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This article in AJ

  1. Vol. 86 No. 2, p. 259-266
     
    Received: Apr 13, 1993
    Published: Mar, 1994


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doi:10.2134/agronj1994.00021962008600020010x

Forage Legume Roots and Nodules and Their Role in Nitrogen Transfer

  1. Markus Dubach and
  2. Michael P. Russelle 
  1. P .O. Box 49/532, Ulaanbaatar 210349, Mongolia, North East Asia;
    U SDA-ARS and Dep. of Soil Science, 439 Borlaug Hall, Univ. of Minnesota, St. Paul, MN, 55108-6028.

Abstract

Abstract

Legumes can transfer significant amounts of symbiotically fixed N to neighboring plants, and a putative pathway for N transfer is decomposition of fine roots (those that are not secondarily thickened) and nodules. Our objective was to quantify the amount of N in living and dead roots and nodules of alfalfa (Medicago sativa L.) and birdsfoot trefoil (Lotus corniculatus L.). These values were used with estimates of root length and nodule numbers that decomposed during a season to estimate the size of this pathway of N transfer. Birdsfoot trefoil and effectively and ineffectively nodulated alfalfa were grown in root observation boxes filled with 15N-labeled topsoil (Typic Hapludolls). Roots and nodules were removed according to age and analyzed for total N and C. Specific N content of fine roots older than 2 wk was 0.22 mg N m−1 in alfalfa and 0.14 mg N m−1 in trefoil, and did not change with age. Specific N content did not decline in dead, nondecomposed roots of N2-fixing plants, indicating either that no significant N remobilization occurred or that N import equaled N export in these organs. Large, active birdsfoot trefoil nodules (>2 mm) had twice the N content of large active alfalfa nodules. Dead nodules, observed in birdsfoot trefoil only, had significantly lower N content than live nodules, indicating N remobilization during senescence. Fine roots contained up to 69% of N from fixation in alfalfa and 47% in birdsfoot trefoil, and nodules contained 89% and 94% fixed N, respectively. We conclude that alfalfa releases more N through decomposing roots than nodules, whereas birdsfoot trefoil contributes more N to the soil through decomposing nodules than roots, but neither process could account fully for published estimates of N transfer.

Joint contribution of the USDA-ARS Plant Science Res, Unit, U.S. Dairy Forage Res. Ctr. (Minnesota Cluster), and Minnesota Agric. Exp. Stn., Paper no. 20 411 of the Minnesota Agric. Exp. Stn. scientific journal series.

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