2,092 research outputs found
Author Peter FitzSimons speaking at the National Library of Australia, Canberra, 13 November 2012 /
No full textTitle from acquisitions documentation.; Part of the collection: Portraits of author Peter FitzSimons speaking at the National Library of Australia, Canberra, 13 November 2012.; Acquired in digital format; access copy available online.; Mode of access: Online.; Photographed by a staff member of the National Library of Australia
Professor Peter Singer speaking at the National Press Club Canberra, 11 February 2009 [picture] /
No full textTitle devised by cataloguer based on information from acquisitions documentation.; Part of the collection: Humanitarian author Professor Peter Singer at the National Press Club, Canberra, 11 February 2009.; Acquired in digital format; access copy available online.; Mode of access: Internet via World Wide Web.; Photographed by a staff member of the National Library of Australia, 2009
Transableism, Disability and Paternalism in Public Health Ethics: Taxonomies, identity Disorders and Persistent Unexplained Physical Symptoms
No full textTransableism is a term which refers to moving between states of being able and disabled by choice rather than by happenstance. Insofar as this may imply a choice to become dependent, claims upon the healthcare system are likely to result. In this piece we aim to explore some ethical and legal implications of such claims. In order to do so, we draw upon current debates over the place of
autonomy, beneficence and paternalism in public health ethics, the taxonomy of disability and the status of persistent unexplained physical symptoms (henceforth, PUPS). We suggest that transableism represents a useful construct which may contribute towards resolution of ongoing difficulties within public health ethics and theories of disability. In addition, we believe that it holds promise for the understanding of a significant proportion of patients presenting PUPS. We focus upon identity disorders, particularly in relation to what is currently termed Body Integrity Identity Disorder
(henceforth, BIID), where sufferers report a subjective conviction that one or more of their limbs are superfluous, requesting medical assistance to remove the offending limb[s], repair the results of
attempts at their self-removal or to provide prostheses and other assistance after removal. We have considered BIID elsewhere in relation to consent, capacity and the doctor/patient relationship
(Mackenzie and Cox, 2005). One of us has also explored how the definition of addiction as a chronic relapsing disease within public health governance enables cycles of transitions between the rigours of rational liberal citizenship and the shriven status of the sick (Mackenzie, 2006). Since a central aim in this piece is evaluate the place of transableism within public health ethics, we
will begin by considering the latter as a discursive context for the arguments which follow
Regulating Reprogenetics: Strategic Sacralisation and Semantic Message
No full textThis paper forms part of the feminist critique of the regulatory consequences of biomedicine's systematic exclusion of the role of women's bodies in the development ofreprogenetic technologies. I suggest that strategic use of notions of the sacred to decontextualise and delimit disagreement fosters this marginalisation. Here conceptions of the sacred a sacralisation afford a means by which pragmatic consensus over regulation may be achieved, through the deployment of a bricolage of dense images associated with cultural loyalties to solidify support or to exclude contradictory elements. Hence an explicit renegoation of the symbolic order structuring salient debates is necessary to disrupt and enrich the entrenched and exclusionary dominant discourse over reprogenetic regulation of infertility treatment and embryo research in the UNited Kingdom, the cultural anthropology of biomedicine and feminist ethnographies of reprogenetics to illustrate these claims
DSpace for e-print archives
No full textDSpaceTM (http://dspace.org/) is the new open source digital repository system from the MIT Libraries and Hewlett-Packard Labs designed to support the digital collections of academic research institutions, as well as the SPARC conception of Institutional Repositories for digital research material. The DSpace system has been described elsewhere in detail so the focus of this article is on its implementation at MIT for archiving e-prints and other artifacts of scholarly communication, and making these available to the public. The MIT Libraries are deeply concerned about the well-documented crisis in scholarly communication and are committed to working
towards innovative solutions. We share this concern with many of the MIT faculty and administration, several of who have been key supporters of the DSpace project and related
initiatives at the university. The MIT Libraries were a founding member of SPARC, and are a signatory of the Budapest Open Access Initiative (BOAI). This article will describe how MIT Libraries have implemented DSpace to support these goals
Streamflow in the Mackenzie Basin, Canada
No full textRivers of the Mackenzie Basin exhibit several seasonal flow patterns that include the nival (snowmelt dominated), proglacial (influenced by glacier melt), wetland, prolacustrine (below large lakes), and regulated flow regimes. The Mackenzie amalgamates and moderates these regimes to deliver spring peak flows, followed by declining summer discharge and low winter flows, to the Arctic Ocean. The mountainous sub-basins in the west (Liard, Peace, and northern mountains) contribute about 60% of the Mackenzie flow, while the interior plains and eastern Canadian Shield contribute only about 25%, even though the two regions have similar total areas (each occupying about 40% of the total Mackenzie Basin). The mountain zone is the dominant flow contributor to the Mackenzie in both high-flow and low-flow years. A case study of the Great Slave system demonstrates the effects of natural runoff, regulated runoff, and lake storage on streamflow, as well as the large year-to-year variability of lake levels and discharge. Despite a warming trend in the past three decades, annual runoff of the Mackenzie Basin has not changed. Significant warming at most climatic stations in April (and at some, also in May or June) could have triggered earlier snowmelt. The first day of hydrograph rise for the main trunk of the Mackenzie (seen as a proxy for breakup) has advanced by about three days per decade, though the trend was not statistically significant for the mountain rivers. Peak flows do not reveal any trend, but the arrival of the spring peaks has become more variable. More evidence is needed to interpret these flow phenomena properly.Les rivières du bassin du Mackenzie manifestent plusieurs modèles d\u27écoulement qui comprennent les régimes d\u27écoulement nival (dominé par la fonte des neiges), proglaciaire (influencé par la fonte glaciaire), de marécages, prolascustre (en aval de grands lacs) et régularisé. Le Mackenzie combine et modère ces régimes pour donner des débits de pointe au printemps, suivis d\u27un débit à la baisse en été, puis de faibles débits en hiver, en direction de l\u27océan Arctique. Les sous-bassins montagneux occidentaux (Liard, Peace et montagnes du Nord) contribuent pour environ 60 % au débit du Mackenzie, tandis que les plaines intérieures et le Bouclier canadien oriental ne contribuent que pour environ 25 %, même si les deux régions ont une superficie globale semblable (chacune occupant environ 40 % de la superficie totale du bassin du Mackenzie). La zone montagneuse apporte la contribution majeure au régime du Mackenzie, dans les années à fort débit comme dans celles à faible débit. Une étude de cas du réseau du Grand lac des Esclaves révèle l\u27impact sur le débit fluvial de l\u27écoulement naturel, de l\u27écoulement régularisé et de la hauteur d\u27eau dans le lac, ainsi que la grande variabilité d\u27une année sur l\u27autre du niveau et du débit des lacs. Malgré la tendance au réchauffement des trois dernières décennies, l\u27écoulement annuel du bassin du Mackenzie n\u27a pas changé. Un réchauffement notable enregistré à la plupart des stations climatiques en avril (et à certaines aussi en mai ou juin) pourrait avoir provoqué une fonte nivale précoce. Le premier jour où se manifeste l\u27augmentation du régime hydrique pour l\u27artère principale du Mackenzie (considéré comme un indicateur de la débâcle) a avancé d\u27environ trois jours par décennie, bien que statistiquement cette tendance ne soit pas significative pour les rivières de montagne. Les débits de pointe ne révèlent aucune tendance, mais l\u27arrivée des pics printaniers est devenue plus variable. Il faudrait des preuves supplémentaires pour interpréter correctement ces phénomènes d\u27écoulement
Geology of Graham Island, British Columbia
No full textby J.D. Mackenzie.Series ; Bulletin (Geological Survey of Canada : 1921). Geological series ; no. 72. Memoir (Geological Survey of Canada) ; 88. Accompanies Southern portion of Graham Island, Queen Charlotte Islands, British Columbia [cartographic material] / geology, J.D. Mackenzie ; geography, British Admiralty and Department of the Naval Service of Canada, Department of Lands, British Columbia, J.D. MacKenzie ; C.O. Senecal, geographer and chief draughtsman. Two folded maps in pocket
Southern portion of Graham Island, Queen Charlotte Islands, British Columbia.
No full textgeology, J.D. Mackenzie ; geography, British Admiralty and Department of the Naval Service of Canada, Department of Lands, British Columbia, J.D. MacKenzie ; C.O. Senecal, geographer and chief draughtsman.Scale 1:126,720. 2 miles to 1 in. (W 132 24'-W 131 55'/N 53 45'-N 53 08'). Contours shown by spot heights. Includes marginal notes and location map. Includes cross-sections and geological notes. Geology, published charts, township plans and surveys, conducted 1913-1914. To accompany Memoir by J.D. MacKenzie, Geology of Graham Island, British Columbia
Graham Island, Queen Charlotte Islands, British Columbia.
No full textgeology, J.D. MacKenzie ; geography, British Admiralty and Department of the Naval Service of Canada, Department of Lands, British Columbia, J.D. MacKenzie ; C.O. Senecal, geographer and chief draughtsman.Scale 1:253,440 (W 133 14'-W 131 36'/N 54 16'-N 53 07'). Includes location map. Geology, published charts, township plans and surveys, conducted 1913-1914. Series: Map (Geological Survey of Canada) ; 176A
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