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SR0082012 SSNL
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SR0082012 SSNL
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Last modified
2/10/2022 2:07:32 PM
Creation date
5/21/2020 9:22:13 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0082012
PE
2602
FACILITY_NAME
16475 S TIDE RD
STREET_NUMBER
16475
Direction
S
STREET_NAME
TIDE
STREET_TYPE
RD
City
RIPON
Zip
95366
APN
20310017
ENTERED_DATE
4/24/2020 12:00:00 AM
SITE_LOCATION
16475 S TIDE RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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16475 TIDE ROAD Project No.2019-00072 Page 14 <br /> A geologic well log (Well Completion Report No. WP0037172) for the nearby site located <br /> approximately 500 feet northwest of the Site at 15127 French Camp Road indicated hardpan from 4 <br /> to 6 feet below ground surface. <br /> 2.2 Mass Transport Soil Properties <br /> Fine sandy loam and sandy loam,such as the fine-grained soil layers reported for the Veritas soil at <br /> the site typically do not provide a large degree of protection between percolating effluent at the <br /> surface and ground water aquifers,however,the cemented pan layer reported will. Therefore,soils <br /> of this type do not typically present a moderate risk of excessive mass transport of nitrate or other <br /> constituents of concern. <br /> 3.0 GROUNDWATER ANALYSIS <br /> 3.1 Regional and Site-Specific Groundwater <br /> The San Joaquin County Flood Control and Water Conservation District(2016)groundwater reports <br /> were reviewed to determine the groundwater levels near the Site. The Fall 2016 and Spring 2016 <br /> maps are the most current official maps available from the County. According to these maps,(Plates <br /> 5 and 6) in Appendix A,groundwater elevation lies between 5 and 0 feet below mean sea level (msl) <br /> in the spring and fall,respectively. The elevation of the land,as previously mentioned in Section 1.1, <br /> is approximately 60 feet above mean sea level.Therefore,the depth to groundwater(the difference <br /> between the elevation of the Site and the elevation of groundwater),ranges between approximately <br /> 55 and 60 feet below the ground surface (bgs), depending on the season. The groundwater in the <br /> vicinity of the Site appears to flow to the north, toward a cone of depression during the spring, and <br /> north-northeast during the fall,at a gradient of approximately 10 feet per mile. <br /> 3.2 Potential Groundwater Contamination Issues <br /> The Site is located within a rural residential area and near parcels involved in agricultural practices; <br /> groundwater contamination can result from activities related to farming practices where chemicals <br /> are applied to crops which may permeate to groundwater. The Site and surrounding properties <br /> utilize septic systems; leakage from septic tanks or failed septic systems can introduce bacteria to <br /> groundwater. <br /> 3.3 Current and Future On-Site Groundwater Uses <br /> The use of ground water for drinking water is planned for the proposed development. There is <br /> currently no domestic well onsite,however,a domestic well is planned for the site. <br /> 4.0 SOURCES AND IMPACT OF NITRATE TO GROUNDWATER <br /> 4.1 Current Off-Site Sources of Nitrate <br /> Septic systems and agriculture in the area may be the most significant sources of nitrate. In an <br /> attempt to determine the septic system density for the vicinity of the site,our office reviewed a recent <br /> aerial photograph available from GoogleEarthTM.We counted the clusters within approximately one <br /> square mile of the site,with the assumption each building cluster has one septic system. Using th' <br /> Petraloglx Engineering,Inc- <br /> 26675 <br /> nc26675 Bruella Road,Galt,Ca 95632 <br /> (209)300-5729 up <br /> www.petraloglx.com <br />
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