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2900 - Site Mitigation Program
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PR0516772
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Last modified
6/1/2020 12:35:35 PM
Creation date
6/1/2020 12:29:36 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
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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EHD - Public
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. Y <br /> Kennedy/Jenks ConsuFtants <br /> moisture observations recorded in Title 27 monitoring well boring logs and the corresponding <br /> depth interval of that moisture. Figures 5 through 7 present cross sections on which the <br /> following discussion is based. <br /> Experience at the Site shows that a field geologist will typically note much of the boring as <br /> "moist" or"damp", and these moisture notations are native moisture in the soil or condensation <br /> from the friction of drilling, not free water(or saturated conditions), and is held in the soil by <br /> tension, or negative pore pressure. These are not water-bearing zones. The moisture analysis <br /> "ignores" moisture that is noted as moist or damp, as these are not potential water bearing <br /> zones. <br /> Well MW-12 has "very moist" logged for a silty sand (SM) layer from 48-49 feet bgs, sandy <br /> gravel (GM) layer from 49-50 feet bgs, sandy gravel (GM)from 60-62 feet bgs, sandy clayey silt <br /> (ML) from 62-63 feet bgs, silty sand/sandy silt from 63-65 feet bgs, and "wet" logged for a silty <br /> sand/sandy silt from 65-68 feet bgs. One additional sandy gravel (GM) is logged as "moist/wet" <br /> from 82-82.5 feet bgs. Three target zones are identified for potential shallow water and/or zones <br /> of higher hydraulic conductivity: 1) 48-50 feet bgs, 2) 60-68 feet bgs, and 3) 82-82.5 feet bgs. It <br /> should be noted that the third target zone above (82-82.5 feet bgs) is a sandy gravel that <br /> appears to correlate with a sandy gravel inside the screened interval of Well MW-18, which has <br /> gone dry (Section 3.1.2). If this sandy gravel layer does correlate with the Well MW-18 screened <br /> interval, it is possible that it has drained (dried) in the process of water levels in Well MW-18 <br /> falling below the screened interval. <br /> Well MW-17 likely did not penetrate the entire water bearing zone as Well MW-18 (installed <br /> approximately 10 feet to the south) has "wet" logged for an additional four feet below the bottom <br /> of the screen of Well MW-17. The target zone identified for potential shallow groundwater is <br /> 65-70 feet bgs. It should be noted that two additional wells are installed in this zone, <br /> Wells MW-19 and MW-21, water was not encountered during installation, and water has not <br /> appeared since quarterly monitoring began in 2006. It is possible that water is not present in this <br /> zone, but it will be evaluated during drilling. <br /> Well MW-18 has a clayey gravel (GC) logged as "wet"from 80-81 feet bgs. The top of the <br /> screen intercepts this clayey gravel layer, and the filter pack extends an additional three feet <br /> above it. If there were water present in this zone, it would be observed in Well MW-18. There <br /> are no target zones identified by examining the boring log for Well MW-18 or cross sections. <br /> Well MW-22 has two silty gravel zones identified in the boring logs, one from 55.5-59 feet bgs <br /> with no moisture notation, and the other from 70-80 feet bgs which is logged as "dry'. Target <br /> zones identified from the boring log of Well MW-22 for a zone of higher hydraulic conductivity <br /> are 55-59 feet bgs and 70-80 feet bgs. <br /> 3.3 Groundwater Flow Direction <br /> Groundwater elevation contours cannot be drawn for existing conditions in the intermediate <br /> zone of the Title 27 groundwater monitoring network because there are not a sufficient number <br /> of active wells. There are however, sufficient historical data and overlap between wells that <br /> have since gone dry to draw a historic groundwater elevation contour map (Figure 8) using <br /> groundwater elevation data from Wells MW-1 OR, MW-12, MW-18, and MW-22. For this Work <br /> Work Plan for Improved Detection Monitoring Program Page 7 <br /> Musco Family Olive Company, Tracy, California <br /> a cs emupWnnwcbON20104mm�wlwN mwWe�27_emmWeaumpwlreport text-09-26.doc <br />
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