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Soil Texture and Methods of Analysis
Soil texture is the basic property of a soil related to the size of individual mineral particles, which cannot be easily altered. It specifically refers to the relative size of soil particles. The rate and extent of many important physical and chemical reactions in soils are governed by texture because it determines the amount of surface on which the reaction can occur. Different size groups of soil particles, termed as soil separates were arbitrarily chosen by International Society of Soil Science (ISSS) as clay, fine sand, coarse sand, and gravel. The United States Department of Agriculture (USDA) has further subdivided the sand fraction. The two systems of textural classification
Explain the Erythropoiesis Erythropoiesis, derived from the word 'erythros' meaning red and 'polesis' meaning making, is a part of a broader process, hemopoiesis, i.e., formati
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What is Parent material Parent material refers to the primary material from which the soil is formed. The parent material may be either a solid rock, a decomposed rock, organic
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Differentiate between soil water content and plant available soil moisture. The mass of water lost relative to mass of dry soil is called soil water content whereas plant avai
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write 2 kinds of energy sources
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