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SSSPof <br /> On November 1, 2011,the perc test borings were drilled in the referenced location. The <br /> i <br /> idf the boring were scored with a pry-bar to open potentially smeared sidewalls. Two <br /> nchene gravel was placed at the bottom and three-inch perforated PVC pipe was inserted in <br /> the borings. The test borings were subsequently pre-saturated with 12 inches of water at 0900 hrs, <br /> 24 hrs before the start of testing. <br /> SSi6. On November 2, 2011, percolation testing commenced. No standing water was <br /> obd r the 24-hr soak period in either test boring. Consequently, EHD Perc Test Procedure <br /> #2 was conducted in which testing was done over a -hour period to induce maximum soil �. <br /> saturation. The test results indicate a pert rate t 8.6 utes per inch(min/in) for the EHD Official <br /> Perc test and 13.2 min/in for the 48-inch depth est depth A summary of the pert test results <br /> with corresponding application rates in gallons of effluent accepted per square foot of soil,per day <br /> are found in Table 3: <br /> TABLE 3 <br /> PERCOLATION TEST RESULTS FOR THE DISPOSAL AREA WITH <br /> CORRESPONDING APPLICATION RATES IN GALLONS/FT2/DAY <br /> 36 INCH DEEP PERC TEST BORING C)8min/inch / 0.857 gallons/ft/day <br /> PERCOLATION RATE/APPLICATION RATE <br /> 48 INCH DEEP PERC TEST BORING 13.2 m' inch / 0.757 gallons/ft/day <br /> PERCOLATION RATE/APPLICATION RATE <br /> Awhcahm Rate adapted from California State Water Resources Control Board Cuu*lrnes for the ig r of Sewage Systems and is based on die Perc Rate. <br /> D. GROUNDWATER INFORMATION <br /> NLS§ . , SSS . . Groundwater depths and elevations throughout San Joaquin County are <br /> maps published by the County Flood Control and Water Conservation District. The <br /> most recent Lines of Equal Depth map(Spring 2011) indicates the groundwater depth to be 55 feet. <br /> This corresponds with actual water table depth determination by boring for the aforementioned St. <br /> Bernard's project. <br /> The 2003 Lines of Equal Elevation Map illustrates the groundwater directional flow to be generally <br /> in a northwesterly direction toward the San Joaquin River. Groundwater flow in this locale is <br /> extremely variable due to several influences such as the time of the year, and surrounding <br /> irrigation. <br /> SS 2. 4.2. Zte'nsely <br /> e the property has been intensely farmed, and since surrounding properties <br /> hav ee farmed for several decades,the probability for nitrate contamination in the <br /> underlying soil and groundwater is significant. A potential rise in the water table elevation may be <br /> attributed to the cropland surrounding the property to the south, east and west. <br /> NLS 2.2 .1, S 4. It is my understanding the projec will ve an on-site water well for <br /> dom c o own at this time if the well wi classified as a public well. Water <br /> chemistry should be done on a test well before conversion the_peermanent well particular for <br /> nitrate concentrations. <br /> 4 <br /> Chesney Consulting <br />