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SU0002496 SSNL
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SU0002496 SSNL
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Entry Properties
Last modified
5/7/2020 11:29:15 AM
Creation date
9/9/2019 9:08:45 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0002496
PE
2633
FACILITY_NAME
SA-01-23
STREET_NUMBER
13124
Direction
S
STREET_NAME
ROBINSON
STREET_TYPE
RD
City
ESCALON
ENTERED_DATE
10/29/2001 12:00:00 AM
SITE_LOCATION
13124 S ROBINSON RD
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\R\ROBINSON\13124\SA-01-23\SU0002496\NL STDY MGMT PLN.PDF
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EHD - Public
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• Second-, the City of Escalon Waste Water Treatment Facility. This facility is located <br /> approximately 1.5 miles southwest of the City of Escalon, on the north side of the <br /> Stanislaus River. The facility receives domestic effluent from the City of Escalon and <br /> industrial effluent from two food processors. Storm runoff is conveyed to the facility through <br /> the industrial pipeline. The domestic and industrial effluent are treated and disposed of in <br /> separate ponds. The City was required by the Regional Water Quality Control Board to <br /> submit a report that documented whether discharges to the ponds have caused, or are <br /> likely to cause, groundwater constituents to rise above background levels. Due to the <br /> highly heterorganic soil characteristic at the site, it was not determined if the location of the <br /> wells at the site are impacted by the force of the Stanislaus River-, thereby, influencing any <br /> downgradient wells. <br /> • Finally, Avena Drain, Lone Tree Creek and Johnny Creek. The Avena Drain runs on the <br /> south boundary of the property-, Lone Tree Creek runs approximately 1 mile south west of <br /> property; Little John Creek runs approximately 1 mile north of property. These resources of <br /> water travel from east to west and drain into the San Joaquin River. <br /> Impact to Underlying Groundwater and Downgradient Wells <br /> In all considerations to the groundwater, the conclusion from the soil samples demonstrate that <br /> the soil profile has layers of clay that have varying percentages of clay content, all being high, <br /> which will slow the penetration from surface water percolation down to the water table. This <br /> slowing of the percolation allows for a greater impact of drying periods. <br /> This dairy system will have a water storage volume that has a capacity greater than the <br /> requirements from both the county and state. These capacities will allow for containment of a full <br /> winter's manure volume, an above average winter rainfall plus a 25 year, 24 hour storm water <br /> volume. <br /> Considering these storage volumes, the manure effluent management system can be managed by <br /> plan, not managed by rainfall events. Well managed irrigation and return water flows, along with <br /> wet-dry cycles, will cause surface water not to penetrate the approximate 75 feet of the depth to <br /> static water table.' <br /> Although the presence of nitrate in the ground water indicate that there may be some agricultural <br /> contribution intrusion, _a",ut one of these values are well below the maximum contaminant level <br /> for drinking water established for nitrate of 45 mg/Liter (ppm). Furthermore, the consistent level of <br /> nitrate in the ground water indicates that the nitrate in these waters is more a result of a regional <br /> infiltration into the water table, rather than contribution from the any localized source. <br /> It is con tided that the proposed dairy expansion will not impact the downgradient ground water if <br /> proper manure effluent management is followed. <br /> Refer to page 30 for Endnotes and Reference Sources <br /> Soil Suitability Study <br /> Property Name and Address: Frank Faha Dairy, Inc., 12182 S. Robinson Road, Escalon,CA 95320 <br /> Page 27 <br /> Western Design/David Avila 2001 <br />
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