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SU0010780 SSNL
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SU0010780 SSNL
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Last modified
5/7/2020 11:34:45 AM
Creation date
9/8/2019 12:44:14 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0010780
PE
2631
FACILITY_NAME
PA-1600007
STREET_NUMBER
9870
Direction
N
STREET_NAME
PEZZI
STREET_TYPE
RD
City
STOCKTON
Zip
95212-
APN
08902008
ENTERED_DATE
2/5/2016 12:00:00 AM
SITE_LOCATION
9870 N PEZZI RD
RECEIVED_DATE
2/5/2016 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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\MIGRATIONS\P\PEZZI\9870\PA-1600007\SU0010780\SS NL STDY.PDF
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' Soil Suitability/ Nitrate Loading Study 1��rracon <br /> Avanti Nut Co. ■ Stockton, CA <br /> May 19, 2016 ■Terracon Project No. NA167038 <br /> 1 1.4 Groundwater Information <br /> 1 .4.1 Groundwater Depth and Gradient <br /> Groundwater was not encountered in our percolation test holes excavated to depth of 41 inches <br /> and 252 inches on May 5, 2016. <br /> The San Joaquin County Flood Control and Water Conservation District Groundwater Report <br /> I (SJCWCD) Spring 2015 groundwater depth and elevation maps were reviewed to determine the <br /> groundwater levels near the Site. According to the Lines of Equal Depth to Groundwater Spring <br /> 2014 and Spring 2015 maps (Plates 3 and 4), depth to groundwater groundwater lies between <br /> approximately 100 to 120 feet bgs. Per the Department of Water Resources (DWR) Water Data <br /> Library an irrigation well', approximately 1,160 feet north-northwest of the site, had a depth to <br /> L groundwater of 130 feet on March 21, 2016. Based on a review of the SJCWCD Lines of Equal <br /> Elevation of Groundwater Spring 2015 map, groundwater flow gradient is generally to the north- <br /> northeast. The groundwater flow direction and the depth to shallow, unconfined groundwater, if <br /> present, would likely vary depending upon seasonal variations in rainfall and other <br /> hydrogeological features. Without the benefit of on-site groundwater monitoring wells surveyed to <br /> a datum, groundwater depth and flow direction beneath the site cannot be directly ascertained. <br /> Based on the topographic map (Plate 1) the approximate site elevation is 55-60 feet above mean <br /> sea level. <br /> 1 1.4.2 Potential Groundwater Contamination Issues <br /> The presence of nitrates is not uncommon in shallow groundwater aquifers in San Joaquin County <br /> and other parts of the Central Valley. Nitrate in groundwater occurs as a result of the application <br /> of fertilizers, livestock waste, and untreated septic tank waste. Nitrate is mobile and often <br /> ' accumulates in the shallow groundwater zones. <br /> In the early 1900s, natural levels of nitrate in groundwater were measured in forty-three (43)wells <br /> throughout the Sacramento Valley by Kirk Bryan (1923). It was thought that groundwater at that <br /> time was close to "natural' conditions. Based on the work by Bryan, it is estimated that under <br /> "natural" conditions, groundwater concentration containing nitrate is no more than about 13.5 <br /> mg/L-NO3 (3 mg/L-N). Areas having 24.75 mg/L-NO3 (5.5 mg/L-N) or more are those in which <br /> nitrate concentrations may be increasing (Hull, 1984). <br /> ' DBCP (dibromochloropropane) is a nematocide and soil fumigant for vegetables and grapes. It <br /> is thought to cause health problems consisting of kidney damage, liver damage, and cancer. The <br /> ' use of DBCP was discontinued in 1979. EDB (ethylene dibromide) was used in gasoline to <br /> prevent lead deposits and build up. It was also used in pesticides and fumigants. Exposure to <br /> EDB is linked to many adverse health effects stemming from organ damage to cancer. <br /> 1 <br /> ' htto://www.water.ca.covAvaterdatalibrary Groundwater level station site code:380578N1212017N001 <br /> Responsive ■ Resourceful m Reliable 5 <br />
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