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Browsing by department "Department of Geosciences and Geography"

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  • Ala-Louko, Veera (2016)
    The conventional understanding and model of development is based on economic growth. This dominant way of creating development has consequences to natural, cultural and social environments, which cannot be overlooked. The transformations within these environments are increasingly connected to the prevailing socio-economic model of neoliberalism, but are often not considered in its contextualization at a local scale. The processes of production of space and nature under the neoliberal doctrine have led to economic restructuration and to conformation of geographies of neoliberal environment, which together transform localities. There is an increasing need to investigate how the local inhabitants understand and experience these processes and their outcomes. In this research, place is introduced as an insight to observe these problematics. Place in this research is understood as a changing and dynamic terrain, which articulates experiences of development. This research is qualitative case study which investigates the consequences of production of space and nature in Curepto, Chile. Curepto is one of the localities where the implementation of a normative framework for economic growth has resulted in extensive areas of foreign tree species monoculture and important physical and socio-spatial transformations related to them. The primary aim of this research is to investigate the local inhabitants' accounts of these transformations. The thesis investigates how the locality has changed, but focuses on what these changes have meant for the local community and their sense of place. Physical, sociocultural and emotive dimensions of place as well as their transformations were investigated using qualitative methods, mainly semi-structured interviews. Residents were interviewed both in urban and rural districts. The findings of this research indicate that the forest industry and tree plantations have been important drivers behind the physical and socio-spatial transformations. The extensive plantations of pine and eucalyptus have changed the physical environment and these transformations are reflected in the social and cultural geography. Environmental degradation, changed circumstances of land property, loss of native forests and drought constitute transformations that affect livelihoods negatively especially in the rural districts, and come in parallel with a loss of local tradition and culture. The meaningful space the inhabitants experience diminishes and is made more one-sided, as access to the natural environment becomes more difficult and the interaction with it is lost. Although transformations within place are considered negative, the meaningful relation inhabitants have with place remains positive. Participants redetermine their practices and livelihoods, and re-articulate the relation with their surroundings in order to stay in their place. The local community lives in a space that is both familiar and foreign to them, loved and hated at the same time.
  • Hård, Petri (2017)
    The aim of this study is to find out about away trips that Finnish ice hockey supporters make within Finland. The idea is also to find out if destination cities of the trips could better benefit from traveling hockey fans. The study aims at finding the basic frame by which the fan organizations choose their destinations, the motives of those who participate and visitors' perceptions of services available at the destination ice halls. Both qualitative and quantitative methods are used. Not many earlier studies about the topic exist. Literature about sport tourism concentrates mostly on people doing the sports themselves. Academic literature about sport fans, in turn, is usually about the psychological side of fandom. Several studies of Finnish ice hockey fans exist though. Also their point of view is often psychological. Many of Finnish studies are also only thesis-level works. Because of lack of earlier research about the topic, this work can be seen as a baseline research. Fan organizations choose their travel destinations mostly based on game schedule. Trips are mainly made to games played on Saturdays. On other days of the week the destination should be within a short distance. Distance to destination isn't very important on Saturdays unless the destination is very far away. Visiting fans don't spend much time at the destination city on a regular trip. Usually the fans enter the ice hall straight after stepping out of the bus and return soon after the game. However, overnight trips might interest the fans especially if the destination is far away. Previous experience about destinations also affects the choices fan organizations make. Most important reasons for participating in a trip are especially seeing the favorite team play and supporting the team. Traveling itself as a process isn't an important factor while making the decision to travel yet there could be interest to go on overnight trips more often than fans currently do. Also company affects travel decisions as people prefer going to games with friends or acquaintances. SM-Liiga ice halls seem to have all the different service types away trippers need. There's not much demand on a variety of services as visiting fans mostly buy just drinks of food. Supply of these services is good but visitors are less happy with quality, variety and price of the products sold. An important factor for game experience are the seating arrangements at the ice hall. They were found to correlate with happiness with overall game experience. Ice halls are considered safe and security works well. All in all visiting fans are happier with the service they receive at the ice halls than with the services itself. To improve their service in the eyes of visiting fans, the hosts should pay attention to variety of food and drinks and offer visitors seats that are suitable for their needs. Host organizations and local stakeholders could benefit from offering visiting fans moderately priced packages that could include for example transportation, game ticket, a meal and accommodation or some of these services. This way they could get visitors spend more money at the destination city and at the same time income would spread to a larger number of stakeholders.
  • Oksanen, Otto (2017)
    The carnivoran fauna in East Africa has changed drastically over the last seven million years. Turnover in the fauna affected taxonomic composition during the Miocene-Pliocene boundary, as well as led to both reduced species richness and functional richness from 3 Ma ago onwards until the modern fauna was in place. The objective of this thesis was to examine how the niche space in the East African carnivore guild has changed over time by making inferences on the feeding ecology of individual taxa from two sites located in the Turkana Basin, a major depository of vertebrate fossils in northern Kenya. The first site, Lothagam, covers the time slice 7.4–5.3 Ma ago, whereas the second site, Koobi Fora, covers the time slice 3.4–1.38 Ma ago. An ecomorphological analysis was performed, which included dental ratios, body mass estimates and jaw measurements of carnivorans, as well as body mass estimates of some of their potential prey animals (bovids). The carnivorans were assigned to four different dietary specializations based on their dental ratios: hypercarnivore, bone-cracking hypercarnivore, mesocarnivore and hypocarnivore. Individual taxa were also identified as small-prey or large-prey specialists based on their body mass estimates and jaw depth. According to the results, the carnivore guild of Lothagam was mostly composed of hypercarnivores along with some mesocarnivores that were trending towards hypercarnivory. There is a notable absence of hypocarnivores and bone-cracking hypercarnivores in the Lothagam sample. The carnivorans of Koobi Fora displayed more variation in the dental ratios between individual taxa. Compared to the Lothagam guild, the Koobi Fora guild also included advanced bone-cracking hypercarnivores, as well as large hypocarnivores that are absent from East Africa today. The changes in the dietary specializations of individual Koobi Fora taxa were accompanied by an overall increase in body size, which coincided to some extent with an increase in prey size, at least with bovids. The results indicate that some of the extinct members of the carnivore guild became more ecologically specialized during the Plio-Pleistocene, which probably made them more vulnerable to extinction than the more generalized taxa during changing environmental conditions.
  • Rissanen, Tuuli (2018)
    Northern and high-altitude environments are expected to change dramatically due to climate change which strongly affects vegetation. Regarding to this, there has been interest on investigating how climatic factors affect vegetation distribution. One of the widely used methods to study species environment relationship is spatial species distribution modelling, in which the aim is to estimate suitable niches for species. However, only a few comprehensive distribution predictions for whole species groups have been made at a fine resolution and covering large extents. In the case of arctic-alpine plants Fennoscandia offers a good research area in terms of northern location, variable topography and wide climatic gradients. In this thesis the aim was to discover how climate affects the distribution and species richness patterns of arctic-alpine vascular plants. Relationship between arctic-alpine vegetation and climate was investigated by producing distribution predictions for each species based on important climatic variables and topography. Species data included observations from national species portals of Sweden and Norway, as well as field observations from three test regions Kevo, Northwestern-Lapland and Rastigaissa. The explanatory variables used were efficient temperature sum, water balance, minimum temperature of the coldest month and relative height. The species distribution predictions were produced using a 1 km2 grid covering whole Fennoscandia. Four different modelling methods (GAM, GLM, GBM, RF) were used and the predictions done with two different data sets. First the models were calibrated using only the observations from species portals, and the predictions were evaluated at the Lapland´s test regions. On the second modelling round the whole data was used in model calibration. From the modelling results both individual species distributions and the distribution of the whole vegetation group were investigated, as well as the relative importance of the explanatory variables. Then individual species distribution predictions were combined to visualize and study arctic-alpine species richness and its hotspots. Distribution of arctic-alpine vegetation was affected most by efficient temperature sum and minimum temperature of the coldest month. However, the relative importance of the variables varied for different species. Also the differences in the calibration data affected the results. Mainly species´ predicted distributions are located on areas where growing season is short and winter temperatures are low, even though there was some variation in the responses caused by the latter variable. Temperature variables were also significant in explaining species richness and its hotspots. It was shown that species richness focuses to the coldest areas and benefits from a bigger topography gradient. The results of this thesis show that climate defines both the distribution and the richness of arctic-alpine vegetation in Fennoscandia. However, resolution of one square kilometer does not fully capture the heterogeneity of the arctic-alpine area since temperature and moisture conditions vary greatly locally, for example depending on snow cover. Research on different scales is still needed to understand complicated species environment relationships.
  • Virtanen, Elina (2015)
    African climate science is still underdeveloped; the related infrastructure is limited and climate observation network is sparse. The lack of observations is usually compensated with coarse macro-climate models (1 km2), of which only few concentrates on tropical Africa and on the spatial variability of rains. The need for fine-resolution data is growing, as more accurate information (5-100m) is utilized in different sciences. There has been a surge in micro-climate studies utilizing small dataloggers to observe climate variability, as loggers can be placed to different environments regardless of the complexity of a terrain. Accurate, fine-scale climate models are needed in ecological research, where species distributions are related to environmental gradients. Most of the studies describing species occurrences rely on macro-scale climate models that have been averaged over years, although the factors restricting species occurrences in an environment are developed even under one growth season, and are dependent on climate extremes. Accurate information of species and its occurrence environment is even more needed as climate is changing; species habitats are threatened through the warming of climate and its resulted effects. Fine-resolution data of micro-climate is needed especially in the studying of epiphytes living in tropical montane cloud forests, as epiphytes are dependent on the surrounding environments' specific atmospheric composition, namely relative humidity. The knowledge of epiphytic species distributions is poorly studied, although epiphytes are known to react fast to quick changes in environmental conditions. In this study small dataloggers were placed around the Taita Hills in a mountainous region of Kenya to record spatial and temporal micro-climate variability. Annual, monthly and extreme temperature and humidity parameters were studied through statistical spatial modelling, with generalized additive models (GAMs). The significance of each thriving factor of climate parameters were studied separately with bootstrapping. Of thousands of models created, temperature was best explained by elevation, and humidities by land cover (e.g. distance to forests), a proxy of canopy cover. Modelling extremes requires more research, as extreme models proved to be most difficult to model. More weight should be put on accurate environment gradients (e.g. canopy cover) when modelling spatial climate variability in a fine-scale. Created fine-resolution grids were tested in modelling the distributions of epiphytic species through Boosted Regression Trees (BRT). Models created gave an insight to the drivers of epiphytic species distributions and to the limitations of their occurrences in a limited environment. Different explanatory variable groups were tested (topographical, in situ, climate groups), of which climate explained most of the variations in epiphytic species occurrences when considered with AUC-values. Some epiphytes seemed to be specialized to certain habitat trees, highlighting the value of not only indigenous trees but exotic ones. Epiphytes were restricted to occur under certain temperatures and humidities ranges that is an indication of the vulnerability of epiphytes to changing climate.
  • Linden, Mecki (2016)
    The purpose of this study was both to establish Finnish geography teachers' experiences on and opinions of the active teaching method flipped classroom, and to examine the impact of the method on high school students learning outcome in natural geography. The aim was to aquire information on how familiar geography teachers are with flipped classroom and what qualifications they have on using an active teaching method that requires technological knowledge. The experiences and opinions about flipped classroom of geography teachers (n=49) were charted using an e-mail survey. The teaching experiment (n=32) was implemented as a field experiment in a first year geography class at a high school in Southern Finland. The results were analysed using a statistical analysis program and presented through graphs and citations. The survey shows that Finnish geography teachers are familiar with flipped classroom but that only a few of the respondents use the method in their work. The most common excuses among the teachers for not using flipped classroom, or not being interested in learning new teaching methods, is a lack of time and resources. The teachers' technology skills are good and they agree on the fact that geography education is better when technology is implemented in the classroom. The teaching experiment shows that the teaching method used didn't affect the students' learning outcomes substantially but a small negative impact was nevertheless shown. Active education methods need to be implemented in the Finnish classrooms in order to meet the goals of the new curriculum. Digitized matriculation examinations, new curricula and a new distribution of courses places new demands on geographical education. Geography is, fortunately, a subject that easly allows different educational ideas and methods to be used.
  • Kuusela, Tytti (2016)
    The Jokisivu gold deposit is a structurally controlled orogenic gold deposit that was formed during the Svecofennian orogeny when the Pirkanmaa belt, a turbidite dominated subduction zone complex, was pushed below the Tampere schist belt in the north. The Jokisivu gold deposit formed in a brittle-ductile shear zone and gold mineralization is related to the youngest deformation stage. The main focus of this study was in fluid inclusions in quartz veins. Quartz grains host fluid inclusions that carry information of the prevailing P–T–X conditions during fluid events in the quartz veins. According to the properties of fluid inclusion assemblages (FIA), six fluid inclusion types were distinguished. Fluid inclusion types A1, A2 and A3 are aqueous and fluid inclusion types B1, B2 and B3 are aqueous–carbonic. Relative chronology of the fluid inclusion types was determined by cross cutting relationships of fluid inclusion assemblages. Relative chronology of fluid inclusion types from oldest to youngest is A1, A2 and A3, B3, B1 and B2 indicating that aqueous fluids came in first and aqueous–carbonic fluids followed them. Microthermometry was conducted for all the FIAs. The melting point of CO2 was generally below the CO2 triple point ranging from -59.15°C to -56.73°C indicating the presence of other gaseous phases that were later confirmed with Raman spectroscopy to be CH4, N2 and even H2S. Raman spectroscopy was conducted for qualitative analysis of the phases presentn the inclusions. Quartz crystallization temperatures were calculated using titanium in quartz geothermometer (TitaniQ). TitaniQ was well suited for Jokisivu samples because titanium concentrations in the hydrothermal quartz were quite constant. Combining TitaniQ P–T slopes and fluid inclusion assemblage isochores from microthermometry and Raman spectroscopy yielded a good estimate for P–T conditions of fluid entrapment of 390–470°C and 170–345 MPa. The estimated temperature range is higher than the previous studies have suggested. However, the P–T range estimated for Jokisivu is in accordance with the P–T conditions of other Svecofennian orogenic gold deposits. Judged by the mineralogy of the quartz vein - host rock contact, the most important factor triggering gold precipitation in Jokisivu has probably been fluid-rock interaction. Strong sulfidation of host rock reduced the sulfur fugacity and enabled gold precipitation.
  • Fredriksson, Johan Rafael (2017)
    Fluid inclusion studies on pegmatitic bodies are performed to gain insight on the conditions during the formation of the pegmatites as FIs can be seen to directly mirror the fluids that were present during the formation of, most commonly, the quartz in the pegmatite. Continued progress in the methodology of measurements specifically of HFSE from FIs with relatively new methods Laser Ablation – Inductively Coupled Plasma – Mass Spectrometry enables us to measure elements that previously have not been able to be quantified. The study reports the pressure-temperature conditions and trace-element compositions of the two pegmatite bodies Altim and Tamanduá formations using microthermometry and LA-ICP-MS on fluid inclusions and shows the major and trace-element composition of the muscovite and feldspars with Electron Probe Microanalyzer (EPMA) and LA-ICP-MS respectively. The rare-element pegmatite bodies Altim and Tamanduá are located within the Borborema Pegmatite Province (BPP) in North-eastern Brazil. The BPP is emplaced within the Northern Domain (Northern Tectonic Sub-Province) of the Borborema Province as a 75 by 150 km large area trending NNE-SSW direction, along the eastern part of the Seridó belt. The rare-element pegmatites are considered to have been formed from the highly undercooled residual melts of the granitic intrusions. The G4 leucocratic pegmatoid granite and the GR3A and GR3B pegmatitic granites are considered to be the source of the pegmatites in the BPP as their ages are the closest match to the 509–525 Ma age measured from the pegmatites. The fluid inclusion analyses were performed on the quartz from the different zones (I–IV) of the pegmatite bodies where zone I is the outermost zone and zone IV the quartz core and from the euhedral quartz found from miarolitic cavities in the pegmatite. The Altim samples are mostly fluid rich, L 80% + V (+ S) (L:Liquid; V:Vapor; S:Solid) inclusions and some of the larger (primary) inclusions within the euhedral quartz samples show multiple S. The Tamanduá samples show larger diversity of Fluid Inclusion Assemblages (FIA); aqueous-carbonic, monophase vapour, vapour-rich two-phase and FIA with immiscible liquids (possible phase separation). The immiscible liquids have possibly been formed through boiling of the fluids within the pegmatite providing a possible deposition mechanism for the columbite-tantalite ore minerals found in the Tamanduá locality. The two pegmatite bodies have clearly different major and trace-element compositions with specifically elevated Zn content in the Altim pegmatite body which clearly defines the two pegmatite bodies as two different formations. Furthermore, the salinities for the two pegmatite bodies have a clear division with low–moderate aqueous-carbonic FI in the Tamanduá and moderate–high salinities in the Altim pegmatite body. The two pegmatite bodies appear to have no connection to each other through a connected evolutionary history and the Tamanduá pegmatite appears to be the more highly fractionated of the pegmatites. LA analyses on fluid inclusions provided trace-element data for the previously poorly reported HFSEs Nb and Ta showing concentrations of 0.1–3.2 ppm (excluding extreme outliers) with Nb/Ta average abundance ratios between 1.5 and 3.5. The highest concentrations of Nb and Ta directly correlating with the highest concentrations of Al.
  • Ranta, Eemu (2017)
    Out of all igneous rocks, carbonatites are perhaps the ones most sensitive to changing chemical environments and P-T conditions. As a result, their primary chemical and textural characteristics are more often than not altered by secondary processes. Discerning between the two is essential in order to make correct petrogenetic inferences from textural and chemical data. In this study, the 1.3 Ga siderite carbonatite of the Grønnedal-IÌ ka alkaline complex of South Greenland is used as a natural laboratory to identify mineral chemical and textural fingerprints of hydrothermal alteration in iron-rich carbonatites, with a second aim of describing the paragenesis of a high-grade magnetite mineralization in the locality. Trace element chemistry of magnetite, calcite, siderite and ankerite-dolomite is analyzed in situ by electron-probe microanalysis (EPMA) and laser ablation inductively coupled mass spectrometry (LA- ICP-MS). Magnetite is shown to be a product of oxidation of siderite and is exclusively of hydrothermal origin, characterized by low Ti (1-12000 ppm) and V (1-200 ppm) concentrations. High Nb/Ta (up to 1000) and Zr/Hf (up to 300) ratios in magnetite suggest formation mediated by fluorine-rich fluids. Hydrothermally reworked siderite is enriched in Mn and light rare earth elements (LREEs) and has a depleted Y/Ho ratio. In contrast, hydrothermally reworked calcite is enriched in Y/Ho and depleted in LREEs. A secondary mineral assemblage of apatite, strontianite, barite, REE-fluorocarbonates and ankerite-dolomite is associated with the alteration, which increases toward the contact to a 55 m wide basaltic dike that cuts the carbonatite. Unusual mineral compositions are found close to the dike contact, including magnetite with up to 1 wt.% Nb and calcite with 1 wt.% REEs, both the highest reported values in the literature. Together, the data point to the dike intrusion as a heat source of a hydrothermal convection cell, driving hot F and CO2 rich fluids that mobilized P, Sr, Ba, Mn, LREE, Nb and Ta and reacted with and altered the composition of the carbonatites up to a distance of 40 m from the intrusion contact. The results underscore the necessity of a careful textural and mineral chemical assessment in studying the petrogenesis and subsolvus evolution of ferrocarbonatites.
  • Ronkainen, Katariina (2014)
    The term 'Third World women' has its connotations back in the history reflecting both the juxtaposition of developed and developing world, and the dichotomy based on sex. It is still a widely used concept in current everyday life. The women of developing countries are portrayed under one category as Third World women in news, journalism and textbooks. As a term Third World women is understood in context of certain geographical locations and stagnant representations of people. In core are also their victim roles in relation for example to religion, culture or men. The aim of this master's thesis is to examine representations of the Third World women in Finnish development journal. Temporal changes in representations are discovered by observing the forty-year long publishing history of Kehitys -journal (former Kehitysyhteistyö). The main premise of this thesis is the idea of social constructionism. In social constructionism actions and thoughts are seen creating the social reality and language used both reflecting and creating it. The thesis questions media's representational power to name, illustrate and portray women in developing countries. This is done by utilizing theories of feminism, postcolonialism and development studies. Caroline Moser's and Janet Momsen's listings about the policy approaches on Third World women can be held as the frame work of this thesis. They have categorized global trends in development discourses relating to women. By comparing these approaches, trends in feminist and development theories, with the Finnish development journals, linkages between context and place specific representations of the Third World were found. Even though Finnish trends in Third World women's representations were less varying, still universal relations were able to be discovered. By conducting critical discourse analysis and content analysis of the women related articles in Kehitysyhteistyö and Kehitys -journals during the publications period from 1969 to 2009, it was possible to find five different kinds of discourses: women in development discourse, welfare discourse, efficiency discourse, misery discourse and life story discourse. Within these discourses main changes were in the ways to write and position women. Changes occurred for example in the themes relating to women and in their subjective narration. During forty years, the representations of the Third World women have changed back and forth, but it seems that the current trend in development journalism in Finland is highlighting the subjectivity and expertise of women. Women's own interests and thoughts are getting more exposure and the representational top-down dictation is decreasing while giving the floor to personal depictions.
  • Stenholm, Noora (2015)
    Involuntary displacements are more common than ever, and the reasons vary from natural disasters, wars and conflicts to environmental degradation and development-induced displacement. Typically, the victims of these phenomena inhabit the Global South, and are further impoverished due to the lack of having a say where and how to live. The lack of social justice and recognition of social development is typical in large-scale involuntary displacements, and also affects to the abilities of people to reconstruct and recover after resettlement. The linkage between forced migration and risk to impoverishment has been widely acknowledged especially in cases that lack participatory measures and proper compensation for the victims. When the impacts are recognized, it is understood that forced resettlement has effects in the economic, social, and physical spheres of life, and can be a major burden for the urban poor. However, involuntary displacement also disrupts the attachments and constructions of sense of place, which have further impacts on social cohesion. The question of community reorganization is crucial in the context where resettlement is simultaneous and combines various heterogeneous groups. The aim of this research is to examine the extent and quality of rehabilitation after involuntary displacement in an urban environment in Sri Lanka. The focus in this research is given to women, as gender is a significant factor in resettlement outcomes, yet it is often ignored in planning and implementation. Gender roles and norms in Sri Lanka are still fixed and conventional, making it an interesting approach to study resettlement and rehabilitation and the daily interactions and perceptions on them. A case study for this research took place in four resettlement sites in the outskirts of Colombo Metro Region, Sri Lanka, which is in the midst of significant urban development plans that aim to relocate tens of thousands of slum dwellers in the need to release prime lands for investments, simultaneously beautifying the city and fighting frequent flooding. The methodological approach applied in this study addresses feminist geography while it looks at rehabilitation measures in the everyday life point of view. It utilized semi-structured interviews of resettled women as a key research method. The case study took place in upgraded underserved settlements that inhabit tsunami-displaced people and development-induced displaced people. Also local experts were interviewed in order to gain a broader understanding of the dynamics and urban policies in the Colombo Metro Region. The case evidences that rehabilitation is a slow process of adaptation, and that physical assets alone cannot improve the livelihoods of slum dwellers. More emphasis should be put into the social relations and community dynamics if participatory measures and development-from-within are to fully deliver. Also full tenure is needed in order to the people to adapt to the mainstream society. For women the question of belonging and reconstructing the sense of place is essential as they spend a lot of their time at home and the immediate environment, and are traditionally in charge of homemaking. Therefore the sense of place and community are essential in the creation of social cohesion and management of the new neighborhood, and along with gender sensitive approaches should not be overlooked if sustainable resettlement is to be pursued as a consequence of ever more crowded cities of the South.
  • Bohm, Katja (2018)
    Mid-Proterozoic mafic dyke swarms in southern Finland are associated with rapakivi magmatism. The dyke swarms are commonly referred to as “Subjotnian” (1.64–1.54 Ga), being older than the rift-filling Jotnian sandstones. Mafic rocks from five dyke swarms located in Åland, Satakunta, Häme, Suomenniemi and Sipoo were studied in this thesis. An X-ray fluorescence (XRF) analysis was made of 110 rock samples from 101 mafic dykes and one mafic intrusion. The analyses were made of the same rock samples as previous paleomagnetic studies. Overall, the Subjotnian mafic dykes in southern Finland are hyperstene-normative tholeiitic basalts or basaltic andesites with varying MgO contents (3–15 wt%). Some dykes show alkaline features with higher total alkali and/or Nb/Y values. They vary from quartz- to olivine-normative types. The dykes of the Åland swarm form two geohemical groups. The division is accompanied with a switch in magnetic polarity and distinct virtual geomagnetic pole positions. These observations imply that two separate magmatic events/pulses that have an age difference have taken place in Åland. The Satakunta dykes form two geochemical groups of which the other includes presumably Svecofennian dykes that show high Nb/Y values at given Zr/Y ratios. The dykes of the Häme swarm form three geochemical groups. Although some Suomenniemi dykes show geochemical and paleomagnetic affinities to Häme dykes, they probably represent a distinct igneous event of the event that formed the nearby Häme swarm. The Sipoo dykes are very homogeneous in their geochemistry and can be distinguished from the emplacement events that formed the other Subjotnian swarms. The Subjotnian dyke swarms in southern Finland that are believed to have emplacement ages of >1.63 Ga (Häme, Suomenniemi and Sipoo swarms in S-SE Finland) generally have higher Nb/Y (and Zr/Y) values than the dyke swarms that are believed to record younger magmatic events at <1.58 Ga (Åland and Satakunta swarms in SW Finland). Some Satakunta dykes, however, have geochemical and/or paleomagnetic implications that suggest they have an older Subjotnian age than the dated 1.57 Ga dyke in Satakunta. Further chronological work on the Satakunta dyke swarm is needed to verify the age of the dykes. Many of the Subjotnian dykes show a secondary magnetization component, called the “B-component”, whose direction is always close to, but distinct of, the Present Earth Field (PEF) at the sampling location. There was no correlation between the B-component and the magma types of the dykes. The B-component occurs mostly in dykes that are very altered. Thus, the results support previous suggestions that the B-component formed due to hydrothermal alteration of the rocks and the subsequent formation of new magnetic minerals.
  • Karesvuori, Tommi (2015)
    Lake Pyhäjärvi, the largest lake in southwestern Finland, has been under considerable external nutrient loading for the past decades. Rivers Pyhäjoki and Yläneenjoki are the only major input rivers of the lake and are the source of most of the external nutrient loading to the lake. The hydrogeochemistry of the Lake Pyhäjärvi catchment, as well as the catchments of the two input rivers, and groundwater-surface water interaction were evaluated using a wide array of geochemical tracers (major ions, dissolved silica, stable isotopes of oxygen and hydrogen, electrical conductivity and radon-222). Additionally, the feasibility of using mass balance based methods to separate river waters of the two input rivers to their respective source components was evaluated independently with each tracer analysed. In the context of this study, stable isotopes alone were deemed plausible and were only usable in the River Pyhäjoki catchment as there was not enough difference between river water and precipitation (new water) stable isotope proportions in River Yläneenjoki. Employing the stable isotopes of oxygen, mass balance based modelling was attempted to separate the hydrograph of River Pyhäjoki to its end-members (new water and old water). Based on the obtained data, the hydrogeochemical content of the surface waters of each subcatchment (Pyhäjärvi, Pyhäjoki and Yläneenjoki) differed significantly. Additionally, the groundwaters were clearly distinguished from surface waters. Differences were most apparent in stable isotope proportions as well as dissolved silica, and in the case of groundwaters in radon-222 concentrations. This categorization was further supported by a hierarchical cluster analysis. Surface waters showed varying signs of evaporation, whereas groundwaters retained the stable isotope characteristics of mean annual precipitation. Dissolved silica concentrations appeared to be mostly affected by the amount of easily soluble silica in the sediment, water residence time, as well as biological uptake in the surface waters. Lithology seemed to be the controlling factor in radon concentrations, with areas of granitic bedrock having the highest concentrations. The hydrograph separation of River Pyhäjoki gave results between 66–88% of old water in the river at the time of sampling, consisting likely mostly of groundwater. Though this result corresponds well with recent similar studies in the area, there were considerable sources of uncertainty, therefore making the result best thought of as indicative. However, there was clear evidence of groundwater-surface water interaction in all of the subcatchments of Lake Pyhäjärvi, with clear evidence of groundwater discharging into the lake, lake water infiltrating into an aquifer near the shore of the lake, as well as signs of groundwater discharging into the two input rivers.
  • Räisänen, Milja (2018)
    As a part of Kumpula Campus Drill Hole Project, a 370 m deep drill hole was drilled on the University of Helsinki, Kumpula campus area in December 2015. Drilling took place on an amphibolitic outcrop, which is the main rock type of the area and part of the 1.9 Ga old Svecofennian orogenic belt. In this work, the geochemistry of the campus bedrock is analyzed, focusing on the amphibolite. Granite, actinolite rock and diopside-actinolite skarn are additional rock types described from the core in this work. The geochemical methods utilized are a portable X-ray fluorescence (P-XRF) spectrometer Niton XL3t GOLDD+ by Thermo Scientific and a laboratory wavelength dispersive X-ray fluorescence (WD-XRF) spectrometer PANAlytical Axios mAX 4kW. WD-XRF device is utilized in quantitative analysis and semi-quantitative Omnian scans. In addition to geochemical interpretation of the bedrock, feasibility of the P-XRF device in outcrop and drill core related studies is evaluated by comparing the methods. The surface of the drill core was analyzed with the P-XRF device. Representative samples of each rock type were sawed of the core and analyzed with both P-XRF and WD-XRF Omnian scans. In addition to surface analyses, a fused bead was prepared from one representative amphibolite sample and analyzed with WD-XRF quantitative method. Outcrop studies focused on the feasibility of the P-XRF device in in situ analyses. Compared to nearest temporally related amphibolite units, the amphibolite of the campus bedrock seems to be more felsic on average. All described rock types are connected to former petrogenetic interpretations of the local bedrock. However, further geochemical analyses are required to verify the interpretations. WD-XRF quantitative method and Omnian scans suggest almost similar results for fused bead of the amphibolite. Changing the sample type to solid rock surface introduces heterogeneity related problems to the quantitative determination of Omnian scans and quality of the results decreases almost to the level of P-XRF. Yet, the advantage of the Omnian scans method in rock surface analyses compared to P-XRF is better detection of light elements. For example, P-XRF device detects Mg, Al and K poorly and Na is not detected at all. On the other hand, SiO2 is on average detected quite accurately from rock surface with P-XRF when compared to WD-XRF quantitative method for fused bead. WD-XRF Omnian scans and quantitative application results of fused bead do not seem to differ remarkably. Broad rock type classification can be made with P-XRF device for drill core, but results cannot be considered quantitative. It should also be noticed, that the major element oxide sum values of P-XRF drill core surface analyses are quite low on average (84.00 wt.%). In outcrop analyses, different features lower the quality of the rock surfaces, resulting in even lower major element oxide sum values in analysis. Although major oxide sum values are very low on outcrops, relatively high amounts of for example Cl, S and P are detected for unknown reasons. Major advantages of the P-XRF device are the ease of use, light weight and rather good detection of for example SiO2. Developing the quantitativeness of the device would make it more comparable to laboratory XRF devices but it already has multiple features that are highly beneficial in a wide range of scientific fields.
  • Hellgren, Daniela (2015)
    Climate change and the threat of an ecological collapse in the near future calls for rapid invention of new methods and tools at the service of informed decision making. Backed by academics Esri, Environmental Systems Research Institute – a multinational company and market leader in GIS (geographic information systems) have spread the word of geodesign as meeting sustainability demands in a variety of forms, allowing design processes based on science as well as values. Esri have been clear on creating a community, collaboratively developing the concept further, to meet global spatially related design challenges. The technological maturity have reach a critical level allowing new forms of fusions between geographic information systems (GIS) and design, but complete technological solutions are not yet available. In the study three research questions are answered. Two are, shortly, what is geodesign and what might it mean for professionals in geoinformatics. The study penetrates the concept of geodesign, using a qualitative and holistic approach. The components central to geodesign are highlighted, keeping the focus on the geospatial dimension of geodesign and the relevance for village planning. Village planning is a design process with deep local roots. The collective vision and will for the future is documented. The study introduces and discusses village planning according to changes in society and the demands it brings upon the villages; decentralized responsibilities and fulfillment of local democracy. The implications of geodesign on the spatial dimension of village planning is answered in the third research question. Finland-Swedish village plans are analyzed in theory-driven illustrative case study. Steinitz framework for geodesign is used as an analytic framework in a theory-driven illustrative case study. Supporting questions included in Steinitz framework, a procedure originally developed for landscape planning but now considered useful for geodesign in general, is used as analytic framework. The framework's analytical contribution is supplemented with interpretation based on knowledge of GIS, geodesign and village planning. The premise in the study is that geodesign have the potential to master a variety design processes while providing a timely concept for village planning. In relation to geodesign, village planning is analyzed as a local endogenous design process, showing high degree of participation. Steinitz framework consists of six models with pairwise relations. On the axis process models-change models a lacking correspondence in the village plans is identified, also a general lack in the holistic approach is identified, especially in systems and process thinking. The village plans also shows distinct strengths. The most prominent is the degree of participation. This means that village planning have potential to be supported by geodesign but also provide a model for citizen-led geodesign. Geodesign can be seen as theoretical and benefits obscure. In this study analytical results and interpretation illustrates what the theoretical approach of geodesign means in practice. Quotes from village plans supplemented with graphics, supporting the comparison of the similarities and differences between Steinitz framework and village planning, highlights the concept geodesign and brings it closer a real application in village planning.
  • Venäläinen, Emilia (2014)
    Geographical Information Systems (GIS) are increasingly used to support the emergency planning. GIS methods can be utilized when planning the emergency response system as well as in the emergency management during and after incident. In this study, GIS methods are applied to maritime Search and Rescue (SAR) planning. Traffic amounts are constantly growing in the Gulf of Finland (GoF) and SAR response has to keep up with them. Means to evaluate the SAR response are needed to ensure the adequacy of rescue resources. The voluntary SAR response in in the Finnish waters of the GoF is evaluated. The focus is on the operations of the Finnish Lifeboat Institution (FLI) that is the umbrella organization for voluntary maritime rescue associations in Finland. However, it is hoped that also other SAR operators can apply the presented methods when planning their SAR operations. The main interest is in boating because leisure boats are most often the object of a rescue mission. Timeliness is crucial in emergency operations and thus the SAR response is evaluated here mainly based on the response times. The response times with the current fleet of the FLI are modelled with cost distance methods. Weather factors affect significantly the speed of the Search and Rescue Units (SRU). Therefore, in order to make the results more realistic, different wave height scenarios are included in the cost distance calculations. The wave heights are modelled with two different wind speeds and three different wind directions. The results contain response time maps for the whole study area in different wave height conditions, response times for past incident sites, response times with two units and response times for high incident density areas. Also the number of concurrent incidents in certain sub-areas is observed. According to the results of the thesis the voluntary SAR response in the GoF is generally good. Some improvements would be necessary if the FLI would be the only SAR operator in the area. However, if the units of Finnish Boarder Guard (FBG) are also taken into account the response seems adequate. Therefore, no major changes in the operations of voluntary SAR organizations in the GoF are suggested. Instead, the adequacy of the SAR response elsewhere in Finland could be evaluated. The lower density of SRUs outside the study area may result in inadequacy of SAR response.
  • Tenkanen, Henrikki (2013)
    A vast amount of spatio-temporal data has become available with the fast development of information technology and different monitoring systems over the last two decades. Position-aware devices are one of the most dominant sources for collecting movement data. Spatio-temporal information that is derived from the tracking devices enable to build movement patterns from the targets, and to calculate measurable motion parameters such as speed, change of speed or the direction of movement. This study utilized a specific pilot GPS-based monitoring system called Amazonian Riverboat Observation System (AROS) that was built to collect movement data of the local riverboats on the departments of Loreto and Ucayali in Peruvian Amazonia. AROS provides real-time GPS-data with coordinates and timestamp that indicate where and when the collaborating vessels are navigating. As an outcome of this thesis a specific analytical tool called Trajectory Reconstruction and Analysis Tool (TRAT) was developed. TRAT utilizes variety of geographic knowledge discovery methods to extract knowledge from movement data provided by AROS. Also spatio-temporal transportation characteristics in the study area were analyzed based on AROS data from the year 2012 and utilizing TRAT. This thesis focused on studying if there is seasonal and directional variation in transportation characteristics along the Amazonian rivers, and if river morphology affects the navigation. Also connection between water height of the rivers and travel speed of individual journeys was studied. Results of the thesis suggest that navigation along the rivers has seasonal and directional variation, and also the river morphology seems to affect the movement patterns of the vessels. On navigation route that was mostly meandering by river morphology, the downstream navigation was over 40% faster than upstream navigation during high water and intermediate, but during low water there was no difference between navigation directions. Seasonal variation was over 30% faster during high water compared to low water (on downstream direction). On upstream direction the navigation was fastest during low water but seasonal differences were considerably lower compared to downstream navigation. On navigation route that was mostly anastomosing by river morphology, the downstream navigation was approximately 20 % faster during the entire year. Results suggest that there is no seasonal difference in navigation characteristics along the larger and wider rivers, since the travel speeds were quite similar throughout the year. Fitting simple regression model between average travel speed of the journeys and water levels of the river revealed that there seems to be strong connection between travel speed and river height on the route along Ucayali river when travelled downstream (R2=0.73). On other cases that were studied, the results suggest that there is not connection between travel speed characteristics and river height. Comparing the results with earlier studies implied that the results of this thesis seemed to be fairly accurate. However, it is necessary to validate the results by doing cross-validations between data from different years observed with AROS. Transportation is in a key role when trying to find the factors affecting on development of a certain location. Thus transportation as means of accessibility has significant role in variety of contexts such as conversation, land use changes and deforestation. Results of this study could provide more accurate data for studies focusing on previously mentioned topics in the study area. Also utilization of TRAT in other contexts, such as studying global transportation patterns of professional vessels, could be possible by making few modifications to the tool.
  • Haapalehto, Sophie (2017)
    The Finnish spent nuclear fuel repository is currently under construction by Posiva Oy, and the repository will be located in Olkiluoto Island, western Finland. After intensive research of the site from surface drillholes, construction of underground rock characterisation facility named ONKALO began in 2004 in the same location for the purposes of detailed site characterization. Additionally, to ONKALO and research drillholes, 58 deep drillholes provide a large database for the geological, geochemical, geophysical and rock mechanics site characterisation. One of the key aspects of rock mechanics site characterisation is to determine the in situ stress field prevailing at Olkiluoto. Mathematically, the stress field is represented as a tensor with both direction and magnitude. The effect of excessive magnitudes of the tensor can be manifested by oriented fractures on the walls of the drillholes forming a phenomena of borehole breakouts along the drillhole length. The breakouts form when compressive stress, induced by the concentration of the in situ stress around the drillhole, exceeds the rock strength. The breakouts occur on the opposite sides of the walls. Due to the breakouts occurring in the areas of maximum compression around the drillhole walls, both the direction of the minimum (σh) and maximum (σH) horizontal in situ stress components can be inferred along the drillhole. This Master's thesis was set to identify and map the breakouts in the deep drillholes in Olkiluoto using the acoustic and optical imaging data of the deep drillholes. Acoustic and optical televiewers are two of the several geophysical measuring methods used in the drillholes. They produce images of the walls of the drillholes by wave reflection. During the study, different types of breakouts were identified along the drillholes in Olkiluoto: dotted, zipper-like and a mix of the two previous types with different intensities. The locations of the identified breakouts and other features (direction of σh, rock type, foliation) were recorded in a mapping form developed during this work. The mapping results show that in the total of 19 imaged drillholes, 40 breakout sections exist in only 5 drillholes. Geophysical data show that the breakouts are highly dependent on the geology and the majority of the breakouts occur in veined gneiss and in less competent rock types such as deformed or fractured rocks. Most of the breakouts were observed below 600 meters depth. Major group of directions of calculated σH from the mapped breakouts is oriented NE-SW (60-90°/245-270°) and secondary groups are oriented 107-150°/285-325° and 10-40°/190-220°. In some drillholes, the directions are rotated about 40° due to a significant brittle fault zone separating the site of Olkiluoto into stress field domains.
  • Haapanen, Minttu (2018)
    Maantieteen ylioppilaskirjoitukset sähköistyivät ensimmäisten joukossa syksyllä 2016. Sähköistymisen myötä maantie- teen ylioppilaskoe tarjoaa uusia monipuolisempia tehtävätyyppejä ja geomedia-aineistoja. Painopisteenä ovat aineisto- jen soveltaminen ja tulkitseminen. Geomedialla tarkoitetaan maantieteellisiä lähteitä, kuten karttoja, tilastoja ja kuvia. Pro gradu -tutkielmani tavoitteena on selvittää kuinka kokelaat osaavat ratkaista uudentyyppisiä soveltavia luonnon- maantieteen tehtäviä ja hallitsevat geomedian käytön osana vastausta. Lisäksi tutkin millaisiin kognitiivisen ajattelun taitoihin tehtävänannot ohjaavat. Tutkimukseni avulla saadaan viitteitä lukionsa päättävien oppilaiden geomediatai- doista, vastausten laadusta sekä pystytään kehittämään ylioppilaskirjoituksia entistä parempaan suuntaan. Työssäni tutkitaan kahta luonnonmaantieteen tehtävää syksyltä 2016 ja keväältä 2017 (N=400). Geomedian käyttöä tutkitaan koko aineistosta ja kokelaiden kirjallisista vastauksista käytetään osaa aineistosta (N=140). Tehtävänannot luokitellaan uudistetun Bloomin taksonomian avulla ajattelun eri tasoille. SOLO-taksonomian avulla luokitellaan sekä kirjalliset että kuvalliset vastaukset. Lopuksi tuloksia verrataan keskenään. Tutkimuksessa kiinnitettiin huomiota eten- kin kuvien ja diagrammien tuottamiseen, aineiston hyödyntämiseen ja viittaamiseen sekä kokelaiden valmiuksiin pär- jätä sähköisissä ylioppilaskirjoituksissa. Tutkimuksessa käytetyt luonnonmaantieteen tehtävät ovat rakennettu niin, että ne sisältävät monipuolisesti erilaisia ajattelun taitoja mittaavia tehtäviä. Siirryttäessä tehtävissä eteenpäin vaaditaan kokelailta korkeamman ajattelutaitojen käyttöä. Tehtävissä tulee soveltaa geomedia-aineistoa, kirjoittaa esseitä ja tulkita aineistoa. Saatujen tuloksien perus- teella kokelaiden geomedian käyttötaidot vaativat vielä harjoittelua ja kuvien tuottaminen osana sähköistä koetta koe- taan vielä haastavana. Omaa ajattelua olisi kaivattu enemmän ja moni vastaus vaikutti ulkomuistista tuotetulta. Haas- tavaksi koettiin rakentaa johdonmukainen, selkeä ja jäsennelty vastaus. Vastaukset sijoittuivat suurimmaksi osaksi yh- den rakenteen vastaustasolle. Vastaustaso nousi korkeammalle SOLO-tasolle tehtävänannon vaatiessa korkeamman ajattelun taitotasoa. Geomedia oli selvästi kokelaille vielä uusi asia. Parhaimmillaan itse tuotetut kuvat olivat informa- tiivisia ja tukivat kirjallista vastausta. Kuvat olivat joko itse piirrettyjä, kuvankaappauksia tai muokattuja kuvankaap- pauksia. Itse tuotetut diagrammit olivat selkeitä ja helppolukuisia sekä esittivät tehtävänannossa kysytyn asian hyvin, mutta niidentulkinta koettiin haastavaksi. Aineistoon ja itse tuotettuihin kuviin oli viitattu harvakseltaan.
  • Elf, Charlotte (2013)
    The purpose of this study was to examine what kind of geomorphologic formations can be found in Hanko, Raasepori, Sipoo, Porvoo and Loviisa districts and which of them can be used for teaching purposes. Questions for the study were: 1) What interesting geomorphologic formations can be found in the areas?, 2) In what way could the formations be used by the geography- and biology teachers in the areas in their geography teaching?, 3) Which of the formations will only be thought through schoolbooks because they can't be found in the nearby grounds? The geomorphologic formations taken into account are the following: a) erractic block, b) roche moutonnée, c) drumlin, d) esker, e) terminal moraine, f) kettle, g) pothole. Besides these formations some nationally valuable formations are described as well. This study was done because other studies have shown that outdoor activities are seldom a part of the curriculum. Other studies showed that the reasons for a minor role of outdoor activities are that (the) teachers feel unsure of themselves about the subject, lack of time and too big groups of students. Studies have also shown that field trips stimulate deep learning by presenting a environment where the student can connect the learnt subject with reality. Field teaching isn't only a benefit when it comes to knowledge but also for the students self-confidence and motivation towards the subject. This is because the affective domain in the brain also influences on the deep learning by raising the motivation level and making the students believe in their own capacity. Map- and literature analysis where made to map to which places are worth visiting. Based on the analysis the field investigations were done at the chosen places and the formations were documented with camera and with GPS. Soilsamples were taken from three places for drysieving in the sedimentlaboratory in Kumpula. The morphoscopical features of these glaciofluvial soil samples were also analyzed. The results of the analysis and the field investigations showed that most of the geomorphologic formations that are describe in the schoolbooks for geography in high school can be found in the districts. Because of this there are possibilities for field trips as a part of the curriculum and there by a chance for a more deep understanding of the Finnish physical landscape and the geomorphologic formations by the students. In addition to the knowledge about the formations and the landscape the field trips also enables the student to get out of the classroom and explore the nature with their own senses instead of through a school book. The students' social skills also have a chance to develop as well as the use of working methods in science subjects.