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Geoelectric Leak Detection Final Report September 18, 2008 <br />Forward Landfill WU-08 Page 3 <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 three dipole operators. As the operators proceeded, they <br />observed the amplitude of change in voltage and watched for spikes or dips in the <br />potential field. Whenever a significant change was encountered, the area was flagged <br />and rechecked immediately until the anomaly could be validated or dismissed. A signal <br />of greater than three times the background noise is validated when it can be reproduced <br />at least five times over the same location. <br />Am The calibration hole consisted of an artificial leak fabricated and placed in accordance <br />in with ASTM D7007-03. The calibration test showed that a one quarter inch diameter <br />hole could be located. ASTM procedures require that the target hole size produce a <br />signal to noise ratio of at least 3. As shown in the following graph, a signal to noise ratio <br />of approximately 800 was created by the quarter inch hole. <br />Figure 3 — Calibration Graph <br />143E Spring Hill Drive • Grass Valley, California 95945 • (530) 272-2448 • Fax: (530) 272-8533 <br />USA 0 CENTRAL & SOUTH AMERICA 0 PHILIPPINES <br />