123 research outputs found
Editor's Note.
The article offers information on change in the editorship of the journal "Irish Journal of Management" which involves replacement of Edel Conway by Michelle O'Sullivan as co-editor
Rick Bragg, 1997 Harry M. and Edel Ayers Lecture Series 1
Author Rick Bragg was featured at the Harry M. and Edel Ayers Lecture Series held November 19, 1997 on the 11th floor of the Houston Cole Library at Jacksonville State University.https://digitalcommons.jsu.edu/lib_ac_histimg_1990/1381/thumbnail.jp
Rick Bragg, 1997 Harry M. and Edel Ayers Lecture Series 2
Author Rick Bragg was featured at the Harry M. and Edel Ayers Lecture Series held November 19, 1997 on the 11th floor of the Houston Cole Library at Jacksonville State University. Shown Rick Bragg chats with Opal A. Lovett after giving his speech.https://digitalcommons.jsu.edu/lib_ac_histimg_1990/1382/thumbnail.jp
EDEL: ENEA dosemeter for eye lens
Since the publication of International Commission on Radiological Protection statement in 2011 on tissue reaction, eye lens radiation protection played an important role in exposed personnel dosimetry. For this reason, the Italian National Agency for New Technologies, Energy and Sustainable Economic Development (ENEA) Individual Monitoring Service decided to study a prototype to fulfil specific requests (e.g. for survey in interventional department and intercomparisons). On the basis of such preliminary investigation, a new eye lens dosemeter was developed. The new dosemeter, named EDEL (ENEA Dosemeter for Eye Lens), was characterised in terms of Hp(3), the operational quantity related to eye lens monitoring. The investigation was performed experimentally and optimised using the Monte Carlo MCNP6 code. The new prototype was thought to fulfil two main requests: the reliability of the dosimetric data and the portability of the dosemeter itself. The new dosemeter will soon be supplied to the collaborating hospitals for workplace test measurements. © The Author 2015. Published by Oxford University Press. All rights reserved
Polyphony and the anxiety of influence in the fiction of Henry James
James's fiction, especially in the Middle Phase, centres
on the figure of the artist and is characterized by, the two
interrelated aspects which previous criticism has largely
overlooked: the Bakhtinian 'polyphonic' -creation of
'author-thinkers'; and the conflict between ephebes and
precursors, for which Harold-Bloom's concept of 'the-anxiety of
influence' is the most illuminating model. Polyphony is the
narrative mode, and influence is the intra-artistic, theme.
These, as the Introduction to the thesis makes clear, are
rehearsed in James's inaugural novel, Roderick Hudson. Rowland
Mallet is an author-thinker, and his failure is caused by
authorial limitations. His monologism -is impaired by his
mistaking empathy for the authorial sympathy. Likewise,
Hudson's failure does not arise from a mercurial temperament,
but from a polyphonic shortcoming: not possessing the power of
fiction to contain the fiction of power in, his mentor. And the
relationships among the three artists - Gloriani, Hudson and
Singleton - perfectly exemplify the Bloomian-theme. It is these
two concepts, polyphony and influence, which are the major
preoccupation in the Middle Phase; as, the works chosen
demonstrate. These are a novella, a novel, and a number of
short stories all of which have been unjustifiably neglected.
Chapter One, on The Aspern Papers, argues that Tina Bordereau,
far from being, the artless victim seen by many critics,
actually challenges and defeats the narrator by the very form
of her narrative. Her 'realist' discourse undermines his
language of 'romance', and shows up its internal unstability.
Chapter Two is an extensive study of the critical reception of
The Tragic Muse. The most common areas of critical attention
have been its contemporary topicality, its relation to previous
novels on similar themes, and the possible genealogy of Gabriel
Nash. Those have all missed the core of the work. - Chapter Three
demonstrates how polyphony and the anxiety of influence make
the novel what it really is. Influence arises from the
juxtaposition of, and the wrestling between, artistic ephebes
and their precursors (Nick and Nash,, Miriam and Madame Carre).
The dialogic quality defined by Bakhtin is crucial to the
proper, and even-handed, characterization of all, the conflicts
in the novel. And since most of James's tales in the eighties
and nineties -are about 'masters - and acolytes, the anxiety of
influence remains central. Chapter Four is a study of 'The
Author of Beltraffiol' and 'The Lesson of the Master'. Again the
characters' manipulations are a crucial focus in a way that
G6rard Genette's terminology helps to illuminate. The fact that
the ephebe is the author-thinker emphasizes the inextricability
of the Bakhtinian and the Bloomian in James. Just as
polyphony offers a different focus for explicating the poetics
of James's fiction; so the ephebal conflict provides the basis
for a fresh perception of James's own artistic struggle
Siegfried In The Interpretations Of The German Film Directors Of The Early 20th – Early 21st Century (Fritz Lang's "The Nibelungs" And Uli Edel`S "Ring Of The Nibelungs")
Film experts and art historians studied German cinema in detail, however, movies based on “The Song of the Nibelungs” as well as on the German and Scandinavian heroic epic have not yet been investigated by means of modern interdisciplinary approaches. The author pays attention to Siegfried, one of the most important heroes of the German and Scandinavian epic, according to Fritz Lang's (1890 – 1976) and Uli Edel`s (1947) interpretations, divided by almost a century (1924 and 2004). The author analyzes various means of expression: visuality, scenery, actor's performance, credits/dialogues. As far as the Lang's movie is concerned, he concludes that one can interpret the figure of Sigfried on two levels of interpretation. The first is the visual one which includes the actor's performance and the work of support staff (e.g. dress makers, set dressers). It describes him as an extraordinary strong hero. The second one is the semantic level which is formed of credits and music. It creates a myth about Siegfried as the national hero. In Edel's movie, the dialogues between heroes and actor's performance are used as the main means of expression. In Lang’s interpretation, Siegfried is described as the neo-romantic superhero, the person possessing a special force. Uli Edel’s Siegfried obtains dialectic nature – he is the prince, the king, and he is also the commoner; courageous soldier, dragon slayer, and obedient vassal, servant; son of Christian parents, pagan's stepson. The author assumes that Fritz Lang and Uli Edel reacted to inquiries of the time. In the 1920s, Germany suffered a difficult period between the two World Wars, the German people were oppressed by military reparations. Powerful Siegfried, as the national hero and embodiment of the German people, was urged to remind Germans of their great heroic past, to return their self-confidence to them. In our era of globalization and multiculturalism, the idea of association, peaceful co-existence of various ideas and religions was embodied in Siegfried.</jats:p
Fawcett, Edgar, 1885 August 15
Copy extant? No record of it in Edel bindersPrivate, Anderson Galleries (NY), 3-4 September 1928: "Autograph Collection of a Late American Author" (#543
Dissolved major element concentration data of the South Pacific Ocean transect during RV SONNE cruise SO289
This dataset presents salinity-normalized dissolved major element (Ca, Mg, K, Sr, Li) concentrations along RV SONNE cruise track SO289 in the South Pacific Ocean collected during GEOTRACES GP21 expedition (Valparaiso, Chile- Nouméa, New Caledonia) between February 23 and April 4, 2022. Samples were collected from the trace-metal clean Ti-frame rosette equipped with a Kevlar-coated winch. Samples were filtered through 0.2 µm AcroPak™ 500 filter capsules, collected in acid-cleaned 4 mL PP tubes, and acidified to pH ~2 with trace metal-grade HCl. Samples were analysed for Na, Ca, Mg, K, Li and Sr using a Varian-720 ES ICP-OES. Samples were diluted by a factor of 78-82 in 0.12 M HCl to the same final salinity. Multiple spectral lines were selected for each element, and samples were corrected for instrumental drift by sample-standard bracketing with IAPSO P157 diluted to the same final salinity. Calibration was performed on 7 dilutions of IAPSO P157. Element-to-sodium ratios were calculated for all combinations of spectral lines. Assuming a constant Na-to-salinity (PSU)=35 ratio, the element/Na ratios were multiplied by 0.46847 µmol kg-1 to obtain the salinity (PSU)-normalized element concentration, and by the ratio of practical to absolute salinity (TEOS-10). The TEOS-10 absolute salinities were calculated from EOS-80 values using the Gibb's Oceanographic Toolbox using the R package 'gsw' (v 1.1-1)
Dissolved major element (Ca, Sr, Mg, K, Li) concentration data of the western Atlantic Ocean meridional section GA02 (GEOTRACES) and Arctic Ocean cruise JR271 (BODC)
This dataset presents salinity-normalized dissolved major element (Ca, Mg, K, Sr, Li) concentrations in the western Atlantic Ocean and the Arctic Ocean. Atlantic samples were collected along the western meridional GEOTRACES section GA02 comprised of cruises JR057 (Punta Arenas (Chile) 02-03-2011 to Las Palmas (Spain) 06-04-2011 ), PE321 (Bermuda 11-06-2010 to Fortaleza (Brazil) 08-07-2010), PE319 (Scrabster 28-04-2010 to Bermuda 25-05-2010), and PE358 (Reykjavik (Iceland) 29-07-2012 to Texel (Netherlands) 19-08-2012). Samples for dissolved major ions were sub-sampled from trace metal sample collection stored at the Royal Netherlands Institute for Sea Research (NIOZ). Samples for the Arctic Ocean were collected on BODC cruise JR271 (Immingham 01-06-2012 to Reykjavik 02-07-2012). Samples were analysed for Na, Ca, Mg, K, Li and Sr using a Varian-720 ES ICP-OES. Samples were diluted by a factor of 78-82 in 0.12 M HCl to the same final salinity. Multiple spectral lines were selected for each element, and samples were corrected for instrumental drift by sample-standard bracketing with IAPSO P157 diluted to the same final salinity. Calibration was performed on 7 dilutions of IAPSO P157. Element-to-sodium ratios were calculated for all combinations of spectral lines. Assuming a constant Na-to-salinity (PSU)=35 ratio, the element/Na ratios were multiplied by 0.46847 µmol kg-1 to obtain the salinity (PSU)-normalized element concentration, and by the ratio of practical to absolute salinity (TEOS-10). The TEOS-10 absolute salinities were calculated from EOS-80 values using the Gibb's Oceanographic Toolbox using the R package 'gsw' (v 1.1-1)
Dissolved major element concentration data of the Equatorial Pacific Ocean transect during RV SONNE cruise SO298
This dataset presents absolute salinity-normalized dissolved major element (Ca, Mg, K, Sr, Li) concentrations along RV SONNE cruise track SO298 along the Equatorial Pacific Ocean collected during GEOTRACES GP11 expedition (Guayaquil, Ecuador - Townsville, Australia) from April 14th to June 2nd, 2023. Samples were collected from the trace-metal clean Ti-frame rosette equipped with a Kevlar-coated winch. Samples were filtered through 0.2 µm AcroPak™ 500 filter capsules, collected in acid-cleaned 4 mL PP tubes, and acidified to pH ~2 with trace metal-grade HCl. Samples were analysed for Na, Ca, Mg, K, Li and Sr using a Varian-720 ES ICP-OES. Samples were diluted by a factor of 78-82 in 0.12 M HCl to the same final salinity. Multiple spectral lines were selected for each element, and samples were corrected for instrumental drift by sample-standard bracketing with IAPSO P166 diluted to the same final salinity. Calibration was performed on 7 dilutions of IAPSO P166. Element-to-sodium ratios were calculated for all combinations of spectral lines. Assuming a constant Na-to-salinity (PSU)=35 ratio, the element/Na ratios were multiplied by 0.46847 µmol kg-1 to obtain the salinity (PSU)-normalized element concentration, and by the ratio of practical to absolute salinity (TEOS-10). The TEOS-10 absolute salinities were calculated from EOS-80 values using the Gibb's Oceanographic Toolbox using the R package 'gsw' (v 1.1-1)
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