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SU0004714
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SU0004714
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Last modified
1/7/2020 1:05:24 PM
Creation date
9/6/2019 11:06:15 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004714
PE
2627
FACILITY_NAME
UP-98-22
STREET_NUMBER
500
Direction
E
STREET_NAME
LOUISE
STREET_TYPE
AVE
City
LATHROP
APN
19119006
ENTERED_DATE
11/18/2004 12:00:00 AM
SITE_LOCATION
500 E LOUISE AVE
RECEIVED_DATE
1/3/1989 12:00:00 AM
P_LOCATION
99
P_DISTRICT
003
QC Status
Approved
Scanner
SJGOV\rtan
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FilePath
\MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\APPL.PDF \MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\CDD OK.PDF \MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\EH COND.PDF \MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\EH PERM.PDF
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EHD - Public
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1 <br /> *AW <br /> SUMMARY <br /> McClelland Consultants conducted a geotechnical study for PSE, Inc., at the <br /> proposed San Joaquin Limited cogeneration site (site 3058) in Lathrop, Califor- <br /> nia. The purpose of our study was to develop criteria to guide the design and <br /> construction of foundations and earthwork for the planned facility. The planned <br /> 2-acre facility is to the southwest of the Libbey Owens Ford (LOF) plant, about <br /> one-half mile southeast of the Interstate 5 and Louise Avenue interchange. <br /> Soil conditions at the site were investigated in December 1988 by eight soil <br /> borings, which were drilled to 13- and 62-ft depths, and three field electrical <br /> resistivity measurements. Previously, in March 1988, the excavations formed by <br /> five backhoe trenches were observed. Subsequent laboratory tests were performed <br /> on recovered samples. <br /> The site is in the Great Valley of California, which is a nearly flat, <br /> alluvial plain underlain by hundreds of feet of sediments. The flat natural <br /> topography and underlying subsurface in the project area has been significantly <br /> altered by glass disposal activities associated with the adjacent LOF plant. <br /> Subsurface materials appear to have been altered over much, if not all, of the <br /> site. The presence of glass ranges from a matrix of glass cullet that includes <br /> little soil to intermixed soil and glass to soil with some glass fragments. <br /> Glass was encountered to a maximum depth of 16 ft. Even where glass was not <br /> observed to be present, the surface sands are likely to be uncontrolled fill. <br /> Beneath the depth of alteration, the soils consist principally of alterna- <br /> ting deposits of clay and sand. A ±20-ft-thick stratigraphic sequence composed <br /> primarily of stiff to very stiff, lean, sandy clay extends from down about 14- to <br /> 16-ft depth. Dense to very dense, silty fine to medium sand was encountered <br /> below the lean clay. Groundwater was encountered at 7- to 11-ft depth in our <br /> borings. <br /> Construction of the cogeneration facilities will require raising the rela- <br /> tively flat, 2-acre plant area about 2 to 5 ft. The presence of substantial <br /> volumes of glass and glass by-products complicates the foundation design and <br /> earthwork considerations for the equipment and structures associated with this <br /> facility. Several approaches can be considered for supporting the cogeneration <br /> facilities' equipment and structures. Selection of appropriate foundation <br /> options will depend on: (a) flexibility in the layout of cogeneration facility <br /> 1144A/H-1 :7 McClelland <br />
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