1,840 research outputs found
Marriage License for Allen, Alfred and Converse, May J.
No full textMarriage license for Alfred Allen and May J. Converse. S.T. Thompson was the officiant
Author Correction: New perspectives on Neanderthal dispersal and turnover from Stajnia Cave (Poland)
No full textThe Author contributions section now reads:“W.N., A.N. and S.T. designed research; A.P., M.H., W.N., S.B., M.U., A.M., H.F., M.D.B., P.S., K.S., M.Ż., A.W., A.N. and S.T. performed research; A.P., M.H., W.N., S.B., M.U., A.M., H.F., M.D.B., P.S., K.S., M.Ż., A.W., A.N. and S.T. analysed data; A.P., M.H., S.T., W.N. and S.B. wrote the paper with the collaboration of all the co-authors.
Author Correction:A 41,500 year-old decorated ivory pendant from Stajnia Cave (Poland)
No full textCorrection to: Scientific Reports https://doi.org/10.1038/s41598-021-01221-6, published online 25 November 2021The original version of this Article contained errors in the author list where Marjolein D. Bosch was omitted from the author list, and Mikołaj Urbanowski was incorrectly listed as an author of the original Article, and has subsequently been removed.The Author contributions section now reads:“S.T. W.N. and A.N. conceived the project; S.T., W.N., A.P., M.B., S.C., M.D., H.F., A.M., M.D. B., D.P., M.P.R., C.M.R., V.S-M., G.M.S., P.S., M.S., K.S., A.V., F.W., H.W., A.W., M.Z., S.B., A.N., J-J. H., performed research; S.T., A.P., W.N., M.B., M.D.B., S.C., M.D., H.F., A.M., D.P., M.P.R., C.M.R., V.S-M., G.M.S., P.S., M.S., K.S., A.V., F.W., H.W., A.W., M.Z., S.B., A.N., J-J. H. analysed all archaeological data; S.T. and A.P. wrote the paper with the collaboration of all the co-authors.”The original Article and its accompanying Supplementary Information file have been corrected
Lovecraft and Religion
No full textThe article was originally published as a chapter in S.T. Joshi’s book Lovecraft and a World in Transition: Collected Essays on H. P. Lovecraft (New York: Hippocampus Press 2014, pp. 187-195). The presented version was kindly provided to „Creatio Fantastica” by the Author without any copyright fee and translated into Polish by Magdalena Wąsowicz
RRS Discovery Cruise 321, 24 Jul-23 Aug 2007. Biophysical interactions in the Iceland Basin 2007
No full textD321 was the first of three National Oceanography Centre ‘process study’ research cruises to be run by the Ocean Biogeochemistry and Ecosystems research group under the NERC Oceans 2025 research programme. The scientific work began by carrying out some of the extended Ellett Line stations on the way out to our study region; which centred around the historical JGOFS Ocean Weather Station India site (~ 59° N, ~ 19° W) and the northward turn of the extended Ellett line at 20° W. The Iceland Basin, like much of the N. Atlantic subpolar gyre, is characterised by a ‘bloom and bust’ seasonal cycle. Spring stratification triggers a major diatom dominated bloom event. This bloom is short lived, limited by silicate (orthosilicic acid) exhaustion (Brown et al., 2003). Two community succession pathways commonly follow the demise of the diatom bloom; typically through dinoflagellate and/or coccolithophore production. The spring bloom is dominated by eddy scale (several 10's of km) patchiness, driven by the upward and downward pumping effect of eddies on the newly forming spring stratification. However these eddy structures have another, more important, impact on phytoplankton production (Allen et al., 2005). In the release of potential energy, eddies effect a real three dimensional exchange of water across the thermocline bringing new dissolved nutrients from deeper waters up into the photic zone and transporting biogenic particles into the deep ocean. Thin ribbon like structures around the edges of eddies are clearly seen in ocean colour satellite images. The four repeated surveys carried out during D321 observed the evolution of an ‘eddy dipole’ in a background ocean full of eddies and other turbulent motions. Daily, near real-time, satellite images and in-situ vessel mounted acoustic current profiling were used to determine the movement of the eddy centres and the dipole central jet. Targeted nets and water collection within the various components of the eddy dipole enabled the assessment of its biological impacts.Since 1996 NOCS and SAMS have been occupying an extended version of the Ellett Line that runs all the way to Iceland. The Extended Ellett line is important oceanographically because it completes the measurements of the warm saline water flowing into the Nordic Seas from the eastern North Atlantic. It also monitors around half of the returning deep and cold current, the overflow water (the rest returns to the Atlantic via the Denmark Strait to the west of Iceland).There is little added cost, either in time or financially, in making a number of biogeochemical measurements using water samples from the hydrographers' CTD stations. Thus, recently, the scientific interests in the Extended Ellett line have become more multidisciplinary; the 2006 occupation was no exception. Samples were filtered for POC, HPLC studies and trace aluminium concentration determination, in addition some extra time was found for a number of zooplankton net hauls.<br/
The role of anti-IgE therapies in the treatment of asthma
No full textThe prevalence of asthma, a chronic inflammatory disease often linked to allergy, is on the increase. The introduction of a blocking anti-IgE monoclonal antibody (omalizumab) as a new therapy has not only confirmed the pathogenic role of IgE in asthma but has also provided a novel therapy for a chronic severe disease where there are limited therapeutic options
Experimental research on the effects of surface screens on a mobile bed
No full textIn 2000 the Dutch government chose a new point of view for the Dutch rivers: “Room for the River”. This viewpoint is the basis for a new approach of high water protection in the Netherlands. Instead of strengthening and raising the dikes, solutions must be based on space and spatial quality. One of the suggested measures is the addition of secondary channels. The purpose of these channels is enlarging the conveyance area and the ecological role of the river. Maintaining the profile of these channels involves substantial financial consequences. Finding a sustainable solution for undesired erosion or sedimentation is the main focus of this study. The research question is stated as follows: “How can the undesired erosion or sedimentation in secondary channels be corrected with a temporary but sustainable solution in the form of surface screens?”. The main part of this study is an experimental study on the effects of surface screens on a mobile bed. The design of the physical experiments requires choices about the geometry of the flume. The experiments were carried out with a straight flume and with a dividing wall. Preparing the experiments requires information about the flume facility. The experiments have been carried out in the Environmental Fluid Mechanics Laboratory of DUT. The upstream boundary conditions are discharge and velocity distribution. The downstream boundary condition consisted of a fixed water level. The water level was kept constant along the natural slope of the surface. The experiments consist of taking velocity and bed level. The angle of attack and the penetration depth were chosen to be variable. The angle of attack was varied between 15 and 25 degrees. With these relatively small angles the screen acts as guidance for the flow, instead of an obstruction. The penetration depth was varied between 20% and 60% of the water column. The initial test run determined the optimal measurement duration and the initial equilibrium. Four representative cases have been described in detail, giving support to the general conclusions. The flow pattern changes under influence of the surface screen. The main flow direction is guided by the screen, introducing a transverse velocity at the surface. As flow continuity in the flume has to be maintained, the water near the bottom is forced to have a transverse velocity in opposite direction. Redistribution of the suspended transport and the bottom transport was induced. This generated locations were the actual transport did not meet the transport capacity, which gives rise to morphological changes. Next to the spiral motion the screen had an effect on the longitudinal flow velocities. The attacked side of the flume experiences a higher velocity, thereby having a higher transport capacity. This higher capacity gives rise to local erosion of the bed. At the unattacked side, sedimentation occurs, thereby rising the bed level. In the B-series of the experiment a dividing wall was added. The screen in front of the bifurcation gave rise to the same two processes, but the wall introduced an extra effect. The screen influenced the bifurcation relationship. The bed level adapted to the new conditions. The upstream effect of the bifurcation is explained by changes in water level topography, thereby influencing the backwater curve. In general the wall amplified the morphological development of the bed. Finally some suggestions have been made for the practical application of surface screens. In general the screens can be applied in a (secondary) channel or in front of a bifurcation. The use of a screen inside a channel has an advantage not to interfere with the navigation channel. The advantage of a screen in front of a bifurcation is influencing two channels simultaneously. One of the main disadvantages of the latter is the possibility of disturbing the delicate bifurcation relationship. When carefully implemented this effect can simultaneously be the main advantage of this screen layout, as the morphological response increases.Hydraulic EngineeringCivil Engineering and Geoscience
Robert Merry's museum.
No full textS.G. Goodrich was editor until 1850, when Rev. S.T. Allen became "home editor." The connection of Goodrich with the magazine ceased with v. 28 in 1854. cf. Goodrich, Recollections. v. 2, p. 543, 545.Title from vol. t.p.Mode of access: Internet
Pedagogical ideas of S.T. Shatsky
No full textU radu se prate osnovne pedagoške ideje poznatog ruskog i sovjetskog društvenog radnika i pedagoga S. T. Šackog. Članak polazi od osnovnih informacija njegove biografije, neprekidno povezane sa radom u prosveti i razmišljanjima o vaspitanju, prikazujući ih kao podlogu razvoja njegovih pedagoških ideja. Dalji tekst kratko iznosi njegove osnovne ideje u tematskim celinama o kritici škole, cilju vaspitanja, škole budućnosti, predškolskom i vanškolskom vaspitanju, didaktičkim shvatanjima, položaju deteta u vaspitnom procesu, radu učitelja i mestu škole u društvenoj sredini. Rad pokušava da dovede u vezu shvatanja Šackog sa savremenim pogledima na iste probleme. U tekstu se, takođe, može uočiti nekoliko tema za razmišljanje koje su naročito izdvojene u zaključnom delu članka: trajnost pitanja o vaspitanju, odnosno pedagoških problema, mogućnosti ostvarivanja ideja o promeni škole kao institucije vaspitnog sistema, odnos rada u prosveti i društvenog angažovanja.The author discusses the pedagogical ides of a well known Russian and Soviet social worker and pedagogue S.T. Shatsky. The report starts with the basic information from his biography, always in connection with his work in education and his contemplation on education, showing them as a background for the development of his pedagogical ideas. It proceeds by' an account on hid ideas in themes on criticism of school, the objective of education of the school of future, pre school and out of school education, didactic ideas, the position of child in the process of education, the work of the teacher and the place of school in the social milieu. The author attempts to bring together Shatsky's ideas and the modern attitudes to the same problems. The text also offers a number of topics for discussion, especially dealt with in the closing part: the duration of the issue of education, i.e. pedagogical problems, the possibility' of realization of the ideas on the change of school as a institution of education system, the relation of work in education and social engagement
Choice allotments & Maryville Cottage & grounds, adjoining "Strathmore" the residence of Sir Geo. W. Allen, Glebe Point Road [cartographic material] : to be sold on the ground _ Saturday 8th December at 3 o'clock /
No full textSales plan for land in the suburb of Glebe in Sydney, bordered by Glebe Point Road, William Street and Cook Street.; In lower left corner: Geo. Bishop, surveyor & c., oppe. city bank.; Oriented with north to the left.; Also available in an electronic version via the internet at: http://nla.gov.au/nla.map-lfsp894
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