Abstract

This study was conducted to determine whether the inhibition of net NO−3 uptake by NH+ 4 in cotton roots is due to inhibition of NO− 3 influx per se, and/or enhancement of efflux. Two cotton species, Pima (Gossypium barbadense L.) and Acala (G. hirsutum L.), which differ in NO− 3 influx and efflux, were used. Seedlings were grown hydroponically for 10 to 11 d and then induced for NO− 3 uptake with 0.01, 0.10, or 1.0 mM NO− 3 Net uptake was determined by following NO− 3 depletion from uptake solutions, containing 0.1 mM NO− 3, in the presence or absence of 10 mM NH+ 4 Roots induced with 0.01 mM NO− 3 contained only 5 to 6 μmol NO− 3 g−1 fresh weight (FW) after the induction treatment. In these roots, net NO− 3 uptake was equivalent to influx, and was not inhibited by NH+ 4 Roots induced with 0.1 mM NO− 3 contained 36 to 38 μmol NO− 3 g−1 FW, and NH+ 4 inhibited net NO− 3 uptake albeit after a lag of ≈12 min. In contrast, roots induced with 1.0 mM NO− 3 contained 65 μmol NO− 3 g−1 FW, and NH+ 4 immediately inhibited net uptake. Exposure to NH+ 4 increased NO− 3 efflux by both species. At similar root NO− 3 concentrations, NH+ 4 inhibited net NO− 3 uptake and stimulated efflux more in Pima than in Acala cotton. These results indicate that the response of both cotton species to NH+ 4 is dependent upon root NO− 3 concentration, and supports the argument that NH+ 4 has little effect on NO− 3 influx, but inhibits net uptake by stimulating efflux.

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