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.