A Widely Used Machine Translation Service and its Migration to a Free/Open-Source Solution : the Case of Softcatalà

Softcatalà is a non-profit associationcreated more than 10 years ago to fightthe marginalisation of the Catalan languagein information and communicationtechnologies. It has led the localisationof many applications and thecreation of a website which allows itsusers to translate texts between Spanishand Catalan using an external closed-sourcetranslation engine. Recently,the closed-source translation back-endhas been replaced by a free/open-sourcesolution completely managed by Softcatalà: the Apertium machine translationplatform and the ScaleMT web serviceframework. Thanks to the opennessof the new solution, it is possibleto take advantage of the huge amount ofusers of the Softcatalà translation serviceto improve it, using a series ofmethods presented in this paper. In addition,a study of the translations requestedby the users has been carriedout, and it shows that the translationback-end change has not affected theusage patterns.

Growth and demise of Permian biogenic chert along northwest Pangea: evidence for end-Permian collapse of thermohaline circulation

The Permian Chert Event (PCE) was a 30 Ma long episode of unusual chert accumulation along the northwest margin of Pangea, and possibly worldwide. The onset of the PCE occurred at about the Sakmarian-Artinskian boundary in the Sverdrup Basin, Canadian Arctic, where it coincides with a maximum flooding event, the ending of high-frequency/high-amplitude shelf cyclicity, the onset of massive biogenic chert deposition in deep-water distal areas, and a long-term shift from warm- to cool-water carbonate sedimentation in shallow-water proximal areas. A similar and coeval shift is observed from the Barents Sea to the northwestern USA. A landward and southward expansion of silica factories occurred during the Middle and Late Permian at which time warm-water carbonate producers disappeared completely from the northwest margin of Pangea. Biotically impoverished and increasingly narrow cold-water carbonate factories (characterised by non-cemented bioclasts of sponges, bryozoans, echinoderms and brachiopods) were then progressively replaced by silica factories. By Late Permian time, little carbonate sediments accumulated in the Barents Sea and in the Sverdrup Basin. where the deep- to shallow-water sedimentary spectrum was occupied by siliceous sponge spicules. By that time, biogenic silica sedimentation was common throughout the world. Silica factories collapsed in the Late Permian, abruptly bringing the PCE to an end. In northwest Pangea, the end- Permian collapse of the PCE was associated with a major transgression and with a return to much warmer oceanic and continental climatic conditions. Chert deposition resumed in the distal oceanic areas during the early Middle Triassic (Anisian) after a 8-10 Ma interruption (Early Triassic Chert Gap). The conditions necessary for the onset, expansion and zenith of the PCE were provided by the thermohaline circulation of nutrient-rich cold waters along the northwestern and western margin of Pangea, and possibly throughout the world oceans. These conditions provided an efficient transportation mechanism that constantly replenished the supply of silica in the area, created a nutrient- and oxygen-rich environment favouring siliceous biogenic productivity. established cold sea-floor conditions, hindering silica dissolution, while increasing calcium carbonate solubility, and provided conditions adverse to organic and inorganic carbonate production, The northwest margin of Pangea was, for nearly 30 Ma. bathed by cold waters presumably derived from the seasonal melting of northern sea ice, the assumed engine for thermohaline circulation. This process started near the Sakmarian-Artinskian boundary. intensified throughout Middle and Late Permian time and ceased suddenly in latest Permian time, It led to oceanic conditions much colder than normally expected from the palaeolatitudes. and the influence of cold northerly-derived water was felt as far south southern Nevada. The demise of silica factories was caused by the rapid breakdown of these conditions and the establishment of a much warmer marine environment accompanied by sluggish circulation and perhaps a reduced input of dissolved silica to the ocean. Complete thawing of northern sea ice would have ended thermohaline circulation and led to warm and sluggish oceanic conditions inimical to the production. accumulation and preservation of biogenic silica.

Polttomoottorin sähkömekaaninen venttiilinohjaus

Työssä tarkastellaanpolttomoottorin venttiilitoimilaitteen toteuttamista sähkömekaanisesti. Tähän mennessä kehitetyt ratkaisut ja rakennetut prototyypit soveltuvat pääosin henkilöautojen vapaasti hengittävien ottomoottoreiden venttiilien ohjaukseen. Venttiilien sähkömekaanisen ohjauksen soveltuvuutta suuriin polttomoottoreihin kuten esimerkiksi voimalaitosdieseleihin on myös tarkasteltu, mutta ongelmaksi muodostuu riittävän suuren magneettisen voiman kehittäminen magneettivuon reitillä esiintyvän suuren ilmavälin takia. Työssä esitetään valmiita ja kehitteillä olevia ratkaisuja polttomoottorin venttiilien ohjaukseen sähkömekaanisesti. Lisäksi käsitellään parannusmahdollisuuksia jo valmiisiin ratkaisuihin ja käydään läpi sähkömekaanisen venttiilinohjauksen ongelmakohtia. Suomeksi ei ole kovin paljon julkaistua materiaalia polttomoottorin venttiilien sähkömekaanisesta ohjauksesta, joten työ tukeutuu pääosin Internetissä julkaistuihin artikkeleihin sekä sähköpostin välityksellä käytyihin keskusteluihin niiden tahojen kanssa, jotka tutkivat ja kehittävät polttomoottorinsähkömekaanista venttiilien ohjausta. Venttiilien sähkömekaanisen ohjauksen tutkiminen tällä hetkellä jakautuu pääpainotteisesti sähkömagneettisen osuuden ja säätöteknisen osuuden tutkimiseen ja kehittämiseen. Työssä ei mennä näiden aihepiirien syvälliseen analysointiin vaan esitetään tämän hetkisentutkimuksen painopisteet ja lähdeviitteet aihepiiriä syventäviin julkaisuihin.