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SITE HISTORY_CASE 1
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SITE HISTORY_CASE 1
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Last modified
5/12/2020 3:16:07 PM
Creation date
5/12/2020 1:57:43 PM
Metadata
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Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
SITE HISTORY
FileName_PostFix
CASE 1
RECORD_ID
PR0545660
PE
3528
FACILITY_ID
FA0003909
FACILITY_NAME
PORT OF STOCKTON
STREET_NUMBER
2201
Direction
W
STREET_NAME
WASHINGTON
STREET_TYPE
ST
City
STOCKTON
Zip
95203
APN
14503001
CURRENT_STATUS
02
SITE_LOCATION
2201 W WASHINGTON ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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EHD - Public
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Ms.-Carol,Oz <br /> February_24, 1999 - <br /> _ : :Page two:. <br /> ._ <br /> Although would cover-the previous PHC~detection in groundwater <br /> " sampled from.this depth at boringwould not:provide evidence for any <br /> potential'containinants at the same depth.at the other two bonrig'lo.cations. As. <br /> such, the cost of;a fourth well:is .not justified and we'.are recommN. <br /> ending against <br /> installing a fourth well-'and instead recommending modifying_the screened.interval <br /> at each of.the three proposed_well locationsfrom 1 O.to 35 feet bgs. In sum, during <br /> the referenced-conference call we collective) agreed <br /> that this Would be a <br /> preferrzd-o ion for,the-following.reasoris:a- - <br /> -� <br /> • Screening from 10.to 35-feet provides a completion across each',of the <br /> coarse`r-grained_units identified beneath the site;(see Figure . of.lnVestigation <br /> _ <br /> _Re rt).-It a.lsoprdVides screens across�frorri all.of the sampled locations-at- <br /> which PHCswere'det�cted;in elthersoils or groundwater during the initial <br /> . -- --in w.estigati.on: <br /> Lowe.n. the op of the screened .interval from 5 feet to-10 feet bgs meets the <br /> g <br /> _spirit of PHSIEHD's rationaleao have-screen across;from"tlie likely maximum <br /> water table. Historical:water levels(1992.71.998)'from irmonitoring;weils at . <br /> - other locations on the Port show-that1998 was--a:-maxirnum-year�for water <br /> _ leve s at the site This maximum corresponds to several=above.average <br /> • '- e = <br /> -rainfall years.; which culminated in=last year'sE1.Nino events.e 1n light of this <br /> -year's-La Nina events,'however,-it-is therefor unl.ikely_that water,levels will rise <br /> substantially:above the'.1998 level:at.this.'location'(6pproximate1 10 feet bgs.). _ <br /> ' The10=foof top of.screen also makes sense'because the re:is-no detectable <br /> or likely contamination above that level The bottom elevation of the tanks <br /> �ia,+wo � .md.. - L. ''• l.., 'i 1,or F 1 F ,I t �f <br /> ¢, rernoveci rron=itnis sne.was at.i i feet=Ylzf- -;Gr, <br /> ;contamination would be present above.hat level:. Additionally., sot samples" <br /> obtained from 10 feet bgs at'all three locations contained-no detectable'ieveI's <br /> of P.HU <br /> M :• Screening.abovEi.the 1046ot level could introduce contaminants into soils that <br /> F <br /> _previously were.not contaminated If the`groundwater beneath the site is <br /> ur.der.confined conditions-(fine7grained;-potentially confining soils are present <br /> beneath the site starting-at 9 to 13.ffeet bgs), contaminated groundwater in. <br /> deeper zones could potentially migrate-upwards,through the casting and into- <br /> - - the surroundingJormations.-- Starting the screenat the 10-foot level would <br /> limit this potential. :. <br /> r . <br />
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