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2900 - Site Mitigation Program
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PR0536710
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SITE INFORMATION AND CORRESPONDENCE
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Last modified
7/11/2019 10:12:44 PM
Creation date
7/11/2019 4:38:04 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
SITE INFORMATION AND CORRESPONDENCE
RECORD_ID
PR0536710
PE
2950
FACILITY_ID
FA0021089
FACILITY_NAME
VACANT
STREET_NUMBER
520
Direction
N
STREET_NAME
EL DORADO
STREET_TYPE
ST
City
STOCKTON
Zip
95202
APN
13906032
CURRENT_STATUS
01
SITE_LOCATION
520 N EL DORADO ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
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Advanced GeoEnvironmental, Inc <br /> January 3, 2012 <br /> Page 2 <br /> The use of these methods is also dictated by the proximity of above ground features to the <br /> survey area. Typically, the VMG cannot be used in close proximity to above ground metal <br /> objects, such as buildings and wrought-iron fences. Magnetic interference from these objects will <br /> often mask the detection of a nearby buried UST. The MD and EMLL are not as sensitive as the <br /> VMG and can typically be used closer to these above ground metal objects. GPR is not effected <br /> by above ground metal objects, and is typically used to survey areas in close proximity to these <br /> features. <br /> Based on the objective of this survey and the specific site conditions, we used the metal <br /> detection (MD), electromagnetic line locating (EMLL), and ground penetrating radar (GPR) <br /> methods. The MD/EMLL method was used to survey for shallow subsurface metal objects that <br /> may represent a UST and possible UST associated utilities. It was scanned over the established <br /> grid along south-north and/or west-east trending traverses spaced approximately 5 ft apart. <br /> When a buried object was detected, the MD was then scanned along additional traverses. <br /> The GPR method was used to image variations in the electrical properties of the shallow <br /> subsurface. These variations can provide information on the location and dimensions of buried <br /> objects and fill boundaries and/or former excavations. We scanned the site with GPR along <br /> south-north trending traverses spaced 2.5-ft apart. The GPR records were processed on site <br /> and examined for reflection patterns characteristic of a UST. Descriptions of the MD and GPR <br /> methods are provided in Appendix A. <br /> 3.0 RESULTS <br /> The results of the MD, EMLL, and GPR surveys are presented on the Geophysical Survey Map, <br /> Plate 1. This map shows the limits of the geophysical investigation, the locations of above <br /> ground features, and the locations of any detected subsurface features and utilities. Since a <br /> utility search was not the primary objective of this survey, there may be additional utilities that are <br /> not shown. <br /> The EMLL and MD surveys detected an electric, storm drain, and two undifferentiated utility <br /> lines. All are located in the north half of the survey area, as shown on Plate 1. The electric line <br /> passes through the northwest corner to a light pole, and the storm drain line trends east from a <br /> catch basin. One of the undifferentiated utilities parallels the electric line. The other trends into <br /> the survey area from the north, where it ends abruptly near a soil boring drilled by Advanced <br /> Geo Environmental. It is uncertain if the undifferentiated utilities represent lines associated with <br /> the present building to the north or abandoned lines associated with former facilities. The MD did <br /> not define any below ground metal objects within the designated survey limits that could <br /> represent a possible UST. However, it should be noted that electromagnetic interference from <br /> the wrought-iron fence precluded the use of the MD within approximately 5-ft of this structure. <br /> The GPR records obtained throughout the survey area exhibit continuous reflection patterns that <br /> we interpret as representing shallow fill horizons associated with the pavement and near surface <br /> soils. These records also show deeper continuous reflections as well as isolated hyperbolic <br />
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