『Abstract
The great spatial and temporal variability of nitrogen (N) processing
introduces large uncertainties for quantifying N cycles in large
scales, e.g. a watershed scale, and hence challenges the present
techniques in measuring ecosystem N mass balance. The dual isotopes
of nitrate (δ18O and δ15N) integrate signals
for both nitrate sources and N processing, making them promising
for studies on large scale N cycling. Here, the dual isotopes,
as well as some ion tracers, from a subtropical river in south
China were reported to identify the main nitrate sources and to
assess the possible occurrence and degree of denitrification in
the context of monsoon climate. Our results indicated that nitrification
of reduced fertilizer N in soil zones was the main nitrate source,
with sewage and manure as another important source in dry winter.
Seasonal changes of denitrification was apparent by the 〜1:2 enrichment
of δ18O and δ15N from April to August, and
suggested to occur over the watershed rather than in the river.
The lowest denitrification (10%) occurred in April, when the fertilizer
application was strongest and the monsoon rainfall abruptly increased,
causing enhancement of leaching. The highest denitrification (48%)
took place in august due to the high soil temperature and moisture.
In December, denitrification was significant (26%) perhaps due
to the high enough temperature for microbial activities, whereas
the low soil moisture appeared to limit the degree of denitrification.
This study suggests that the seasonal variations in denitrification
should be taken into account when estimating regional N mass balance.
Keywords: Nitrate; Dual isotope; Denitrification; River』
Introduction
Samples collection and analysis
Background
Samples and experiment
Results
Discussion
Seasonal variations of nitrate sources and dynamics
Denitrification
Conclusions
Acknowledgments
References