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SU0002206
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SU0002206
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Entry Properties
Last modified
5/7/2020 11:29:06 AM
Creation date
9/4/2019 6:45:08 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0002206
PE
2626
FACILITY_NAME
UP-99-01
STREET_NUMBER
11900
Direction
N
STREET_NAME
FURRY
STREET_TYPE
RD
City
LODI
Zip
95240
APN
06116026
ENTERED_DATE
10/26/2001 12:00:00 AM
SITE_LOCATION
11900 N FURRY RD
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\F\FURRY\11900\UP-99-01\SU0002206\APPL.PDF \MIGRATIONS\F\FURRY\11900\UP-99-01\SU0002206\CDD OK.PDF \MIGRATIONS\F\FURRY\11900\UP-99-01\SU0002206\EH COND.PDF \MIGRATIONS\F\FURRY\11900\UP-99-01\SU0002206\EH PERM.PDF
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EHD - Public
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WASTE DISCHARGE REQUIR9%dNTS ORDER NO. <br /> GOLDSTONE LAND COMPANY,LLC AND KURT KAUTZ <br /> BEAR CREEK WINERY <br /> SAN JOAQUIN COUNTY <br /> GROUNDWATER CONDITIONS <br /> 28. The winery is served by two deep groundwater production wells. The primary well is 135 feet <br /> deep and the backup well is 342 feet deep. The well locations are shown on Attachment B2, <br /> which is attached hereto and is made part of this Order by reference. <br /> 29. The primary well (shallow) produces water of lower quality than the backup (deep) well. Based <br /> on analytical testing performed in April 2001, the water supply is characterized in the RWD as <br /> follows: <br /> Constituent Unit Primary Well Backun Well <br /> pH std. 6.1 6.2 <br /> Specific Conductance µmhos/cm 915 576 <br /> Total Dissolved Solids mg/L 550 400 <br /> Calcium mg/L 82 55 <br /> Magnesium mg/L 34 21 <br /> Sodium mg/L 42 29 <br /> Potassium mg/L 2 2 <br /> Total Cations meq/L 8.8 5.8 <br /> Bicarbonate mg/L 300 250 <br /> Sulfate mg/L 31 23 <br /> Chloride mg/L 97 30 <br /> Nitrate as Nitrogen mg/L 9.5 5.7 <br /> Total Anions meq/L 9.0 5.8 <br /> 30. The Discharger constructed three groundwater monitoring wells at the facility in May 2001. The <br /> well locations are shown on Attachment B 1. <br /> 31. Based on monitoring events in June 2001, September 2001, April 2002, and July 2002 (the <br /> Discharger failed to perform groundwater monitoring in the Fourth Quarter 2001) the water table <br /> exists approximately 80 feet below the ground surface and groundwater flows toward the south <br /> with minor variations of the flow direction to the southwest and southeast. Monitoring well MW- <br /> 1 is near the eastern boundary of the facility site, cross-gradient of the existing LTU. MW-2 is at <br /> the upgradient edge of the LTU, and MW-3 is only slightly down-gradient from the LTU. The <br /> data are summarized in the following table. <br /> TDS NO3 as N EC Na Cl <br /> Well Name Date vHH (mg/L) (mgU (µmhos/cm) (mg(L) (mg/L) <br /> MW-1 June 2001 6.86 960 22 1,500 72 98 <br /> MW-1 Sept. 2001 6.92 1,000 30 1,600 NS NS <br /> MW-1 March 2002 6.84 723 24.3 1,440 54 75 <br /> MW-1 April 2002 6.30 932 18.5 1,480 NS NS <br /> MW-1 July 2002 6.41 1,212 18.6 1,720 NS NS <br /> Average 6.67 965 22.7 1,548 63 86.5 <br /> V,�m Joaquin Non]SS Oloie Pgcn Filcs� Cr=k\W R.tl c <br />
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