'Please Mr Hay, what are my poss(abilities)?': Legitimation of ability through physical education practices

This paper provides two vignettes that draw on data from projects that interrogate how a student can be positioned by practices within physical education (PE) and directed by the PE teacher in relation to their valued or legitimated ability. Through the use of Pierre Bourdieu's conceptual tools of field, habitus and capital we investigate the complex legitimation processes that shape student poss(abilities) and that are situated in the space of the PE class. The first vignette is from the perspective of a student and draws on data from interviews, a journal, questionnaires and photos of her PE experiences in upper primary and lower secondary school. The second vignette focuses on teacher practices and his constitution of the field of a PE class highlighting the significance of teacher perspectives of 'ability' in informing assessment in senior secondary PE. Using these examples we discuss the symbolic violence that works against each student by positioning them as 'less able' or 'unable' despite their participation in a learning context. We argue that by not attending to the possible abilities of students that could have been recognized, developed and legitimated, and through the misuse of capital assignment by teachers, PE may well be counterproductive to students' ongoing engagement with the subject area and the espoused potential upon which such a subject area justifies itself.

Possible role of iron in the restless legs syndrome

DUE TO COPYRIGHT RESTRICTIONS ONLY AVAILABLE FOR CONSULTATION AT ASTON UNIVERSITY LIBRARY AND INFORMATION SERVICES WITH PRIOR ARRANGEMENT

Re-written by machine and new technology: Did the Internet kill the Video Star

The traditional way of understanding television content consumption and viewer reactions may be simply summarised: information about the program, viewing at airing time, and interpersonal discussion after the program. In our digital media environment due to crossmedia consumption and platform shifts, the actual trend in audiovisual, and traditionally television content consumption is changing, the viewer’s journey is different across contents and platforms. Content is becoming independent from the platform and the medium is increasingly in the hands of technologically empowered viewers. Our objective is to uncover how traditional content expressly manufactured for television (series, reality shows, sports) can now be consumed via other platforms, and how and to what extent audiovisual content consumption is complemented or replaced by other forms (text, audio). In our exploratory research we identify the typical patterns of interaction and synergies of consumption across classical media content. In this study we used a multimethodology qualitative research design with three research phases including focus groups, online content analysis, and viewers’ narratives. Overall, the Video Star stays alive, but has to deal with immediate reactions and has to change according to his or her audiences’ wishes

Dressed to Kill demonstration

General note: Title and date provided by Bettye Lane. Digital reproduction

Dear DTCA, Please Don’t Deceive Me, Don’t Play on My Fantasy

Travail créatif / Creative Work

Geochemistry of carbon at DSDP Legs 58 and 59 Holes

I obtained 68 quarter sections of cores from the JOIDES Organic Geochemistry Panel for studying type, distribution, and stages of organic diagenesis of sedimentary organic matter in the West Philippine and Parece Vela basins and Mariana Trough area (Figure 1). The present chapter compares (1) 11 geochemical parameters used to determine organic source and its stage of genesis within the 9 site locations in this study area and (2) compares these 11 with the same parameters reported from Leg 56, outer trench slope of the Japan Trench, and Leg 60, Mariana Trough and Trench (Schorno, in press a, b). Even though these sediments are considered pelagic, the organic content in most of the core sections appears to be hemipelagic. The sedimentary organic matter in these cores is believed to be in an early stage of diagenesis. Both conclusions are based primarily on the fl-alkane distribution within the organic matter. This particular parameter, I note later, has a major weakness. As Hunt (Hunt, 1979) and I (in press b) observed, marine organisms synthesize /z-alkanes with distributions containing neither odd nor even preferences. Thus those sediments that did contain w-alkane distributions with OEP near 1, suggesting a late stage of catagenesis, may in actuality be immature marine sediments.

Coarse-silt-fraction mineralogy at DSDP Legs 56 and 57 Holes

Soviet sedimentologists use the term "coarse silt" to denote the size fraction 0.1 to 0.05 mm (50-100 µm). Petelin (1961) has shown that this fraction is most diagnostic for terrigeneous and volcanogenic mineral assemblages and provinces in Recent deep-sea sediments, because of its greatest variability of both heavy and light non-opaque minerals, which may be easily identified by the common immersion method. We believe that the fraction is suitable for mineralogical study of unconsolidated and friable sediments from DSDP cores as well, if the objective is to investigate their source area and transporation tracks. In the case of fine-grained oceanic sediments, mineral composition of the coarse silt does not differ markedly from that of the "coarse fraction" (>62 µm).