wAbstract
@We used stream chemistry and hydrogeomorphology data from 549
stream and 447 river sites to estimate NO3-N
removal in the Upper Mississippi, Missouri, and Ohio Rivers. We
used two N removal models to predict NO3-N
input and removal. NO3-N input ranged from
0.01 to 338 kg km-1 d-1 in the Upper Mississippi
River to 0.01-54 kg km-1 d-1 in the Missouri
River. Cumulative river network NO3-N input
was 98700-1012676 Mg year-1 in the Ohio River, 85961-89288
Mg year-1 in the Upper Mississippi River, and 59463-61541
Mg year-1 in the Missouri River. NO3-N
output was highest in the Upper Mississippi River (0.01-329 kg
km-1 d-1), followed by the Ohio and Missouri
Rivers (0.01-236 kg km-1 d-1) sub-basins.
Cumulative river network NO3-N output was
97499 Mg year-1 for the Ohio River, 84361 Mg year-1
for the Upper Mississippi River, and 59200 Mg year-1
for the Missouri River. Proportional NO3-N
removal (PNR) based on the two models ranged from 0.01 to 0.28.
NO3-N removal was inversely correlated with
stream order, and ranged from 0.04 to 8.57 kg km-1
d-1 in the Upper Mississippi River to 0.001-1.43 kg
km-1 d-1 in the Missouri River. Cumulative
river network NO3-N removal predicted by
the two models was: Upper Mississippi River 4152 and 4152 Mg year-1,
Ohio River 3743 and 378 Mg year-1, and Missouri River
2277 and 197 Mg year-1. PNR removal was negatively
correlated with both stream order ( r = -0.80--.87) and the percent
of the catchment in agriculture (r = -0.38-0.76).
Keywords: Nitrogen removal; River networks; Mississippi River
basinx
Introduction
Methods
@Site selection
@Stream chemistry
@River networks, hydrology, and land use
@Nitrate input, output and removal
@Statistical analyses
Results
Discussion
Acknowledgements
References