Micronutrients and Fertilizers for Improving and Maintaining Crop Value: A Review

Abstract

The effect of mineral and organic fertilization on the contents of Fe, Cu, Zn, Mn, B, and Mo in soil and the dirt solution just as on accessibility of these elements for crops were researched in the drawn-out preliminary. The most elevated contents of Zn, Fe, Mn, and Cu in soil and soil solution were seen in the treatment with the least pH (NPK). In this equivalent mix, the substance of B and Mo was the least. On the convergence of Zn, B, and Fe in the dirt solution, significantly expanded under farmyard manure application. Natural fertilizers provide the normal and physical activities of the soil but contain very few supplements, so more are needed to improve plants. Plant take-up of nutrients can continue when they are available in a plant-accessible structure. Much of the time, nutrients are caught up in an ionic structure from (or along with) soil water. Even though minerals are the beginning of most nutrients, and most supplement components in the dirt are held in a glasslike structure inside essential and optional minerals, the climate is too leisurely to help quick plant development. For instance, the use of finely ground minerals, feldspar, and apatite, to soil rarely gives the fundamental measures of potassium and phosphorus at a rate adequate for great plant development, as a large portion of the nutrients stays bound in the precious stones of those minerals.