bluuebunny/crossref_metadata_2025_split huggingface dataset:
Quand la charité fabrique des hommes
Authors: Dubrulle Luc 
Published: October 2017

Mgr Jean Rodhain (1900-1977), génial patron du Secours catholique, s’est employé à réhabiliter la charité. Si sa tentative théorique n’a pas franchement fonctionné, l’entreprise pédagogique qu’il met en place constitue une formidable matrice de structuration des sujets par l’action caritative. Rodhain la décompose dans les fameux 4 R : Regarder la misère, Révéler la charité, Réaliser contre la misère, Réunir les charitables. L’analyse de ces phases pédagogiques permet de mettre en évidence une reconstruction anthropologique par la pratique. Ainsi émerge la manière dont le corps ecclésial peut contribuer à la restructuration du corps social et politique dans l’horizon divin.
A Phenomenology of One Southeastern African American Church Choir
Authors: Parker Elizabeth Cassidy 
Published: October 2017

Abstract
The purpose of this phenomenological inquiry was to describe the essence of long-term singing experiences for participants in one Southeastern African American church choir in the United States. Specific areas of inquiry included how participants described the evolution of their singing over their long-term membership, how they articulated pivotal moments that connected singing experiences to self-growth, and what kept them singing in the same church choir. The data collection included 24 individual interviews with 18 different participants and 16 observations over a 3-month period. Participants ranged from 25 to 62 years of membership. Data sources included memos, artifacts, interview transcripts, and field notes. Using embodiment as a lens, data were reduced, horizontalized, and synthesized into a textural portrayal, structural description, and essence. Findings indicated 6 textural themes beginning with Themes 1 and 2, “growing as young people” and “building and sustaining the choir family.” Participants highlighted the importance of their directors within Theme 3, “inspiring directors with vision” and how music related to their self-growth in Theme 4, “becoming part of my music.” The final two textural themes, “contributing and ministering to others” and “loving God and gospel music” represented the strongest descriptions of participant lived experience as long-term members of the choir. The essence of participants’ lived experiences was development of the spiritual self. Implications for music education as spiritually relevant pedagogy are offered.
When Mary Went through the Hole: Constructing and Contesting Individual and Family Identity through Narrative
Authors: Tye Diane 
Published: October 2017

Abstract
This article explores how a brother and sister, now in their eighties, position themselves in their stories based on an episodic childhood memory. It considers the narratives as important resources for the tellers’ identifying of both self and family and explores how sometimes conflicting accounts based on childhood memories, and shaped by adult interpretations, connect and separate family members, help individuals articulate who they are, and suggest how they should move forward.
Co-Narration, Intersubjectivity, and the Listener in Family Storytelling
Authors: Borland Katherine 
Published: October 2017

Abstract
Storytelling in an intimate group, such as the family, underscores the intersubjective nature of the self, and co-narration illuminates the active role of audience members in oral narrative performance. By shifting my focus from analyzing a discrete text within a stream of discourse to a consideration of the dynamics of interaction in a storytelling event, I discern how a listener takes up, reshapes, and dialogizes the words of another as she moves from receptive audience member to responsive performer. At the same time, even the most monologic and complete narrative performances contain unvoiced dimensions that gesture toward meanings not given by the discourse, meanings that may or may not be recoverable for a given listener. I conclude with a plea for greater attention to the multiple and sometimes conflicting ways that tellers and listeners make sense of oral personal narratives.
Obscene Sounds: Sex, Death, and the Body On-Screen
Authors: Walsh Caitríona 
Published: October 2017

Abstract
Corporeality is an incipient theme in the scholarship of on-screen sound, and one with significant scope for additional investigation, coinciding with the argument that the proclivity for corporeal screen media has gathered momentum in recent years. This article examines standout instances of fleshly film sound in titles like There Will Be Blood (2007) and Under the Skin (2013) via an eros and thanatos framework, evincing film’s enduring fixation with provocative themes of sex and death. This doublet of instinctual drives is borne of classical ideas and the psychical constructs of Freud and Lacan. It dominates on-screen manifestations of the corporeal, and holds special significance when it comes to auditory aspects of the physical body on-screen. Sex-death duality is a central conceit in Under the Skin, where eroticism and mortality are artfully intermingled, and where seductive and frightening entrapment processes are elicited through foreboding percussive beats and the upward-edging motion of looped and distorted chromatic string figures. Expanding on existent research around cinema’s horror heartbeats in titles like There Will Be Blood, along with obscene sonic evocations of eros and thanatos, these investigations are intended as a viable means of framing corporeal research, constituting an appeal for visceral, multisensory spectatorship. This advocates for a move away from ocularcentrism, which staunchly prioritizes film’s opticality, toward an actively engaged and embodied mode of film viewership.
Synthesis of 8-Trifluloromethyl-2-Thioquinazolin-(3H)-4-One Nucleosides
Authors: Break Laila M. 
Published: October 2017

Synthesis of 8-trifluloromethyl-2-thioquinazolin-(1H,3H)-4-one 2. which have been ribosylated by coupling with 1-O-acetyl-2,3,5-tri-O-benzoyl-
Entre '20 centímentros' e 'Pó de arroz': a estética fílmica como póetica de desestigmatizacão do universo transexual
Authors: Alós Anselmo Peres , Yokoyama Adriana , Lavorati Carla 
Published: October 2017

Este artigo problematiza as relações de gênero no filme espanhol 20 centímetros (2005), de Ramón Salazar, e no curta-metragem brasileiro Pó de arroz (2015), de Lucas Moratelli. A partir das discussões da teoria queer e dos estudos de gênero, analisa-se como a personagem Marieta, de Salazar, e a personagem sem nome de Moratelli, contribuem para a desestigmatização da cultura transexual masculina (male-to-female).Entre 20 centímetros y Polvo de arroz: la estética fílmica como poética del término del estigma del universo transexualResumen: Este estudio analiza las relaciones de género en las películas española 20 centímetros (2005), de Ramón Salazar, y la brasileña Polvo de arroz (2015), de Lucas Moratelli. A partir de las discusiones de la teoría queer y los estudios de género, se analizará cómo la personaje Marieta, de Salazar, y la personaje sin nombre de Moratelli contribuyen a la desestigmatización de la cultura transexual (male-to-female). Palavras clave: Teoria Queer; Estudios de Género; Transexualidad; Narrativas FílmicasBetween 20 centimeters and Rice powder: the filmic aesthetics as a subversive poetics of the transexual universeAbstract: This article aims at discussing gender relations in the Spanish movie 20 centimeters (2005), by Ramón Salazar, as well as in the Brazilian movie Rice powder (2015), by Lucas Moratelli. Taking as a point of departure the discussions of Queer Theory and Gender Studies, we analyse how the character Marieta, from Salazar’s movie, and the unnamed character from Moratelli’s movie contribute to the de-stigmatization of male-to-female transexual culture.Keywords: Queer Theory; Gender Studies; Transexuality; Filmic Narratives.
Onset Timing and Slip History of the Teton Fault, Wyoming: A Multidisciplinary Reevaluation
Authors: Brown Summer J. , Thigpen J. Ryan , Spotila James A. , Krugh William C. , Tranel Lisa M. , Orme Devon A. 
Published: October 2017

AbstractThe dramatic relief of the Teton Range in northwestern Wyoming results from motion along the Teton normal fault. New apatite (U‐Th)/He (AHe) and fission track (AFT) ages of samples collected in the footwall yield fundamental constraints on contrasting models of Teton fault activity and consequent relative footwall uplift. Low‐elevation samples in the immediate footwall of the fault range from 12.5 to 6.5 Ma. AHe ages of samples from subvertical transects range from 57.8 to 6.5 Ma (Rendezvous), 54.0 to 6.8 Ma (Grand), and 20.5 to 7.1 Ma (Moran), with all three transects yielding an expected trend of decreasing age with decreasing elevation. AFT ages obtained from the three transects range from 55.4 to 45.7 Ma (Rendezvous), 43.2 to 13.3 Ma (Grand), and 38.0 to 11.7 Ma (Moran). Inverse thermal history modeling indicates that the onset of relatively rapid cooling, as a proxy for relative footwall uplift, initiated first in the northern part of the range (15–13 Ma) and then migrated south as fault displacement continued (7 Ma to present at Rendezvous). Thus, this work suggests that although the Teton fault likely initiated due to Basin and Range extension, this structure remains active. Normal fault displacement models also suggest a minimum of ~6 km displacement for footwall uplift of ~2 km. If evaluated in the context of established normal fault length‐displacement relationships, this yields a length of ~180 km, substantially longer than current estimates of Teton fault length and putting the northern end of the fault well into, and potentially beyond, the bounds of Yellowstone National Park.
The Spatial Structure of the 128 ka Antarctic Sea Ice Minimum
Authors: Holloway Max D. , Sime Louise C. , Allen Claire S. , Hillenbrand Claus‐Dieter , Bunch Pete , Wolff Eric , Valdes Paul J. 
Published: October 2017

AbstractWe compare multi‐ice core data with δ18O model output for the early last interglacial Antarctic sea ice minimum. The spatial pattern of δ18O across Antarctica is sensitive to the spatial pattern of sea ice retreat. Local sea ice retreat increases the proportion of winter precipitation, depleting δ18O at ice core sites. However, retreat also enriches δ18O because of the reduced source‐to‐site distance for atmospheric vapor. The joint overall effect is for δ18O to increase as sea ice is reduced. Our data‐model comparison indicates a winter sea ice retreat of 67, 59, and 43% relative to preindustrial in the Atlantic, Indian, and Pacific sectors of the Southern Ocean. A compilation of Southern Ocean sea ice proxy data provides weak support for this reconstruction. However, most published marine core sites are located too far north of the 128,000 years B.P. sea ice edge, preventing independent corroboration for this sea ice reconstruction.
Investigating Dynamic Triggering of Seismicity by Regional Earthquakes: The Case of the Corinth Rift (Greece)
Authors: De Barros Louis , Deschamps Anne , Sladen Anthony , Lyon‐Caen Hélène , Voulgaris Nicholas 
Published: October 2017

AbstractDynamic triggering has been commonly observed after large teleseismic events, but the physics behind it is still under debate. To broaden observations, we here focus on the dynamic triggering by regional earthquakes, that is, by events with magnitude lower than 6.2 at distances smaller than 600 km. The western part of the Corinth Rift (Greece) is characterized by intense seismic swarms and is therefore adapted to study such responses. The microseismicity rates before and after the transient perturbations are high enough to analyze 30 regional earthquakes out of the 59 occurring in 2013. More than 40% of those 30 events, including earthquakes with magnitude as small as 4.5, are associated with a significant seismicity rate increase. The triggerability primarily depends on the amplitude of the seismic waves. However, triggering is mainly observed when the seismic perturbations are orthogonal to the faults, which suggests that fluid pressurization is likely involved.
Determining Coastal Mean Dynamic Topography by Geodetic Methods
Authors: Huang Jianliang 
Published: October 2017

AbstractIn geodesy, coastal mean dynamic topography (MDT) was traditionally determined by spirit leveling technique. Advances in navigation satellite positioning (e.g., GPS) and geoid determination enable space‐based leveling with an accuracy of about 3 cm at tide gauges. Recent CryoSat‐2, a satellite altimetry mission with synthetic aperture radar (SAR) and SAR interferometric measurements, extends the space‐based leveling to the coastal ocean with the same accuracy. However, barriers remain in applying the two space‐based geodetic methods for MDT determination over the coastal ocean because current geoid modeling focuses primarily on land as a substitute to spirit leveling to realize the vertical datum.
Mobility Effect on Poroelastic Seismic Signatures in Partially Saturated Rocks With Applications in Time‐Lapse Monitoring of a Heavy Oil Reservoir
Authors: Zhao Luanxiao , Yuan Hemin , Yang Jingkang , Han De‐hua , Geng Jianhua , Zhou Rui , Li Hui , Yao Qiuliang 
Published: October 2017

AbstractConventional seismic analysis in partially saturated rocks normally lays emphasis on estimating pore fluid content and saturation, typically ignoring the effect of mobility, which decides the ability of fluids moving in the porous rocks. Deformation resulting from a seismic wave in heterogeneous partially saturated media can cause pore fluid pressure relaxation at mesoscopic scale, thereby making the fluid mobility inherently associated with poroelastic reflectivity. For two typical gas‐brine reservoir models, with the given rock and fluid properties, the numerical analysis suggests that variations of patchy fluid saturation, fluid compressibility contrast, and acoustic stiffness of rock frame collectively affect the seismic reflection dependence on mobility. In particular, the realistic compressibility contrast of fluid patches in shallow and deep reservoir environments plays an important role in determining the reflection sensitivity to mobility. We also use a time‐lapse seismic data set from a Steam‐Assisted Gravity Drainage producing heavy oil reservoir to demonstrate that mobility change coupled with patchy saturation possibly leads to seismic spectral energy shifting from the baseline to monitor line. Our workflow starts from performing seismic spectral analysis on the targeted reflectivity interface. Then, on the basis of mesoscopic fluid pressure diffusion between patches of steam and heavy oil, poroelastic reflectivity modeling is conducted to understand the shift of the central frequency toward low frequencies after the steam injection. The presented results open the possibility of monitoring mobility change of a partially saturated geological formation from dissipation‐related seismic attributes.
Characteristics of Upward Lightning on the Beijing 325 m Meteorology Tower and Corresponding Thunderstorm Conditions
Authors: Yuan Shanfeng , Jiang Rubin , Qie Xiushu , Wang Dongfang , Sun Zhuling , Liu Mingyuan 
Published: October 2017

AbstractComprehensive observation on lightning striking the 325 m meteorology tower has been conducted in Beijing, China, during the summer season from 2012 to 2016. For the 20 tower flashes captured by high‐speed video camera, 19 (95%) cases were initiated from the tower (termed as upward lightning (UL)), with duration of 42–844 ms. Most ULs (84.2%, 16/19) were triggered by nearby lightning, of which positive cloud‐to‐ground flashes (+CGs) account for 87.5% (14/16). Analysis on the characteristics of the causal or triggering lightning flashes suggests that the approaching of negative leader process through in‐cloud horizontal channel is the vital condition for the initiation of upward leader. Generally, the UL initiation follows the nearby discharges, while for a special case in our data set, the nearby positive return stroke was found to occur after the establishment of an upward channel from the tower. It is worth noting that this +CG led to a significant enhancement of the tower‐initiating leader, with eight subsequent return strokes and two M component processes occurring to the tower thereafter. The radar echo of the corresponding thunderstorm indicates that the other‐triggered UL (OTUL) tended to occur at the dissipation stage of the thunderstorm with relatively low cloud top height and weak radar echo, while the self‐initiating UL (SIUL) was more likely to occur when the thunderstorm was in the mature stage and the tower was underneath the stratiform clouds behind the convective region. The meteorology condition for SIUL involved lower ambient temperature and higher wind speed, as compared to the OTUL.
Landslide Frequency and Failure Mechanisms at NE Gela Basin (Strait of Sicily)
Authors: Kuhlmann J. , Asioli A. , Trincardi F. , Klügel A. , Huhn K. 
Published: October 2017

AbstractDespite intense research by both academia and industry, the parameters controlling slope stability at continental margins are often speculated upon. Lack of core recovery and age control on failed sediments prevent the assessment of failure timing/frequency and the role of prefailure architecture as shaped by paleoenvironmental changes. This study uses an integrated chronological framework from two boreholes and complementary ultrahigh‐resolution acoustic profiling in order to assess (1) the frequency of submarine landsliding at the continental margin of NE Gela Basin and (2) the associated mechanisms of failure. Accurate age control was achieved through absolute radiocarbon dating and indirect dating relying on isotope stratigraphic and micropaleontological reconstructions. A total of nine major slope failure events have been recognized that occurred within the last 87 kyr (~10 kyr return frequency), though there is evidence for additional syndepositional, small‐scaled transport processes of lower volume. Preferential failure involves translational movement of mudflows along subhorizontal surfaces that are induced by sedimentological changes relating to prefailure stratal architecture. Along with sequence‐stratigraphic boundaries reflecting paleoenvironmental fluctuations, recovered core material suggests that intercalated volcaniclastic layers are key to the basal confinement and lateral movement of these events in the study area. Another major predisposing factor is given by rapid loading of fine‐grained homogenous strata and successive generation of excess pore pressure, as expressed by several fluid escape structures. Recurrent failure, however, requires repeated generation of favorable conditions, and seismic activity, though low if compared to many other Mediterranean settings, is shown to represent a legitimate trigger mechanism.
Can Seismic Observations of Bed Conditions on Ice Streams Help Constrain Parameters in Ice Flow Models?
Authors: Kyrke‐Smith Teresa M. , Gudmundsson G. Hilmar , Farrell Patrick E. 
Published: October 2017

AbstractWe investigate correlations between seismically derived estimates of basal acoustic impedance and basal slipperiness values obtained from a surface‐to‐bed inversion using a Stokes ice flow model. Using high‐resolution measurements along several seismic profiles on Pine Island Glacier (PIG), we find no significant correlation at kilometer scale between acoustic impedance and either retrieved basal slipperiness or basal drag. However, there is a stronger correlation when comparing average values along the individual profiles. We hypothesize that the correlation appears at the length scales over which basal variations are important to large‐scale ice sheet flow. Although the seismic technique is sensitive to the material properties of the bed, at present there is no clear way of incorporating high‐resolution seismic measurements of bed properties on ice streams into ice flow models. We conclude that more theoretical work needs to be done before constraints on mechanical conditions at the ice‐bed interface from acoustic impedance measurements can be of direct use to ice sheet models.
Grain Yield Observations Constrain Cropland CO2 Fluxes Over Europe
Authors: Combe M. , de Wit A. J. W. , Vilà‐Guerau de Arellano J. , van der Molen M. K. , Magliulo V. , Peters W. 
Published: October 2017

AbstractCarbon exchange over croplands plays an important role in the European carbon cycle over daily to seasonal time scales. A better description of this exchange in terrestrial biosphere models—most of which currently treat crops as unmanaged grasslands—is needed to improve atmospheric CO2 simulations. In the framework we present here, we model gross European cropland CO2 fluxes with a crop growth model constrained by grain yield observations. Our approach follows a two‐step procedure. In the first step, we calculate day‐to‐day crop carbon fluxes and pools with the WOrld FOod STudies (WOFOST) model. A scaling factor of crop growth is optimized regionally by minimizing the final grain carbon pool difference to crop yield observations from the Statistical Office of the European Union. In a second step, we re‐run our WOFOST model for the full European 25 × 25 km gridded domain using the optimized scaling factors. We combine our optimized crop CO2 fluxes with a simple soil respiration model to obtain the net cropland CO2 exchange. We assess our model's ability to represent cropland CO2 exchange using 40 years of observations at seven European FluxNet sites and compare it with carbon fluxes produced by a typical terrestrial biosphere model. We conclude that our new model framework provides a more realistic and strongly observation‐driven estimate of carbon exchange over European croplands. Its products will be made available to the scientific community through the ICOS Carbon Portal and serve as a new cropland component in the CarbonTracker Europe inverse model.
Microengineering of Optical Properties of GeO2 Glass by Ultrafast Laser Nanostructuring
Authors: Zhang Fangteng , Cerkauskaite Ausra , Drevinskas Rokas , Kazansky Peter G. , Qiu Jianrong 
Published: October 2017

AbstractNanostructuring in glass by ultrafast laser paves the way for integrated optics. In this paper, form birefringence induced by ultrafast laser direct writing in GeO2 glass is systematically investigated. It is shown that the pulse energy for maximum retardance in GeO2 glass is ≈65% lower than in fused silica. The induced retardance by laser scanning is two times higher than that by stationary irradiation under the same processing conditions. The optimum pulse duration for maximum retardance in GeO2 glass lies within sub‐picosecond region, i.e., typically around 500 fs, while in fused silica it is in the picosecond regime at around 1–2 ps. A reversed polarization dependence of retardance at low pulse densities and low pulse repetition rates is observed in GeO2 glass. As a result, two optical applications including a radial polarization vortex converter and a computer‐generated hologram are demonstrated in GeO2 glass by spatial manipulation of the optical axis of the locally induced form birefringence. The microengineering of optical properties of GeO2 glass by ultrafast laser direct writing may lead to new applications in near‐/mid‐infrared optics.