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Diploma thesis in Physics submitted by Florian Freundt born in ...

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C Additional plots and figures<br />

� � � � � � � � � � � ��� � �<br />

Figure C.8: Temperature measurements taken at Site A at 0.1 m, 1.0 m and 2.5 m depth<br />

and s<strong>in</strong>usoidal fits. Depth placement accuracy is ±0.1 m, temperature accuracy is ±0.5 ◦ C.<br />

The atmospheric daily mean temperatures were provided <strong>by</strong> meteomedia, measured <strong>by</strong> a<br />

weather station close to Site A. The offset visible at 1.0 m depth <strong>in</strong> August 2010 is caused<br />

<strong>by</strong> a moisture <strong>in</strong>trusion <strong>in</strong>to the sensor <strong>in</strong> August 2010 after refill<strong>in</strong>g the borehole with<br />

sludge. Comparison with the data from Site B leads to the conclusion that the sensor was<br />

affected <strong>by</strong> this until early October 2010. The smaller offset at 2.5 m depth <strong>in</strong> December 2010<br />

and January 2011 co<strong>in</strong>cide with heavy precipitation (Figure C.10). The low atmospheric<br />

temperatures at the time <strong>in</strong>dicate that this also is an offset caused <strong>by</strong> moisture <strong>in</strong>trusion<br />

rather than an actual temperature change <strong>by</strong> <strong>in</strong>filtrat<strong>in</strong>g ra<strong>in</strong> water of different temperature.<br />

Such an event is visible <strong>in</strong> May 2011, when cold tap water was used for irrigation, lead<strong>in</strong>g to<br />

spikes <strong>in</strong> the temperature curves of 1.0 m and 2.5 m. The sensor at 0.1 m depth was shielded<br />

aga<strong>in</strong>st these sudden and short-lived temperature changes <strong>by</strong> be<strong>in</strong>g <strong>in</strong>sulated <strong>by</strong> air <strong>in</strong>side<br />

the <strong>in</strong>strumentation box.<br />

93

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