Soil Structure

Soil Structure - Sand, Silt, and Clay are defined by their particle size Bacteria and Fungi (B&F) break down Parent Material (rocks & pebbles, etc.) into smaller and smaller particles, resulting in sand, silt, and clay particles. They do this so they can extract the nutrients they need, e.g. Iron, Boron, Magnesium, etc., by producing enzymes; acidic (Fungi) or alkaline (Bacteria) which enable them to deconstruct the crystalline structure of the parent materials and that of the sands, silts, and clays. This process releases nutrients that are absorbed by B&F, which are then on their way to becoming available to plants (plant-available nutrients). Soil results in clean water; dirt results in problems Thank you for reading. Vishal Vanashala Please contact me for below services Soil Nutrition Consultancy (fulfilling the complete biology in your soil so that you maximize the produce and will not need fertilizers, pesticides or herbicides for rest of your life)...