Abstract
IT type would of mechanism appear that involved plant physiologists in the longitudinal are not transport yet agreed of as materials to the type of mechanism involved n the lon itudinal ransport of m terials through the sieve-tube. Munch (8) has elaborated a theory involving a directed mass flow of solution, while others (1, 4) favour a movement of solute rather than solution and stress (2) the resemblance between the gross phenomena of transport and diffusion. The Druckstrom theory possesses a completeness and simplicity that has much to recommend it, while the theory of activated diffusion is rather vague concerning the method whereby diffusion through the sieve-tube is accelerated. As protoplasmic streaming has apparently to be rejected as a method of accelerating diffusion, and as respiration appears to be a factor in transport, the suggestion (7) has been 1 Paper No. 13 from the Physiological Department of the Cotton Research Station, Trinidad. [Annals of Botany, Vol. L. No. CXCVII, January, 1936.] M
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