Data from a 14-yr double-crop rice (Oryza sativa L.) experiment allowed com
parison of the long-term effects of N fertilizer from different sources (ur
ea and in situ grown azolla [Azolla microphylla Kaulf.] and sesbania [Sesba
nia rostrata Bremek. & Oberm.]) on IV balances, soil N pools (both total an
d available), and yields. Although data show that plant-available N was mai
ntained over time in both wet (WS) and dry seasons (DS), yields declined si
gnificantly, indicating a decline in physiological IV use efficiency. The y
ield declines were generally similar regardless of N source in both seasons
. The WS decline averaged 150 kg ha(-1) yr(-1) in the three added-N treatme
nts, while the DS decline averaged 185 kg ha(-1) yr(-1). After 27 crops, th
e cumulative positive N balance was estimated at 1244, 348, 646, and 1039 k
g N ha(-1) in control, urea, sesbania, and azolla treatments, respectively.
There was no significant change in soil total N content in the control and
urea treatments, whereas it increased to 344 to 541 kg after 27 crops in t
he sesbania and azolla treatments. Conservation of the soil N status and po
sitive N balance, in spite of the high amounts of N removed through grain a
nd straw, reflect the N contribution (13-46 kg ha(-1) crop(-1)) from nonsym
biotic N-2 fixation. In addition, sesbania and azolla were estimated to add
approximate to 57 to 64 kg ha(-1) crop(-1) through symbiotic N-2 fixation.
These results demonstrate that in rice-rice cropping systems biological N
fixation plays a vital role in replenishing the soil N pool. However, conti
nuous application of green manure N (GM-N) did not increase crop N availabi
lity, perhaps because of the presence of a recalcitrant soil organic matter
fraction. Residual effects on rice grain yield and N uptake were observed
only with GM-N sources.