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SU0004463_SSNL
EnvironmentalHealth
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99 (STATE ROUTE 99)
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2600 - Land Use Program
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SA-01-04
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SU0004463_SSNL
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Entry Properties
Last modified
11/19/2024 1:52:15 PM
Creation date
9/8/2019 12:51:21 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0004463
PE
2632
FACILITY_NAME
SA-01-04
STREET_NUMBER
11492
Direction
N
STREET_NAME
STATE ROUTE 99
City
LODI
ENTERED_DATE
5/20/2004 12:00:00 AM
SITE_LOCATION
11492 N HWY 99
RECEIVED_DATE
1/22/2001 12:00:00 AM
QC Status
Approved
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SJGOV\sballwahn
Supplemental fields
FilePath
\MIGRATIONS\N\HWY 99\11492\SA-01-04\SU0004463\NL STDY.PDF
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EHD - Public
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April 3,2001 <br /> Job Number: LGO1-074 <br /> Page 5 <br /> mobile and often accumulates in the shallow ground-water zones. <br /> In the early 1900's, natural levels of nitrate in ground water were measured in forty-three <br /> (43) wells throughout the Sacramento Valley by Bryan.2 It was thought that ground water at that <br /> time was close to "natural"conditions. Based on the work by Bryan, it is estimated that under <br /> "natural" conditions, ground water concentration containing nitrate is no more then about 13.5 <br /> NO3 (3 mg/L-N). Areas having 24.75 mg/L NO3 (5.5 mg/L-N) or more are those in which nitrate <br /> concentrations may be increasing.' <br /> DBCP was not detected in the water sample. DBCP is a nematocide and soil fumigant <br /> for vegetables, and grapes. It is thought to cause health problems consisting of kidney damage, <br /> liver damage, and cancer. The use of DBCP was discontinued in 1979. The Environmental <br /> Protection Agency(EPA) set the maximum contaminate limit(MCL) at 0.2 parts per billion <br /> (ppb) because the EPA believes that given present technology and resources,this is the lowest <br /> level to which water systems can reasonably be required to remove this contaminate should it <br /> occur in drinking water.' <br /> VI. GEOLOGY, SOIL, AND PERCOLATION TEST <br /> The surface geology at the site is shown on Atwater's map and is composed of the <br /> Holocene and (or) upper Pleistocene age alluvium of Calaveras River and Vicinity' (Plate 6). <br /> Alluvium of the Calaveras River and Vicinity was deposited by Calaveras River, Bear Creek, and <br /> several lesser streams between the Mokelumne and Stanislaus Rivers. The alluvium of Calaveras <br /> River appears to overlie part of the Pleistocene age(about 10,000 to 2-million years old) <br /> Modesto Formation near the site. The Modesto Formation is generally composed of river <br /> 2 Bryan,K., 1923,Geology and ground-water resources of Sacramento Valley of California:U.S. <br /> Geological Survey Water-Supply Paper 495,285p. <br /> 3 Hull,L.C., 1984,Geochemistry of Ground Water in the Sacramento Valley,California:U.S.Geological <br /> Survey Professional Paper 1401-B. <br /> 'EPA, 1999,Drinking water and health,National Primary Drinking Water Regulations,consumer fact <br /> sheet on:DIBROMOCHLOROPRPOANE. Internet:http://www.epa.gov./OGWDW/dwh/c-soc/dibromoc.html <br /> 5 Atwater,B.F., 1982,Geologic Maps of the Sacramento-San Joaquin Delta,California: U.S.Geologic <br /> Survey Miscellaneous Field Survey Map MF-1401,21 Sheets,Scale 1:24,000. <br /> �cRs i <br /> s <br /> z '• <br /> o � <br /> mss o c� <br />
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