Bus bar aeolian vibration field tests

Large amplitude bus bar aeolian vibration may lead to post insulator damage. Different damping applications are used to decrease the risk of large amplitude aeolian vibration. In this paper the post insulator load caused by the bus bar aeolian vibration and the effect of damping methods are evaluated. The effects of three types of bus bar connectors and three types of primary structures are studied. Two actual damping devices, damping cable and their combinations are studied. The post insulator loads are studied with strain gage based custom made force sensors installed on the both ends of the post insulator and with the displacement sensor installed on the midpoint of the bus bar. The post insulator loads are calculated from the strain values and the damping properties are determined from the displacement history. The bus bar is deflected with a hanging weight. The weight is released and the bus bar is left to free damped vibration. Both actual bus bar vibration dampers RIBE and SBI were very effective against the aeolian vibration. Combining vibration damper with damping cable will increase the damping ratio but it may be unnecessary considering the extra effort. Bus bar connector type or primary structure have no effect on the vertical load. The bending moment at the post insulator with double sided bus bar connector is significantly higher than at the post insulator with single sided bus bar connector. No reliable conclusions about bus bar connector type effect can be done, but the roller bearing type or central bearing type connector may reduce the bending moment. The RHS steel frame as primary structure may increase the bending moment peak values since it is the least rigid primary structure type and it may start to vibrate as a response to the awakening force of the vibrating bus bar.

Automaattisen nukleiinihappoeristyslaitteen ja reaaliaikaisen PCR-menetelmän soveltuvuus herpes simplex -virusten keskushermostoinfektiodiagnostiikkaan

Keskushermosto- ja neonataali-infektiot ovat herpes simplex -virusten aiheuttamista taudeista vakavimpia. Niihin on olemassa lääkitys, joka on tehokkain, kun se aloitetaan aivan sairauden alkuvaiheessa. Näiden infektioiden diagnostiikassa PCR-menetelmä on herkin. Tämä menetelmä on kuitenkin työläs ja aikaa vievä, joten uudet nopeammat menetelmät ovat tervetulleita. Opinnäytetyö tehtiin HUSLABin virologian osastolle. Työssä testattiin QIAGENIN artus®HSV-1/2 LC PCR-reagenssipakkausta, joka on tehty käytettäväksi Roche diagnosticsin reaaliaikaisella PCR-laitteella LightCyclerillä. Lisäksi työssä testattiin automaattista bioMérieuxin NucliSens easyMAG- nukleiinihappoeristyslaitetta. Referenssinä käytettiin HUSLABin virologian osastolla testaushetkellä käytössä olevia menetelmiä. Reaaliaikaisen PCR-menetelmän herkkyyttä testattiin positiivisilla HSV-1 ja HSV-2 kontrollilaimennussarjoilla. Menetelmän oikeellisuutta testattiin määrittämällä laaduntarkkailu- ja potilasnäytteitä, jotka olivat likvoria. Tuloksia verrattiin QCMD:n antamiin ja perinteisellä ”in house”- PCR-menetelmällä saatuihin referenssituloksiin. Spesifisyyttä testattiin muiden ihmisten herpesvirusten positiivisilla kontrolleilla. Automaattisen nukleiinihappoeristysmenetelmän toimivuutta testattiin HSV-positiivisilla ja -negatiivisilla likvornäytteillä, jotka oli aikaisemmin eristetty fenoli-kloroformiuutolla. Tulokset QIAGENIN artus®HSV-1/2 LC PCR-reagenssipakkauksesta olivat hyviä. Kont-rollilaimennussarjan määrityksessä reaaliaikainen PCR-menetelmä osoittautui perinteistä ”in house”- PCR-menetelmää herkemmäksi. Potilasnäytteiden määrityksessä tulokset olivat yhtenevät. EasyMAG- nukleiinihappoeristysmenetelmällä eristettyjen potilasnäytteiden määrityksistä saadut tulokset olivat myös hyviä. Kun tuloksia verrattiin fenoli-kloroformiuutolla saatuihin tuloksiin, olivat tulokset yhtä näytettä lukuun ottamatta yhtenevät. Molemmat testattavat menetelmät ovat nopeita ja virhelähteiden mahdollisuus on vähäisempi kuin perinteisessä ”in house”-PCR menetelmässä ja fenoli-kloroformiuutolla nukleiinihappoa eristettäessä. Tutkimusten tulokset osoittivat molempien menetelmien soveltuvan hyvin HSV:n eristykseen ja määritykseen likvornäytteistä.

Twelve Etudes, Op. 25

Soitinnus: Piano.

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.

A Digital Repository for the Herbarium Collection of Brasília Botanical Garden

Presentation at Open Repositories 2014, Helsinki, Finland, June 9-13, 2014