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This article in AJ

  1. Vol. 73 No. 4, p. 660-664
     
    Received: June 5, 1980
    Published: July, 1981


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doi:10.2134/agronj1981.00021962007300040022x

Nitrogen Sources for Bean Seed Production1

  1. D. T. Westermann,
  2. G. E. Kleinkopf,
  3. L. K. Porter and
  4. G. E. Leggett2

Abstract

Abstract

Beans (Phaseolus vulgaris L.) often respond to N fertilization; however, N fertilization is not practiced for maximum seed production in southern Idaho. This suggests that the symbiotic relationship and/or soil N sources can provide most of the N needed by this legume. Our objective was to evaluate the relative contribution of the symbiotic-nonsymbiotic N sources by studying the effects of N fertilization on the symbiotic N2 fixation and seed yields under field conditions. Experiments were conducted on silt loam soils belonging to the Portneuf series (Xerollic Calciortnids). An acetylene reduction (AR) method was used to determine the effect of N fertilization treatments on the relative seasonal N2 (AR) fixation. The symbiotic N2 fixation was also estimated by the equation, N2 = Nup − (Ni + Nm − Nh)−αNf, where Nup is the accumulated N uptake measured near physiological maturity, N1 and Nh are the amounts of soil NO3-N in the root zone before planting and near physiological maturity, Nm is the N mineralized from soil organic N sources, and a is the recovery of the N fertilizer (Nf) applied. Estimates of the N fertilizer recoveries were obtained from two experiments using 15N-depleted (NH4)2 SO4.

The symbiotic N2 relationship contributed up to 90 kg N/ha, which was 40 to 50% of the total N found in bean plants near physiological maturity. The amount of symbiotic N2 fixed decreased as the available soil N or fertilizer N increased, and increased as the N required by the individual cultivars increased. The response to N fertilization depended upon the cultivar, as well as on the N available from soil sources. Measured fertilizer N recoveries ranged from 7 to 33%. An average of 52% of the total N uptake near physiological maturity was taken up after the maximum symbiotic N2(AR) rate occurred; while the seed contained an average of 60% of the total N uptake. A low N fertilization rate (< 50 kg N/ha) when the soil N1 was low (<50 kg N/ha) ensured an early vigorous plant growth but did not always increase seed yields. Higher N fertilization rates may be required on soils with lower amounts of mineralizable N.

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