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SU0000094 SSNL
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SU0000094 SSNL
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Entry Properties
Last modified
11/22/2019 10:54:07 AM
Creation date
11/22/2019 10:09:29 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0000094
PE
2622
FACILITY_NAME
MS-99-16
STREET_NUMBER
11200
Direction
E
STREET_NAME
MONCURE
STREET_TYPE
RD
City
RIPON
ENTERED_DATE
8/8/2001 12:00:00 AM
SITE_LOCATION
11200 E MONCURE RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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SJGOV\gmartinez
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EHD - Public
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November 24, 1999 <br /> Job Number.S99272 <br /> Page 4 <br /> attached in the appendix. Test results indicate that DBCP was not detected(ND) and nitrate was <br /> found at 22 mg/1 as NO3 (4.8 mg/1 as N). The nitrate detected in the ground water was reported <br /> as NO3 by FGL and is below the maximum drinking water standard of 45 mg/l. This level is <br /> equivalent to 4.8 mg/1 as N for the maximum drinking water standard of 10 mg/l. <br /> The presents of nitrates and DBCP are not uncommon in shallow ground-water aquifers in <br /> San Joaquin County and other parts of the Central Valley. Nitrate in ground water originates <br /> from agricultural fertilizers, livestock waste, and untreated septic tank waste. Nitrate is mobile <br /> and often accumulates in the shallow ground-water zones. In the early 1900's,natural levels of <br /> nitrate in ground water were measured in 43 wells throughout the Sacramento Valley by Bryan.' <br /> It was thought that ground water at that time was close to"natural"conditions. Based on the <br /> work by Bryan it is estimated that under"natural"conditions, groundwater concentration of <br /> nitrate is no more then about 3 mg/1-N. Areas having 5.5 mg/1-N or more are those in which <br /> nitrate concentrations may be increasing. 2 <br /> DBCP is a nematocide and soil fumigant for vegetables, and grapes. It is thought to cause <br /> health problems consisting of kidney damage,liver damage, and cancer. The use of DBCP was <br /> discontinued in 1979. <br /> VL GEOLOGY,SOILS,AND PERCOLATION TEST <br /> The geology of the site and surrounding area is reported to be the lower member of the <br /> Pleistocene age Modesto Formation consisting of unconsolidated and unweathered gravel, sand, <br /> silt, and clay3 (Plate 6). These types of deposits are commonly unconsolidated arkosic sediment, <br /> often heterogeneous in nature, and correspond with the Tioga glaciation in the Sierra Nevada. <br /> The soils located on the site are reported to be the Veritas fine sandy loam(Plate 7). The <br /> Veritas fine sandy loam is described by the Soil Survey report as"moderately well drained, nearly <br /> I Bryan,K, 1923,Geology and ground-water resources of Sacramento Valley of California:U.S. <br /> Geological Survey Water-Supply Paper 495,285p. <br /> 2 Hull,L.C., 1984, Geochemistry of Ground Water in the Sacramento Valle}. California: U.S. Geological <br /> Survey Professional Paper 1401-B. <br /> 3 RW.Page, 1986,Geology of the Fresh Ground-Water Basin of the Central Valley,California,with <br /> Texture Maps and Sections. Unites States Geologic Survey Professional Paper 1401-C. <br /> ?pE RSO <br /> 1 � <br /> Z W <br /> O ti <br /> r <br /> �SSOG\ <br />
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