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ARCHIVED REPORTS_2006_23
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ARCHIVED REPORTS_2006_23
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Last modified
7/17/2020 3:53:24 PM
Creation date
7/3/2020 10:51:41 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
2006_23
RECORD_ID
PR0440005
PE
4433
FACILITY_ID
FA0004516
FACILITY_NAME
FORWARD DISPOSAL SITE
STREET_NUMBER
9999
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
MANTECA
Zip
95336
APN
20106001-3, 5
CURRENT_STATUS
01
SITE_LOCATION
9999 AUSTIN RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4433_PR0440005_9999 AUSTIN_2006_23.tif
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EHD - Public
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Geoelectric Leak Detection Final Report October 18, 2006 <br />Forward Landfill WMU FU -06 Page 2 <br />was checked periodically (at least every 20 minutes) by passing the equipment over a <br />known hole or over a ground wire to confirm functionality of the equipment, and then again <br />at the end of the day of surveying. The calibration holes were repaired by the Installer. <br />Results <br />The GCL underlying the sump area was determined to be too dry to conduct electricity <br />during the calibration process. This area was therefore vigorously inspected visually for <br />defects and one hole was found. The water lance survey of the remaining area of WMU- <br />06 did not locate any further holes. <br />A description of the holes and locations are described in Table 1 and shown in Figure 2. <br />1 Panel 12 - Top of Sloe Calibration Hole <br />2 Panel 14 - Top of Sloe Calibration Hole over GCL <br />3 Corner of Sump Hole in extrusion weld <br />The holes located were repaired by the Installer. <br />Dipole Method for Geomembrane covered with soil material <br />Method / Procedure <br />The method used to perform the geoelectric leak detection survey on the soil covered <br />geomembrane was the dipole method. Testing was performed in accordance with ASTM <br />D7007-03. For this electrical leak location method, a voltage potential is introduced <br />between the insulative geomembrane and the earth beneath it. In the case of holes in <br />the geomembrane, current exits through the hole in the membrane, causing an anomaly <br />in the voltage potential field at that location. Measurements of voltage potential are <br />taken in a grid pattern throughout the survey area in order to locate these perturbations. <br />The survey was performed by two dipole operators. The operators recorded and <br />observed voltage potential measurements every meter in a grid pattern throughout the <br />cell. As the operators proceeded, they observed the amplitude of change in voltage and <br />watched for spikes or dips in the potential field. Whenever a significant change was <br />encountered, the area was flagged and rechecked immediately until the anomaly could <br />be validated or dismissed. A signal of greater than three times the background noise is <br />validated when it can be reproduced at least five times over the same location. The <br />surface of the cell was watered by the site water truck when conditions were dry to <br />ensure electrical conductivity to the surface. <br />Calibration <br />Prior to the survey, a calibration test was performed to determine the minimum hole size <br />that can be located by the dipole equipment and the maximum grid spacing for voltage <br />measurements. The WMU FU -06 calibration was performed without watering the <br />
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