Marl Prairie/Slough Gradients; Patterns and Trends in Shark Slough and Adjacent Marl Prairies (CERP monitoring activity 3.1.3.5), First Annual Report (2005)

The work on CERP monitoring item 3.1.3.5 (Marl prairie/slough gradients) is being conducted by Florida International University (Dr Michael Ross, Project Leader), with Everglades National Park (Dr. Craig Smith) providing administrative support and technical consultation. As of January 2006 the funds transferred by ACOE to ENP, and subsequently to FIU, have been entirely expended or encumbered in salaries or wages. The project work for 2005 started rather late in the fiscal year, but ultimately accomplished the Year 1 goals of securing a permit to conduct the research in Everglades National Park, finalizing a detailed scope of work, and sampling marsh sites which are most easily accessed during the wet season. 46 plots were sampled in detail, and a preliminary vegetation classification distinguished three groups among these sites (Sawgrass marsh, sawgrass and other, and slough) which may be arranged roughly along a hydrologic gradient from least to most persistently inundated . We also made coarser observations of vegetation type at 5-m intervals along 2 transects totaling ~ 5 km. When these data were compared with similar observations made in 1998-99, it appeared that vegetation in the western portion of Northeast Shark Slough (immediately east of the L-67 extension) had shifted toward a more hydric type during the last 6 years, while vegetation further east was unchanged in this respect. Because this classification and trend analysis is based on a small fraction of the data set that will be available after the first cycle of sampling (3 years from now), the results should not be interpreted too expansively. However, they do demonstrate the potential for gaining a more comprehensive view of marsh vegetation structure and dynamics in the Everglades, and will provide a sound basis for adaptive management.

Fragm. lat. V 97 - Summa casuum (Zu den Dekretalen Gregors IX.: 2.27 - 28; 3.1 - 3, 8, 10)

Trägerband: Inc. qu. 960; Vorbesitzer: Zacharias Konrad von Uffenbach

(Tables 1, 3) Details of Agassiz trawl stations and numbers of specimens per macro- and megazoobenthic taxon collected during POLARSTERN cruise ANT-XXII/3 (ANDEEP III)

The assemblages inhabiting the continental shelf around Antarctica are known to be very patchy, in large part due to deep iceberg impacts. The present study shows that richness and abundance of much deeper benthos, at slope and abyssal depths, also vary greatly in the Southern and South Atlantic oceans. On the ANDEEP III expedition, we deployed 16 Agassiz trawls to sample the zoobenthos at depths from 1055 to 4930 m across the northern Weddell Sea and two South Atlantic basins. A total of 5933 specimens, belonging to 44 higher taxonomic groups, were collected. Overall the most frequent taxa were Ophiuroidea, Bivalvia, Polychaeta and Asteroidea, and the most abundant taxa were Malacostraca, Polychaeta and Bivalvia. Species richness per station varied from 6 to 148. The taxonomic composition of assemblages, based on relative taxon richness, varied considerably between sites but showed no relation to depth. The former three most abundant taxa accounted for 10-30% each of all taxa present. Standardised abundances based on trawl catches varied between 1 and 252 individuals per 1000 m2. Abundance significantly decreased with increasing depth, and assemblages showed high patchiness in their distribution. Cluster analysis based on relative abundance showed changes of community structure that were not linked to depth, area, sediment grain size or temperature. Generally abundances of zoobenthos in the abyssal Weddell Sea are lower than shelf abundances by several orders of magnitude.

Prophecy as a narrative world : a study of the world-constructing conventions and narrative techniques in Hosea 1-3

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Aplicação informática para verificação de perfis enformados a frio segundo a EN1993-1-3

Os perfis enformados a frio estão em crescente uso na indústria da construção, utilizados como estruturas secundárias e primárias, por apresentar resistência em relação ao baixo peso, facilidade de utilização em obra e sustentabilidade. A norma europeia EN1993-1-3, também adotada em Portugal, que apresenta as especificações normativas sobre o uso estrutural de perfis enformados a frio é de difícil aplicação para os projetistas devido à quantidade e complexidade de cálculos para que sejam efetuadas as verificações de segurança necessárias, pelas limitações dos programas informáticos e complexidade de compreensão dos fenómenos da instabilidade local e distorcional que condicionam o comportamento deste tipo de secções, classificadas como de classe 4. O presente trabalho procura explicar os procedimentos do eurocódigo e os seus aspetos mais controversos, como, por exemplo, o processo de cálculo da distribuição de tensões numa secção arbitrária constituída por segmentos retos, o cálculo de larguras efetivas e espessuras reduzidas e as verificações de segurança em termos de resistência e estabilidade global requeridos pela norma. O principal objetivo deste trabalho é o desenvolvimento um programa de cálculo para verificar barras com secções de classe 4 que tenha a abrangência das especificações do Eurocódigo (EC3-1-3), que possa auxiliar engenheiros no processo de projeto, dimensionamento e verificação regulamentar de estruturas metálicas que utilizem este tipo de secções. Para isso foi criada uma aplicação informática, em ambiente Windows®, que está ligada ao programa Autodesk® Robot Structural Analisys® para obtenção de dados de cálculo e executar os cálculos de secções efetivas e verificações de segurança de acordo com a norma europeia. São apresentados diagramas de blocos com a sequência do procedimento de cálculo das várias fases de cálculo de secções efetivas e de verificação de barras, com vista a mostrar a lógica de funcionamento interno da aplicação criada no âmbito deste trabalho. Por fim desenvolve-se um manual de utilização da aplicação e um exemplo comparativo, de cálculo das propriedades efetivas de uma secção, entre os resultados do programa e documentos de referência com cálculos manuais

Prophecy as a narrative world : a study of the world-constructing conventions and narrative techniques in Hosea 1-3

Thèse numérisée par la Direction des bibliothèques de l'Université de Montréal.

Chemical analysis of water samples of station M1_1207, Red Sea (Table 1-3)

Two water samples and two sediment samples taken in 1965 by the R. V. "Meteor" in the area of the hot salt brine of the Atlantis II-Deep were chemically investigated, and in addition the sediment samples were subjected to X-ray and optical analysis. The investigation of the sulfur-isotope-ratios showed the same values for all water samples. This information combined with the Ca-sulfate solubility data leads us to conclude that, for the most part, the sulfate content of the salt brine resulted from mixing along the boundary with the normal seawater. In this boundary area gypsum or anhydrite is formed which sinks down to the deeper layers of the salt brine where it is redisolved when the water becomes undersaturated. In the laboratory, formation of CaS04 precipitate resulted from both the reheating of the water sample from the uppermost zone of the salt brine to the in-situ-temperature as well as by the mixing of the water sample with normal Red Sea water. The iron and manganese delivered by the hot spring is separated within the area of the salt brine by their different redox-potentials. Iron is sedimented to a high amount within the salt brine, while, as evidenced by its small amounts in all sediment samples, the more easily reducible manganese is apparently carried out of the area before sedimentation can take place. The very good layering of the salt brine may be the result of the rough bottom topography with its several progressively higher levels allowing step-like enlargements of the surface areas of each successive layer. Each enlargement results in larger boundary areas along which more effective heat transfer and mixing with the next layer is possible. In the sediment samples up to 37.18% Fe is found, mostly bound as very poorly crystallized iron hydroxide. Pyrite is present in only very small amounts. We assume that the copper is bound mostly as sulfide, while the zinc is most likely present in an other form. The sulfur-isotope-investigations indicate that the sulfur in the sediment, bound as pyrite and sulfides, is not a result of bacterical sulfate-reduction in the iron-rich mud of the Atlantis II-Deep, but must have been brought up with the hot brine.

(Tables 1-3) Silicon dioxide, Corg and trace element concentrations in sediments of the outer Eckernfoerder Bay, Western Baltic Sea

The main question, posed in the work scheme before laboratory analysis was started, was expressed as follows: Do marked seasonal fluctuations occur in trace element content of the sediment surface, and what are the probable influences of factors such as changing hydrographical parameters, plankton sequence etc. ? Special attention was paid to elements known as pollutants, for example mercury. Within this framework samples have been analysed for their contents of manganese, iron, zinc, lead, and mercury. The amounts of silica and organically-bound carbon serve in most cases as reference values for the trace element content. On sand temporary conditions of increased C org content raise the concentrations of all determined elements. Especially the values reached for mercury in July are worth nothing. It is concluded that Zn, Pb, and Hg tend to enrich with respect to C org as the decomposition of organic matter progresses. On mud-sand flocculation and precipitation of Mn/Fe-hydroxides probably represent an additional concentrating factor for the other elements as the relationship of the results for zinc and manganese shows. Manganese may indicate a seasonally related concentrating cycle at the sediment surface.

Planktonic foraminiferal flux and shell geochemistry data in the sediment trap time series JAM 1-3 off south Java

Results from sediment trap experiments conducted in the seasonal upwelling area off south Java from November 2000 until July 2003 revealed significant monsoon-, El Niño-Southern Oscillation-, and Indian Ocean Dipole-induced seasonal and interannual variations in flux and shell geochemistry of planktonic foraminifera. Surface net primary production rates together with total and species-specific planktonic foraminiferal flux rates were highest during the SE monsoon-induced coastal upwelling period from July to October, with three species Globigerina bulloides, Neogloboquadrina pachyderma dex., and Globigerinita glutinata contributing to 40% of the total foraminiferal flux. Shell stable oxygen isotopes (d18O) and Mg/Ca data of Globigerinoides ruber sensu stricto (s.s.), G. ruber sensu lato (s.l.), Neogloboquadrina dutertrei, Pulleniatina obliquiloculata, and Globorotalia menardii in the sediment trap time series recorded surface and subsurface conditions. We infer habitats of 0-30 m for G. ruber at the mixed layer depth, 60-80 m (60-90 m) for P. obliquiloculata (N. dutertrei) at the upper thermocline depth, and 90-110 m (100-150 m) for G. menardii in the 355-500 mm (>500 µm) size fraction corresponding to the (lower) thermocline depth in the study area. Shell Mg/Ca ratio of G. ruber (s.l. and s.s.) reveals an exponential relationship with temperature that agrees with published relationships particularly with the Anand et al. (2003) equations. Flux-weighted foraminiferal data in sediment trap are consistent with average values in surface sediment samples off SW Indonesia. This consistency confirms the excellent potential of these proxies for reconstructing past environmental conditions in this part of the ocean realm.

(Tables 1-3) Geochemical composition of seepage water in soils obtained in Schleswig-Holstein, Germany

Under defined laboratory and field conditions, the investigation of percolating water through soil columns (podsol, lessive and peat) down to groundwater table shows that the main factors which control the chemical characteristics of the percolates are: precipitation, evaporation, infiltration rate, soil type, depth and dissolved organic substances. Evaporation and percolation velocity influences the Na+, SO4**2- and Cl- concentrations. Low percolation velocity leads also to longer percolation times and water logging in less permeable strata, which results in lower Eh-values and higher CO2-concentrations due to low gas exchange with the atmosphere. Ca2+ and Mg2+ carbonate concentration depends on soil type and depth. Metamorphism and decomposition of organic substances involve NO3 reduction and K+, Mg2+, SO4**2-, CO2, Fe2+,3+ transport. The analytical data were evaluated with multi variate statistical methods.

Utemiljön som undervisningsverktyg inom matematiken : En studie om fyra lärares uppfattningar och användning av utomhusmatematik i årskurs 1-3

Syftet med denna studie var att undersöka hur lärares uppfattningar om utomhusmatematik som undervisningsmetod är i årskurserna 1-3 samt i vilken utsträckning de använder detta. De frågeställningarna som var bärande i studien var hur användandet av utomhusmatematik ser ut, vilka för- och nackdelar informanterna ser med utomhusmatematik, om något kunskapsområde inom matematiken lämpar sig bättre eller sämre vid användning av undervisningsformen samt om det är någon av de matematiska förmågorna eleverna lättare kan utveckla med detta. Metoden som tillämpades var kvalitativa semistrukturerade intervjuer med fyra lärare vilka har arbetat olika länge samt arbetar i delvis olika årskurser och på olika skolor. Resultatet visade att användande av utomhusmatematik inte är allt för stort men intresset för undervisningsformen är desto större. En bidragande orsak till att det inte används är storleken på klasserna idag. En fördel som informanterna ser med undervisningsformen är att eleverna får arbeta konkret, praktiskt, röra på sig samt att de får frisk luft. Med hjälp av utomhusmatematiken anser informanterna att både kunskapsområdena inom matematiken och de matematiska förmågorna går att utveckla med utomhusmatematik.

Effects of Purified Saccharomyces cerevisiae (1→3)-β-Glucan on Venous Ulcer Healing

Water-insoluble glucan was isolated from the baker’s yeast Saccharomyces cerevisiae. The yeast cells were treated with alkali and the residue then with acid. Chemical and NMR (1D and 2D) analyses showed that a linear (1→3)-β-glucan was purified that was not contaminated with other carbohydrates, proteins or phenolic compounds. The effects of the glucan on wound healing were assessed in human venous ulcers by histopathological analysis after 30 days of topical treatment. (1→3)-β-glucan enhanced ulcer healing and increased epithelial hyperplasia, as well as increased inflammatory cells, angiogenesis and fibroblast proliferation. In one patient who had an ulcer that would not heal for over 15 years, glucan treatment caused a 67.8% decrease in the area of the ulcer. This is the first study to investigate the effects of (1→3)-β-glucan on venous ulcer healing in humans; our findings suggest that this glucan is a potential natural biological response modifier in wound healing

Att utveckla elevers grundläggande begreppsförståelse i matematik : En litteraturstudie om hur matematikundervisningen i årskurs 1-3 kan utformas för att ge elever möjlighet att utveckla en god begreppsförståelse i matematik

Studier visar att svenska elevers resultat i matematik har försämrats och att en av de bakomliggande orsakerna till resultatnedgången är bristande begreppsförståelse. Samtidigt rapporteras det om att eleverna i undervisningen allt mer lämnas ensamma i sitt lärande i så kallat individuellt arbete. Tolkningen som kan göras är att det finns ett samband mellan elevers försämrade matematikkunskaper och undervisningen de möter i matematik. Syftet med denna studie är att få kunskap om hur matematikundervisningen kan utformas för att ge elever i årskurs 1-3 möjlighet att utveckla en god begreppsförståelse i matematik. Svaret söktes genom en systematisk litteraturstudie där litteratur och aktuell forskning söktes systematiskt. I studiens resultat exemplifieras en rad kommunikationsverktyg för läraren att använda direkt i undervisning, men också andra typer av verktyg, för att stödja och utveckla elevers förståelse för matematiska begrepp. Vidare synliggörs också fördelar med en lärare som möjliggör en undervisning där eleverna själva får kommunicera matematik och som agerar resurs för dem i deras övergång från det vardagliga till det matematiska språket. Kommunikation kan därför ses som ett viktigt verktyg i matematikundervisningen då det kommer till att utveckla elevers begreppsförståelse. Undervisningsmiljön behöver därför utformas till att passa en mer kommunikativ undervisning; en tillåtande miljö där eleverna tillåts och stöttas i att prata matematik.

Prevention of bacterial translocation using β-(1-3)-D-glucan in small bowel ischemia and reperfusion in rats

To investigate the role of β-(1-3)-D-glucan on 99mTc labelled Escherichia coli translocation and cytokines secretion in rats submitted to small bowel ischemia/reperfusion injury. Methods: Five groups (n=10 each) of Wistar rats were subjected to control(C), sham(S), group IR subjected to 45 min of bowel ischemia/60 min of reperfusion(I/R), and group I/R+glucan subjected to 45 min of bowel ischemia/60 min of reperfusion(I/R) and injected with 2mg/Kg intramuscular. Translocation of labelled bacteria to mesenteric lymph nodes, liver, spleen, lung and serum was determined using radioactivity/count and colony forming units/g(CFU/g). Serum TNFα, IL-1β, IL-6, IL-10 were measured by ELISA. Results: CFU/g and radioactivity/count were higher in I/R than in I/R+glucan rats. In C, S and S+glucan groups, bacteria and radioactivity/count were rarely detected. The I/R+glucan rats had enhancement of IL-10 and suppressed production of serum TNFα, IL-1β and, IL-6, compared to I/R untreated animals. Conclusion: The β-(1-3)-D-glucan modulated the production of pro-inflammatory and anti-inflammatory cytokines during bowel ischemia/reperfusion, and attenuated translocation of labelled bacteria