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The Effects of Pollution Reduction
on a Wild Trout Stream
Baseline Studies Report: 2005
November 2005
Note:
The 2005 & 2006 baseline report and the 2007
progress report are posted.
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Spring Run
Dumpling Run |
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The Effects of Pollution Reduction on a Wild Trout Stream
Baseline Studies Report: 2005
Introduction
Spring Run is a
unique aquatic resource in the Potomac Highlands region of West
Virginia. Unlike many small headwater streams that tend to go dry,
it is fed by the largest spring in the region, with discharge
typically ranging from 3000-3500 gallons per minute. With a
temperature of ~53 °F at the spring and a pH of ~8, aquatic
conditions are ideal for trout and the aquatic insects they eat.
Spring Run flows about two miles from the spring source to its
confluence with South Mill Creek, which is about four miles from the
South Branch of the Potomac River. Spring Run has no tributaries.
Much of the stream is shallow, and does not provide the complex
habitat that trout need - but that is not the case in a
three-fourths mile section in the middle of the Run.
Since the early
1960’s, landowner’s have issued permits for fly fishing,
catch-and-release on three-fourths mile of Spring Run. Landowners
and other interested parties have installed and maintained various
structures to form pools and overhead cover that provide hiding and
feeding habitat for trout. Spring Run is recognized as one of the
best "wild" rainbow trout fisheries in West Virginia. Friends of
Springs Run’s Wild Trout, was formed in 1996 to restore structure to
Spring Run following flooding in 1996.
In the last few
years, however, fishermen have noted a decline in the fishery.
Emergence of the mayfly, Ephemerellidae (sulfurs) disappeared in the
late 1990s. The number of large trout (14” and above) has decreased
and trout in the 11-13” range are also fewer. The population of
trout is considerably lower in the lower reach of the three-fourths
mile section. Algae formation is heavy in the upper reach of the
three-forth mile section, much heavier than in the past, and algae
reforms soon after washout by high water.
There have long
been plenty of nutrients in Spring Run, contributed largely in
effluent from the Spring Run Trout Hatchery located about one-half
mile upstream near the spring. (SRH is a rearing facility; trout are
not spawned there). In recent years, however, SRH has been producing
more rainbow and “golden trout” for stocking West Virginia streams,
and it seems that the effluent stream now may be a problem for the
health of Spring Run. WVDEP issued a citation for violation of the
Spring Run Trout Hatchery NPDES permit in January 2004, specifically
for discharging excess biochemical oxygen demand (BOD) and total
suspended solids (TSS). WVDNR, which operates SRH, is now preparing
to install an effluent treatment process at the facility to meet
their permit requirements.
Installation of
effluent treatment at SRH provides a unique opportunity to address a
number of issues of both regional and national significance:
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Will the
hatchery effluent treatment process significantly reduce
nutrient discharge? Fish hatcheries throughout the country
produce nutrient-rich effluents of concern to receiving waters.
This study will evaluate the downstream result of effluent
reduction of BOD and TSS, as well as nutrients, from a small but
high throughput point source. The results of renovation at SRH
and this study will provide important information to the WV
Potomac Tributary Strategy point source innovation process.
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What are the
biological impacts of Spring Run's high nutrient levels, and how
is the biota affected by reductions in nutrients, TSS and BOD
following hatchery upgrades? This issue is of importance to the
nutrient criteria development process that WV and the other 49
states are currently struggling through, as one of the key
questions is: "what does nutrient impairment look like?"
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Is the wild
trout population in Spring Run being harmed by hatchery
effluent, and does improvement in that effluent improve the
trout fishery?
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Is the
benthic invertebrate population in Spring Run being harmed by
hatchery effluent, and does improvement in that effluent improve
diversity? Spring Run fishermen have noted the loss in recent
years of a certain family of mayflies, the Ephemerellidae (Spiny
crawler mayfly) that used to emerge regularly in the
springtime. Also, WV DEP’s Tim Craddock did a benthic
assessment of Spring Run in 2002, and found the lower part of
the fly fishing section to be dominated by Chironomidae (midge)
larvae, a group often indicative of pollution by organic waste.
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Why do
trout, especially larger fish, favor the upper part of the
fly-fishing section? Why has the density-center of the trout
population moved upstream in recent years? Is there a
relationship between distribution of benthic invertebrates in
the stream and trout distribution? If the Ephemerellidae mayfly
rebound after the hatchery effluent is treated, will the trout
population improve also? In particular, are trout avoiding areas
they used to frequent that are now dominated by midge larvae? If
upgrades to the hatchery reduce organics in the stream and also
the midge populations, will trout return to those areas? If
that turns out to be true, and we could demonstrate that it is
true, that would buttress public acceptance of benthic
invertebrate stream assessments.
Overall, this
project will have the potential to be used to address many questions
beyond the five questions identified above.
Partners
Friends of
Spring Run’s Wild Trout, Cacapon Institute (CI), the WV Conservation
Agency (WVCA), WV Department of Agriculture (WVDA), WV Division of
Natural Resources (WVDNR), WV Department of Environmental Protection
(WVDEP), and the Freshwater Institute are partnering in this study.
This project is funded primarily by West Virginia Conservation
Agency’s participation through the Chesapeake Bay Program. An
associated sediment reduction project is funded through a Friends of
Spring Run’s Wild Trout 2005 Stream Partners Grant.
WVDA, WVDEP and
WVDNR are all contributing in-kind services to the project. WVDA is
collecting water samples, taking flow measurements, and performing
field and laboratory water quality analyses. WVDEP is participating
in collections of benthic invertebrate and periphyton and helping to
cover the costs of analysis. WVDNR is performing fish surveys and
Friends of Spring Run’s Wild Trout is providing information on size
and location of trout caught and released by permitted fly
fisherman.
The Freshwater
Institute provided guidance to WVDNR on treatment methods for their
effluent and is providing technical guidance for the project. WVCA
is acting as project coordinator. Cacapon Institute has overall
technical oversight for the project, will participate in field work,
and will, in cooperation with partnering organizations, be
responsible for data analysis and production of annual reports.
Methods
The project has
two experimental components, an upstream/downstream design in Spring
Run, and a control/experimental design that includes Dumpling Run,
another spring fed stream nearby. Both streams have their origins
in the same geology: limestone (Helderberg and Tonoloway/Wills
Creek) and sandstone (Oriskany, McKenzie) formations. Spring Run
flows off the ridge to the northwest into South Mill Creek, a
tributary of the South Branch of the Potomac River. Dumpling Run
flows east into the South Fork of the South Branch of the Potomac
River.
The
upstream/downstream part includes three sites in Spring Run: the
first site is near the spring upstream of the hatchery; the second
site is in the upper part of the fly fishing stream section; and the
third is in the lower part of the fly fishing section. There are two
sites on Dumpling Run, one just below the spring, the other some
distance downstream. Overall, this design allows within stream and
between stream comparisons. Under most conditions of flow the
springs constitute the main source of water in both streams, but
both streams also have periodic surface flow entering the main
channel upstream of the spring.
Water
chemistries are collected monthly from April through September,
typically on Wednesday. We chose to avoid collections on Mondays at
the time of the hatchery cleanout because the "biosolids from the
aquaculture effluent are notoriously patchy and difficult to
characterize in sampling. . . . my thoughts on the nutrients is to
focus on the residual chronic impacts, not the pulse of the cleaning
plume" (Joe Hankins, Freshwater Institute, personal communication).
Water quality
parameters include nitrogen in the forms of ammonia-nitrogen,
nitrate/nitrite, total Kjeldahl nitrogen, total nitrogen (the sum of
nitrate/nitrite and TKN), soluble reactive phosphorus, total
phosphorus, total suspended solids (TSS), biochemical oxygen demand
(BOD5), and basic field parameters (pH, temperature,
conductivity) (see Appendix 2 for laboratory methods). Flow
measurements are collected at the same time as water samples at one
site in each stream. This work is done primarily by the WVDA.
Benthic
invertebrate and periphyton samples are collected twice each year at
all sites, in May and August, according to the standard protocols in
use by the WVDEP. WVDEP format Rapid Bioassessment Protocol habitat
analyses will be conducted once each year. Primarily WVDEP and
Cacapon Institute will do the fieldwork for this component.
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WVDNR will conduct electro shocking fishery assessments,
and the permitted fly fishermen of Spring Run have been enlisted to
record information on size and location of trout caught and
released.
Since changes to
the system may not occur rapidly, an assessment will be made at the
end of the third year to determine if “out year” monitoring might be
needed?
The methods used to analyze water quality data were
graphical and statistical. Data distributions were displayed using
box plots (figure at right), which are useful for side-by-side
visual comparisons of data distributions. Because the data set is
small (six data points at each site), traditional box plots with
25th and 75th quartiles were deceptive. Rather than use
quartiles, the box boundaries are the 2nd and 5th
data point in each series. One way analysis of variance (ANOVA) was
run on rank transformed data for comparison of median concentration
distributions. An alpha value of 0.05 was used as the threshold for
statistical significance. If a significant difference among group
medians was detected, Tukey’s multiple comparison test was used on
the rank transformed data to determine where differences were
located (Helsel and Hirsh, 1992). Statistics were calculated using
JMP Statistical Discovery Software (version 4.0.2). Summary
statistics and raw data are provided in Appendix XX.
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Baseline Water
Chemistry & Flow Data Results
Pre-treatment
results and analysis the water quality data will focus on five
questions:
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How does the
spring source water of the two streams compare? It is assumed
that the springs constitute the main source of water in both
streams, certainly true at most conditions of flow. Note: both
streams have surface flow entering the main channel upstream of
the spring.
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How does the
water in the control stream change as it flows downstream?
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How does the
water in the experimental stream change as it flows downstream?
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Are there
significant differences in water chemistry at any of the sites?
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How did
water quality vary over time?
While viewing
the baseline results, it is important to recognize that the data set
is small (six monthly samples each site), which reduces the power of
statistical tests to detect differences. |
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RESULTS |
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Field
Parameters:
pH,
Dissolved Oxygen and Conductivity (see Appendix 1 for
summary statistics). |
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pH
Source
Water:
pH in
the main source water for the two streams was similar, with
data ranging narrowly from 7.4 to 8.0 and 7.4 to 8.2 in
Dumpling Run and Spring Run, respectively.
Control
Stream Trends:
median pH tended to increase in a downstream direction.
Experimental Stream Trends:
median pH tended to decrease in a downstream direction in
Spring Run, with Spring Run at the bottom station
distinctly, although not significantly, lower than the other
two sites.
Significant differences:
pH in SR Bottom was significantly lower than DR Lower. |
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Conductivity
Source
Water:
Median
conductivity in the two streams was very similar, with data
ranging broadly from 45.8 to 372 and 64.6 to 390.0 (μs/cm)
in Dumpling Run and Spring Run, respectively.
Control
Stream Trends:
median conductivity did not change in a downstream
direction.
Experimental Stream Trends:
Median conductivity was lower (not significantly) at the two
downstream sites than the source water in Spring Run.
Significant differences:
No sites were significantly different. |
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Dissolved Oxygen
Source
Water:
Median
dissolved oxygen in the two streams was similar and high,
with data ranging from 9.2 to 11.1 and 10.0 to 11.5 (mg/l)
in Dumpling Run and Spring Run, respectively.
Control
Stream Trends:
DO
trended slightly higher in a downstream direction.
Experimental Stream Trends:
DO was slightly higher at SR Bottom.
Significant differences:
there were no significant differences. |
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Laboratory Parameters:
Ammonia, TKN, Nitrate, Nitrite, Total Nitrogen, Total
Phosphorus, Total Suspended Solids, Biochemical Oxygen
demand. (See Appendix 1 for summary statistics). |
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Ammonia-Nitrogen
Source
Water:
Median
ammonia in the main source water for the two streams was
similar and low. However, while the data range in Dumpling
Run was relatively small (0.003 to 0.082 mg/l), the range in
Spring Run was large (0.003 to 0.915 mg/l). It is possible
that the one high value was a one-time anomaly, but we have
no way to know.
Control
Stream Trends:
no
trends are apparent.
Experimental Stream Trends:
Ammonia was higher at the middle site, then decreased in
the downstream direction. The reduction in ammonia between
SPR Middle and SPR Bottom is likely due to normal in-stream
processes that convert ammonia to nitrate.
Significant differences:
SR
Middle is significantly higher than DR Spring. |
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Total Kjeldahl NItrogen
Source
Water:
Median
TKN in the two streams was very similar, with data ranging
broadly from 0.041 to 0.758 and 0.099 to 0.271 (mg/l) in
Dumpling Run and Spring Run, respectively.
Control
Stream Trends:
median TKN did not change in a downstream direction.
Experimental Stream Trends:
Median TKN was higher (not significantly) at the two
downstream sites than the source water in Spring Run.
Significant differences:
No sites were significantly different. |
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Nitrate-Nitrogen
Source
Water:
Median
nitrate (NO3-N) in the two streams was
significantly higher in SR than DR. Data in both streams
ranged narrowly from 0.17 to 0.38 and 0.37 to 0.59 (mg/l) in
DR and SR, respectively.
Control
Stream Trends:
median nitrate did not change in a downstream direction.
Experimental Stream Trends:
Median nitrate and the range of values increased in the
downstream direction (not significantly).
Significant differences:
All SR sites had significantly higher nitrate than DR at its
source; SR Middle and Lower had higher nitrate than DR
Lower. |
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Nitrite-Nitrogen
Source
Water:
Median
nitrite (NO2-N) concentrations in the two streams
were below detection limits. Each site had a single
measurable concentration during a high water event in
August.
Control
Stream Trends:
median nitrite did not change in a downstream direction.
Experimental Stream Trends:
Nitrite was typically detectable at low concentrations at
the two downstream sites.
Significant differences:
All SR sites had significantly higher nitrite than DR at its
source; SR Middle and Lower had higher nitrite than DR
Lower. |
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Total Nitrogen
Source
Water:
Median
Total N was distinctly (not significantly) higher in SR than
DR. Data in both streams ranged broadly from 0.25 to 1.14
and 0.48 to 2.45 (mg/l) in DR and SR, respectively.
Control
Stream Trends:
median TN did not change in a downstream direction.
Experimental Stream Trends:
Median TN was higher (not significantly) at the two
downstream sites than in the source water in SR.
Significant differences:
TN in SR Middle was higher than DR at the source. |
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Total Phosphorus
Source
Water:
Median
Total Phosphorus in the two streams was very similar, with
data ranging from 0.007 to 0.059 and 0.013 to 0.046 (mg/l)
in DR and SR, respectively.
Control
Stream Trends:
median TP did not change in a downstream direction.
Experimental Stream Trends:
TP was distinctly (and significantly) higher at the two
downstream sites than in the source water in Spring Run.
Significant differences:
TP in SR Middle and SR Bottom was significantly higher than
all other locations. |
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Total Suspended Solids
Source
Water:
Median
Total Suspended Solids was similar, ranging broadly from
45.8 to 372 and 64.6 to 390.0 in Dumpling Run and Spring
Run, respectively.
Control
Stream Trends:
median TSS decreased slightly in a downstream direction.
Experimental Stream Trends:
Median TSS increased in a downstream direction (not
significantly.
Significant differences:
No sites were significantly different. |
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Biochemical Oxygen Demand
Source
Water:
Median
Biochemical Oxygen Demand was distinctly (but not
significantly) higher in DR than SR. Data ranged broadly in
DR from 1.01 to 3.13 and narrowly in SR from 0.86 to 1.58
(mg/l).
Control
Stream Trends:
median BOD did not change in a downstream direction,
although the range of values was lower downstream.
Experimental Stream Trends:
Median BOD did not change in a downstream direction, but the
range of values was greater downstream than at the
source.
Significant differences:
No sites were significantly different.
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Flow measurements were
taken at the Dumpling Run Lower and Spring Run Bottom sites. Flow
in Dumpling Run ranged from about one third to one half of the flow
in Spring Run (figure at left). Water samples were collected on
three days with fairly low water (June, July, and September), two
moderate flow (April and May), and one high water (August).
Since we are
most concerned with local effects in this study, concentration is
the most relevant way to look at the data. However, flow is
necessary for interpretation of the time series data presented
below.
The flow
stations are not suitable surrogates for flows at all of the
stations. This is particularly an issue in Spring Run, where a
significant portion of the total stream flow is diverted at the
springhouse to the trout hatchery and does not flow through the
upper channel where samples are collected. This means that we
cannot reasonably estimate parameter loadings at any sites but those
with flow measurements.
How did water
quality vary over time?
The following four time-series bar graphs and
associated text show how total N, total P, TSS and BOD5 varied
during the baseline sampling period. |
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Total nitrogen varied widely and generally tracked with
flows at all sites (see correlation tables below). The
highest levels were observed in August during a high water
event. |
Total phosphorus varied widely over time at all sites and
did not vary with flow levels (see correlation tables
below). The phosphorus from the hatchery was evident at all
flows, and the three highest readings at SR Middle and
Bottom occurred at lowest, highest and second lowest flows. |
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TSS varied widely and very roughly tracked with flows at all
sites (see correlation tables below). The highest levels
were observed in August during a high water event. |
BOD5 varied substantially between sites. BOD in Spring Run
sites varied with flows, while concentrations in Dumpling
Run had no discernable pattern (see correlation tables
below). |
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Correlation Analysis
The following
four tables present simple correlation analysis on the
un-transformed sample data for key parameters: total N, total P, TSS,
BOD5, and flow. The purpose of the four tables is to partition
effects that might be due to different factors, such as point and
non point sources of pollution. The first table offers correlations
on all sites, the second Spring Run only, the third Dumpling Run
only, and the fourth excludes point source impacted sites in Spring
Run. More sophisticated approaches will be used in future reports
when the size of the data set makes them more appropriate.
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Table 1. Correlations for key parameters and flow at all stations.
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Total N (mg/L) |
TP (mg/L) |
TSS (mg/L) |
BOD5 (mg/L) |
FLOW (cfs) |
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Total
N (mg/L) |
1.0000 |
** |
*** |
* |
*** |
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TP
(mg/L) |
0.4216 |
1.0000 |
n.s. |
n.s. |
n.s. |
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TSS
(mg/L) |
0.9191 |
0.2813 |
1.0000 |
** |
*** |
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BOD5
(mg/L) |
0.3759 |
-0.0505 |
0.4365 |
1.0000 |
n.s. |
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FLOW
(cfs) |
0.8365 |
0.2197 |
0.7987 |
0.2874 |
1.0000 |
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Table 2. Correlations for key parameters and flow for Spring Run
stations only. |
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Total N (mg/L) |
TP (mg/L) |
TSS (mg/L) |
BOD5 (mg/L) |
FLOW (cfs) |
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Total
N (mg/L) |
1.0000 |
n.s. |
*** |
** |
*** |
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TP
(mg/L) |
0.3173 |
1.0000 |
n.s. |
n.s. |
n.s. |
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TSS
(mg/L) |
0.9832 |
0.2411 |
1.0000 |
** |
*** |
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BOD5
(mg/L) |
0.6300 |
0.0432 |
0.5862 |
1.0000 |
*** |
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FLOW
(cfs) |
0.8293 |
-0.0597 |
0.8269 |
0.7771 |
1.0000 |
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Table 3. Correlations for key parameters and flow for Dumpling Run
stations only. |
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Total N (mg/L) |
TP (mg/L) |
TSS (mg/L) |
BOD5 (mg/L) |
FLOW (cfs) |
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Total
N (mg/L) |
1.0000 |
n.s. |
*** |
n.s. |
*** |
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TP
(mg/L) |
0.2753 |
1.0000 |
n.s. |
* |
n.s. |
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TSS
(mg/L) |
0.9217 |
0.2572 |
1.0000 |
n.s. |
*** |
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BOD5
(mg/L) |
0.4981 |
0.6347 |
0.4650 |
1.0000 |
n.s. |
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FLOW
(cfs) |
0.8873 |
0.0368 |
0.9013 |
0.3905 |
1.0000 |
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Table 4. Correlations for key parameters and flow for all stations
except SR Middle and SR Bottom (i.e. NPS stations).
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Total N (mg/L) |
TP (mg/L) |
TSS (mg/L) |
BOD5 (mg/L) |
FLOW (cfs) |
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Total
N (mg/L) |
1.0000 |
n.s. |
*** |
n.s. |
*** |
|
TP
(mg/L) |
0.3636 |
1.0000 |
n.s. |
n.s. |
n.s. |
|
TSS
(mg/L) |
0.9338 |
0.3814 |
1.0000 |
n.s. |
*** |
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BOD5
(mg/L) |
0.1290 |
0.4550 |
0.1904 |
1.0000 |
n.s. |
|
FLOW
(cfs) |
0.8625 |
0.1273 |
0.7669 |
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