Particle size distribution is a fundamental characteristic of soil that determines the ratio of mineral particles of different sizes. The physical properties of the soil—its water-holding capacity, aeration, and ability to retain nutrients—directly depend on this indicator. Understanding the particle size distribution is necessary for an accurate assessment of soil fertility and for choosing an optimal strategy for the cultivation of agricultural crops, as the soil structure forms the environment for the plant root system and influences the efficiency of fertilizer application.
This collection brings together materials that reveal the process of mineral soil formation through rock weathering and the classification of soils by their composition. Readers will find articles here on key agrophysical and chemical indicators, methods for increasing soil fertility, acidity regulation, and maintaining a non-deficit humus balance. The selection also includes materials on agrochemistry: from the fundamentals of crop nutrition for specific crops, such as sugar beet, vegetables, and potatoes, to methods for calculating nutrient balance and the history of the development of the national scientific school in the works of D.N. Pryanishnikov and K.K. Gedroyts.