Title: Shoal River RBF Evaluation Project Update
1Shoal River RBF Evaluation Project Update
- Erin Cox, CH2M HILL
- Jeff Littrell, Director Okaloosa County Water
Sewer - Steve Hubbs, WaterAdvice Associates
2Future Water Supply Options Under Evaluation for
Okaloosa County
- Riverbank Filtration (RBF)
- Direct Withdrawal
- Direct Withdrawal with Offline Storage Reservoirs
3Major Considerations and Constraints Related to
Project Feasibility
- Physical
- Geology, Hydrology, Soils, Topography
- Technical
- Engineering, Land Suitability and Availability,
Legal and Political Issues - Environmental
- Permits, Water Quality, Endangered Species
- Economic
- Cost/1000 Gallons, Resale Value, Ability to
Finance - Demands
- Ensure that existing and future demands justify
project need
4Project Background
- Okaloosa County has purchased 353 acres of high
quality riparian land along the Shoal River - A comprehensive evaluation of RBF feasibility is
underway
5Project Description
- The County is evaluating RBF and Direct Surface
Withdrawal at Shoal River property - Project is mainly focused on RBF first since it
provides pre-treatment (potential cost savings
for WTP) - Comprehensive literature review performed for
site, including geology, aquifer characteristics,
wetlands, water quality, etc. - CH2M HILL is performing geotechnical analyses
such as borings, piezometers, and potentially
near-capacity wells for further site suitability
evaluation - Test Boring and piezometer installation completed
- Slug testing performed to evaluate hydraulic
conductivity of aquifer
6Site Characteristics
7Site Characteristics
- Aquifer Characteristics
- Yellow shows extent of shallow sand and gravel
aquifer - Locally, aquifer exists in Citronelle Formation
most important water-yielding formation in upper
part of sand and gravel aquifer (USGS) - Citronelle formation is characterized white and
brown sand - Alum Bluff low permeability
8Site Characteristics
- Shoal River Hydrogeology
- Substantial flow
- average flow from 1939 2003 was 717 mgd
- Fluctuates appreciably with respect to stage and
flow, favorable for routine scour - 7-day, 10 year low flow 300 cfs, or 200 mgd
- Characteristics acceptable for up to 20-mgd
extraction
Flow 1997-2008
9Site Characteristics
- Geology
- The Citronelle Formation (Sand and Gravel
Aquifer) is characterized as reworked alluvial
sediments (sands, gravels, silts) - The Alum Bluff Formation is predominantly clay
(aquitard)
10Site Characteristics
- Streambed Slope
- The stream slope and hydrographs indicate that
the Shoal River in the area of concern has
adequate energy to maintain a clean coarse sand
bed which is favorable to bank filtration
11Why Riverbank Filtration?
12Riverbank Filtration (RBF) Benefits
- Turbidity and pathogens
- NOM, taste and odor, biodegradable compounds
- Nitrates
- Trace organics
- Pesticides
- Pharmaceuticals and Personal Care Products as
Pollutants (PPCPs) - Endocrine disrupting compounds
Riverbank Filtration (RBF)
13RBF Removal Mechanisms
14Factors that Impact RBF
- Stream and Riverbed Characteristics
- Water quality and temperature
- Stream flow, velocity, and slope
- Area of exposure of the aquifer to the river
bottom - Riverbed sheer stress
- Riverbed media composition and conductance
- River bottoms width and configuration
- Biological processes taking place within river
bottom - Aquifer Transmissivity
- Site hydrogeology
- Total driving head available from the aquifer
- Wellscreen Dynamics
15Riverbed Characteristics
16Aquifer Characteristics
17Exploratory Geological Boring
- Objectives
- To evaluate the presence and general
characteristics of the sands associated with the
Citronelle Formation in the vicinity of the
testing location along the Shoal River. - Test borings constructed as part of these
investigations penetrated the remaining
Citronelle Formation at the site and to terminate
at the top of the Alum Bluff Group.
18Exploratory Geological Boring
- Geotechnical borings have been completed in the
power line corridor on both the East and West
sides of the Shoal River
19Shoal River Preliminary Results
- Streambed Characteristics
- 10 streambed cores were taken, up to 4 feet deep
- Prevalent media was medium to coarse white sand,
originating from Citronelle Formation - Banks and low-flow areas contained alluvial
deposits from upstream cuts into the Alum Bluff - At every location probed, bed material favorable
for RBF to at least 3 feet deep
20Shoal River Geotechnical Preliminary Results
21Shoal River Geotechnical Preliminary Results
- The upper zone of the Citronelle Formation is
dark organic silty sands to sandy silts (0-8'
bls) - The lower zone of the Citronelle Formation is
fine to course quartz sand with minor sub-rounded
fine gravel (8-23' bls) - The sand varies from 15 to 20 feet thick and the
grain size coarsens with depth - The elevation of the Citronelle contact with the
Alum Bluff Formation is generally flat-lying
perpendicular to the Shoal River
22Shoal River Geotechnical Preliminary Results
23Preliminary Field Investigation Results
- The formation isnt as deep as we would like (20
to 25 feet saturated thickness as opposed to 35
to 50 feet desired) - The formation is better than anticipated with
regards to sand size and gradation - The results do not rule out RBF, but do point
towards a low-head collection system - Horizontal collector wells or siphon connected
vertical wells are viable options
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26Next Steps
- Compare the data from the pilot wells to the data
from the I-10 bridge borings for consistency - Develop the two piezometers and pump on a longer
term basis to confirm a good connection to the
river - Develop conceptual designs from options
- Model to estimate capacity
- Confirm consistency in aquifer throughout the
entire reach of stream (more test wells) - Test-pump the most desirable location