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SR0084710_SSNL
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Last modified
2/8/2022 10:34:44 AM
Creation date
2/8/2022 9:45:33 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0084710
PE
2602
FACILITY_NAME
16133 N MOORE RD
STREET_NUMBER
16133
Direction
N
STREET_NAME
MOORE
STREET_TYPE
RD
City
LODI
Zip
95242
APN
02702016
ENTERED_DATE
1/11/2022 12:00:00 AM
SITE_LOCATION
16133 N MOORE RD
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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EHD - Public
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Soil Suitability / Nitrate Loading Study <br />Munsch Property ■ Lodi, California Irerracon <br />January 7, 2022 ■ Terracon Project No. NA217092 <br />Table 4. <br />Expected On -Site Maximum Septic Tank Usage <br />vauons per day (gpd) <br />The maximum daily flow rate for the proposed 3 -bedroom residence is 420 gpd. The proposed 2 - <br />bedroom second residence is 280 gpd. <br />1.4 Groundwater Information <br />1.4.1 Groundwater Depth and Gradient <br />Groundwater was not encountered within our percolation test borings which were hand augered <br />between 3.0 and 8.0 feet below grade surface (bgs). According to the California Department of <br />Water Resources Sustainable Groundwater Management Act (SGMA) Data Viewer, in Spring <br />2021 depth to groundwater was reported between approximately 40 to 50 feet bgs, in Spring of <br />2020 depth to groundwater was between 30 and 40 feet bgs and in Fall of 2019 depth to <br />groundwater was between 30 and 40 feet bgs. Based on a review of the Spring and Fall elevation <br />contours groundwater gradient was reported to the southeast with a southwest groundwater <br />gradient. <br />The groundwater flow direction and the depth to shallow, unconfined groundwater, if present, <br />would likely vary depending upon seasonal variations in rainfall and other hydrogeological <br />features. Without the benefit of on-site groundwater monitoring wells surveyed to a datum, <br />groundwater depth and flow direction beneath the site cannot be directly ascertained. <br />1.4.2 Potential Groundwater Contamination Issues <br />Potential groundwater contamination can occur from a number of sources including historical <br />petroleum hydrocarbon use, agricultural activities, dairies, septic systems, and storm water <br />infiltration. As per EHD requirements nitrate as N and 1,2-dibromo-3-chloropropane (DBCP) have <br />been included as part of the SSS discussion. Identifying potential groundwater contamination <br />other than nitrates and DBCP is beyond the scope of work for this report. <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 />Responsive ■ Resourceful ■ Reliable 7 <br />Number of people per <br />Average effluent <br />Maximum Septic <br />Residence <br />Number of bedrooms <br />bedroom <br />quantity per person <br />Tank Usage <br />(gpd') <br />(gpd`) <br />Proposed 3 -Bedroom <br />Residence <br />3 <br />2 <br />70 <br />420 <br />Proposed 2 -Bedroom <br />Second Residence <br />2 <br />2 <br />70 <br />280 <br />vauons per day (gpd) <br />The maximum daily flow rate for the proposed 3 -bedroom residence is 420 gpd. The proposed 2 - <br />bedroom second residence is 280 gpd. <br />1.4 Groundwater Information <br />1.4.1 Groundwater Depth and Gradient <br />Groundwater was not encountered within our percolation test borings which were hand augered <br />between 3.0 and 8.0 feet below grade surface (bgs). According to the California Department of <br />Water Resources Sustainable Groundwater Management Act (SGMA) Data Viewer, in Spring <br />2021 depth to groundwater was reported between approximately 40 to 50 feet bgs, in Spring of <br />2020 depth to groundwater was between 30 and 40 feet bgs and in Fall of 2019 depth to <br />groundwater was between 30 and 40 feet bgs. Based on a review of the Spring and Fall elevation <br />contours groundwater gradient was reported to the southeast with a southwest groundwater <br />gradient. <br />The groundwater flow direction and the depth to shallow, unconfined groundwater, if present, <br />would likely vary depending upon seasonal variations in rainfall and other hydrogeological <br />features. Without the benefit of on-site groundwater monitoring wells surveyed to a datum, <br />groundwater depth and flow direction beneath the site cannot be directly ascertained. <br />1.4.2 Potential Groundwater Contamination Issues <br />Potential groundwater contamination can occur from a number of sources including historical <br />petroleum hydrocarbon use, agricultural activities, dairies, septic systems, and storm water <br />infiltration. As per EHD requirements nitrate as N and 1,2-dibromo-3-chloropropane (DBCP) have <br />been included as part of the SSS discussion. Identifying potential groundwater contamination <br />other than nitrates and DBCP is beyond the scope of work for this report. <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 />Responsive ■ Resourceful ■ Reliable 7 <br />
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