Abstract: That toxic substances may be given out to soil by higher plants and that these substances may affect the growth of the same or other species is a theory which while old is not yet generally accepted. DeCandolle (8) noted that certain species appeared to be specifically inhibitory to the growth of associated species, as, for example, Euphorbia versus flax and thistles versus oats. On the basis of these observations deCandolle developed a theory of crop rotation embodying the general idea that each member in a rotation should be a species not inhibited in its growth by toxic substances left from the preceding crop. Liebig (15), while he originally supported the theory of deCandolle-, later and as a result of his exhaustive analyses on the depletion of soil minerals by crops, came to the conclusion that not only the amounts but the balances between inorganic materials in the soil are of importance in the growth of plants. On this basis he ultimately discounted the notion that toxic substances may be of importance in regulating crop yields. From the time of Liebig until the present day, plant growth interactions have been almost unanimously interpreted in terms of mineral nutrition effects, or more recently in terms of water competition. The interest in toxic secretions of plants arose in part from a consideration of so-called soil sickness due to one-crop agriculture. Thus it was frequently observed in early experiments that as a piece of ground was continuously cropped to one plant the yields decreased and that these decreases could not be made up by additional fertilizer. Besides the injurious after-effects or yieldlowering effects of one-crop agriculture, several cases of harmful interaction between plants grown adjacent to each other in a field, or of one crop on a succeeding crop, were also recorded. Thus effects of grass on fruit trees, of walnut trees on other plants, of corn, rye, thistles, turnips, sesame, rutabaga and others, were ob-