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SU0006024 SSNL
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SU0006024 SSNL
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Last modified
5/7/2020 11:32:02 AM
Creation date
9/6/2019 9:54:54 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0006024
PE
2656
FACILITY_NAME
PA-0500776
STREET_NUMBER
24500
Direction
S
STREET_NAME
MACARTHUR
STREET_TYPE
DR
City
TRACY
APN
25024001
ENTERED_DATE
5/5/2006 12:00:00 AM
SITE_LOCATION
24500 S MACARTHUR DR
RECEIVED_DATE
5/3/2006 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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SJGOV\rtan
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\MIGRATIONS\M\MACARTHUR\24500\PA-0500776\SU0006024\NL STDY.PDF
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EHD - Public
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B. SOIL PHYSICAL CHARACTERISTICS AND ANALYTICAL TEST RESULTS <br /> The United States Department of Agriculture-Soil Conservation Service(USDA-SCS)indicates the on-site <br /> soils to consist of a Capay Clay-UrbanLand Complex (#122). This correlates with the average clay soil <br /> texture test results o£38% from the samples analyzed from the future filter bed soil. <br /> SS 5.2 a surface and subsurface soil investigation and testing began with three, 15464t deep borings 7 <br /> drill$d wi atruck-mounted drill rig: One boring near the center of the Future Filter Bed area, one boring in <br /> the Ex' mg LeachBeldarea,and one boring near the center of the Reserve.Le�chfield area. The Existing <br /> Leachfield area is presumably directly west of the office building, where there appeared to be a"green <br /> stripe"in the lawn area signifying a potential leachline. The soil boring was drilled next to this green stripe. <br /> Soil samples were taken every five feet for chemical and physical a lysis. In addition; soil samples were <br /> also taken from two shallow percolation test borings at the 24",and 366 depths from the future filter bed. <br /> These three deep borings provided: 1.)A profile of the underlying sl characteristics, 2.)Depth to <br /> groundwater, which was found to be approximately 11 feet below grade, 3.) Saturated formation(first <br /> aquifer)material type, analyzed to be predominately a clay soil type,and 4.)A water table sample for <br /> analysis, which is discussed on Page 7. No rust mottling was observed in any of the borings that would be <br /> indicative of seasonal soil saturation caused by a dramatic rise in the water table elevation. As discussed <br /> below,the water table has apparently risen t 8 feet below gr nd surface(bgs)from on-site monitoring <br /> well data. <br /> NLS§ 1.1, 1.�2�As the noted on the SOIL ANALYSIS REPORTS,chemical analyses of the soil samples <br /> quantify several constituents that will influence_nitrate.loading from this project. The important parameters <br /> for nitrate loading assessment are the organic matter,pH cation exchange capac-4(CEC ,clay dontent <br /> percentage,along with nitrate-nitrogen content and Total Kjeldahl Nitrogen(TKN)content.TION measures <br /> the organic and ammonia fractions of nitrogen. It was tested for two reasons: 1.)To determine any increase <br /> in TKN concentrations under the existing leachfield for comparison with the other two sample sites, and 2.) <br /> To establish a baseline in the event soil under the future filter bed is ever tested for a monitoring program. <br /> There was no significant difference among the three soil samples for TKN. <br /> As noted,the organic matter in the soil is expectedly low. This suggests a very low potential for future <br /> nitrate-nitrogen loading from indigenous nitrogen soil content. Since septic effluent is composed <br /> predominately of ammonium(NH4), the pH, along with the CEC, are significant influences on ammonium <br /> molecules. The pH of the soil is moderately alkaline which may slightly inhibit ammonium formation and j <br /> stability,and may create a small propensity for ammonia(NH,) formation. The CEC measures the ability of <br /> the soil to theoretically trap and hold ammonium molecules. Cation Exchange Capacities of the soil <br /> samples are in the high teens and twenties, which suggests there is some potential for the retention of <br /> LLdniveway <br /> onium molecules for microbial uptake, and suppression of nitrification. <br /> Standard Penetration Test(SPT)results illustrated i Table l are the number of blows required to drive <br /> ndard two-inch O.D. split spoon sampler one foot into-undisturbed soil with a 140-pound weight falling <br /> ches. Relative condition of clay soils from this procedure can be classified as soft,medium, stiff,very <br /> and hard. As observed,only two of the SPT tests show a very stiff clay soil, while the remaining soil is <br /> ified as stiff. These two tests classifying the soil as stiff were found in the future filter bed area. <br /> equently, it was decided to drill two additional 15 ft deep borings south of the existing entrance <br /> to test for not only for this very stiff clay stratum,but also for more permeable strata(borings <br /> d not be drilled to the north because of railroad tracks). The very stiff stratum was not encountered to <br /> outh of the proposed filter bed location, signifying this stratum is intermittent. Strata with greater <br /> eability(e.g., sand, silty sand)were also not encountered. <br /> 3 <br /> Chesney Consulting <br />
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