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Fort Hood Data Summary
(Storm Water Data)
Fort Hood streams are monitored using ISCO 4230 Bubble
Flow Meters and ISCO 3700 Automatic Water Samplers. A typical BREC
monitoring station is shown in this photo:

The equipment includes: shelter, rain gauge (top of
shelter on left) the 3700 water sampler, 4230 Flow Meter, and power system
(battery - located in blue tray- and solar panel - located on top
center of shelter). The 4230 Bubble Flow Meters have programmed to initiate
storm water sampling when streams rise above a determined depth (the programmed
depth is site specific for each of the 13 locations).
Three water samples are used to estimate loading for
each storm event using the following protocol:
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First
sample bottle taken for laboratory analysis is selected from the
sample that is collected closest to one-foot above base flow (the 4230
hydrograph records depth, and time when each sample is collected)
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Second water sample selected for laboratory analysis is
collected nearest peak of hydrograph
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Third sample is selected at the mid-point between
initiation and max on the descending arm of hydrograph
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Samples
and data are retrieved from the field and delivered to the laboratory
after storm events.
Record keeping, Field Data protocol:
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Retrieved weekly or following storm water runoff event
from ISCO 4230/6712 Bubble Flow Meter
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Stored
and managed in ISCO FlowLink database software Parameters stored in
FlowLink database include: Time,
Level, Flow, and Precipitation. FlowLink allows the manipulation and exportation of
data and summarizes it over any selected time interval
Data is stored and managed in a BREC Water Science
Laboratory Database.
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Lab
ID number (sequential)
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Sample
collection date
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Location
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Sample
type (grab, storm)
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Field
comments
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Bottle
number (from ISCO 3700 Automated Sampler)
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Lab
processing date
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Data -
(NO3, PO4, TSS, etc.)
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Lab
comments
Data Evaluation
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Flow is determined from measured level or stage
and slope/area method..
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Open channel estimated of flow based on level
using the Manning formula.
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Channel shape, slope and roughness is determined
for each gauging location; stage/discharge curve developed with
FlowMaster (Haestad Methods).
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Loading Calculation; ISCO
FlowLink data (stream flow and sampler events) exported to Excel for
merging with laboratory data from BREC Water Quality Database
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Field
data associated with laboratory data to estimate loading
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Determine
time intervals between samples are determined
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Determine
sample concentrations that are associated with
time intervals
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Determine
flow volume for a time interval.
The flow volume is multiplied by concentration to give load
estimates for each time interval
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Determine
loads for each time interval, which are summed for
individual storm loads
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Maintain final loading estimates in an MS Access
database for analysis and storage.
Data Summary
The following charts were prepared using Storm
Water Samples collected during 1996-2001.
Storm water samples are collected during storm events using ISCO 3700 auto
samplers. Samples were analyzed in our laboratory
using QAQP procedures and SOP's developed specifically for the Fort Hood
Water Quality Project using the same protocol used for grab
samples. The primary focus for storm samples is sediment
determination, however
our evaluation of storm samples includes: Nitrates, Ortho Phosphates,
TSS (sediment) rainfall, and flow. These four charts represent only nitrate concentrations
during the dates storm events were recorded, it is necessary to integrate
this data with
flow data to calculate stream loading during these events.




The final figure in this two part series is a comparison
of loading determined by integrating grab sample data (Base Load) and
storm water data (Storm Load) during the year 2000. To evaluate
“background” stream conditions, monthly grab samples are collected
during periods of “normal flow” to evaluate overall stream health. To
determine water quality conditions during storm water events when both
stream flow (quantity) and velocity (movement down stream) is dramatically
increased, ISCO Storm Water monitors and samplers are used.
Problems arise when monthly grab sampling data is
used to predict water quality conditions and determine total loading
during storm events. The pollution load dramatically increases during a
storm, which is rarely accounted for by the usual monthly sampling data.
Using monthly sample data in this manner assumes that the sample
concentration represents the concentration in the stream between samples.
This leads to errors when concentrations are not steady, which is
the case during storms.
Most of the total yearly stream loading is
transported during storm periods. Therefore, to determine accurate stream
loading, storms events need to be intensively sampled.
To demonstrate these differences, BREC scientists have used data
collected from one site on Cowhouse Creek during 2000 to express the
loading differences.
BREC Grab Sample Data Summary
Fort Hood Main Page
March 5, 2002
Dennis Hoffman, Project Leader;
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