Nitrogen is considered an important limiting element in ricefields. Th
e importance of fertilizer as a source of nitrogen for rice and denitr
ification as a pathway of nitrogen varies among ricefields depending o
n agricultural practices. Ecological network analysis was applied to r
icefields of the Ebro Delta (N. E. Spain) in order to establish (1) th
e fate of nitrogen sources to the fields (2) the importance of and int
eraction between aquatic and benthic processing of nitrogen cycling an
d (3) the importance of internal recycling and the role of straw burie
d in sediment at the end of the cultivation period. Fertilizer is the
major source of nitrogen during the first month of the cultivation per
iod. During the initial (INI) phase rice incorporates the equivalent o
f 92.8% of the nitrogen added. Only about half of the fertilizer added
is incorporated during the second addition. Aquatic compartments are
highly dependent upon sediment nitrogen as a source. The loss of phyto
plankton between submersed (SUB) and emergent (EME) phases can be part
ially explained by a decrease of nitrogen flux from sediment to water.
An important dependence of rice upon straw was observed: about 20% of
the nitrogen comes from straw. High Finn Cycling Index (FCI) values o
ccur at the beginning of the cultivation period but the highest FCI va
lue was for the end phase according to the high nutrient loads to rice
fields. The indirect relationship between FCI and the number of cycles
can be explained by a correlation based on the removal of phytoplankt
on during the latter phases.