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Location: 2605 IN . 4 i ;or, 11--V <br /> rjwner: Alfred iia_jor <br /> Date Drilled: 11 ib <br /> Use: dater Well <br />' CONCLUSIONS <br /> The ground water gradient :las remain-gid basically unchanged for the <br />' last two quarters (Figure 2) . <br /> Monitoring well 2 s'iows a decrease in TPF r nd '3rE&N concentrations <br /> over time. Tne decwE.aSe in TPH and 2TESX -:orcor!n- tac,-s over ti-11@ <br /> is consistent T%7Jth a narcura? Oegraµ-ticn c'- con aninants over <br /> tire. However_, TPH and B-2f -xY conccntra-u for-3 in rio itf]-lna walls I-T41 <br /> and M473 are still flucti it-jil d. <br /> /The limits of zhe ground -.at er cr--t ani nant ctr,i zlt--z contaninant <br /> plumes have r_o- fete-mirea. <br />' RECOHMENDAT IONS <br /> ased on the high concent rations of TPH and BTEX in MW1 Applied <br /> illConsultants recommends at least two additional monitoring. wel e <br /> ... established on the sub3ect site. <br /> Applied Consultants is also preparing a cnmiprehensive Site <br /> Assessment Workplan for the uk ject site 'This, workplan. 1r. expected , <br /> to be --ompleted shortly <br /> Copies of this report has tfeen tcrwarded to t'ie San T---+aq?in County, <br /> Public Healtn Sarvices, Env- r on enca] 'iPd i*. "1 filvi cion for their <br />' review. <br /> If you have any questions please fe-1 Free to call ot.-r office. <br /> Since <br />' chael J. Barnett !Berriar'd '-:ether, CEG 1356 <br /> Staff Geologist President <br /> cc: (1) Mr. Art Borba, U--Haul yG1 EER/�y�, <br /> 1 <br /> ^tp Na CEG1356 -A <br /> u-HAUL \ 2709 WILSON WAY .� �OF <br /> �� <br /> mjB-93-I \ UH-WILSON RPT (SD5020 2. <br /> 11 JANUARY 1993 <br /> 4_ <br />