2,871 research outputs found
Data Set for The eLoaD platform endows centrifugal microfluidics with on-disc power and communication
No full textData supporting the paper Sarai M. Torres Delgado, Jan G. Korvink, Dario Mager 2018 The eLoaD platform endows centrifugal microfluidics with on-disc power and communication Biosensors and Bioelectrronics https://doi.org/10.1016/j.bios.2018.05.056</span
M. Friedrich Mager, le paysage agraire du Schleswig
No full textM. Friedrich Mager, le paysage agraire du Schleswig. In: Annales d'histoire sociale. 3ᵉ année, N. 3-4, 1941. p. 190
M. Friedrich Mager, le paysage agraire du Schleswig
No full textM. Friedrich Mager, le paysage agraire du Schleswig. In: Annales d'histoire sociale. 3ᵉ année, N. 3-4, 1941. p. 190
Ménage et famille de la société proto-industrielle: le cas exemplaire de Spenge dans la première moitié du XIXe siècle
No full textMager W. Ménage et famille de la société proto-industrielle: le cas exemplaire de Spenge dans la première moitié du XIXe siècle. In: Acerra M, ed. État, marine et société. Paris: Presses de l'Université de Paris-Sorbonne; 1995: 283-308
Mixing Methods: Practical Insights from the Humanities in the Digital Age
No full textDigitality is a cause and a consequence of different data cultures. It applies to the 10 research projects that are included in this volume. They are rooted in various humanities disciplines such as art history, philosophy, musicology, religious studies, architectural history, media studies, and literature studies. As diverse as the disciplines are the objects and their formats, which are the subject of this book. The cultural data of the projects include recordings of music and spoken word, photographs and other types of images, handwriting, typoscripts and maps. The oldest material dates back to 500 BCE, followed by medieval times, the 18th and 19th centuries, early 20th century and the present. All projects share that they study their material with digital methods, although digitality comes into play at different moments and layers in each of the projects. Hardly readable manuscripts from the 18th century have to be treated with specialized OCR-methods while Plato’s texts are already available in digital form, and therefore open up other affordances for analysis. Special analysis possibilities had to be developed for certain image sources. For all projects, however, it is equally true that only the digitization of the objects makes them accessible to the methods that are the subject of this book.History, Form & Aesthetic
Paris - Bielefeld: La naissance d'un réseau
No full textMager W, Bulst N. Paris - Bielefeld: La naissance d'un réseau. In: Espagne M, ed. L' école normale supérieure et l'Allemagne. Deutsch-französische Kulturbibliothek, 6. Leipzig: Leipziger Univ.-Verl; 1995: 231-240
Intermediate-&lt;I&gt;m&lt;/I&gt; ULF waves generated by substorm injection: a case study
No full textAbstract. A case study of SuperDARN observations of Pc5 Alfvén ULF wave activity generated in the immediate aftermath of a modest-intensity substorm expansion phase onset is presented. Observations from the Hankasalmi radar reveal that the wave had a period of 580 s and was characterized by an intermediate azimuthal wave number (m=13), with an eastwards phase propagation. It had a significant poloidal component and a rapid equatorward phase propagation (~62° per degree of latitude). The total equatorward phase variation over the wave signatures visible in the radar field-of-view exceeded the 180° associated with field line resonances. The wave activity is interpreted as being stimulated by recently-injected energetic particles. Specifically the wave is thought to arise from an eastward drifting cloud of energetic electrons in a similar fashion to recent theoretical suggestions (Mager and Klimushkin, 2008; Zolotukhina et al., 2008; Mager et al., 2009). The azimuthal wave number m is determined by the wave eigenfrequency and the drift velocity of the source particle population. To create such an intermediate-m wave, the injected particles must have rather high energies for a given L-shell, in comparison to previous observations of wave events with equatorward polarization. The wave period is somewhat longer than previous observations of equatorward-propagating events. This may well be a consequence of the wave occurring very shortly after the substorm expansion, on stretched near-midnight field lines characterised by longer eigenfrequencies than those involved in previous observations.
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The Nurse\u27s Role in Promoting Optimal Health of Older Adults: Thriving in the Wisdom Years
No full textDiana Mager is a contributing author, Chapter 16 - Living safely in the community.
Book description: Why focus on the negative aspects of growing old while most older adults are leading positive, fulfilling, and active lives even while dealing with the changes associated with aging and chronic illnesses? Promote healthy aging; learn what it means to age successfully; and develop the tools and resources that can optimize well-being during the later years in life with the guidance you\u27ll find inside. The author, a nationally recognized expert in the field of gerontology addresses the physical, psychosocial, and spiritual needs of older adults based on a holistic, mid-range nursing theory of successful aging. Contributions from healthcare professionals in exercise physiology, nutrition, pharmacy and elder law help you understand how these disciplines work together to benefit patients.https://digitalcommons.fairfield.edu/nursing-books/1034/thumbnail.jp
Intermediate-m ULF waves generated by substorm injection: a case study
No full textA case study of SuperDARN observations of Pc5 Alfvén ULF wave activity generated in the immediate aftermath of a modest-intensity substorm expansion phase onset is presented. Observations from the Hankasalmi radar reveal that the wave had a period of 580 s and was characterized by an intermediate azimuthal wave number (m=13), with an eastwards phase propagation. It had a significant poloidal component and a rapid equatorward phase propagation (~62° per degree of latitude). The total equatorward phase variation over the wave signatures visible in the radar field-of-view exceeded the 180° associated with field line resonances. The wave activity is interpreted as being stimulated by recently-injected energetic particles. Specifically the wave is thought to arise from an eastward drifting cloud of energetic electrons in a similar fashion to recent theoretical suggestions (Mager and Klimushkin, 2008; Zolotukhina et al., 2008; Mager et al., 2009). The azimuthal wave number m is determined by the wave eigenfrequency and the drift velocity of the source particle population. To create such an intermediate-m wave, the injected particles must have rather high energies for a given L-shell, in comparison to previous observations of wave events with equatorward polarization. The wave period is somewhat longer than previous observations of equatorward-propagating events. This may well be a consequence of the wave occurring very shortly after the substorm expansion, on stretched near-midnight field lines characterised by longer eigenfrequencies than those involved in previous observations
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