Borehole samples from the mounds
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![Page 1: Borehole samples from the mounds](https://reader031.fdocuments.in/reader031/viewer/2022020117/568bd6df1a28ab20349da733/html5/thumbnails/1.jpg)
After the soil samples have been brought into the laboratory, they are placed in water and sodium
diphosphate overnight. This procedure means that the soil and organic material are not bound so strongly
to one another and therefore become easier to sieve.
![Page 2: Borehole samples from the mounds](https://reader031.fdocuments.in/reader031/viewer/2022020117/568bd6df1a28ab20349da733/html5/thumbnails/2.jpg)
The dissolved soil samples are afterwards sieved manually and sorted into different sizes. Three samples
are produced by this method: material over 1mm, between 1 and ½ mm and between ½ and ¼ mm.
![Page 3: Borehole samples from the mounds](https://reader031.fdocuments.in/reader031/viewer/2022020117/568bd6df1a28ab20349da733/html5/thumbnails/3.jpg)
Here the final results of the sieving of the soil sample can be seen. The different size of the material in the
individual samples is clearly visible. Material of approximately the same size is easier to investigate under
the microscope.
![Page 4: Borehole samples from the mounds](https://reader031.fdocuments.in/reader031/viewer/2022020117/568bd6df1a28ab20349da733/html5/thumbnails/4.jpg)
Peter Steen Henriksen from the National Museum’s Natural Sciences Research Department analyses the
cleaned borehole samples from the mounds under the microscope. Here the different types of seeds and
other forms of organic material are counted and compared. Photo: Mads Dengsø Jessen.