Kumpulan tiedekirjaston matematiikan monografiat

Matematiikan lainattavien monografioiden kokoelma sisältää 12439 (18.8.2006) nidettä (n. xxx hyllymetriä). Kokoelma on luokiteltu AMS-luokituksen (American Mathematical Society) mukaisesti. AMS:lla ei ole käytössä omaa tesaurusta, mutta jonkin verran on käytetty kongressin kirjaston asiasanoja. Kopioinnissa tulleita asiasanoja ei ole poistettu, vaan ne ovat käytössä (esim. YSA). Samoin UDC-luokat on jäetty tietueisiin myös Helkassa. Monografiat ovat pääosin englannin-, saksan- ja ranskankielisiä. Kirjat ovat vapaasti käytettävissä ja lainattavissa. Laina-aika on 28 vuorokautta. Kokoelman kehittäjien tavoitteena on aina ollut korkeatasoinen matematiikan tieteellinen kokoelma, joka vastaa ainelaitoksen tutkijoiden, opettajien ja opiskelijoiden tarpeita. Laitoksen johto on pitänyt tärkeänä riittävää budjetointia hankinnan tarpeisiin. Hankintapäätökset on tehnyt tieteenalan asiantuntija, yleensä joku laitoksen professoreista. Käyttäjät ovat pääsääntöisesti olleet omalta ainelaitokselta. Noin 65% oli oman tiedekunnan henkilökuntaa ja HY:n muuta henkilökuntaa noin 8% sekä muiden korkeakoulujen henkilökuntaa 10%, muita tutkijoita 2%. Opiskelijoiden osuus jäi noin 15%:iin. (luvut vuodelta 2000). Kumpulassa opiskelijoiden tarvitseman kirjallisuuden osuus kasvanut opiskelijakirjaston matematiikan ja tilastotieteen aineiston siirryttyä kokoelmiin. Matematiikan kokoelma sisältää myös laajan matemaattisen tilastotieteen kokoelman.

Past, present and future - assessing changes in aquatic environments using subfossil diatoms

The deterioration of surface waters is one of the most important issues in the environmental management of the European Union. Thus, the EU Water Framework Directive 2000/60/EC (WFD) requires “good ecological and chemical status” of surface waters by 2015 allowing only a slight departure from ecological reference conditions characterized by the biological communities typical for the conditions of minimal anthropogenic impact. The WFD requires the determination of ecological reference conditions and the present ecological status of surface waters. To meet this legislative demand, sedimentary diatom assemblages were used in these studies with various methods 1) to assess natural and human activity induced environmental changes, 2) to characterize background conditions 3) to evaluate the present ecological status and 4) to predict the future of the water bodies in the light of palaeolimnological data. As the WFD refers to all surface waters, both coastal and inland sites were included. Two long and two short sediment cores from the Archipelago Sea in the northern Baltic Sea were examined for their siliceous microfossils in order to assess (1) the Holocene palaeoenvironmental history and (2) the recent eutrophication of the area. The diatom record was divided into local diatom assemblage zones (LDAZ, long cores) and diatom assemblage zones (DAZ, short cores). Locally weighted weighted averaging regression and calibration (LWWA) was applied for the quantitative reconstruction of past TN concentrations (short cores). An age model for the long cores was constructed by using independent palaeomagnetic and AMS-14C methods. The short cores were dated using radiometric (210Pb, 226Ra and 137Cs) methods. The long cores date back to the early history of the Archipelago Sea, which was freshwater – no salinity increase referable to the brackish phase of the Yoldia Sea is recognized. The nutrient status of the lacustrine phase was slightly higher in the Archipelago Sea than in the Baltic Proper. Initial brackish-water influence is observed at 8 150 ±80 cal. BP (LDAZ4), but fully brackish conditions were established at 7 700 ±80 cal. BP (LDAZ5). The diatom assemblages indicate increasing salinity, warming climate and possible eutrophic conditions during the lacustrine to brackish-water transition. The decreasing abundance of Pseudosolenia calcar-avis (Schultze) Sundström and the increasing abundance of the ice-cover indicator species Pauliella taeniata (Grunow) Round and Basson indicate decreasing salinity and climatic cooling after ca. 5 000 cal. BP. Signs of eutrophication are visible in the most recent diatom assemblage zones of both short cores. Diatom-inferred total nitrogen (DI-TN) reconstructions partially fail to trace the actual measured total nitrogen concentrations especially from the late 1980s to the mid 1990s. This is most likely due to the dominating diatom species Pauliella taeniata, Thalassiosira levanderi Van Goor and Fragilariopsis cylindrus (Grunow) W. Krieger being more influenced by factors such as the length of the ice-season rather than nutrient concentrations. It is concluded that the diatom assemblages of the study sites are principally governed by climate fluctuations, with a slight influence of eutrophication visible in the most recent sediments. There are indications that global warming, with reduced ice cover, could impact the spring blooming diatom species composition in the Archipelago Sea. In addition, increased sediment accumulation in the early 90s coincides with the short ice-seasons suggesting that warming climate with decreasing ice-cover may increase sedimentation in the study area. The diverse diatom assemblages dominated by benthic species (54 %) in DAZ1 in the Käldö Fjärd core can be taken as background diatom assemblages for the Archipelago Sea. Since then turbidity has increased and the diatom assemblages have been dominated by planktonic diatoms from around the mid 1800s onwards. The reconstructed reference conditions for the total nitrogen concentrations fluctuate around 400 μg l-1. Altogether two short sediment cores and eight short cores for top-bottom analysis were retrieved from Lake Orijärvi and Lake Määrjärvi to assess the impact of the acid mine drainage (AMD) derived metals from the Orijärvi mine tailings on the diatom communities of the lakes. The Cu (Pb, Zn) mine of Orijärvi (1757 – 1956) was the first one in Finland where flotation techniques (1911 – 1955) were used to enrich ore and large quantities of tailings were produced. The AMD derived metal impact to the lakes was found to be among the heaviest thus far recorded in Finland. Concentrations of Cu, Pb and Zn in Lake Orijärvi sediments are two to three orders of magnitude higher than background values. The metal inputs have affected Lake Orijärvi and Lake Määrjärvi diatom communities at the community levels through shifts in dominant taxa (both lakes) and at the individual level through alteration in frustule morphology (Lake Orijärvi). At present, lake water still has elevated heavy metal levels, indicating that the impact from the tailings area continues to affect both lakes. Lake Orijärvi diatom assemblages are completely dominated by benthic species and are lacking planktonic diatoms. In Lake Määrjärvi the proportion of benthic and tychoplanktonic diatoms has increased and the planktonic taxa have decreased in abundance. Achnanthidium minutissimum Kützing and Brachysira vitrea (Grun.) R. Ross in Hartley were the most tolerant species to increased metal concentrations. Planktonic diatoms are more sensitive to metal contamination than benthic taxa, especially species in the genus Cyclotella (Kützing) Brébisson. The ecological reference conditions assessed in this study for Lake Orijärvi and Lake Määrjärvi comprise diverse planktonic and benthic communitites typical of circumneutral oligotrophic lakes, where the planktonic diatoms belonging to genera Cyclotella , Aulacoseira Thwaites, Tabellaria Ehrenberg and Asterionella Hassall dominate in relative abundances up to ca. 70%. The benthic communities are more diverse than the planktonic consisting of diatoms belonging to the genera Achnanthes Bory, Fragilaria Lyngbye and Navicula St. Vincent. This study clearly demonstrates that palaeolimnological methods, especially diatom analysis, provide a powerful tool for the EU Water Frame Work Directive for defining reference conditions, natural variability and current status of surface waters. The top/bottom approach is a very useful tool in larger-scale studies needed for management purposes. This “before and after” type of sediment sampling method can provide a very time and cost effective assessment of ecological reference conditions of surface waters.

Osaamisen siirtäminen prosessikuvauksen avulla. Case: tehtäväpohjainen arkistonmuodostussuunnitelma

The aim of this master’s thesis was to study can an organization use process descriptions for transferring knowledge from an employee to another. The case-organization was South Carelia Joint Authorisation for Education. The data used in the experiment was the case-organization’s archives formation plan including process descriptions (tehtäväpohjainen AMS). A new empirical investigation environment was formed. Four people, who could be recruited for working in the department of salary calculation, were asked to write an instruction for themselves following the AMS so they could complete the necessary tasks concerning salary calculation and processing the originated documents without any other help but the written instruction. After that they were asked to estimate, would the instruction be enough or would they need someone’s help to do the work. The instructions were also evaluated by a professional and the writer of this thesis. After evaluating the written instructions there was evidence that some knowledge – what should be done and in which order – has been transferred from the process descriptions to the written instructions. Anyway the complete task could not be correctly performed without any other help, because the knowledge on how it should be done did not transfer.

Structure-related magnetic fabric studies : implications for deformed and undeformed Precambrian rocks

The aim of this thesis research was to gain a better understanding of the emplacement of rapakivi granite intrusions, as well as the emplacement of gold-bearing hydrothermal fluids in structurally controlled mineralizations. Based on investigations of the magnetic fabric, the internal structures could be analysed and the intrusion mechanisms for rapakivi granite intrusions and respectively different deformation stages within gold-bearing shear and fault zones identified. Aeromagnetic images revealed circular structures within the rapakivi granite batholiths of Wiborg, Vehmaa and Åland. These circular structures represent intrusions that eventually build up these large batholiths. The rapakivi granite intrusions of Vehmaa, Ruotsinpyhtää within the Wiborg batholith and Saltvik intrusions within the Åland batholith all show bimodal magnetic susceptibilities with paramagnetic and ferromagnetic components. The distribution of the bimodality is related to different magma batches of the studied intrusions. The anisotropy of magnetic susceptibility (AMS) reveals internal structures that cannot be studied macroscopically or by microscope. The Ruotsinpyhtää and Vehmaa intrusions represent similar intrusion geometries, with gently to moderately outward dipping magnetic foliations. In the case of Vehmaa, the magnetic lineations are gently plunging and trend in the directions of the slightly elongated intrusion. The magnetic lineations represent magma flow. The shapes of the AMS ellipsoids are also more planar (oblate) in the central part of the intrusion, whereas they become more linear (prolate) near the margin. These AMS results, together with field observations, indicate that the main intrusion mechanism has involved the subsidence of older blocks with successive intrusion of fractionated magma during repeated cauldron subsidence. The Saltvik area within the Åland batholith consists of a number of smaller elliptical intrusions of different rapakivi types forming a multiple intrusive complex. The magnetic fabric shows a general westward dipping of the pyterlite and eastward dipping of the contiguous even-grained rapakivi granite, which indicates a central inflow of magma batches towards the east and west resulting from a laccolitic emplacement of magma batches, while the main mechanism for space creation was derived from subsidence. The magnetic fabric of structurally controlled gold potential shear and fault zones in Jokisivu, Satulinmäki and Koijärvi was investigated in order to describe the internal structures and define the deformation history and emplacement of hydrothermal fluids. A further aim of the research was to combine AMS studies with palaeomagnetic methods to constrain the timing for the shearing event relative to the precipitation of ferromagnetic minerals and gold. All of the studied formations are dominated by monoclinic pyrrhotite. The AMS directions generally follow the tectonic structures within the formations. However, internal variations in the AMS direction as well as the shapes of the AMS ellipsoids are observed within the shear zones. In Jokisivu and Satulinmäki in particular, the magnetic signatures of the shear zone core differ from the margins. Furthermore, the shape of the magnetic fabric in the shear zone core of Jokisivu is dominated by oblate shapes, whereas the margins exhibit prolate shapes. These variations indicate a later effect of the hydrothermal fluids on the general shear event. The palaeo-magnetic results reveal a deflection from the original Svecofennian age geomagnetic direction. These results, coupled with correlations between the orientation of the NRM vectors and the magnetic and rock fabrics, imply that the gold-rich hydrothermal fluids were emplaced pre/syntectonically during the late stages of the Svecofennian orogeny.

Metalli-ionin ja hapon erotus toisistaan kalvosuodatuksella

Työn tarkoituksena oli kuparin ja hapon erottaminen toisistaan malliaineliuoksesta membraanitekniikalla. Kaivannaisteollisuudessa happoja käytetään metalleiden liuottamiseen. Lisäksi happamia jätevesiä syntyy sulfidikaivoksissa, sadeveden liuottaessa metalleja. Raskasmetallit ovat erittäin myrkyllistä vesieliöille. Työn tavoitteena oli saada happo ja metalli hyödynnettävään muotoon. Työn kokeellisessa osassa vertailtiin kahta polymeeristä ja keraamista membraania hapon ja metallin erotuksessa. Mittauksissa käytetyt membraanit olivat: AMS Technologies A-3012 ja A-3014 sekä Inopor ® Type SKR. Syöttöliuos sisälsi kuparisulfaattia ja rikkihappoa. Suodatukset tehtiin 30 ºC lämpötilassa useissa paineissa ja pH-arvoissa. Polymeeristen membraanien suodatusnäytteistä saadut retentiot kuparille olivat vastaavia aikaisempien tutkimusten tuloksien kanssa. A-3012 kalvon kuparin retentio oli 95 % ja A-3014 kalvolle kuparin retentio oli 90 %. Lisäksi mittausten korkeimmissa pH-arvoissa (2,9-2,3) happo konsentroitui permeaattiin. Polymeerisillä membraaneilla ei ollut merkkejä kalvon likaantumisesta tai hajoamisesta. Keraamisella membraanilla mitatut tulokset eivät olleet vastaavia aikaisempien tutkimusten tuloksien kanssa. Kuparin retentio olivat 2 ja 20 prosentin välillä, eikä liuoksen pH eronnut syötön ja permeaatin välillä. Tulosten perusteella molemmat tutkitut polymeeriset membraanit soveltuvat kuparin erottamiseen happamasta liuoksesta. Mittauksissa käytetty keraaminen membraani ei sovellu tähän tehtävään.