Soil structure refers to the arrangement of soil particles into aggregates, which influences water movement, root growth, and soil aeration. It plays a crucial role in determining soil fertility and its ability to support plant life by affecting its physical, chemical, and biological properties.
Soil pH is a crucial factor in determining nutrient availability and microbial activity, which directly influence soil fertility and plant growth. Managing soil pH within the optimal range for specific crops enhances nutrient uptake and promotes a healthy ecosystem for sustainable agriculture.
Soil compatibility refers to the suitability of soil to support specific plant growth, factoring in various soil characteristics like texture, structure, pH, and nutrient availability. Understanding soil compatibility is crucial for maximizing agricultural productivity and ensuring sustainable land use practices.