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The Effect of Soil Structure on the Character of Alfalfa Root‐Systems 1
Author(s) -
Carlson F. A.
Publication year - 1925
Publication title -
agronomy journal
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.752
H-Index - 131
eISSN - 1435-0645
pISSN - 0002-1962
DOI - 10.2134/agronj1925.00021962001700060006x
Subject(s) - character (mathematics) , citation , state (computer science) , root (linguistics) , agricultural experiment station , library science , mathematics , history , computer science , agriculture , linguistics , archaeology , algorithm , philosophy , geometry
During the past decade considerable attention has been given to the study of the influence of soil structure on the development of alfalfa root-systems. Experiments (~ and 2)~ have been reported showing that compact soil appears to cause greater branching and less pronounced taproots, while the open or porous soils tend to produce long, slender taproots with few branches. These results characterize in part the features of the root-systems of the hardy alfalfas and the non-hardy alfalfas, as it is generally accepted that the hardy alfalfas have broad deep-set cro~vns, well-developed rooting rhizomes, and numerous branch roots, while the non-hardy alfalfas have small highset crowns and slender taproots with few branches. This would seem to indicate that the features of the root-systems of, the hardy alfalfas and the non-hardy alfalfas are dependent, at least partially, upon soil structure. The tendency is, however, to attribute inherent characteristics to the hardy alfalfas and non-hardy alfalfas irrespective of soil structure. This has been particularly true among commercialists who have given a great deal of publicity to the hardy alfalfas as having resistant qualities due to inherent characteristics. In order to obtain further information concerning the development of alfalfa root-systems various varieties and strains of alfalfa were grown; first, in field plats which offered different soil structure; second, in tanks which had been filled with different classes of soil; and third, in water cultures.

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