FORAGE LEGUME ROOTS AND NODULES AND THEIR ROLE IN NITROGEN TRANSFER

Citation
M. Dubach et Mp. Russelle, FORAGE LEGUME ROOTS AND NODULES AND THEIR ROLE IN NITROGEN TRANSFER, Agronomy journal, 86(2), 1994, pp. 259-266
Citations number
35
Categorie Soggetti
Agriculture
Journal title
ISSN journal
00021962
Volume
86
Issue
2
Year of publication
1994
Pages
259 - 266
Database
ISI
SICI code
0002-1962(1994)86:2<259:FLRANA>2.0.ZU;2-S
Abstract
Legumes can transfer significant amounts of symbiotically fixed N to n eighboring plants, and a putative pathway for N transfer is decomposit ion of fine roots (those that are not secondarily thickened) and nodul es. Our objective was to quantify the amount of N in living and dead r oots and nodules of alfalfa (Medicago sativa L.) and birdsfoot trefoil (Lotus corniculatus L.). These values were used with estimates of roo t length and nodule numbers that decomposed during a season to estimat e the size of this pathway of N transfer. Birdsfoot trefoil and effect ively and ineffectively nodulated alfalfa were grown in root observati on boxes filled with N-15-labeled topsoil (Typic Hapludolls). Roots an d 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 i n alfalfa and 0.14 mg N m-1 in trefoil, and did not change with age. S pecific N content did not decline in dead, nondecomposed roots of N2-f ixing plants, indicating either that no significant N remobilization o ccurred or that N import equaled N export in these organs. Large, acti ve birdsfoot trefoil nodules (>2 mm) had twice the N content of large active alfalfa nodules. Dead nodules, observed in birdsfoot trefoil on ly, 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 con tained 89% and 94% fixed N, respectively. We conclude that alfalfa rel eases more N through decomposing roots than nodules, whereas birdsfoot trefoil contributes more N to the soil through decomposing nodules th an roots, but neither process could account fully for published estima tes of N transfer.