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SR0080203 SSNL
Environmental Health - Public
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SR0080203 SSNL
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Last modified
5/12/2020 4:21:25 PM
Creation date
4/30/2020 8:40:19 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0080203
PE
2602
FACILITY_NAME
PA-1000010
STREET_NUMBER
12
Direction
W
STREET_NAME
LORENZEN
STREET_TYPE
RD
City
TRACY
Zip
95304
APN
23914003
ENTERED_DATE
2/12/2019 12:00:00 AM
SITE_LOCATION
12 W LORENZEN RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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• Physical soil testing included percolation testing and particle size analysis,correlated with <br /> application rates to ensure management of future wastewater flows. Chemical testing included <br /> analyses for the constituents that influence nitrate loading. <br /> II. SOIL SUITABILITY STUDY FINDINGS <br /> A. SUBJECT PROPERTY AND SURROUNDING STUDY AREA INFORMATION <br /> SSS§ 1.1 Surrounding land use to the east, west, north and south of the project is, and has been, in <br /> agricultural production for many decades. The San Joaquin River is directly to the east, north and <br /> northwest. To the west is Interstate 5,the Town of Banta and the City of Tracy. New development <br /> is not occurring anywhere in close proximity to the subject property. The closest development is <br /> Oakwood Lakes, a residential community approximately two miles to the north. <br /> B. SOIL PHYSICAL CHARACTERISTICS AND ANALYTICAL TEST RESULTS <br /> The UC Davis SoilWeb indicates the majority of the disposal area to consist of a Columbia fine <br /> sandy loam, which is partially drained, 0 to 2 percent slopes, and is occasionally flooded (#131). <br /> However,the A&L Laboratory particle size analysis determined the soil to be a clay fraction at 21% <br /> sand, 38% silt and 41%clay. <br /> The soils can also be classified as "hydric soils." A hydric soil is a soil that formed under conditions <br /> of saturation, flooding, or ponding long enough during the irrigation and/or rainy season to develop <br /> anaerobic conditions in the upper portions of the soil. Anaerobic conditions promote denitrification. <br /> NLS§ 1.1, 1.2. Chemical analysis of a soil sample that was retrieved from the bottom of the 40-inch <br /> depth percolation test boring is noted on the A&L Laboratory Soil Analysis Report found in <br /> Appendix C. The important parameters for nitrate loading assessment are the organic matter, pH, <br /> cation exchange capacity(CEC), clay content percentage, and nitrate-nitrogen content. <br /> The nitrate-nitrogen at 1 ppm is very low, with the organic matter content at a surprisingly high <br /> percentage at 2.3%. The estimated nitrogen release (ENR) Organic matter, in combination with <br /> anaerobic soils are highly beneficial for denitrification. This is a significant explanation for the very <br /> low nitrate-nitrogen concentrations. <br /> Since septic effluent is composed predominately of ammonium(NH4),the pH, along with the CEC, <br /> are significant influences on ammonium molecules. The pH of the soil is neutral at 7.0 which may <br /> have very little affect on ammonium stability such as creating a propensity for ammonia(NH3) <br /> formation, which would likely occur under alkaline conditions. The CEC measures the ability of the <br /> soil to theoretically trap and hold positively charged ammonium molecules. The Cation Exchange <br /> Capacity of the soil sample is what was to be expected with a clay soil. Given the clay content, this <br /> suggests there is fair potential for the retention of ammonium molecules for microbial uptake and <br /> protein synthesis, and the suppression of nitrification. <br /> 2 <br /> Chesney Consulting <br />
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