53 resultados para magneettiset mittaukset


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Pystynävertäjä on Suomessa yksi merkittävimpiä mäntyjen tuhohyönteisiä. Se syö männynversoja ontoiksi, minkä seurauksena nämä tippuvat maahan. Tästä aiheutuu puulle kasvutappioita ja metsänomistajalle tulonmenetyksiä. Pystynävertäjän ekologiaa on tutkittu paljon, mutta ei tiedetä, miten se vaikuttaa versojen fotosynteesiin ja haihtuvien orgaanisten yhdisteiden eli VOC-yhdisteiden emissioihin ennen versojen putoamista. Monissa muissa tutkimuksissa on havaittu herbivoreilla olevan vaikutusta isäntäkasviensa fotosynteesiin. Lisäksi herbivorian seurauksena isäntäkasvin VOC-emissiot ovat voineet muuttua laadultaan tai määrältään. Pystynävertäjän vaikutuksia versoihin tutkittiin kokeellisesti SMEAR II -asemalla Pirkanmaalla. Pystynävertäjän vaurioittamien ja kontrolliversojen fotosynteesiä mittattiin kahden männyn latvuksessa heinä–syyskuussa 2010. Mittaukset tehtiin kannettavalla fotosynteesimittauslaitteistolla. Samalla otettiin VOC-näytteitä neulasten emissioista adsorbenttiputkiin. Lisäksi toisesta koepuusta suljettiin pystynävertäjäja kontrolliverso raamikyvettiin, johon mahtui oksan kärkeä n. 20 cm. Raamikyvetin läpi kierrätetystä ilmasta kerättiin VOC-näytteitä SPME-kuituun ja siihen sitoutuneet yhdisteet analysoitiin enantiomeereittain. Pystynävertäjä- ja kontrolliversojen välillä ei ollut selvää eroa hiilen assimilaatiossa, transpiraatiossa, ilmarakokonduktanssissa, vedenkäytön tehokkuudessa tai fotokemiallisessa saannossa. Vain pahimmin vaurioituneissa versoissa vaurio vaikutti fotosynteesiin huomattavasti. Esimerkiksi fotokemiallinen saanto laski selvästi vasta, kun verso oli juuri katkeamaisillaan pystynävertäjän sisäänmenoreiän kohdalta. Neulaskyvettimittausten perusteella vaikuttaa siltä, että pystynävertäjä toisella koepuulla lisää monoterpeeniemissioita ja toisella vähentää niitä. Raamikyvettimittauksessa pystynävertäjä lisäsi (+)-enantiomeerin osuutta ?- ja ?-pineeni- sekä limoneeniemissioista, mutta emissioiden kokonaismäärä ei juuri eronnut kontrolliversosta. Pystynävertäjän vaikutukset versojen fotosynteesiin jäivät vähäisiksi, vaikka pystynävertäjä olikin tehnyt versoihin yhdestä neljään reikää ja niiden kohdalta poistanut suuren osan verson poikkileikkauspinta-alasta. Pystynävertäjän aiheuttamat kasvutappiot vaikuttavatkin olevan seurausta lähes yksinomaan versojen putoamisesta. Pystynävertäjä ei juuri vaikuttanut versosta haihtuvien yhdisteiden kokonaismäärään, mutta se muutti niiden keskinäisiä runsaussuhteita ja erityisesti enantiomeerien runsaussuhteita. Pystynävertäjien vaikutukset VOC-emissioihin näyttävät riippuvan suuresti kemotyypistä. Laajempien johtopäätösten tekeminen pystynävertäjän vaikutuksista männyn VOC-emissioihin vaatisi tutkimuksen toistamista suuremmalla koepuumäärällä.

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In order to evaluate the influence of ambient aerosol particles on cloud formation, climate and human health, detailed information about the concentration and composition of ambient aerosol particles is needed. The dura-tion of aerosol formation, growth and removal processes in the atmosphere range from minutes to hours, which highlights the need for high-time-resolution data in order to understand the underlying processes. This thesis focuses on characterization of ambient levels, size distributions and sources of water-soluble organic carbon (WSOC) in ambient aerosols. The results show that in the location of this study typically 50-60 % of organic carbon in fine particles is water-soluble. The amount of WSOC was observed to increase as aerosols age, likely due to further oxidation of organic compounds. In the boreal region the main sources of WSOC were biomass burning during the winter and secondary aerosol formation during the summer. WSOC was mainly attributed to a fine particle mode between 0.1 - 1 μm, although different size distributions were measured for different sources. The WSOC concentrations and size distributions had a clear seasonal variation. Another main focus of this thesis was to test and further develop the high-time-resolution methods for chemical characterization of ambient aerosol particles. The concentrations of the main chemical components (ions, OC, EC) of ambient aerosol particles were measured online during a year-long intensive measurement campaign conducted on the SMEAR III station in Southern Finland. The results were compared to the results of traditional filter collections in order to study sampling artifacts and limitations related to each method. To achieve better a time resolution for the WSOC and ion measurements, a particle-into-liquid sampler (PILS) was coupled with a total organic carbon analyzer (TOC) and two ion chromatographs (IC). The PILS-TOC-IC provided important data about diurnal variations and short-time plumes, which cannot be resolved from the filter samples. In summary, the measurements made for this thesis provide new information on the concentrations, size distribu-tions and sources of WSOC in ambient aerosol particles in the boreal region. The analytical and collection me-thods needed for the online characterization of aerosol chemical composition were further developed in order to provide more reliable high-time-resolution measurements.

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Objectives. This study concentrated on the aspect of physical safety in the learning environment of primary and secondary schools in Helsinki. Taking a broad perspective, the study analysed the safety culture of Helsinki schools, ranked them with a point rating system, and thoroughly investigated reasons behind their differences. Safety culture in educa-tional institutions has not been studied previously although research related to safety culture in business is abundant and some studies have considered safety culture in the healthcare sector. The study focused on the attitudes and practices of teachers concerning safety. The main research question is as follows: "What factors related to safety culture distinguish schools with an exceptional safety culture from those weaker one?" Research methods. The study used a mixed-methods approach. It s quantitative part charted the safety attitudes, values and expertise of employees in selected schools. The study also analysed physical safety in selected schools through specific safety inspections. The 14 schools in the study were selected randomly, two from each district. Altogether 388 of 475 employees returned a Webropol questionnaire (N= 475, 81,68 %). The qualitative part of the study analysed the reasons behind perceived differences in school s safety cul-ture using theme interviews with school principals. Elements of a phenomenographic research approach were also used. Results and conclusions. According to the study the distinctive features of good safety cultures in the Helsinki schools included a well-developed understanding of safety hazards and the requirements of basic safety, good safety management practices, a developed understanding of the systematic nature of safety, an appreciation of safety evidenced through everyday practices and open and communal safety-related work. The study offers result-based safety culture improvements for teachers, those responsible for school safety, principals, educational administrators, teacher educators and authorities.

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The Baltic Sea is one of the largest brackish water bodies in the world. Primary production in the Baltic Sea is limited by nitrogen (N) availability with the exception of river outlets and the northernmost phosphorus limited basin. The excess human induced N load from the drainage basin has caused severe eutrophication of the sea. The excess N loads can be mitigated by microbe mediated natural N removal processes that are found in the oxic-anoxic interfaces in sediments and water column redoxclines. Such interfaces allow the close coupling between the oxic nitrification process, and anoxic denitrification and anaerobic ammonium oxidation (anammox) processes that lead to the formation of molecular nitrogen gas. These processes are governed by various environmental parameters. The effects of these parameters on N processes were investigated in the northern Baltic Sea sediments. During summer months when the sediment organic content is at its highest, nitrification and denitrification reach their maximum rates. However, nitrification had no excess potential, which was probably because of high competition for molecular oxygen (O2) between heterotrophic and nitrification microbes. Subsequently, the limited nitrate (NO3-) availability inhibited denitrification. In fall, winter and spring, nitrification was limited by ammonium availability and denitrification limited by the availability of organic carbon and occasionally by NO3-. Anaerobic ammonium oxidation (anammox) was not an important N removal process in the northern Baltic Sea. Modeling studies suggest that when hypoxia expands in the Baltic Sea, N removal intensifies. However, the results of this study suggest the opposite because bottom water hypoxia (O2< 2 ml l-1) decreased the denitrification rates in sediments. Moreover, N was recycled by the dissimilatory nitrate reduction to ammonium (DNRA) process instead of being removed from the water ecosystem. High N removal potentials were found in the anoxic water column in the deep basins of the Baltic Proper. However, the N removal in the water column appeared to be limited by low substrate availability, because the water at the depths at which the substrate producing nitrification process occurred, rarely mix with the water at the depths at which N removal processes were found. Overall, the natural N removal capacity of the northern Baltic Sea decreased compared to values measured in mid 1990s and early 2000. The reason for this appears to be increasing hypoxia.

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The urban heat island phenomenon is the most well-known all-year-round urban climate phenomenon. It occurs in summer during the daytime due to the short-wave radiation from the sun and in wintertime, through anthropogenic heat production. In summertime, the properties of the fabric of city buildings determine how much energy is stored, conducted and transmitted through the material. During night-time, when there is no incoming short-wave radiation, all fabrics of the city release the energy in form of heat back to the urban atmosphere. In wintertime anthropogenic heating of buildings and traffic deliver energy into the urban atmosphere. The initial focus of Helsinki urban heat island was on the description of the intensity of the urban heat island (Fogelberg 1973, Alestalo 1975). In this project our goal was to carry out as many measurements as possible over a large area of Helsinki to give a long term estimate of the Helsinki urban heat island. Helsinki is a city with 550 000 inhabitants and located on the north shore of Finnish Bay of the Baltic Sea. Initially, comparison studies against long-term weather station records showed that our regular, but weekly, sampling of observations adequately describe the Helsinki urban heat island. The project covered an entire seasonal cycle over the 12 months from July 2009 to June 2010. The measurements were conducted using a moving platform following microclimatological traditions. Tuesday was selected as the measuring day because it was the only weekday during the one year time span without any public holidays. Once a week, two set of measurements, in total 104, were conducted in the heterogeneous temperature conditions of Helsinki city centre. In the more homogeneous suburban areas, one set of measurements was taken every second week, to give a total of 52.The first set of measurements took place before noon, and the second 12 hours, just prior to midnight. Helsinki Kaisaniemi weather station was chosen as the reference station. This weather station is located in a large park in the city centre of Helsinki. Along the measurement route, 336 fixed points were established, and the monthly air temperature differences to Kaisaniemi were calculated to produce monthly and annual maps. The monthly air temperature differences were interpolated 21.1 km by 18.1 km horizontal grid with 100 metre resolution residual kriging method. The following independent variables for the kriging interpolation method were used: topographical height, portion of sea area, portion of trees, fraction of built-up and not built-up area, volumes of buildings, and population density. The annual mean air temperature difference gives the best representation of the Helsinki urban heat island effect- Due to natural variability of weather conditions during the measurement campaign care must be taken when interpretation the results for the monthly values. The main results of this urban heat island research project are: a) The city centre of Helsinki is warmer than its surroundings, both on a monthly main basis, and for the annual mean, however, there are only a few grid points, 46 out of 38 191, which display a temperature difference of more than 1K. b) If the monthly spatial variation is air temperature differences is small, then usually the temperature difference between the city and the surroundings is also small. c) Isolated large buildings and suburban centres create their own individual heat island. d) The topographical influence on air temperature can generally be neglected for the monthly mean, but can be strong under certain weather conditions.

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In this work, a colossal magnetoresistive (CMR) Pr1−xCaxMnO3 (PCMO) man- ganite thin films and polycrystalline samples were studied with the main focus on the properties of the insulator to metal Mott phase transition. The polycrystalline PCMO samples were fabricated with the solid state reaction method. The polycrystalline sam- ples were further processed into the epitaxial thin films with the pulsed laser deposition method (PLD). The structural and magnetic properties of the samples were systemat- ically investigated and the thin films samples were further investigated with magneto- transport measurement where the thin films response to illumination was also studied. After the successful synthesis of polycrystalline PCMO samples with varying x = between 0.0 - 0.5, the magnetic characterization of the samples showed rich magnetic properties having the signatures of the magnetic phase coexistence of antiferromag- netic (AFM) and ferromagnetic (FM) ordering and cluster glass behaviour. With the increased doping concentration from x = 0.3 to 0.5, the AFM charge-order (CO) phase started to form up being strongest on the sample x = 0.5. This AFM CO phase could be melted with the high external magnetic field at temperatures below Neel’s tempera- ture TN inducing an irreversible first order metamagnetic AFM to FM phase transition. The strength of the AFM CO phase decreased with decreasing Ca concentration and increasing temperature. The polycrystalline PCMO samples with Ca concentrations of 0.3 - 0.5, showing metamagnetic behaviour, were selected for the fabrication of the thin film samples. The films were grown using two different in situ oxygen treatment temperatures at 500 ◦C and 700 ◦C in the PLD system. The films with x = 0.4 and 0.5 showed weaker AFM CO phase with greatly reduced melting fields when compared to polycrystalline samples. Also, the robustness of the AFM CO phase was further decreased in thin films with the lower oxygen treatment temperature of 500 ◦C. The magneto-transport measurements made on the thin films showed that the melting of AFM CO phase was connected to CMR effect where the increasing magnetic field induced an insulator to metal phase transition, which reduces the resistivity of the film around nine orders of magnitude. The use of illumination during the magneto-transport measurements showed a vari- ety of intriguing phenomena including magnetophotoresistance. The illumination had a huge effect to the insulator to metal transition (IMT) reducing the transition magnetic field significantly. Moreover, by magnetically biasing the thin films with the constant external magnetic field, the IMT could be induced by switching on the illumination.

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Yhtymän viestijärjestelmä YVI2 on kenttäviestijärjestelmä, jolla luodaan prikaatin sotatoimessa tarvittavat kenttäviestiyhteydet. Järjestelmällä luodaan viestipalvelut koko yhtymän tulenkäytön, tiedustelun ja johtamisen viestiyhteystarpeisiin. Järjestelmän toimivuus on sotatoimen onnistuneen suorittamisen kannalta erittäin tärkeätä. Tutkimusympäristönä on YVI2- järjestelmä, johon tutkimuksessa on määritelty järjestelmäkomponenttien ja keskeisten palveluiden testien ja mittausten raja-arvot. Järjestelmätestauksella kyetään paikallistamaan viestijärjestelmässä mahdollisesti olevat virheet. Lisäksi järjestelmätestaus tuottaa tietoja, joiden perusteella voidaan määrittää viestiverkon suorituskyky sekä analysoida sitä. Järjestelmätestaus käsittää testauksen suunnittelun, mittaukset ja testit, tietojen koostamisen, tietojen analysoinnin ja testiraportin laatimisen. Testiraportti on yhtenä seuraavan vaiheen tai testauskierroksen suunnittelua. Järjestelmätestauksen tuloksia voidaan analysoida sekä järjestelmän suorituskyvyn että luotettavuuden ja kattavuuden perusteella. Näihin molempiin tutkimuksessa esitetään joitain malleja ja ajatuksia. Järjestelmätestaus soveltuu monipuolisesti viestitoiminnan suunnittelun ja johtamisen tueksi.

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Stress is a phenomenon that on some level affects everyone’s lives on a daily basis. The autonomic nervous system controls the varying levels of stress at any given time. The responses of the autonomic nervous system adjust the body to cope with changing external and internal conditions. During high-stress situations the body is forced into a state of heightened alertness, which passes when the stressor is removed. The stressor can be any external or internal event that causes the body to respond. Stress is a very versatile phenomenon that can be both a cause and an indicator of other medical conditions, for example cardiovascular disease. Stress detection can therefore be helpful in identifying these conditions and monitoring the overall emotional state of a person. Electrodermal activity (EDA) is one of the most easily implemented ways to monitor the activity of the autonomic nervous system. EDA describes changes occurring in the various electrical properties of the skin, including skin conductivity and resistance. Increased emotional sweating has been proven to be one possible indication of stress. On the surface of the skin, increased sweating translates to increased skin conductivity, which can be observed through EDA measurements. This makes electrodermal activity a very useful tool in a wide range of applications where it is desirable to observe changes in a person’s stress level. EDA can be recorded by using specialized body sensors placed on specific locations on the body. Most commonly used recording sites are the palms of the hands due to the high sweat gland density on those areas. Measurement is done using at least two electrodes attached to the skin, and recording the electrical conductance between them. This thesis implements a prototype of a wireless EDA measurement system. The feasibility of the prototype is also verified with a small group of test subjects. EDA was recorded from the subjects while they were playing a game of Tetris. The goal was to observe variations in the measured EDA that would indicate changes in the subjects’ stress levels during the game. The analysis of the obtained measurement results confirmed the connection between stress and recorded EDA. During the game, random occurrences of lowered skin resistance were clearly observable, which indicates points in the game where the player felt more anxious. A wireless measurement system has the potential of offering more flexible and comfortable long-term measuring of EDA, and could be utilized in a wide range of applications.