Wastewater treatment plants (WWTP) are known spreaders of per- and polyfluoroalkyl substances (PFAS) into the environment. Luleå University of Technology is conducting a yearlong study in which PFAS concentrations in the different treatment steps are measured at Uddebo treatment plant. This report covers the first four months of the year-long study. The aims of this study are to see what happens with the PFAS concentrations in the treatment processes, if they are above regulated limits, and to see if concentrations at Uddebo are comparable toreference concentrations in Sweden. Sampled PFAS concentrations were taken once per fortnight in incoming wastewater, after primary sedimentation, after Moving Bed Biofilm Reactor (MBBR), after secondary sedimentation and after the pilot treatment plant containing granulated active carbon (GAC) filter when it was in use. Precursors in incoming wastewater and PFAS in sludge were measured in samples taken once per month. Comparing the 33 analysed PFAS in wastewater at each sampling point, 30 analysed precursors for PFAS in incoming wastewater and 30 analysed PFAS in sludge, only PFOS and PFOA wereregularly found in both wastewater and in outgoing sludge. This indicates a separation of PFAS in the different medium, with sludge having PFAS where the perfluorinated carbon chain length is grater than 6. Out of the analysed 33 PFAS in wastewater PFOA had the highest median concentration of about 7 ng/l with no significant variation between the wastewater sample points. Similarly, the median concentration of total detected 33 PFAS was around 35 ng/l with no significant variation between the wastewater sample points, indicating no significant treatment of measured PFAS during WWTP. This was also comparable to other WWTP in Sweden. PFBA, PFHxA and PFPeA precursors had the highest concentration of the measured 30 PFAS precursors, however, except for one sampling occasion, no significant deviation in precursor PFAS could be detected during the sampling period. Out of the 30 analysed PFAS in outgoing sludge, PFOS had the highest concentration of 6.8 μg/kg dry weight (dw), but no discernible pattern could be identified between sampling dates due to too few samples. PFOS was foundabove the recommended concentration for sensitive land use (3.0 μg/kg dw), but still within recommendations for less sensitive land use (20.0 μg/kg dw) in Sweden. The median concentration of 13.6 μg/kg dw measured PFAS in sludge makes it well below median Swedish concentration. However, all comparisons to other Swedish WWTPs and background concentrations in Sweden were based on a few studies with few samples, potentially increasing or decreasing the median concentration as more research is conducted.

Very often remote peripheral locations with scarce unique attractions find it difficult to attract investment and development in many spheres including tourism. Yet some innovative entrepreneurs have taken advatage of some of these locations, using the natural resources (though not scarce) that they posses to develop themed tourism. The success of these themed establishments located in remote peripheries is renounced as they attract tourists world wide. This thesis therefore explores the fantasy and themed hotel product and location as elements of attraction in peripheral locations. Information obtained  through consultation with expersts will not only bring new knowlege to academia on the subject; it would also be useful in planning new themed destination products in the periphery since it provides inside knowledge on what to consider when setting up establishments of like characteristics.

In glacierised regions, suspended sediment fluxes are highly responsive to climate-driven environmental change and can provide important information regarding the relationships between glacier variations, climate and geomorphic change. As a result, understanding patterns of suspended sediment transport and their relationship with meltwater delivery is of critical importance. However, studies of glacial suspended sediment transport are often limited by interpreting patterns of suspended sediment transfer based on whole-season data, allowing precise patterns to become masked. This thesis aims to contribute to the understanding of suspended sediment transfer in glacierised basins through the investigation of patterns of suspended sediment delivery to the proglacial area of Storglaciären, a small polythermal valley glacier located in the Tarfala valley, Arctic Sweden. High temporal resolution discharge and suspended sediment concentration data were collected during two summer field campaigns at Storglaciären. Interpretations of suspended sediment transport data were made using diurnal hysteresis and sediment availability data, combined with suspended sediment shape and magnitude data classified by applying principal component and hierarchical cluster analyses. Analysis of the dominant discharge generating processes at Storglaciären was also conducted using principal component analysis, allowing patterns of discharge to be better understood. This was complemented by analysis of the structure and evolution of the glacier drainage system by linear reservoir modelling and flow recession analysis. The results suggest that patterns of discharge and suspended sediment transport at Storglaciären are complex, with distinct processes and magnitudes of transport evident at both proglacial outlet streams, Nordjåkk and Sydjåkk. These processes are intrinsically linked to meteorological variables, with both ablation-driven and precipitation-driven discharge exerting influence over patterns of suspended sediment transport in the proglacial area of Storglaciären.

Freshwater ecosystems are under increasing pressure from a variety of contaminants, including heavy metals from mining operations, which can have complex effects that are difficult to evaluate. To detect early warnings from elevated concentrations of metals, organisms are sought to be used as monitoring tools. For example, mouthpart deformities in Chironomid larvae have been proposed as a bioindicator of stress in aquatic environments. However, the frequency and cause of these deformations, and their sensitivity to different stressors remain uncertain. In this study, I evaluated the usefulness of mouthpart deformities as a tool to monitor the effects of heavy metals from mining in northern Sweden. To do this, the mouthparts of 3789 Chironomid individuals analyzed from 17 sites closely located to mining operations and tested against concentrations of metals and DOC in the water chemistry of lakes and rivers. The frequency of deformities ranged from 0.00 – 4.79 % across all sites. Metal concentrations ranged from ‘very low’ to ‘low’ based on biological effect risk assessments. Of these, copper (R2 = 0.73) and cobalt (R2 = 0.66) were found to be significantly correlated with frequency of deformities. Additionally, the occurrence of deformities declined with DOC concentration, this was a nonlinear relationship. Frequencies of deformities observed in this study were lower than what have been reported to similar studies. The result from this study, together with other studies, suggest that deformities in Chironomid larvae are sensitive to even low levels of certain metals and could potentially be a good biomonitoring tool for early warnings of contamination in freshwater environments.

This essay will present the driving forces behind the liquidation of log-driving from 1930 to log-drivings end in 1980 in Umeälven. The debate about the log-drivers status in the river was multifold. The locals saw log-driving as an inhibiting process where, besides work, nothing good came. The hydroelectric stations saw the log-driving as an unnecessary tool because the hydroelectric stations had a larger purpose and were more prosperous than the log-driving. The underlying factors that evoked the log-drivings dismantling were several. Local people, fishing, hydro, but also the increased demand for forest and technology development. The timber became less ”float-friendly” and the forest road network was developed so that trucks became a more efficient and cheaper alternative, which led to the fact that log-floating was an unnecessary tool for the forest industry.

This is an ecocritical analysis of the novel Glupahungern by Andrea Lundgren. I investigate how nature is viewed by looking at two things. First, I look at two functions in the novel. I analyze the function of characters that seem to be in between the human side and the animal side. I call them creatures of the border. I also analyze the function of places that can be seen as borderlands. Places between nature and society. Second, I do a small comparison between Glupahungern and the novel Hjortronlandet by Sara Lidman since they both are written by authors from the north of Sweden and the novels also takes place in the northern parts. Through this comparison I find similarities between the novel and how nature is viewed in them and I come to the conclusion that the place has an impact on the view of nature. Keywords: Nature, Border, Ecocriticism, View on nature, Northern Sweden

<p>This study deals with the influence of topography on glacial dynamics and the genesis of till in an area of moder-ate bedrock relief. An area 25 km west of Lycksele, northern Sweden, was investigated using geomorphological and sedimentological methods. The bedrock is dominated by coarse-grained granites and the topography, ranging in altitude between 310 and 490 m. a.s.l., is characterized by relatively wide, free-lying hills.</p><p>The erosional and depositional features provide evidence of several glacial events, with regional ice flows from approximately the same direction (NW-NNW). The gravel fraction of the till is dominated by material transported more than 10 km. However, the total glacial erosion has been modest, as indicated by the frequent occurrence of residual pre-glacial weathering features. There is no evidence of warm-based conditions during the period when the ice divide of the Late Weichselian ice sheet was situated E-SE of the study area. The major mor-phological impact is most likely by pre-Late Weichselian ice sheets.</p><p>The general stratigraphy at the valley floors is a complex sequence of heterogeneous till and beds of sorted sediments with some evidence of glacial deformation covered by an up to 2.5-m-thick, texturally homogeneous till layer with distinct fissility structure and clast fabric orientation. The lower unit is interpreted as pre-Late Weichselian marginal deposits, and the upper till as mainly formed during rigid-bed conditions, i.e. by lodgement, during the last deglaciation. The role of pervasive deformation and melt-out in the formation of the upper till are discussed. Inferred mainly from till fabrics it is evident that the ice flow was strongly topographically controlled within a relatively wide marginal zone of the retreating ice.</p><p>At the summits of the hills there are only signs of very weak glacial abrasive and depositional activity, sug-gesting frozen based conditions over the summits until a very late stage of the deglaciation. The very thin till at the summits, which also lay as a drape over the thick lee-side deposits, consists of a mixture of relatively fine-grained, distantly derived debris and of local bedrock fragments entrained during a very late phase of plucking.</p><p>On the stoss- and lateral slopes of the hills the till is thin and discontinuous. The irregular bedrock surface in these areas created a “mosaic” of small-scale subglacial depositional environments, which were superimposed on the changes in the conditions for deposition along the hillslope. This till is comparatively coarse-grained, which is interpreted as an effect of syn-depositional winnowing of fines, and locally also because of the incorporation of local bedrock material largely from pre-glacially weathered zones.</p><p>On the lee-sides of the hills the deposits are considerably thicker than on slopes facing other directions. They are characterized by highly variable texture and structure, suggesting a depositional environment characterized by large temporal and spatial variations in meltwater activity and stress/strain conditions. The lee-side tills are inter-preted as mainly pre-Late Weichselian in age.</p><p>The overall conclusion is that the local topography strongly controlled the basal ice flow and produced a com-plex pattern of thermal variations within a relatively wide marginal zone of the ice sheet during the last deglacia-tion. The study supports the view that there are complete transitions between the different genetical types of sub-glacial tills, although the role of deformation by pervasive shearing is uncertain in this type of coarse-grained till.</p>

<p>During the last four decades, acidifications has been seen as a great environmental hazard. To combat the effects of the acidification, the Swedish government is funding liming of affected areas. This practice has been questioned in northern Sweden, since there is no general agreement about the origin of the acidity there. This thesis aims to explain the administrative handling of the scientific disputes, and thereby the relation between the responsible authority, the Swedish Environmental Protection Agency (SEPA) and the research exrecised on the matter. Research findings are therefore compared with the content of interviews, performed by civil servants at SEPA. It is concluded that the liming in northern Sweden is a very complicated issue, involving many groups and individuals - so much so that it might not just be an issue of acidification science.</p>

This study deals with the influence of topography on glacial dynamics and the genesis of till in an area of moder-ate bedrock relief. An area 25 km west of Lycksele, northern Sweden, was investigated using geomorphological and sedimentological methods. The bedrock is dominated by coarse-grained granites and the topography, ranging in altitude between 310 and 490 m. a.s.l., is characterized by relatively wide, free-lying hills. The erosional and depositional features provide evidence of several glacial events, with regional ice flows from approximately the same direction (NW-NNW). The gravel fraction of the till is dominated by material transported more than 10 km. However, the total glacial erosion has been modest, as indicated by the frequent occurrence of residual pre-glacial weathering features. There is no evidence of warm-based conditions during the period when the ice divide of the Late Weichselian ice sheet was situated E-SE of the study area. The major mor-phological impact is most likely by pre-Late Weichselian ice sheets. The general stratigraphy at the valley floors is a complex sequence of heterogeneous till and beds of sorted sediments with some evidence of glacial deformation covered by an up to 2.5-m-thick, texturally homogeneous till layer with distinct fissility structure and clast fabric orientation. The lower unit is interpreted as pre-Late Weichselian marginal deposits, and the upper till as mainly formed during rigid-bed conditions, i.e. by lodgement, during the last deglaciation. The role of pervasive deformation and melt-out in the formation of the upper till are discussed. Inferred mainly from till fabrics it is evident that the ice flow was strongly topographically controlled within a relatively wide marginal zone of the retreating ice. At the summits of the hills there are only signs of very weak glacial abrasive and depositional activity, sug-gesting frozen based conditions over the summits until a very late stage of the deglaciation. The very thin till at the summits, which also lay as a drape over the thick lee-side deposits, consists of a mixture of relatively fine-grained, distantly derived debris and of local bedrock fragments entrained during a very late phase of plucking. On the stoss- and lateral slopes of the hills the till is thin and discontinuous. The irregular bedrock surface in these areas created a “mosaic” of small-scale subglacial depositional environments, which were superimposed on the changes in the conditions for deposition along the hillslope. This till is comparatively coarse-grained, which is interpreted as an effect of syn-depositional winnowing of fines, and locally also because of the incorporation of local bedrock material largely from pre-glacially weathered zones. On the lee-sides of the hills the deposits are considerably thicker than on slopes facing other directions. They are characterized by highly variable texture and structure, suggesting a depositional environment characterized by large temporal and spatial variations in meltwater activity and stress/strain conditions. The lee-side tills are inter-preted as mainly pre-Late Weichselian in age. The overall conclusion is that the local topography strongly controlled the basal ice flow and produced a com-plex pattern of thermal variations within a relatively wide marginal zone of the ice sheet during the last deglacia-tion. The study supports the view that there are complete transitions between the different genetical types of sub-glacial tills, although the role of deformation by pervasive shearing is uncertain in this type of coarse-grained till.

The overall aim of this thesis is to survey and analyse young peoples’ geographical movements, and illustrate the similarities and differences that exist between different individuals.. The aim of the thesis is also to examine and discuss youth’s attitudes and motivation for different forms of geographical mobility. The youth focused on in this project reside in Norrland. The first phase, Mapping of the Geographical Movement of Youth, was carried out through the use of a questionnaire, sent to graduating students in upper secondary school. The second phase, Umeå  Students Abroad, was carried out by interviewing Umeå students who had either completed or were about to begin a period of foreign exchange. The third phase, Emigrants from Sweden, is based on statistics acquired from Sweden Statistics’ (SCB) and from the TOPSWING database. Home: The starting point of this thesis is the conception of “home”. The choice of path to take in life, and where students wanted to live in the future had significance for how they examined the choice between moving and staying; and the role of the home town in a longer perspective as to how the students viewed Umeå. Away: It is not just the place that a person comes from that says something about who she is, but also the place where she is going and the way in which she takes herself there. Many of the upper secondary school students that took part in the questionnaire had been abroad one or more times. Furthermore, many of the students would like to travel abroad again. At the same time, it can be said that there are also young people that do not have extensive experiences in travelling to other countries. Somewhere between home and away: The study shows that students may have very different views of their time abroad. The Tourist Student is one who chooses his/her destination in order to fulfil certain criteria and then mainly stays in the university town, “taking one day at a time.” He or she does not have a thought-out strategy for how the stay abroad should be carried out. The Travelling Student is the student who searches for a particular destination and later also has the ambition to get to know the country and the people that live there. The travelling student can be said to have a thought-out strategy for how to make the most out of his or her time in a foreign country. When away becomes home – or when home becomes home again: The interview study shows that to live abroad or to live in Sweden acquired a different meaning if you had a family. To have a family gives rise to a reason why one may choose to move back to Sweden. On the other hand there were also students for whom the home country was not important. A large portion of those who emigrated from Sweden during the study period moved back again. For those with a college or university education, a few years abroad can be a part of their choice of life path. It is something that one wants and from a career prospective, possibly should do. Rooted, rootless or restless young? The rooted are those who mainly live their entire lives in one place. The rootless represent a mobile life, where there is no home base, instead they create new ones as life passes. I would like to characterise most of the young people that in one way or another is featured in my study as restless. The restless combine, in different ways, the characteristics of both the rooted and the rootless. They are not unwilling to move, within the country, as well as to other countries, but they are at the same time rooted in their home town or in their home country.