. The nature and properties of soils; a college text of edaphology. Soils. J^EFLECTWJ^ SOIL sir/?rACE. coNDacT/a/^/ COSrVECTiON OlfCAWC OECAY !'AI350nPT/0N COL 0/?9 SL OPE Z-SPECIFJC MEAT 7EXn//?E STJ?UCri/J?E MOtSTl/nE 3-MOVEMENT ^*LOSS or HEAT j?iSE or TEMPERATl/J^E Fig. 41.—^A diagram showing the heat relations of soil. does work either on the land or water surfaces of the earth. The atmosphere and its impurities probably deflect on an average more than three-fourths of the insolation by absorp- tion, reflection, and refraction. Little or none of such energy ever reaches the earth itself. C


. The nature and properties of soils; a college text of edaphology. Soils. J^EFLECTWJ^ SOIL sir/?rACE. coNDacT/a/^/ COSrVECTiON OlfCAWC OECAY !'AI350nPT/0N COL 0/?9 SL OPE Z-SPECIFJC MEAT 7EXn//?E STJ?UCri/J?E MOtSTl/nE 3-MOVEMENT ^*LOSS or HEAT j?iSE or TEMPERATl/J^E Fig. 41.—^A diagram showing the heat relations of soil. does work either on the land or water surfaces of the earth. The atmosphere and its impurities probably deflect on an average more than three-fourths of the insolation by absorp- tion, reflection, and refraction. Little or none of such energy ever reaches the earth itself. Clouds and dust play an im- portant role in such interception, affecting to a marked degree the energy received at any particular location. Part of the original insolation reaching the earth's surface is immediately reflected and is lost as radiant energy, having undergone no ^The earth and its atmosphere receives but one two-billionth of the sun's energy. On such a trifling proportion of the sun's energy depend almost all of the earth's 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; Buckman, Harry Oliver, 1883-. New York, Macmillan


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Keywords: ., bookauthorlyontlth, bookcentury1900, bookdecade1920, bookyear1922