Quantitative effects of soil nitrate, growth potential and phenology on symbiotic nitrogen fixation of pea (Pisum sativum L.)

• Published in: Plant and soil Vol. 243; no. 1; pp. 31 - 42
• Main Authors: Voisin, Anne-Sophie, Salon, Christophe, Munier-Jolain, Nathalie G., Ney, Bertrand
• Format: Journal Article
• Language: English
• Published: Dordrecht Kluwer Academic Publishers 01-06-2002; Springer; Springer Nature B.V; Springer Verlag
• Subjects: Absorption; Agricultural soils; Bacteria; Biological and medical sciences; Crops; Filling period; Fundamental and applied biological sciences. Psychology; Growth rate; Heat sums; Life Sciences; Microbiology; Minerals; Nitrates; Nitrogen; Nitrogen fixation; Nodules; Peas; Phenology; Plants; Soils; Vegetal Biology; Water availability; TECHNIQUE DES TRACEURS
• ISSN: 0032-079X; 1573-5036
• DOI: 10.1023/A:1019966207970

The influence of soil nitrate availability, crop growth rate and phenology on the activity of symbiotic nitrogen fixation (SNF) during the growth cycle of pea (Pisum sativum cv. Baccara) was investigated in the field under adequate water availability, applying various levels of fertiliser N at the time of sowing. Nitrate availability in the ploughed layer of the soil was shown to inhibit both SNF initiation and activity. Contribution of SNF to total nitrogen uptake (%Ndfa) over the growth cycle could be predicted as a linear function of mineral N content of the ploughed layer at sowing. Nitrate inhibition of SNF was absolute when mineral N at sowing was over 380 kg N ha-1. Symbiotic nitrogen fixation was not initiated unless nitrate availability in the soil dropped below 56 kg N ha-1. However, SNF could no longer be initiated after the beginning of seed filling (BSF). Other linear relationships were established between instantaneous %Ndfa and instantaneous nitrate availability in the ploughed layer of the soil until BSF. Instantaneous %Ndfa decreased linearly with soil nitrate availability and was nil above 48 and 34 kg N ha-1 for the vegetative and reproductive stages, respectively, levels after which no SNF occurred. Moreover, SNF rate was shown to be closely related to the crop growth rate until BSF. The ratio of SNF rate over crop growth rate decreased linearly with thermal time. Maximum SNF rate was about 40 mg N m-2 degree-day-1, equivalent to 7 kg N ha-1, regardless of the N treatment. From BSF to the end of the growth cycle, the high N requirements of the crop were supported by both SNF and nitrate root absorption but, of the two sources, nitrate root absorption seemed to be less affected by the presence of reproductive organs. However, since soil nitrate availability was low at the end of the growth cycle, SNF was the main source of nitrogen acquisition. The onset of SNF decrease at the end of the growth cycle seemed to be first due to nodule age and then associated to the slowing of the crop growth rate.