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ARCHIVED REPORTS_1993_1
Environmental Health - Public
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EHD Program Facility Records by Street Name
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4400 - Solid Waste Program
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PR0440001
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ARCHIVED REPORTS_1993_1
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Last modified
7/17/2020 3:53:09 PM
Creation date
7/3/2020 10:39:46 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1993_1
RECORD_ID
PR0440001
PE
4433
FACILITY_ID
FA0004514
FACILITY_NAME
AUSTIN ROAD/ FORWARD LANDFILL
STREET_NUMBER
9069
Direction
S
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
STOCKTON
Zip
95215
CURRENT_STATUS
02
SITE_LOCATION
9069 S AUSTIN RD
P_LOCATION
01
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\SW\SW_4433_PR0440001_9069 S AUSTIN_1993_1.tif
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EHD - Public
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III. Environmental Setting, Impacts, and Mitigations <br /> K Hydrology, Geohydrology,and Water Quality <br /> Johns Creek and Lone Tree Creek converge and enter French Camp Slough(U.S.G.S, 1987a and <br /> 1987b). French Camp Slough discharges to the San Joaquin River on the southwest side of the <br /> City of Stockton, and the waters enter the Sacramento-San Joaquin Delta. French Camp Slough <br /> drains a total area of approximately 250 square miles, with a maximum watershed elevation of <br /> 2,700 feet MSL(City of Stockton, 1990). French Camp Slough is the tidewater terminous of the <br /> Little Johns Creek system. Due to historical modifications for various purposes,former <br /> connections with Duck Creek have been eliminated,except under flood flow conditions(City of <br /> Stockton, 1990). The Department of Water Resources has collected streamflow data since 1950 <br /> on French Camp Slough at Airport Way(DWR, 1985). <br /> Site Hydrology <br /> Topographic modifications of the landscape associated with the current landfill,and historical <br /> agricultural practices have influenced site hydrology. <br /> The North Branch of the South Fork Little Johns Creek flows through the project site,along the <br /> eastern and southern margin of the existing landfill area(Figure III.K.1). The channel meanders <br /> for a total channel distance of about 6,500 feet on the site,with a bed gradient of 0.0411 percent <br /> (R.W. Beck and Associates, 1992b). The modified natural channel is of fairly uniform width and <br /> depth throughout the site,typically 25 to 35 feet wide, and 10 to 12 feet deep. Channel banks are <br /> earthen and steep,and a strongly cemented soil hardpan forms the channel bed and lower bank <br /> for most of the reach. Bank erosion and down cutting of gullies through the banks has occurred <br /> in several locations along the channel,particularly on the outer bank of stream bends. Surface <br /> runoff draining from the landfill surfaces has contributed to the formation of gullies <br /> perpendicular to the banks. Riprap has been placed in strategic positions to absorb stream energy <br /> on channel bends. <br /> A small agricultural drainage ditch empties into Little Johns Creek on the eastern edge of the <br /> project, via a piped outfall near the existing landfill entrance. Drainage ditches that parallel the <br /> western property boundary also have piped outfalls that discharge to the creek on site <br /> (Figure III.K.1). The stormwater drainage system for the CYA facility discharges through an <br /> engineered open channel along the northern boundary of the proposed project to a detention basin <br /> (see Figure III.K1). The basin outfall to Little Johns Creek is located on the upstream side of the <br /> landfill entrance. <br /> III.K2 <br />
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