Publication Date

1989

Description

The 15N natural abundance method for measuring N2 fix­ation by legumes has compared favourably with other methods (reviewed by Shearer and Kohl, 1986). This method is based on the small difference in 15N abundance between nitrogen (N) derived from N2 fixation and N derived from soil. The pro­portion of legume N fixed from atmospheric N2 (PN) is cal­culated using :

PN = (o15Nref - o15N1egume)/(015Nref - B)

where o15N is the per mil 15N excess over atmospheric N2 ; ref is a reference plant which obtains all of its N from soil; and B is the o15N of fixed N (a measure of isotopic fractionation during N2 fixation). Several authors (e.g. Mariotti el al., 1980; Steele et al., 1983) have estimated isotopic fractionation during N2 fixation, but it is unknown how constant that these estimates are. This paper reports on a study examining the effects of host plant, rhizobial strain, nutrition and moisture on isotopic fractionation during N2 fixation.

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Factors Affecting Isotopic Fractionation During Nitrogen Fixation by Pasture Legumes

The 15N natural abundance method for measuring N2 fix­ation by legumes has compared favourably with other methods (reviewed by Shearer and Kohl, 1986). This method is based on the small difference in 15N abundance between nitrogen (N) derived from N2 fixation and N derived from soil. The pro­portion of legume N fixed from atmospheric N2 (PN) is cal­culated using :

PN = (o15Nref - o15N1egume)/(015Nref - B)

where o15N is the per mil 15N excess over atmospheric N2 ; ref is a reference plant which obtains all of its N from soil; and B is the o15N of fixed N (a measure of isotopic fractionation during N2 fixation). Several authors (e.g. Mariotti el al., 1980; Steele et al., 1983) have estimated isotopic fractionation during N2 fixation, but it is unknown how constant that these estimates are. This paper reports on a study examining the effects of host plant, rhizobial strain, nutrition and moisture on isotopic fractionation during N2 fixation.