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ONE DOES not need to delve far into the voluminous literature pertaining to mineral absorption by plants to be convinced that there are many factors which may, either directly or indirectly, affect this process. Therefore, it seems only reasonable that to measure the effects of transpiration upon mineral absorption it will be necessary to keep all of these other influential factors as nearly constant as possible.For example, in an earlier paper by the writer on this subject (Freeland, 1936) the significance of the data was somewhat obscured by inequalities in growth and dry weight of the plants. Furthermore, the importance of such factors upon mineral absorption as synthesis of foods, assimilation, and shoot-root growth is well illustrated by the work of Gustafson (1934), Muenscher (1922), Mendiola (1922, and others.