Abstract

Subterranean clover (Trifolium subrerraneum L.) was grown under controlled environmental conditions in pots containing a variety of soils. Non-destructive assays were used to measure rates of acetylene (C2H2) reduction by the plants. Soil mineral nitrogen (N) status and, to a lesser extent, soil salinity were found to be the most important soil properties relating to the development of C2H2reduction activity in subterranean clover. Application of KNO3 to pots resulted in an immediate decrease in the rate of C2H2reduction. A linear relationship was found between the loss in C,H, reduction activity and the amount of N applied up to 40 mg N kg-1 soil. Addition of salt (NaCl) to pots caused an immediate decrease in C2H2 reduction activity, followed by a gradual recovery. A linear relationship was found between the loss in C2H2 reduction activity and the level of soil salinity induced by salt addition. The loss in C2H2reduction \vas reflected in the lower total N content of the plants when soil salinity levels exceeded 4 mS cm-1.

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