. Soils, their properties and management. Soils. SOIL'FOBMING PROCSSSBS 29 As shown by the diagrams, the soil from the granite does not differ greatly from the original rock, except in loss of bases, assumption of water, and increase of organic. (^Fre^h rock Fig. 2. — Diagram showing the chemical composition of Virginia lime- stone and its residual clay. See analyses above. matter. The residual clay from the limestone presents greater differences, due to the almost entire disappear- ance of calcium carbonate. The diagrams for the two clays resemble each other fairly closely in spite of their w


. Soils, their properties and management. Soils. SOIL'FOBMING PROCSSSBS 29 As shown by the diagrams, the soil from the granite does not differ greatly from the original rock, except in loss of bases, assumption of water, and increase of organic. (^Fre^h rock Fig. 2. — Diagram showing the chemical composition of Virginia lime- stone and its residual clay. See analyses above. matter. The residual clay from the limestone presents greater differences, due to the almost entire disappear- ance of calcium carbonate. The diagrams for the two clays resemble each other fairly closely in spite of their widely differing sources. Because weathering causes the persistence and accumulation of sihca, aluminium, and iron, and a loss of the basic materials, all soils as they weather tend to approach a similar composition. Yet, owing to a difference in the adjustment of the forces at work and in the time element, no two soils will ever be exactly alike. Soils will differ, then, from the original rock and from one another according to the intensity. Please note that these images are extracted from scanned page images that may have been digitally enhanced for readability - coloration and appearance of these illustrations may not perfectly resemble the original Lyon, T. L. (Thomas Lyttleton), 1869-1938; Fippin, Elmer O. (Elmer Otterbein), 1879-1949; Buckman, Harry Oliver, 1883-. New York, Macmillan


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Keywords: ., bookauthorlyontlth, bookcentury1900, bookdecade1910, bookyear1915