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2900 - Site Mitigation Program
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PR0516772
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SITE INFORMATION AND CORRESPONDENCE
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Last modified
6/1/2020 12:44:39 PM
Creation date
6/1/2020 12:23:17 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
SITE INFORMATION AND CORRESPONDENCE
RECORD_ID
PR0516772
PE
2965
FACILITY_ID
FA0012793
FACILITY_NAME
MUSCO OLIVE LAND APP/TITLE 27
STREET_NUMBER
17950
Direction
W
STREET_NAME
VIA NICOLO
STREET_TYPE
RD
City
TRACY
Zip
95377
APN
20911032
CURRENT_STATUS
01
SITE_LOCATION
17950 W VIA NICOLO RD
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
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} T <br /> Mr. Benjamin Hall - 2 - 15 October 2004 <br /> Musco Family Olive Company <br /> Your expectation appeared to be that the analysis would prove the return system unnecessary. The <br /> 10 June 2004 Kennedy/Jenks technical letter report (hereafter report) completed the analysis. <br /> Reservoir Construction <br /> The memorandum makes no claim that Project Manual for the New Retention Pond prepared by FoodPro <br /> International was used by Musco for the final reservoir design/construction as implied in your letter. The <br /> memorandum refers to the manual's description of a liner because, had it been installed by Musco, it <br /> would likely have been adequate to comply with the requirements of Task 16. You letter identifies the <br /> 2001 Process Water Storage Reservoir Contract Documents and Specifications and the August 2001 <br /> construction drawings by HDR Engineering, Inc. as the correct references for the 84-million gallon <br /> reservoir design/construction. Our files contain two sets of drawings prepared by HDR, one dated <br /> November 2001 and one dated September 2001,but none dated August 2001. Unless otherwise noted, <br /> the drawings referenced below are in the November 2001 set. <br /> Drawing C-1 (SITE PLAN) depicts a small area straddling the drainage on the upstream toe as <br /> "SCARIFIED AND RECOMPACTED SUBGRADE." It also shows a borrow area of about 1.7 acres <br /> within the reservoir area. Our files do not contain documentation showing the final elevation contours of <br /> the borrow area. Your letter and the report both state Musco directed the contractor responsible for <br /> reservoir and dam construction to scarify and compact the native clay soil over as much of the reservoir <br /> bottom ground surface as possible. Musco has not provided the Regional Board with documentation that <br /> it directed the contractor to perform this work, or with documentation that the work was performed as <br /> Musco directed. Further,Musco has not provided the Regional Board with a delineation of the area the <br /> contractor found possible to rework and actually reworked. <br /> Reservoir Soils <br /> Although the report states that there is insufficient information available to determine the thickness of the <br /> native clay soil underlying the reservoir over its entire surface, it nevertheless estimates the bottom of the <br /> reservoir has"up to" 17 feet of natural clay soil. The report bases this estimate on information obtained <br /> from boring logs and "information from construction" (presumably notes and records generated during the <br /> construction process) documented in a 8 June 2001 Hydrogeologic Investigation prepared by Kleinfelder. <br /> We could not validate the estimate with information we reviewed in the Kleinfelder report, and have to be <br /> more concerned with areas where natural clay soil is the least thick anyway. Your letter refers to the <br /> results of permeability tests performed on soil samples collected from the reservoir area and documented <br /> in the same Kleinfelder report. This Kleinfelder report documents the results of laboratory permeability <br /> tests of two samples collected from one boring(TW-2) on a slope near the reservoir's upstream end. <br /> While this 26.5-ft boring penetrated clay layers that yielded permeabilities of 9.0 x 10'6 and <br /> 4.14 x 10-7 cm/sec in the laboratory, it also penetrated sandy gravel layers containing up to %2-inch <br /> diameter gravel. Additional evidence that soils underlying the reservoir area contain occasional and <br /> unpredictable sand and gravel lenses is contained in Drawing G-4 (LOG OF TEST BORING PROFILE) <br /> dated September 2001. Your letter and the report are not enough to justify the laboratory permeability test <br /> results of two samples taken from one boring as conservatively representative of the permeabilities of all <br /> soils forming the invert of the entire 42-acre reservoir area. hi addition to the probable variability in <br /> permeability of soils now inundated with wastewater, Musco provided no documentation that would <br /> enable an independent party to conclude that excavation in the borrow area did not compromise the <br /> integrity of clayey deposits and create conduits for impounded wastewater to enter groundwater. <br />
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