Titlebook: Simple Methods to Study Pedology and Edaphology of Indian Tropical Soils; D. K. Pal Book 2019 Springer International Publishing AG, part o

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Cracking Depths in Indian Vertisols: Evidence of Holocene Climate Change,arid dry (AD) climatic environments indicate their occurrence in a climosequence. The soils show a change in their morphological, physical, chemical and micromorphological properties due to change of climate from humid to arid during the Holocene period. Formation of pedogenic CaCO. (PC), illuviatio

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Unique Depth Distribution of Clays in SAT Alfisols: Evidence of Landscape Modifications,tely disappears and fulfills the textural criterion of an Alfisol. In contrast, many SAT red ferruginous Alfisols, mainly Paleustalfs and Rhodustalfs of southern India have clay content of about 10–15% in the Ap horizon, immediately followed by a well-developed argillic (Bt) horizon with a clay cont

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Hydraulic Conductivity to Evaluate the SAT Vertisols for Deep-Rooted Crops,e Vidarbha region in central India indicate that the retention and release of soil water are governed by the nature and content of clay minerals, and also by the nature of the exchangeable cations. The available water content (AWC) is not available during the growth of crops. In fact, moisture remai

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Clay and Other Minerals in Selected Edaphological Issues,d soil properties of agricultural importance, difficult. Nevertheless, it is very much necessary to investigate the properties of these minerals relevant to the properties of the soil in bulk even when soil minerals often differ from “type” minerals and also when soil clay minerals exist as their mi