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SU0000074 SSNL
Environmental Health - Public
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SU0000074 SSNL
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Entry Properties
Last modified
11/1/2019 2:30:34 PM
Creation date
9/9/2019 8:58:40 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0000074
PE
2622
FACILITY_NAME
MS-00-11
STREET_NUMBER
5533
Direction
E
STREET_NAME
QUASHNICK
STREET_TYPE
RD
City
STOCKTON
ENTERED_DATE
8/8/2001 12:00:00 AM
SITE_LOCATION
5533 E QUASHNICK RD
RECEIVED_DATE
6/5/2000 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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SJGOV\sballwahn
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\MIGRATIONS\Q\QUASHNICK\5533\MS-00-11\SU0000074\SS STDY.PDF
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EHD - Public
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September 30,2002 <br /> .Tab Number.LG02-310 <br /> Page 4 <br /> The presence of nitrates and DBCP are not uncommon in shallow ground-water aquifers <br /> in San Joaquin County and other parts of the Central Valley. Nitrate in ground water occurs as a <br /> r.,. result of the application of fertilizers, livestock waste, and untreated septic tank waste. Nitrate is <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.' It was thought that ground water at that <br /> time was close to a"natural'condition_ Based on the work by Bryan, it is estimated that under <br /> 4 natural conditions, ground-water concentration of nitrate is no more then about 13.5 NO3(3 <br /> mg/L-N). Areas having 24.75 mg/L NO3 (5.5 mg/L-N) or more are those in which nitrate <br /> r.. <br /> concentrations may increasing.3 <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 /> V. GEOLOGY, SOIL,AND PERCOLATION TEST <br /> �- The surficial geologic deposits near the site are reported to be composed of Pleistocene <br /> age(10,000 year to 2 million years ago) Modesto Formation. Foothill-derived alluvial silt, clay, <br /> and minor sand forming terraces,upper fans, and following distributaries across lower fans-, <br /> abundant volcanic detritus (Honcut, Wyman, Capay soils).' <br /> ' Bryan,K., 1923,Geology and ground-water resources of Sacramento Valley of California: U.S. <br /> Geological Survey Water-Supply Paper 495,285p. <br /> Hull,L.C., 1984,Geochemistry of Ground Water in the Sacramento Valley,California:U.S. Geological <br /> Survey Professional Paper 1401-B. <br /> i- 4 EPA, 1999,Drinking water and health,National Primary Drinking Water Regulations,consumer fact <br /> sheet on:DIBROMOCHLOROPRPOANE. Internet:http:l/www.epa.gov./OGWDW/dwh/c-soc/dibromoc.html <br /> ►.. 5 Marchand,D.E.and Bartow,J.A., 1979,Geologic Map of the Cenozoic deposits of the Bellota <br /> quadrangle,California. Scale 1:62:500. " <br /> DE RS H <br /> � N <br /> x + <br /> o - <br /> Ir. <br /> L.. <br />
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