Soils are crucial for agricultural production, nourishing plants with essential nutrients, and providing a habitat for soil microorganisms that benefit plants. However, soil management is a complex process that involves various factors such as tillage, fertilizer application, weed management, soil pH, and moisture management.
Soil moisture content is the percentage of water present in soil by volume. This moisture content affects the availability of soil nutrients and the growth and yield of crops. Typically, soils have an upper and lower limit of moisture content, and the optimal moisture content lies between these limits. The optimum moisture content varies based on soil type, climate, and crop type.
Maintaining soil moisture at the optimum level is vital for successful soil management. Soil moisture content affects the microbial activity, nutrient availability, and soil structure, which ultimately affect crop growth and yield. Soil moisture level below the optimum causes nutrient deficiency, plant stunting, and decreased yield. Excess soil moisture, on the other hand, causes poor soil aeration, leaching of soil nutrients, and increased soil erosion.
There are several techniques that farmers and agronomists use to achieve optimal soil moisture content.
Optimal soil moisture management plays a vital role in the success of crop production. Farmers and agronomists must understand the different factors that affect soil moisture content and use appropriate techniques to achieve optimum soil moisture levels.