Åland

kuv., 11 x 15 cm

Åland

kuv., 11 x 15 cm

Åland

kuv., 12 x 20 cm

Åland

kuv., 12 x 20 cm

Åland

kuv., 11 x 15 cm

Biodiversity and ecosystem functioning in angiosperm communities in the Baltic Sea

The biological variation in nature is called biodiversity. Anthropogenic pressures have led to a loss of biodiversity, alarming scientists as to what consequences declining diversity has for ecosystem functioning. The general consensus is that diversity (e.g. species richness or identity) affects functioning and provides services from which humans benefit. The aim of this thesis was to investigate how aquatic plant species richness and identity affect ecosystem functioning in terms of processes such as primary production, nutrient availability, epifaunal colonization and properties e.g. stability of Zostera marina subjected to shading. The main work was carried out in the field and ranged temporally from weeklong to 3.5 months-long experiments. The experimental plants used frequently co-occur in submerged meadows in the northern Baltic Sea and consist of eelgrass (Z. marina), perfoliate pondweed (Potamogeton perfoliatus), sago pondweed (P. pectinatus), slender-leaved pondweed (P. filiformis) and horned pondweed (Zannichellia palustris). The results showed that plant richness affected epifaunal community variables weakly, but had a strong positive effect on infaunal species number and functional diversity, while plant identity had strong effects on amphipods (Gammarus spp.), of which abundances were higher in plant assemblages consisting of P. perfoliatus. Depending on the starting standardizing unit, plant richness showed varying effects on primary production. In shoot density-standardized plots, plant richness increased the shoot densities of three out of four species and enhanced the plant biomass production. Both positive complementarity and selection effects were found to underpin the positive biodiversity effects. In shoot biomass-standardized plots, richness effects only affected biomass production of one species. Negative selection was prevalent, counteracting positive complementarity, which resulted in no significant biodiversity effect. The stability of Z. marina was affected by plant richness in such that Z. marina growing in polycultures lost proportionally less biomass than Z. marina in monocultures and thus had a higher resistance to shading. Monoculture plants in turn gained biomass faster, and thereby had a faster recovery than Z. marina growing in polycultures. These results indicate that positive interspecific interactions occurred during shading, while the faster recovery of monocultures suggests that the change from shading stress to recovery resulted in a shift from positive interactions to resource competition between species. The results derived from this thesis show that plant diversity affects ecosystem functioning and contribute to the growing knowledge of plant diversity being an important component of aquatic ecosystems. Diverse plant communities sustain higher primary productivity than comparable monocultures, affect faunal communities positively and enhance stability. Richness and identity effects vary, and identity has generally stronger effects on more variables than richness. However, species-rich communities are likely to contain several species with differing effects on functions, which renders species richness important for functioning. Mixed meadows add to coastal ecosystem functioning in the northern Baltic Sea and may provide with services essential for human well-being.

Lithostratigraphy and age of pre-Late Weichselian sediments in the Suupohja area, western Finland

Different types of laterally extensive sand- and gravel-dominated deposits, up to several tens of metres thick, were investigated in the Suupohja area of western Finland. The studied sediments were deposited in glacial, ice-marginal, glaciofluvial, sea or lake, littoral and terrestrial environments during several glacial-non-glacial cycles. Seventeen pre-Late Weichselian and three Late Weichselian/Holocene sedimentary units were identified. These were divided into ten formally and two informally defined formations that were together termed the Suupohja Group. Every unit are nevertheless not detectable throughout the study area. The informally defined “Karhukangas lower deposits” represent the lowest units in the Suupohja Group. The Karhukangas lower deposits with 5 till units, 3 glaciolacustrine/-marine units and 2 sand units, were interpreted as having been deposited during possibly four glacial-non-glacial cycles before the Late Pleistocene Subepoch (MIS 6 or earlier). The Kankalo Sand above the Karhukangas lower deposits comprises glaciofluvial and aeolian sands of Late Saalian, Eemian or Early Weichselian origin (MIS 6–MIS 5c). The Kariluoma Till above the Kankalo Sand was possibly deposited during the Late Saalian glacial advance, although an Early Weichselian origin is also possible. The Harrinkangas Formation, with glaciofluvial and quiet-water sediments, is interpreted as having been deposited during the Late Saalian and Eemian Stages (MIS 6–MIS 5e). The uppermost units in the deposits studied, the Kodesjärvi Formation (shore deposit), Isojoki Sand (aeolian), Rävåsen Formation (glaciofluvial), Vanhakylä Formation (shore line deposit), Dagsmark Till and Kauhajoki Till, were deposited during the Weichselian Stage (MIS 5d–MIS 2). In addition, Early Holocene (MIS 1) eskers without till cover were informally termed the “Holocene esker deposits”. The Lumikangas Formation represents gravelly shore deposits formed in the Holocene Epoch, when these areas last emerged from the sea. The first Weichselian ice expansion possibly reached the western part of Suupohja in the Early Weichselian Substage (MIS 5d?), but it did not expand further to the east. The second Weichselian glaciation of relatively short duration occupied the southern part of Finland in the later part of Middle Weichselian (MIS 3). Thus, the southern half of the country remained ice-free for the majority (~65–75%) of the Weichselian Stage. Instead, both humid temperate and periglacial conditions alternated. In the initial part of Middle Weichselian, this area was partly submerged, which indicates eastward expansion of the Scandinavian ice sheet(s), depressing the lithosphere. The exceptionally thick sediment cover, multiple lithofacies, relict landscape and preserved preglacially weathered bedrock are evidence of weak glacial erosion in the Suupohja area during the latest as well as earlier glaciations, making this area one of the key areas in Quaternary research.

Puristussylinterien valmistuksen kehittäminen

Tässä diplomityössä kehitettiin yksitoimisten puristussylinterien valmistusta Rautessa. Sylinterien valmistuksessa haastavin vaihe on sylinteriputken ja pohjan välinen hitsaus. Hitsauksen avuksi suunniteltiin sylinterin sisäpuolinen juuritukilaite. Hitsauskokeita suoritettiin hitsin pohjan jauhekaarihitsaukselle ja MAG-hitsaukselle. Juuritukilaitteen toimivuutta testattiin koehitsauksilla. Puristussylinterien materiaali on S355J2-terästä, jonka ainevahvuus on 20 – 60 mm. Paksujen rakenneterästen hitsauksessa täytyy ottaa huomioon hitsausliitoksen mekaanisten ominaisuuksien muuttuminen sekä eri halkeamien synty. Hitsauksen laatuun ja laadunhallintaan voidaan vaikuttaa monien eri tekijöiden avulla. Hitsausohjeen avulla, ja muut laatutekijät huomioiden, voidaan hitseille asetetut laatukriteerit täyttää. Juurituen käyttö nopeuttaa puristussylinterien hitsausta vähintään 50 %. Jauhekaarihitsaus kuparista juuritukea vasten synnyttää vaikeasti poistettavan kuonan juuren puolelle. Perinteinen MAG-hitsaus kuparista juuritukea vasten sisältää liian monta muuttujaa, mikä tekee siitä epäluotettavan pohjapalon hitsaukseen. Työssä suunnitellun juuritukilaitteen käyttö tuotannossa vaatii lisää hitsauskokeita.

Hitsaustuotannon kehittäminen tuulivoimalan tornin valmistuksessa

Tuulivoima on Euroopassa nopeimmin kasvava energian tuotantomuoto. Tuulivoimateollisuuden arvioidaan kasvavan Suomessa huomattavasti lähivuosien aikana ennakoidun syöttötariffipäätöksen myötä, jolloin kilpailu alalla tulee kasvamaan. Tavoitteena oli kehittää tuulivoimalan tornin valmistusta Levator Oy:ssä hitsaustuotantoa tehostamalla ja tuotannon ohjattavuutta parantamalla. Kehitystyöhön kuului toisen hitsauslinjan käyttöönoton suunnittelu ja ohjeiston laatiminen työnjohdolle. Toisen hitsauslinjan käyttöönoton suunnittelun tarkoituksena oli suunnitella muutokset nykyiseen tuotantoon uuden linjan käyttöönoton mahdollistamiseksi. Suunnittelu aloitettiin valitsemalla hitsausprosessit, jonka jälkeen suunniteltiin laitetarpeet työvaihe-analyysien pohjalta. Tuotantolayout muutettiin nykyisestä funktionaalisesta tuotannosta tuotantosoluista koostuvaksi tuotantolinjaksi, jolloin materiaalien virtautus parani huomattavasti. Tuotannon ohjaustavaksi valittiin kapeikko-ohjaus. Ohjeiston laatimisen tarkoituksena oli kerätä ja dokumentoida kaikki tuotannossa tarvittava tieto. Ohjeiston sisältää laadunohjaus, materiaalivirtojen ohjaus ja työnohjaus osiot, joiden tarkoituksena on helpottaa työnjohtamista. Ohjeisto määrittelee yhtenäiset tuotannon toimintatavat, jolloin tuotannon ohjattavuus helpottuu. Tavoitteet täyttyivät, kun toisen tuotantolinjan käyttöönoton vaatimat muutokset aloitettiin suunnitelmien mukaisesti syyskuussa 2009. Ohjeiston sisältö saatiin määriteltyä ja eri osioiden pilotit saatiin valmiiksi joulukuun aikana. Tuotannon ohjattavuus kehittyi huomattavasti ja samalla tuottavuus parani merkittävästi.

Lean Duplex -terästen hitsaus

Viime vuosien aikana tapahtunut nikkelin hinnan nouseminen on vaikuttanut austeniittis-ferriittisten ruostumattomien terästen, ns. duplex -terästen kehittämiseen. Niukkaseosteisemmissa lean duplex -teräksissä seostetun nikkelin määrää on vähennetty ja sitä on korvattu typellä ja mangaanilla. Nämä muutokset ko. terästen seostuksessa aiheuttavat haasteita hitsaukselle, erityisesti austeniitti-ferriitti -suhteen säilyttämisessä, sekä sitä kautta iskusitkeyden ja korroosio-ominaisuuksien säilyttämiselle. Suurempi typen osuus myös lisää teräksen hitsisulan viskositeettia, mikä heikentää juuripalkojen hitsauksessa tunkeumaa. Tässsä diplomityössä on tutkittu keinoja helpottaa paksujen (yli 20 mm) lean duplex -teräslevyjen hitsausta käytännön näkökulmasta, sekä parantaa hitsattujen levyjen iskusitkeyttä. Hitsauskokeilla löydettiin hitsausta helpottavia menetelmiä ja kokeista saatiin karsimalla valikoitua hitsausarvot, joilla pystytään hitsaamaan painelaitedirektiivin mukaisesti hyväksyttäviä hitsejä lean duplex -laatuihin LDX2101 ja UR2202.

Pukanluoman Natura 2000 -alueen hoito- ja käyttösuunnitelma

Pukanluoman Natura-alue (FI0200119) sijaitsee Satakunnassa Kankaanpään kaupungin alueella. Pikkujoki on osa Karvianjoen vesistöä, ja eräs maamme edustavimmista ja suurimmista lähdepuroista. Alue kuuluu Euroopan yhteisön Natura 2000 –suojeluverkostoon alueella esiintyvien luontotyyppien perusteella eli ns. SCI-alueena (Sites of Community Importance). Alueen suojeluarvot liittyvät pääosin jokielinympäristöjen luonnontilaisuuteen ja niiden edustavuuteen, vedenlaatuun ja alueella esiintyvään saukkoon ja taimeneen. Jokiosuus ja pienet, lähes luonnontilaiset luomat ovat tärkeitä kalojen lisääntymisalueita. Pukanluoman luontoarvojen säilyttämisen suurimpana haasteena on veden ekologista tilaa heikentävät tekijät; vesistörakentaminen, ojitukset, vesistökuormitus ja ranta-alueiden luonnontilaisuuden häviäminen sekä mahdollinen laaja pohjaveden otto Pohjankankaan pohjavesialueelta. Alue on paikallisille tärkeä virkistyspaikka. Osana Varsinais-Suomen elinkeino-, liikenne- ja ympäristökeskuksen (ELY-keskus) vastuualueen johtamaa ja Euroopan maatalouden kehittämisen maatalousrahaston tukemaa vesien ja luonnonhoidon alueellinen ja paikallinen toteuttaminen Lounais-Suomen vesistö- alueilla –hanketta (VELHO) alueelle laadittiin hoito- ja käyttösuunnitelma, jonka tavoitteena on ohjata alueen hoitoa ja käyttöä luontoarvojen turvaamiseksi. Suunnitelma tehtiin Varsinais-Suomen ELY:n ohjauksessa, ja suunnittelua varten perustettiin suunnitteluryhmä, joka koottiin eri viranomaistahojen ja käyttäjäryhmien edustajista sekä maanomistajista. Työryhmän tavoitteena oli tunnistaa alueen suojeluun ja käyttöön liittyvät mahdolliset ongelmat ja ristiriidat, ratkaista ja sovittaa niitä. Tämän hoito- ja käyttösuunnitelman aikajänne on 15 vuotta. Suunnitelman tavoitteena on ohjata alueen hoitoa ja käyttöä niin, että alueen luontoarvot turvataan.

Jauhekaari- ja tandem-MIG/MAG-hitsauksen vertailu

Tässä kanditaatintyössä vertaillaan jauhekaari- ja tandem-MIG/MAG-hitsausta kirjallisuustutkimuksena. Vertailun kohteena ovat hitsausprosessien tuottavuus ja kustannukset sekä hitsausprosesseilla saavutettava laatu. Lisäksi kandidaatintyössä esitetään hitsausprosesseille tyypilliset käyttökohteet CASE -esimerkkeinä.

Pasvik Water Quality until 2013 ; Environmental Monitoring Programme in the Norwegian, Finnish and Russian Border Area

The Pasvik monitoring programme was created in 2006 as a result of the trilateral cooperation and with the intention of following changes in the environment under variable pollution levels. Water quality is one of the basic elements of the programme when assessing the effects of the emissions from the Pechenganikel mining end metallurgical industry (Kola GMK). In this report temporal trends of the water chemistry during 2000–2013 are examined on the basis of the data gathered from lake Inari, River Pasvik and directly connected lakes, Lake Kuetsjarvi and 25 small lakes in three areas: Pechenganikel (Russia), Jarfjord (Norway) and Vätsäri (Finland). The lower parts of the Pasvik watercourse are impacted by both atmospheric pollution and direct wastewater discharge from the Pechenganikel smelter and the settlement of Nikel. The upper section of the watercourse and the small lakes and streams which are not directly linked to the Pasvik Watercourse only receive atmospheric pollution. Lake Inari is free of direct emissions from the Pechenganikel and the water quality is excellent. In River Pasvik and the directly connected lakes copper, nickel, and sulphates are the main pollutants. The most polluted water body is the Kolosjoki River as well as the stream connecting the Lakes Salmijarvi and Kuetsjarvi. The concentration of metals and sulphates in the water notably increases downstream the river lower Lake Kuetsjarvi. In Lake Kuetsjarvi copper and nickel concentrations are clearly elevated and have changed insignificantly in the last years of the research period. In the small border area lakes recovery from acidification in Vätsäri and Jarfjord is evident. Nickel and copper oncentrations have fluctuated but remained on clearly elevated level in Jarfjord and Pechenga. Copper concentrations have been slightly rising in the recent years. In Pechenga area nickel concentrations during the last four monitoring years are decreasing in some places but the regional trend through whole time series is still positive.

Spatial modeling techniques for mapping and characterization of acid sulfate soils

Acid sulfate (a.s.) soils constitute a major environmental issue. Severe ecological damage results from the considerable amounts of acidity and metals leached by these soils in the recipient watercourses. As even small hot spots may affect large areas of coastal waters, mapping represents a fundamental step in the management and mitigation of a.s. soil environmental risks (i.e. to target strategic areas). Traditional mapping in the field is time-consuming and therefore expensive. Additional more cost-effective techniques have, thus, to be developed in order to narrow down and define in detail the areas of interest. The primary aim of this thesis was to assess different spatial modeling techniques for a.s. soil mapping, and the characterization of soil properties relevant for a.s. soil environmental risk management, using all available data: soil and water samples, as well as datalayers (e.g. geological and geophysical). Different spatial modeling techniques were applied at catchment or regional scale. Two artificial neural networks were assessed on the Sirppujoki River catchment (c. 440 km2) located in southwestern Finland, while fuzzy logic was assessed on several areas along the Finnish coast. Quaternary geology, aerogeophysics and slope data (derived from a digital elevation model) were utilized as evidential datalayers. The methods also required the use of point datasets (i.e. soil profiles corresponding to known a.s. or non-a.s. soil occurrences) for training and/or validation within the modeling processes. Applying these methods, various maps were generated: probability maps for a.s. soil occurrence, as well as predictive maps for different soil properties (sulfur content, organic matter content and critical sulfide depth). The two assessed artificial neural networks (ANNs) demonstrated good classification abilities for a.s. soil probability mapping at catchment scale. Slightly better results were achieved using a Radial Basis Function (RBF) -based ANN than a Radial Basis Functional Link Net (RBFLN) method, narrowing down more accurately the most probable areas for a.s. soil occurrence and defining more properly the least probable areas. The RBF-based ANN also demonstrated promising results for the characterization of different soil properties in the most probable a.s. soil areas at catchment scale. Since a.s. soil areas constitute highly productive lands for agricultural purpose, the combination of a probability map with more specific soil property predictive maps offers a valuable toolset to more precisely target strategic areas for subsequent environmental risk management. Notably, the use of laser scanning (i.e. Light Detection And Ranging, LiDAR) data enabled a more precise definition of a.s. soil probability areas, as well as the soil property modeling classes for sulfur content and the critical sulfide depth. Given suitable training/validation points, ANNs can be trained to yield a more precise modeling of the occurrence of a.s. soils and their properties. By contrast, fuzzy logic represents a simple, fast and objective alternative to carry out preliminary surveys, at catchment or regional scale, in areas offering a limited amount of data. This method enables delimiting and prioritizing the most probable areas for a.s soil occurrence, which can be particularly useful in the field. Being easily transferable from area to area, fuzzy logic modeling can be carried out at regional scale. Mapping at this scale would be extremely time-consuming through manual assessment. The use of spatial modeling techniques enables the creation of valid and comparable maps, which represents an important development within the a.s. soil mapping process. The a.s. soil mapping was also assessed using water chemistry data for 24 different catchments along the Finnish coast (in all, covering c. 21,300 km2) which were mapped with different methods (i.e. conventional mapping, fuzzy logic and an artificial neural network). Two a.s. soil related indicators measured in the river water (sulfate content and sulfate/chloride ratio) were compared to the extent of the most probable areas for a.s. soils in the surveyed catchments. High sulfate contents and sulfate/chloride ratios measured in most of the rivers demonstrated the presence of a.s. soils in the corresponding catchments. The calculated extent of the most probable a.s. soil areas is supported by independent data on water chemistry, suggesting that the a.s. soil probability maps created with different methods are reliable and comparable.

Remote sensing for three-dimensional modelling of hydromorphology

Successful management of rivers requires an understanding of the fluvial processes that govern them. This, in turn cannot be achieved without a means of quantifying their geomorphology and hydrology and the spatio-temporal interactions between them, that is, their hydromorphology. For a long time, it has been laborious and time-consuming to measure river topography, especially in the submerged part of the channel. The measurement of the flow field has been challenging as well, and hence, such measurements have long been sparse in natural environments. Technological advancements in the field of remote sensing in the recent years have opened up new possibilities for capturing synoptic information on river environments. This thesis presents new developments in fluvial remote sensing of both topography and water flow. A set of close-range remote sensing methods is employed to eventually construct a high-resolution unified empirical hydromorphological model, that is, river channel and floodplain topography and three-dimensional areal flow field. Empirical as well as hydraulic theory-based optical remote sensing methods are tested and evaluated using normal colour aerial photographs and sonar calibration and reference measurements on a rocky-bed sub-Arctic river. The empirical optical bathymetry model is developed further by the introduction of a deep-water radiance parameter estimation algorithm that extends the field of application of the model to shallow streams. The effect of this parameter on the model is also assessed in a study of a sandy-bed sub-Arctic river using close-range high-resolution aerial photography, presenting one of the first examples of fluvial bathymetry modelling from unmanned aerial vehicles (UAV). Further close-range remote sensing methods are added to complete the topography integrating the river bed with the floodplain to create a seamless high-resolution topography. Boat- cart- and backpack-based mobile laser scanning (MLS) are used to measure the topography of the dry part of the channel at a high resolution and accuracy. Multitemporal MLS is evaluated along with UAV-based photogrammetry against terrestrial laser scanning reference data and merged with UAV-based bathymetry to create a two-year series of seamless digital terrain models. These allow the evaluation of the methodology for conducting high-resolution change analysis of the entire channel. The remote sensing based model of hydromorphology is completed by a new methodology for mapping the flow field in 3D. An acoustic Doppler current profiler (ADCP) is deployed on a remote-controlled boat with a survey-grade global navigation satellite system (GNSS) receiver, allowing the positioning of the areally sampled 3D flow vectors in 3D space as a point cloud and its interpolation into a 3D matrix allows a quantitative volumetric flow analysis. Multitemporal areal 3D flow field data show the evolution of the flow field during a snow-melt flood event. The combination of the underwater and dry topography with the flow field yields a compete model of river hydromorphology at the reach scale.