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Parcel 3: 0.5 in. water drop= 60 min/in <br /> Parcel 4: 1.9 in. water drop= 16 min/in <br /> As can be noted,the perc rates are quite variable for each parcel which confirms the variability of the <br /> underlying soil structures. The backhoe trench pump-in test calculations demonstrate an avera e <br /> acceptance rate (AR) in gals/sq ft/day as follows: <br /> ❑ Length of trench= -16 ft @ grade, Hydraulic area= 6 ft <br /> ❑ Width of trench= 8 ft @ grade, Hydraulic area=4 ft <br /> ❑ Depth of trench= 15 ft from grade, Hydraulic area= 5 ft <br /> ❑ Depth of water maintained on the floor of trench= 5 ft <br /> ❑ Depth below bottom of trench at periphery of plume=4 ft (est) <br /> ❑ Total water volume applied during test= 1000 gals <br /> ❑ Extent of water plume area: water surface= 4 ft x 6 ft :. plume area is estimated to be: <br /> 12 ft width x 18 ft length= 216 sq. ft. <br /> ❑ Acceptance Rate (AR) =total flow absorbed-(area)(time) <br /> ❑ AR= 1000 gals_(216 sq. ft.)(4 hrs _24 hrs/day) = 28 gals/sq. ft./day <br /> Theoretical Effluent Acceptance: If the bottom 5 feet of a 36 in dia. x 25 ft deep seepage pit accepts <br /> effluent at the calculated rate, each seepage pit will initially accept 89 sq. ft. x 28 gals/sq. ft./day= <br /> 2487 gals/day. This seepage pit acceptance rate will decline significantly as biomat formation is <br /> increased. <br /> Since the groundwater is deep in this locale, seepage pits are allowed and are almost always installed. <br /> The subject property soils possess virtually no percolative capacity at shallow depths due to the heavy <br /> clay soils and the underlying hardpan. This is the reason for not conducting 42 inch deep perc tests. <br /> [4] LOCAL GROUNDWATER AND SURFACE WATER INFORMATION <br /> The static water table depth,or the zone of saturation is located at approximately 79 feet below grade <br /> according to the 1997 "Lines of Equal Depth" published by the San Joaquin County Flood Control <br /> District. There is a slight possibility there may be perched water table conditions under the subject <br /> property at a higher elevation than the static water level. There is no potential for future septic <br /> impact to any surface waters, namely the Angel Lateral, providing applicable distance requirements <br /> are followed. The groundwater directional flow appears to be toward the northwest as depicted on <br /> the attached "Lines of Equal Elevation" map. <br /> Analysis of water obtained from the domestic well which serves the homesite, reveals a nitrate <br /> concentration of<1 ppm NO3. The Maximum Contaminant Level(MCL)for NO3 in drinking water <br /> is 45 ppm. Therefore, the underlying drinking water aquifers have not been impacted from various <br /> nitrate sources. It can be assumed that the recharge for the aquifer(s) that serve this well are not in <br /> L <br /> Halley Ag research <br />