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Some Relations of Organic, Matter in Soils: A Thesis Presented to the Faculty of the Graduate School of Cornell University for the Degree of Doctor of Philosophy (Classic Reprint) - Softcover

 
9781332197866: Some Relations of Organic, Matter in Soils: A Thesis Presented to the Faculty of the Graduate School of Cornell University for the Degree of Doctor of Philosophy (Classic Reprint)

Synopsis

Excerpt from Some Relations of Organic, Matter in Soils: A Thesis Presented to the Faculty of the Graduate School of Cornell University for the Degree of Doctor of Philosophy

In a comparison of 22 rotation plots no distinct relation has been found between the composition of the soil and the nature of the rotation. In a long cultivated field the till was found poorer in humus, nitrogen and organic carbon than the lacustral clay. The amounts of the above three constituents found in any of the plots depend more upon the relative proportions of the two types of soil occurring on the plots than upon the previous treatment.

The longer the fields have been kept in grasses mown for hay, the less has been the change in composition of the soil. Continuous bare cultivation. Along tree rows has caused greater losses than the alternation of fallow and crop in the adjacent fields. The extreme loss of nitrogen, humus and organic carbon in 25 years is about one-third of the amounts originally present in the prairie.

Bradley (1912) conducted pot experiments from which he pointed out that the nitrogen loss was appreciably reduced by legumes.

Mooers, Hampton, and Hunter (1912) reported that the loss of nitrogen was appreciably greater on limed plats than on unlimed plats, and that the effect extended below the depth of plowing. These investigators stated also that there was an increase in percentage of humus on the unlimed sections.

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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.

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  • PublisherForgotten Books
  • Publication date2024
  • ISBN 10 1332197868
  • ISBN 13 9781332197866
  • BindingPaperback
  • Number of pages31

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Paperback. Condition: New. Print on Demand. This book analyzes the effects of lime on organic matter in soils. The author studied the impact of lime applications on soil composition and crop yields across various treatments and cropping systems. The findings highlight discrepancies in previous research and underscore the necessity for further investigation. The experiments showcased that limed plots generally exhibited higher levels of organic carbon and nitrogen compared to unlimed plots, suggesting that lime may enhance soil fertility. However, the author notes that these effects can vary depending on soil conditions, climatic factors, and experimental methods. This book is a valuable resource for researchers, agriculturalists, and farmers seeking to understand the complex interactions between soil management practices and soil health. Forgotten Books publishes hundreds of thousands of rare and classic books. 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. The digital edition of all books may be viewed on our website before purchase. print-on-demand item. Seller Inventory # 9781332197866_0

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