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SITE INFORMATION AND CORRESPONDENCE_1988-1991
Environmental Health - Public
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PR0506824
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SITE INFORMATION AND CORRESPONDENCE_1988-1991
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Last modified
4/7/2020 3:14:45 PM
Creation date
4/7/2020 2:36:16 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
SITE INFORMATION AND CORRESPONDENCE
FileName_PostFix
1988-1991
RECORD_ID
PR0506824
PE
2960
FACILITY_ID
FA0007648
FACILITY_NAME
DDRW - SHARPES
STREET_NUMBER
850
Direction
E
STREET_NAME
ROTH
STREET_TYPE
RD
City
LATHROP
Zip
95330
APN
19802001
CURRENT_STATUS
01
SITE_LOCATION
850 E ROTH RD BLDG S-108
P_LOCATION
07
P_DISTRICT
003
QC Status
Approved
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EHD - Public
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ENCLOSURE <br /> PRELIMINARY SUMMARY PROBLEM <br /> S AND GAT ON (RI) REPORT RECOMMENDATIONS FOR THE REMEDIAL <br /> SUMMARY OF PROBLEMS WITH HYDROGEOLOGIC ANALYSIS AND PRESENTATIONS <br /> • Cross-sections were drawn incorrectly which reduces the reliability of the <br /> sections and conclusions drawn from the sections. The following <br /> deficiencies or errors in the construction were found with the cross- <br /> sections. <br /> • Redundant sections; some sections fold back on each other. <br /> • Discrepancies between same wells on different cross-sections. <br /> • Some well lithology as shown on cross-sections are inconsistent with <br /> the actual well log. <br /> • Cross-sections contain acute angles. <br /> • No cross-section in north-south direction off-site. <br /> • There were no horizontal scales on the sections. Vertical <br /> exaggeration cannot be determined. <br /> • Classification of sandy-clay (SC) and sometimes sandy silts with clay (ML) , <br /> as an aquifer. These type of sediments tend to be more of an aquitard to <br /> the movement of fluids rather than as an "aquifer" . The term "aquifer" in <br /> the sense which it has been used, implies a rather transmissive unit. <br /> However, the transmissivity (T) values calculated for the A and B zones are <br /> more representative of an aquitard, and not an aquifer. If the cross- <br /> sections were redrafted classifying these type of sediments as aquitards, <br /> then it may be that there are fewer significant correlatable, highly <br /> transmissive hydrostratigraphic units than is currently depicted. <br /> • No typing of the different water bearing zones. Minerals analyses have not <br /> been consistently performed from different well clusters to type the water <br /> bearing zones and to verify if the water bearing zones are indeed <br /> different. <br /> • Conceptual model which consists of four different aquifers (A, B, C, and D <br /> zones) may be wrong. My preliminary scan of the data indicated that only <br /> the D zone could consistently be differentiated based on heads and aquifer <br /> parameters. The A and B zone may be one zone or may be combined with the C <br /> zone. <br /> • Only about six hydrographs were presented in the Report. Hydrographs need <br /> to be constructed especially for the wells with the longest historical <br /> record and the well clusters within the four zones. <br /> • The water level contour maps were computer generated and apparently were <br /> not verified by hand contouring. These maps show equipotential lines with <br /> acute angles. The flow maps were constructed for November of 1984, 1985, <br /> 1987, 1988 and 1989. This does not give enough information about the <br /> seasonal changes which occur due to pumpage by the agricultural supply <br /> wells, of which is acknowledged throughout the report. November is neither <br /> at the height of the wet or dry season. <br />
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