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

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3 Sampl<strong>in</strong>g sites and methods 3.1. Setup of the sampl<strong>in</strong>g sites<br />

SITE B<br />

SITE A<br />

SITE C<br />

Figure 3.2: Location of the sites created and sampled for this study [Source: Google Maps,<br />

map data provided <strong>by</strong> Tele Atlas].<br />

of sand and gravel and another layer of about 450 cm of clay (see Figure 3.3). Below a depth of<br />

5 m the ground primarily consists of sand and gravel.<br />

The site was equipped with three soil air sampl<strong>in</strong>g tubes, the <strong>in</strong>let screens located at depths 6 m,<br />

4 m and 2 m. Temperature sensors were <strong>in</strong>stalled at 2.5 m, 1.0 m and 0.1 m, the latter located<br />

<strong>in</strong>side the buried equipment box.<br />

Site B<br />

Sampl<strong>in</strong>g Site B (see Figures 3.4 and C.3) was located <strong>in</strong> an agricultural environment near<br />

Handschuhsheim, at the coord<strong>in</strong>ates N49 ◦ 25.775 ′′ E8 ◦ 39.760 ′′ at 109 m above sea level, see Figure<br />

3.2. The borehole was placed very close to the end of a hedge, partly covered <strong>by</strong> its leaves. A<br />

paved road of approximately 2 m width runs from north to south, at a distance of 1.5 m to the<br />

borehole. The immediate surround<strong>in</strong>g consists of a small meadow with apple trees, enclosed <strong>by</strong><br />

agriculturally used land.<br />

The soil at the site consists predom<strong>in</strong>antly of clay as well: The first 5 cm of turf are followed <strong>by</strong><br />

320 cm of clay, <strong>in</strong>creas<strong>in</strong>gly humid with depth. The follow<strong>in</strong>g layer consisted of 25 cm of humid,<br />

sandy clay. Below 3.5 m the clay displays a reddish gravel fraction.<br />

37

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