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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
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Mechanical or Physical Weathering Processes A rock broken into smaller pieces is said to be physically or mechanically weathered. It has a large exposed surface area which fur
Excretory Function of Bile Excretory function: Bile pigments (bilirubin and biliverdin) are the waste products of the breakdown of red blood cells and bile is their route of ex
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What types of rocks are formed by the lithification of sediments: Sedimentary Rocks
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The Ptolemaic System: The theoretical n'mdel of the universe given by the Greeks had a stationary Earth at its centre, around which the Sun, the Moon and the planets moved in c
Explain the Control of Salivary Secretion The autonomic control of saliva secretion occurs in two ways, as unconditioned and conditioned reflex. What are these? Let's find out.
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