polysaccharides and bacterial or fungal ‘skeletons’, and fungal hyphae weave them together. Microaggregates develop and mature over time. Eventually, the activities of living organisms and the remains of dead ones bind clusters of microaggregates into macroaggregates. This process continues as long as plant roots remain active in the structure of soil aggregates.
5. Microorganisms: These organisms have many tasks and are central to crop fertility. Soil is teeming with beneficial microorganisms such as bacteria, fungi, and earthworms. These microorganisms contribute to soil fertility by breaking down organic matter, releasing nutrients, and improving soil structure. They also help protect plants from harmful pathogens, purifying the environment from pollutants, regulating carbon storage stocks, and production/consumption of many significant greenhouse gases (GHGs), such as methane and nitrous oxides.
6. Nutrient Cycling: Nutrient cycling is the process by which nutrients are absorbed by plants, returned to the soil through plant residues and organic matter, and made available for future plant growth. I have thoroughly described soil nitrogen, phosphorus, and organic matter cycling in my website. Efficient nutrient cycling is vital for maintaining soil fertility.
7. Fertilization: In agricultural and gardening practices, fertilizers are often used to supplement soil nutrients when they are deficient. However, improper or excessive fertilizer use can harm the soil and the environment, so it should be done thoughtfully.
8. Crop Rotation and Cover Crops: Cover crops are part of the soil health component. Cover crops are planted to protect the soil between main crop seasons, i.e., after corn, soybean, and wheat. Cover crops help reduce nitrate leaching, soil erosion, and improve soil health through their root’s decomposition process. While Crop rotation involves planting different crops in a sequence to prevent nutrient depletion and disease buildup. Rotating crops can have important production benefits such as increasing yields, improving nutrients and organic matter in the soil, and it can help disrupt the lifecycle of crop pests, reducing chemical use.
9. Soil Testing: A soil test is important for several reasons: to optimize crop production, to protect the environment from contamination by runoff and leaching of excess fertilizers, to aid in the diagnosis of plant culture problems, to improve the nutritional balance of the growing media and to save money and conserve energy applying only the amount of fertilizer needed based on the 4-R principles.
Helps in making informed decisions about fertilization and soil management. Therefore, regular soil testing is a fundamental practice to assess nutrient levels and pH in the soil.
10. Sustainable Practices: Sustainable agriculture helps to preserve natural resources while promoting social equity and economic profitability. Not only does it reduce the environmental impact of the traditional farming system, but it also results in higher yields and healthier products for consumers. Maintaining soil fertility through sustainable practices, such as no-till farming, organic farming, and agroecology, is essential for long-term food security and environmental conservation.
The conclusion is that soil fertility is a dynamic and multifaceted concept crucial for agricultural and environmental sustainability.