Single-function approach to calibrating whatman n.º 42 filter paper based on suction versus water content relationships

Several suction–water-content (s-w) calibrations for the filter paper method (FPM) used for soil-suction measurement have been published. Most of the calibrations involve a bilinear function (i.e., two different equations) with an inflection point occurring at 60 kPa

Generalized descriptive set theory and classification theory

Descriptive set theory is mainly concerned with studying subsets of the space of all countable binary sequences. In this paper we study the generalization where countable is replaced by uncountable. We explore properties of generalized Baire and Cantor spaces, equivalence relations and their Borel reducibility. The study shows that the descriptive set theory looks very different in this generalized setting compared to the classical, countable case. We also draw the connection between the stability theoretic complexity of first-order theories and the descriptive set theoretic complexity of their isomorphism relations. Our results suggest that Borel reducibility on uncountable structures is a model theoretically natural way to compare the complexity of isomorphism relations.

Potential isomorphism of elementary substructures of a strictly stable homogeneous model

"Vegeu el resum a l'inici del document del fitxer adjunt."

The non-absoluteness of model existence in uncountable cardinals for Lw1,w

"Vegeu el resum a l'inici del document del fitxer adjunt"

On Borel equivalence relations in generalized Baire space

"Vegeu el resum a l'inici del document del fitxer adjunt."

Lire, écrire : d'un désir l'autre : le "roman de Meliadus" du XIIIe au XVIIIe siècle

Continuation elleptique du Tristan en prose, qui s'inscrit dans l'interstice séparant la naissance de Tristan du remariage de Méliadus avec la fille du roi Hoël, le Roman de Meliadus (1235-1240) est une oeuvre fondamentalement ouverte, de par son inachèvement et de par le dialogue constant qu'il instaure avec les autres romans arthuriens. S'il revendique sa filiation et assume son statut de récit puîné, les réminiscences qu'il exhibe masquent aussi les gauchissements, les infléchissements qui lui permettent de faire du neuf avec du vieux. C'est ce jeu - aux deux sens du terme - que cette étude se propose de mettre en lumière et de voir fonctionner, non seulement dans le Roman de Meliadus proprement dit, mais également dans trois de ses relectures, qui actualisent et renouvellent la signification du roman en profondeur. La première est une continuation qui date de la toute fin du XIIIe ou du début du XIVe siècle et qui est aujourd'hui conservée par le seul manuscrit Ferrell 5. La deuxième actualisation retenue est celle qu'offre Meliadus de Leonnoys, l'imprimé publié en 1528 par Galliot du Pré, puis en 1532 par Denis Janot, fruit d'un minutieux travail de découpage et de remontage. La dernière enfin est l'extrait paru en 1776 dans la Bibliothèque Universelle des Romans sous le titre Méliadus de Léonnois. An ellipitic continuation of the Prose Tristan, which inscribes itself in the space separating the birth of Tristan from Meliadus' new marriage with king Hoël's daughter, the Meliadus' romance (1235-1240) is essentially an open text on account of its incompleteness and the dialogue it establishes with other arthurian romances. Even asserting filiation status, the reminiscences also show the reshaping and the inflection that allow the text to transform old into new. Analyzing this game is the central purpose of this work; to observe the operation in the Meliadus' romance, as well as in three of its recuperations that profoundly renew the significance of the novel; beginning with a continuation from the end of the 13th century or the early 14th century, preserved nowadays in only one manuscript (Ferrel 5); followed by the meticulous work of cutting and reassembling offered by the Meliadus of Leonnoys (printed by Galliot du Pré in 1528 first and again by Denis Janot in 1532) and finally an excerpt published in 1776 in the Bibliothèque Universelle des Romans with the title Méliadus of Leonnois.

Early Cretaceous (late Berriasian to early Aptian) palaeoceanographic change along the northwestern Tethyan margin (Vocontian Trough, southeastern France): δ13C, δ18O and Sr-isotope belemnite and whole-rock records

Stable carbon, oxygen, and strontium isotope records were obtained from uppermost Hauterivian to lowermost Aptian belemnite rostra, which were collected in well-dated sections from the Vocontian Trough (southeastern France). This data set complements previously published belemnite-isotope records from the uppermost Berriasian-Hauterivian interval from the same basin. The belemnite carbon and oxygen isotope record is compared to the carbonate bulk-rock isotope record from the same sections, and from additional Italian sections. With regards to their long-term trends, both belemnite and whole-rock delta O-18 records are well correlated, except for the uppermost Hauterivian-lower Barremian interval, within which they deviate. This discrepancy is interpreted to be linked to the latest Hauterivian Faraoni oceanic anoxic event and its early Barremian aftermath. The Faraoni level is characterized by enhanced sea-water stratification, probably induced by the onset of a warmer and more humid climate along the northern Tethyan margin. The early Barremian was characterized by stronger vertical sea-water mixing reflected by a decrease in density contrast between sea-surface and deeper waters. The belemnite oxygen isotope record shows a more stable evolution with smaller fluctuations than its bulk-rock counterpart, which indicates that deeper water masses were not as much subjected to density fluctuations as sea-surface water. The comparison of belemnite and bulk-rock carbon isotope records allows observing the impact of regional influence exerted by platform carbonate ooze shedding on the carbon cycle. Discrepancies in the two records are observed during time of photozoan carbonate platform growth. The strontium isotopic record shows a gradual increase from the uppermost Berriasian to the uppermost lower Barremian followed by a rapid decrease until the uppermost Barremian and a renewed small increase within the lowermost Aptian. The major inflection point in the uppermost lower Barremian appears to predate the onset in the formation of the Ontong-Java volcanic plateau.

Horizontal, but not vertical, biotic interactions affect fine-scale plant distribution patterns in a low-energy system

Studies of species range determinants have traditionally focused on abiotic variables (typically climatic conditions), and therefore the recent explicit consideration of biotic interactions represents an important advance in the field. While these studies clearly support the role of biotic interactions in shaping species distributions, most examine only the influence of a single species and/or a single interaction, failing to account for species being subject to multiple concurrent interactions. By fitting species distribution models (SDMs), we examine the influence of multiple vertical (i.e., grazing, trampling, and manuring by mammalian herbivores) and horizontal (i.e., competition and facilitation; estimated from the cover of dominant plant species) interspecific interactions on the occurrence and cover of 41 alpine tundra plant species. Adding plant-plant interactions to baseline SDMs (using five field-quantified abiotic variables) significantly improved models' predictive power for independent data, while herbivore-related variables had only a weak influence. Overall, abiotic variables had the strongest individual contributions to the distribution of alpine tundra plants, with the importance of horizontal interaction variables exceeding that of vertical interaction variables. These results were consistent across three modeling techniques, for both species occurrence and cover, demonstrating the pattern to be robust. Thus, the explicit consideration of multiple biotic interactions reveals that plant-plant interactions exert control over the fine-scale distribution of vascular species that is comparable to abiotic drivers and considerably stronger than herbivores in this low-energy system.

Rakennustekniikan lämpökuvauspalvelujen kehittäminen

Tämä insinöörityö tehtiin Helsingin ammattikorkeakoulu Stadian Rakennustekniikan koulutusohjelmalle. Helsingin ammattikorkeakoulu Stadia on yksi Suomen suurimmista ammattikorkeakouluista, jonka opiskelijat ovat valmistuessaan alansa asiantuntijoita. Työn tavoitteena oli kehittää Rakennustekniikan koulutusohjelman tuottamia lämpökuvauspalveluja. Työssä selvitettiin, mitkä ovat lämpökuvauspalvelujen kehittämiskohteet ja mihin kehittämistoimenpiteisiin tulisi ryhtyä, jotta palvelujen menestyksekäs tuottaminen tulevaisuudessa varmistetaan. Työ aloitettiin perehtymällä palvelujen johtamisen ja kehittämisen menetelmiin sekä lämpökuvaamisen teknologiaan ja perusteisiin. Lämpökuvauspalvelujen kehittämismenetelmäksi valittiin palveluprosessin kuvaaminen ja siihen kytkeytyvän teknologian, osaamisen ja asiakassuhteiden kehittäminen. Työssä laadittiin seuraavaksi prosessikuvaus lämpökuvauspalveluille, määritettiin prosessiin kytkeytyvä teknologia ja osaaminen sekä kuvattiin palvelun asiakassuhteiden hoitomalli. Kuvausten perusteella kartoitettiin keskeiset kehittämiskohteet ja arvioitiin kehittämismahdollisuuksia. Työn lopputuloksena syntyi lämpökuvauspalvelujen prosessikuvaus sekä toimenpidesuositukset kehittämistoimenpiteistä. Keskeisinä suosituksina kehittämistoimenpiteiksi esitetään panostamista ajantasaiseen lämpökuvausteknologiaan hankkimalla uusi lämpökamera, palveluhenkilöstön osaamisen kehittämistä valmennuksia hyödyntäen sekä systemaattista asiakassuhteiden hoitoa ryhtymällä perusmarkkinointitoimenpiteisiin. Jatkotutkimuskohteeksi ehdotetaan selvitystä Rakennustekniikan koulutusohjelman lämpökuvauslaboratorion perustamismahdollisuuksista.

Stable isotope compositions of mammoth teeth from Niederweningen, Switzerland: Implications for the Late Pleistocene climate, environment, and diet

Oxygen and carbon isotope compositions of well-preserved mammoth teeth from the Middle Wurmian (40-70 ka) peat layer of Niederweningen, the most important mammoth site in Switzerland, were analysed to reconstruct Late Pleistocene palaeoclimatic and palaeoenvironmental conditions. Drinking water (delta(18)O values of approximately -12.3 +/- 0.9 parts per thousand were calculated front oxygen isotope compositions of mammoth tooth enamel apatite using a species-specific calibration for modern elephants. These delta(18)O(H2O) values reflect the mean oxygen isotope composition of the palaeo-precipitation and are similar to those directly measured for fate Pleistocene groundwater from aquifers in northern Switzerland and southern Germany. Using a present-day delta(18)O(H2)o-precipitation-air temperature relation for Switzerland, a mean annual air temperature (MAT) of around 4.3 +/- 2.1 degrees C can be calculated for the Middle Wurmian at this site. This MAT is in good agreement with palaeotemperature estimates on the basis of Middle Wurmian groundwater recharge temperatures and beetle assemblages. Hence, the climatic conditions in this region were around 4 degrees C cooler during the Middle Wurmian interstadial phase, around 45-50ka BP, than they are today. During this period the mammoths from Niederweningen lived in an open tundra-like, C(3) plant-dominated environment as indicated by enamel (delta(13)C values of -11.5 +/- 0.3 parts per thousand and pollen and macroplant fossils found in the embedding peat. The low variability of enamel delta(13)C and delta(18)O values from different mammoth teeth reflects similar environmental conditions and supports a relatively small time frame for the fossil assemblage. (C) 2006 Elsevier Ltd and INQUA. All rights reserved.

Runosta lauluksi : mitä nuottijulkaisut kertovat tekijöistään

Tapani Boman

Den finländska teologin under frihetstiden

Bill Widén