Low Root Temperature Retardation of the Mineral Nitrogen Induced Decline in N2Fixation by a Northern Ecotype of White Clover

Nodulated white clover plants (Trifolium repensL.) of a Norwegian ecotype from Pasvik (70°N) were grown in flowing solution culture. Root temperature was 17°C until 51d after sowing, when it was lowered decrementally over 5d to 7°C in four of the eight plant culture units. After a further 24h, mineral N was supplied automatically at 20μMNH₄NO₃in three culture units at each root temperature (7 and 17°C) over 17d. The remaining two units provided control plants solely dependent on N₂fixation at 7 and 17°C.The supply of NH₄NO₃greatly reduced the nodule biomass per plant at 17°C over 17d compared with control plants, but had little effect at 7°C. The nodule decline at 17°C accompanied an acute and progressive decrease in specific rate of N₂fixation, from 9mmolN d^-1g^-1nodule d.wt on day 0 to zero by day 10. Whilst initial rates of N₂fixation were lower at 7°C, the mineral N-induced decrease in fixation rates was also less severe than at 17°C and specific fixation rates recovered after reaching a minimum on day 11. N₂fixation accounted for 36% of the total uptake of N by +min.N plants during the treatment period at 7°C as opposed to only 13% at 17°C. The total N₂fixed at 7°C was 86% of that fixed at 17°C, although the specific growth rate (d.wt) at 7°C was only 55% of that at 17°C. Addition of NH₄NO₃at 7°C had little effect on the gross amount of N₂fixed subsequently. In contrast, total N₂fixation by +min.N plants at 17°C was only 24% of that fixed by the corresponding controls. The possible mechanisms by which mineral N affects N₂fixation are discussed.