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ARCHIVED REPORTS PR0544462
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ARCHIVED REPORTS PR0544462
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Entry Properties
Last modified
11/19/2024 10:19:00 AM
Creation date
5/16/2019 8:34:58 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
PR0544462
RECORD_ID
PR0544462
PE
3528
FACILITY_ID
FA0003551
FACILITY_NAME
B J J COMPANY INC
STREET_NUMBER
757
Direction
E
STREET_NAME
ELEVENTH
STREET_TYPE
ST
City
TRACY
Zip
95376
APN
25026001
CURRENT_STATUS
02
SITE_LOCATION
757 E ELEVENTH ST
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
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EHD - Public
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. Water Sample Labeling and Handling <br /> Sample containers are labeled in the field with the ,lob number, sample location, depth of <br /> sample (if appropriate), and date of sample and promptly placed in iced storage for transport to <br /> the laboratory. A Cham of Custody Record is initiated by the geologist and updated <br /> throughout handling of the samples and accompanies the samples to a laboratory certified by <br /> the State of California. Samples are transported to the laboratory promptly to help ensure that <br /> recommended sample holding times are not exceeded. <br /> Reporting Results of Analyses <br /> Hydrocarbon constituents in soil samples are typically reported in units of parts per million <br /> (ppm). Hydrocarbon constituents in groundwater samples are typically reported by the <br /> laboratory in units of parts per billion (ppb). <br /> Evaluating he Grgundwater Flow Direction-and Gradient <br /> The elevations and positions ("x" and "y" lateral coordinates) of the monitoring well are <br /> surveyed with respect to a local datum that references the elevation according to mean sea <br /> level The elevation of the monitoring wells are measured within 0.01 foot of the local datum <br /> The horizontal distances are measured to the nearest 0 1 foot The elevations are typically <br /> measured from ether a notch or an arrow marked on the top northern edge of the well casing <br /> The groundwater elevation for each monitoring well is calculated by subtracting the depth to <br /> water from the wellhead elevation The groundwater elevation information is used to construct <br /> a potentiometric surface map, which is used to evaluate the direction of groundwater flow and <br /> the magnitude of the groundwater gradient <br /> SHELLSIFLDMTHDS doe 4 <br />
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