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Excerpt from Soils of the Eastern United States and Their Use, Vol. 16: The Dekalb Silt Loam A wide variety of small fruits may be grown upon the Dekalb silt loam both for home use and for market supply where such demands exist. The later varieties of strawberries yield well both in respect to quantity and to quality. Raspberries may be grown and blackberries are particularly successful upon areas of some eleva tion in the more northern regions. Local market demands should rule the classes of small fruits to be planted. Market-garden empa - Potatoes should constitute the chief market garden crop upon the Dekalb silt loam wherever the local market conditions justify their production. The precautions necessary to secure a favorable yield have been discussed under general farm crops. Cabbages may also be grown to advantage both for local sale and for shipment. Usually it will be better to apply lime to the soil before a cabbage crop is attempted, and the land should be in a good condition of general fertility and Should be well prepared with deep plowing and good tillage. Beets, turnips, and other root crops may be grown to advantage where a local market for them exists. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work was reproduced from the original artifact, and remains as true to the original work as possible. Therefore, you will see the original copyright references, library stamps (as most of these works have been housed in our most important libraries around the world), and other notations in the work. This work is in the public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work. As a reproduction of a historical artifact, this work may contain missing or blurred pages, poor pictures, errant marks, etc. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.
Excerpt from Soils of the Eastern United States and Their Use IV: The Sassafras Silt Loam It is apparent from the textural characteristics of the Sassafras silt loam, from its level to gently undulating surface topography, and from the classes of creps best suited for production upon this soil that the equipment required for its most economical tillage will dif fer very materially from the equipment to be used upon such other Coastal Plain soils as the Norfolk fine sand or Sandy loam, which are more easily worked and are not so universally planted to the general farm crops. The Sassafras silt loam should be plowed to a depth of 8 or 9 inches, and if the natural soil is not so deep as this the depth should be gradually increased from year to year. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.
Unlike some other reproductions of classic texts (1) We have not used OCR(Optical Character Recognition), as this leads to bad quality books with introduced typos. (2) In books where there are images such as portraits, maps, sketches etc We have endeavoured to keep the quality of these images, so they represent accurately the original artefact. Although occasionally there may be certain imperfections with these old texts, we feel they deserve to be made available for future generations to enjoy.
Unlike some other reproductions of classic texts (1) We have not used OCR(Optical Character Recognition), as this leads to bad quality books with introduced typos. (2) In books where there are images such as portraits, maps, sketches etc We have endeavoured to keep the quality of these images, so they represent accurately the original artefact. Although occasionally there may be certain imperfections with these old texts, we feel they deserve to be made available for future generations to enjoy.
This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work was reproduced from the original artifact, and remains as true to the original work as possible. Therefore, you will see the original copyright references, library stamps (as most of these works have been housed in our most important libraries around the world), and other notations in the work. This work is in the public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work. As a reproduction of a historical artifact, this work may contain missing or blurred pages, poor pictures, errant marks, etc. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.
Excerpt from Soils of the Eastern United States and Their Use XXXVI: The Volusia Silt Loam Its surface varies, therefore, from nearly level or gently rolling to steeply sloping and almost precipitous. The greatest part of the type lies at altitudes ranging from 1,200 to 2,000 feet above tide level. Some portions of it rise to an extreme elevation of approximately 2,300 feet, while the areas found in northeastern Ohio are much less hilly and lie between 900 and 1,100 feet. The surface drainage of the Volusia silt loam is fairly adequate over the greater part of the type. Numerous springs found upon the hill slopes give rise to small swampy areas and some of the more level tracts are so closely underlain by impervious rock as to be poorly drained. The greatest difficulty with drainage, however, arises from the compacted and dense condition of the subsoil just below plow depth. Long-continued plowing to the same depth, often at times when the subsoil was too wet, has compacted and hardened the layer upon which the plow sole rides, forming what is locally known as "hardpan." This hardpan seriously interferes with the natural internal drainage of the type. Upon the more level areas of this soil erosion is not a serious problem, but there are many steep slopes within its boundaries which may be protected from destructive washing only through remaining in permanent pasture or in woodlot or forest. From many such slopes, denuded of forest when the region was cleared, practically all of the original soil has been removed, leaving only a mass of shale fragments mingled with a small amount of earth. Such slopes should never have been cleared. They comprise possibly 15 per cent of the total area of the type. The Volusia silt loam occurs at high elevations in a cold northern region. It is a moderately well drained soil, of rather heavy texture, suited under ordinary conditions only to the production of hardy crops which mature in a short growing season. The greater proportion of the type lies at too great an elevation to permit of maturing any variety of corn except the flint, and even this can only be grown for silage in the majority of years. The crop adaptation of the type is therefore restricted by its inherent characteristics and by its climatic surroundings to buckwheat, oats, Irish potatoes, and hay. Other crops are grown to a limited extent, and the better drained areas, which may also lie at lower elevations, possess a greater range in crop adaptations than the general average of the type. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.