. Dry-farming;. Dry farming. [from old catalog]. iiG. 29. Rainwater moving downward through soil becomes changed into a capillary film of water around the soil particles. sandy loam, 14 per cent. Leather found that in the calcareous arid soil of India the upper 5 feet con- tained 18 per cent of water at the close of the wet season. It may be concluded, therefore, that the field-water capacities of ordinary dry-farm soils are not very high, ranging from 15 to 20 per cent, with an average for ordinary dry-farm soils in the neighborhood of. Please note that these images are extracted from scanned
. Dry-farming;. Dry farming. [from old catalog]. iiG. 29. Rainwater moving downward through soil becomes changed into a capillary film of water around the soil particles. sandy loam, 14 per cent. Leather found that in the calcareous arid soil of India the upper 5 feet con- tained 18 per cent of water at the close of the wet season. It may be concluded, therefore, that the field-water capacities of ordinary dry-farm soils are not very high, ranging from 15 to 20 per cent, with an average for ordinary dry-farm soils in the neighborhood of. 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 Widtsoe, John Andreas, 1872-1952. New York, The Macmillan company
Size: 1510px × 1655px
Photo credit: © The Book Worm / Alamy / Afripics
License: Licensed
Model Released: No
Keywords: ., bookcentury1900, bookdecade1910, bookpublishernewyorkthemacmilla
