|
Nutrients in the Swan-Canning
Estuary || Stream
restoration of Wilson Creek
Ohio River ecosystem study ||
James River ecosystem study
Ohio River ecosystem study
The Ohio River ecosystem study is a collaborative research effort
with a fellow faculty member, Dr. Jeff Jack, initiated while I
was
at the University of Louisville. Diverse projects were supported
through funding from various sources, including comparative work
on the Ohio, Tennessee and Cumberland rivers with funding from
the Department of Energy through Murray State Center for Reservoir
Research, and
studies
of drinking-water contaminants, funded by the Environmental Protection
Agency through Western Kentucky University Technical Assistance
Program.
Most recently we have received funding to participate in EPA’s
Environmental Monitoring and Assessment Program focusing on great
river ecosystems. Much of the credit for the work we have accomplished
goes to three of my former Ph.D. students: Debbie Guelda and Rick
Koch, now at Bemidji State University, and Tim Sellers at Keuka
College. Dr. Kumud Acharya joined our research group in January
2004 and
has initiated new work focusing on nutritional energetics of riverine
zooplankton. Information presented below highlights some of our
forthcoming findings.
Effects of point source loadings, sub-basin inputs and longitudinal
variation in material retention on C, N and P delivery from
the
Ohio River basin. Bukaveckas et al. (forthcoming in Ecosystems;
due 2005).
LandSat7 image showing the Ohio River (from
top), two of its principal tributaries (Tennessee and Cumberland
rivers; from bottom) and
the confluence with the Mississippi (at left).
Spatial variability in material fluxes within large river basins
may arise from point source inputs, variable contributions from
sub-basins and longitudinal variation in material transformation
and retention. By measuring instantaneous fluxes throughout the
Ohio River basin, we were able to draw inferences about the importance
of these factors in determining the overall export of C, N and
P
from the basin. Our study spanned the lower 645 km of the Ohio
River and included all tributaries that contributed at least one
percent
of the volume of the Ohio River at its confluence with the Mississippi.
The intensively cultivated northern sub-basin (Wabash River) contributed
a large fraction of N and P entering the Ohio River. In the southern
sub-basins (Tennessee and Cumberland rivers), impoundments and
less
intense cultivation appear to diminish and delay material delivery,
particularly with respect to N. The southern rivers account for
a proportionately larger fraction of the water entering the Mississippi
River during low discharge conditions and this fraction has increased
during the past 50 years. The upper portion of the study reach
was found to be a net source of CHLa and DOC and a net sink for
inorganic
N, suggesting that this portion of the river provided a generally
favorable environment for autotrophic production. Point source
loadings of NH4 were significant inputs to the upper sub-reach
but a relatively small component of the overall budget for dissolved
inorganic N.
Experimental evidence for density-dependent effects and the
importance of algal production in determining population growth
rates of riverine
zooplankton. Guelda et al. (forthcoming in River Research and
Applications; due in 2005)
Photo of Bosmina longirostris, a common
zooplankter found in the Ohio River
and rivers throughout the world.
Food limitation effects on life-history traits of
lake zooplankton have been well documented, but few
studies have examined linkages
between population growth rates and food resources in riverine
environments. In rivers, allochthonous inputs of particulate
organic matter may
mitigate food limitation effects allowing density-independent mechanisms
associated with washout (discharge) and feeding interference
(turbidity)
to assume greater importance. We experimentally manipulated densities
of commonly occurring riverine zooplankton, Bosmina
longirostris
and cyclopoid copepods, within 2000 L mesocosms containing ambient
or algal-enriched food resources. The experiment was
repeated through
time (July, August, September) to represent the range of zooplankton
densities and food-resource levels observed in the
Ohio River during
warm-water, low-flow conditions. High growth rates and low sensitivity
to density-dependent effects were observed during
July when POC
and chlorophyll concentrations were highest. Lower growth rates
and stronger response to density-dependent effects
were observed
during August and September experiments when POC and chlorophyll
concentrations were lower. Direct manipulations of
algal abundance
resulted in higher growth rates when gains in chlorophyll were
accompanied by increases in the edible size fraction
(September experiment).
Algal C concentrations were found to be a significant predictor
of variation in population growth rates for Bosmina
but not cyclopoids.
Algal C concentrations in the Ohio River rarely fell below experimentally
derived minimum food thresholds but were often below saturation
thresholds,
suggesting that population growth rates were constrained by autochthonous
food resources despite the prevalence of allochthonous carbon.
Photo
of the Ohio River
experimental station (at the University of Louisville) used to
study riverine plankton communities in semi-controlled conditions.
|