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chapter 4: temperature inside the landfill

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steady rise in <strong>the</strong> <strong>temperature</strong>s. The rate of heating for <strong>the</strong> all <strong>the</strong> depths was approximately<br />

5 0 C/year. The rates have been estimated assuming a linear progression from Day 550 to Day<br />

1200. Yesiller and Hanson (2003) reported <strong>the</strong> rate of increase in <strong>temperature</strong> in a newly placed<br />

waste (for a <strong>landfill</strong> cell with leachate recirculation) at around 4 0 C/year.<br />

The effect of leachate injection can also be observed in Figure 4-1. The cooling effect is<br />

demonstrated early during continuous injection between Day 450 and Day 730 and <strong>temperature</strong><br />

depression<br />

around Day 500 to 530. The <strong>temperature</strong> started rising again after 4-6 months due to<br />

enhanced biological activity.<br />

Lastly, <strong>the</strong> effect of ambient <strong>temperature</strong> was investigated by attempting to correlate <strong>the</strong><br />

ambient <strong>temperature</strong> for <strong>the</strong> site. R 2 waste <strong>temperature</strong> against <strong>the</strong><br />

values for <strong>temperature</strong>s at<br />

deep, middle<br />

and shallow depths were found to be 0.0036, 0.014 and 0.038 respectively. These<br />

R 2 values clearly indicate that <strong>the</strong>re is no relationship between ambient <strong>temperature</strong> and <strong>the</strong><br />

waste <strong>temperature</strong>. The explanation may be <strong>the</strong> location of <strong>the</strong> <strong>landfill</strong> site in Florida having<br />

moderate <strong>temperature</strong> range of 13 0 C to 27 0 C. Fur<strong>the</strong>r, liquid injection appears to more<br />

dominantly control <strong>temperature</strong> as it initially cools, <strong>the</strong>n leads to heating from biological activity.<br />

To identify <strong>temperature</strong> events at <strong>the</strong> injection wells, a value of Y of 20 days and X of<br />

0.5 0 C were used after a certain number of trials. After identifying <strong>the</strong> significant <strong>temperature</strong><br />

drop (t- drop) events, <strong>the</strong> recorded injection events and <strong>the</strong> <strong>temperature</strong> drop events were plotted<br />

toge<strong>the</strong>r to compare <strong>the</strong> times as shown in Figures 4-2, 4-3. Looking at <strong>the</strong>se plots, <strong>the</strong><br />

coincidence of injection event and t-drop events can be observed.<br />

Looking at <strong>the</strong> immediate drop in <strong>the</strong> <strong>temperature</strong> at <strong>the</strong> time of injection, 20-day average<br />

of <strong>the</strong> <strong>temperature</strong> data does not, at first, seem to be logical. Before trying 20-days average, 4-<br />

days, 8-days and 15-days were tried too but with less agreement with injection records. The<br />

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