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SU0004741 SSNL
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SU0004741 SSNL
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Entry Properties
Last modified
5/7/2020 11:31:10 AM
Creation date
9/4/2019 9:52:23 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0004741
PE
2663
FACILITY_NAME
PA-0400705
STREET_NUMBER
767
Direction
N
STREET_NAME
ALPINE
STREET_TYPE
RD
City
STOCKTON
APN
10126007
ENTERED_DATE
12/13/2004 12:00:00 AM
SITE_LOCATION
767 N ALPINE RD
RECEIVED_DATE
11/30/2004 12:00:00 AM
P_LOCATION
99
P_DISTRICT
002
QC Status
Approved
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SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\A\ALPINE\767\PA-0400705\SU0004741\NL STDY.PDF
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EHD - Public
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PERCOLATION TEST yRE.SULTS <br /> PPERCDEPTH <br /> WEST PARCEL - MIDDLE PARCEL EAST PARCEL <br /> H PERC RATE PERC RATE PERC RATE <br /> 35.7 min/in @ 42 Inch Depth 41.7 minlin @ 42 Inch Depth Failed @ 42 Inch Depth <br /> TE No Pere Test Conducted at the 13.0 min/in @ 10.2 Ft.Depth Failed @ 8 Ft.Depth <br /> C <br /> H Intermediate Depth - <br /> Failed @ 23.5 Ft.Depth 5.0 min/in @24.5 Ft.Depth 7.3 min/in @ 24.5 Ft.Depth <br /> H (Possibly due to cave-in) <br /> III. NITRATE LOADING STUDY RESULTS <br /> A. GROUNDWATER INFORMATION <br /> 1. GROUNDWATER GRADIENT, VELOCITY AND ANALYSES <br /> The static water level under the center of the project is located approximately 73 feet below grade <br /> according to the 1999 Lines of Equal Depth Map published by the San Joaquin County Flood Control <br /> District. 'The 1999 Lines_ofEqual Elevation map illustrate the groundwater to be approximately -25 <br /> ft MSL. The 1992 Lines of Equal Elevation map illustrates the groundwater to be -62 ft MSL. <br /> Therefore, the static groundwater level appears to have risen 37 feet in the past seven years. �-/ <br /> Current groundwater directional flow is in a north-northeasterly direction according to the Lines of <br /> Equal Elevation Contour map.. From this map,.it appears the gradient is to the north-northeast under <br /> the property, and then changes to an east-northeasterly direction south of the property. The 1992 <br /> Equal Elevation Map indicates the groundwater flow to the north-northwest due to apparent heavy <br /> groundwater pumping in this area. <br /> The groundwater gradient under the subject site is estimated to be -20 ft - (-30 ft)- 5,800 ft <br /> j� 0.00172 ft/ft,based on the distance between-contour lines under the property. The velocity of the top <br /> groundwater formation under the-site can be estimated by the following formula: <br /> Kms,-12A <br /> Vaquifer L <br /> 7.5 p <br /> l <br /> Where: <br /> K=Hydraulic conductivity of aquifer formation in gals/day/fF ;z500 gals/day/ftz <br /> (Estimated based on a silty clay formation denoted on well log for 7425 Orford Road below the 70-foot depth.) <br /> h,_ -20 ft <br /> h2= -30 ft <br /> L= 5,800 ft <br /> p = porosity of aquifer z 35% (estimated) <br /> Vaquifer=2.3 ft/day or 840 ft/yr <br /> Chesney Consulting- <br />
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