HOW CHILDREN PLACE THEMSELVES AND OTHERS IN LOCAL SPACE

This study examines the ways in which children aged 11 to 15 in six adjacent neighbourhoods in a medium-sized Swedish town place themselves and others in local space. Special attention is given to how they discuss a neighbourhood stigmatized in the public discourse and how children who live in this neighbourhood react to the negative representations of the place in which they live. The study is based on group interviews and maps. The study shows that children construct representations of their own neighbourhoods as "quiet" neighbourhoods and place objects of "trouble" and "danger" somewhere else. It is argued that this is done both in relation to their personal knowledge of the neighbourhood and in relation to local and/or media representations of their own and other neighbourhoods. It is shown that the children are influenced by media representations of a stigmatized neighbourhood, but also that they are not passive reproducers of these discourses and that some of them are able to offer counter-discourses. The children living in this neighbourhood experience difficulties in defending it as the quiet place which they perceive it to be to outsiders because of the negative discourses.     

Soil formation in archaeological pits and adjacent loess soils in Southern Germany

The soil formation in a number of pits on a neolithic excavation was compared with that in adjacent loess soils (Hapludalfs) under forest and arable and in Bavaria, Southern Germany. The differences between the soils under consideration were mainly characterized by micromorphological quantification of the illuviated fine clay. In the archaeological pits the amount of illuviated fine clay proved to be nearly twice as much as that in the undisturbed soils. The amount of illuviated coarser matrix components (fine and coarse clay and fine silt) in the neolithic pits did not differ significantly from that in the natural soils. The large amount of illuviated fine clay in the pits was ascribed to the presence of potash during the period of their formation. The formation of coarse grained illuviation cutans was related to deforestation, after which illuviation of the fine clay decreased in intensity and came to a stop.