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Corn (Zea mays L.) plants were grown for 4 and 6 weeks in sand culture at root-zone temperatures of 15, 20, and 25 C and P levels of 2, 9, and 30 ppra P to test the hypothesis that increased P could overcome the effects of low root-zone temperature. Growth of roots, sheaths, and blades was restricted when plants were exposed to rootzone temperatures of 15 or 20 C and P levels of 2 or 9 ppm P, compared to growth at 25 C and 30 ppm P. Concentration of total P in all plant parts was as great at 15 as at 25 C. The harmful effects of low root-zone temperature were not overcome by the application of higher P rates. Concentration of inorganic P and the fraction of total P that was inorganic P were higher at the lower temperature for shoots and P-deficient roots. Free sugar levels in roots were lower at 25 than at 15 C at all P levels. Sugar levels in sheaths and blades, however, were lower at the higher temperature only under P-deficient conditions. Concentrations of aconitate and soluble amino acids were highest at 15 C, irrespective of P supply. Since metabolism of photosynthate to the level of organic and amino acids was not impeded by low root-zone temperature, it is suggested that low temperature stress was depressing growth by restricting incorporation of amino acids into protein.
Key Words: Zea mays (L.) P nutrition Soluble N Low temperature stress
2 Research Assistant, Department of Agronomy; Soil Scientist, USDA, and Associate Professor, Cornell University; and Professor, Cornell University, respectively. The senior author is now Assistant Professor, Department of Crop Science, North Carolina State University at Raleigh.
Received for publication November 1, 1971.
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