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SU0008376 SSNL
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SU0008376 SSNL
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Entry Properties
Last modified
5/7/2020 11:33:28 AM
Creation date
9/6/2019 10:31:39 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0008376
PE
2622
FACILITY_NAME
PA-1000155
STREET_NUMBER
390
Direction
W
STREET_NAME
JAHANT
STREET_TYPE
RD
City
ACAMPO
APN
00309024 28
ENTERED_DATE
7/23/2010 12:00:00 AM
SITE_LOCATION
390 W JAHANT RD
RECEIVED_DATE
7/22/2010 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\J\JAHANT\390\PA-1000155\SU0008376\SS STDY.PDF
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EHD - Public
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The sample was placed on ice and transported under chain of custody to FGL <br /> Environmental, Stockton. Results of the tests are forthcoming. <br /> Nitrate is commonly detected in shallow ground water aquifers of the Central Valley. <br /> Application of fertilizers, livestock waste, and untreated septic tank waste can all <br /> contribute to nitrate in ground water. Nitrate is mobile and tends to accumulate in <br /> shallow ground water zones. Based on work in the Sacramento Valley from the early <br /> 1900s, it is estimated that under "natural" conditions, ground water contains nitrate at <br /> concentrations no more then about 13.5 mg/L-NO3 (3 mg/L-N). Nitrate may be <br /> increasing in areas with concentrations of 24.75 mg/L-NO3 (5.5 mg/L-N) or more (Hull, <br /> 1984). <br /> DBCP is a nematocide and soil fumigant for vegetables and grapes. It is known to <br /> cause male reproductive effects and is classified as a probable human carcinogen. <br /> Most domestic use of DBCP was discontinued in 1977 through 1979. The US EPA set <br /> the MCL at 0.2 parts per billion (ppb) because it believes that given present technology <br /> and resources, this is the lowest level to which water systems can reasonably be <br /> required to remove this contaminant should it occur in drinking water. The Maximum <br /> Contaminant Level Goal (MCLG) for DBCP is zero. <br /> tlioil Profile and-Geologic Information <br /> The Site is depicted on the Preliminary geologic map showing Quatemary deposits of <br /> the Lodi Quadrangle, California (Marchand and Atwater, 1979). The Site is depicted <br /> primarily within the Riverbank Formation middle unit, described as "arkosic alluvium <br /> forming Mokelumne River terraces and alluvial fan; chiefly sand; probably glacial <br /> outwash." Portions of the Site also fall within the Modesto Formation upper member, <br /> described as " arkosic sand forming low dunes on the Mokelumne River fan in the Delta; <br /> probably eolian, although not well sorted." Holocene intertidal deposits, described as <br /> "marsh, swamp, and channel sediments generally at least 1 m thick; mainly peat, muck, <br /> and mud," are present along the west side of the Site (Plate 7). <br /> The surface and near surface soils located at the Site are reported by the USDA Web <br /> Soil Survey to be composed of Bruella sandy loam, Jahant loam, and San Joaquin loam <br /> (Plate 8) (USDA, 2009). The table below presents some selected properties of these <br /> soils. <br /> L.OGE1015 <br /> Page 4 <br /> s <br />
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