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chapter 4: temperature inside the landfill

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suggested that interferences by ferrous materials were negligible when <strong>the</strong> moisture content in<br />

<strong>the</strong> waste is below 20% for leachate or 40% for tap water.<br />

2.4.4 Electrical resistivity tomography<br />

Electrical Resistivity Tomography (ERT) consists of measuring <strong>the</strong> potential distribution<br />

when electrical current is injected into <strong>the</strong> underground via galvanic or capacitive contact<br />

(Imhoff et al, 2007). The galvanic contact requires direct contact of <strong>the</strong> electrode with <strong>the</strong> waste<br />

while in capacitive contact, electrodes can be placed above a geomembrane. Changes in moisture<br />

content are expressed by <strong>the</strong> resistivity variations that occur during liquid injection (Guerin et al,<br />

2004).<br />

Guerin et al (2004) performed experiments on a <strong>landfill</strong> in France using various<br />

geophysical methods including electromagnetic slingram mapping and electrical 2D imaging.<br />

Although a definitive relationship between resistivity and moisture content was not developed in<br />

<strong>the</strong> study, it was concluded that ERT methods allow water to be located within a <strong>landfill</strong>. Also<br />

<strong>the</strong> influence zone of <strong>the</strong> leachate recirculation system can be located using ERT methods.<br />

2.4.5 Partitioning gas tracers<br />

Two gas tracers are injected and <strong>the</strong>n extracted under steady gas flow in Partitioning Gas<br />

Tracers Tests (PGTT). One of tracers (<strong>the</strong> conservative tracer) is inert while <strong>the</strong> o<strong>the</strong>r tracer (<strong>the</strong><br />

water-partitioning tracer) being hydrophilic, partitions into and out of water while passing<br />

through <strong>the</strong> solid waste <strong>inside</strong> <strong>the</strong> <strong>landfill</strong> (Imhoff et al., 2007). The parameter used to estimate<br />

moisture content is <strong>the</strong> difference in <strong>the</strong> arrival times of <strong>the</strong> two tracers at a gas collection well or<br />

an intermediate sampling well. The arrival times of <strong>the</strong> tracers are measured by gas<br />

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