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Literary criticism, particularly ecocriticism, occupies an uneasy position with regard to activism: reading books (or plays, or poems) seems like a rather leisurely activity to be undertaking if our environment—our planet—is in crisis. And yet, critiquing the narratives that structure worlds and discourses is key to the activities of the (literary) critic in this time of crisis. If this crisis manifests as a ‘crisis of imagination’ (e.g. Ghosh), I argue that this not so much a crisis of the absence of texts that address the environmental disaster, but rather a failure to comprehend the presences of the Anthropocene in the present. To interpret (literary) texts in this framework must entail acknowledging and scrutinising the extent of the incapacity of the privileged reader to comprehend the crisis as presence and present rather than spatially or temporally remote. The readings of the novels Carpentaria (2006) and The Swan Book (2013) by Waanyi writer Alexis Wright (Australia) trace the uneven presences of Anthropocenes in the present by way of bringing future worlds (The Swan Book) to the contemporary (Carpentaria). In both novels, protagonists must forge survival amongst ruins of the present and future: the depicted worlds, in particular the representations of the disenfranchisement of indigenous inhabitants of the far north of the Australian continent, emerge as a critique of the intersections of capitalist and colonial projects that define modernity and its impact on the global climate.
By using synchrotron X-ray powder diffraction, the temperature dependent phase diagram of the hybrid perovskite tri-halide compounds, methyl ammonium lead iodide (MAPbI3, MA+ = CH3NH3+) and methyl ammonium lead bromide (MAPbBr3), as well as of their solid solutions, has been established. The existence of a large miscibility gap between 0.29 ≤ x ≤ 0.92 (±0.02) for the MAPb(I1−xBrx)3 solid solution has been proven. A systematic study of the lattice parameters for the solid solution series at room temperature revealed distinct deviations from Vegard's law. Furthermore, temperature dependent measurements showed that a strong temperature dependency of lattice parameters from the composition is present for iodine rich compositions. In contrast, the bromine rich compositions show an unusually low dependency of the phase transition temperature from the degree of substitution.
HexagDLy is a Python-library extending the PyTorch deep learning framework with convolution and pooling operations on hexagonal grids. It aims to ease the access to convolutional neural networks for applications that rely on hexagonally sampled data as, for example, commonly found in ground-based astroparticle physics experiments.
Electronic health is one of the most popular applications of information and communication technologies and it has contributed immensely to health delivery through the provision of quality health service and ubiquitous access at a lower cost. Even though this mode of health service is increasingly becoming known or used in developing nations, these countries are faced with a myriad of challenges when implementing and deploying e-health services on both small and large scale. It is estimated that the Africa population alone carries the highest percentage of the world’s global diseases despite its certain level of e-health adoption. This paper aims at analyzing the progress so far and the current state of e-health in developing countries particularly Africa and propose a framework for further improvement.
SiO(2 )is the main component of silicate melts and thus controls their network structure and physical properties. The compressibility and viscosities of melts at depth are governed by their short range atomic and electronic structure. We measured the O K-edge and the Si L-2,L-3-edge in silica up to 110 GPa using X-ray Raman scattering spectroscopy, and found a striking match to calculated spectra based on structures from molecular dynamic simulations. Between 20 and 27 GPa, Si-[4] species are converted into a mixture of Si-[5] and Si-[6] species and between 60 and 70 GPa, Si-[6] becomes dominant at the expense of Si-[5] with no further increase up to at least 110 GPa. Coordination higher than 6 is only reached beyond 140 GPa, corroborating results from Brillouin scattering. Network modifying elements in silicate melts may shift this change in coordination to lower pressures and thus magmas could be denser than residual solids at the depth of the core-mantle boundary.
The aim of this paper is to discuss Nicolai Hartmann’s conception of personhood as developed in his philosophy of spiritual being. Many contemporary accounts of personhood are systematically focused on rational phenomena as self-consciousness or practical reasoning, which are understood as ‘conditions of personhood’. Apart from having some technical problems, those accounts limit our self-under-standing as persons on distinct rational properties and often fail to consider the sociocultural aspects of the personal situation. Nicolai Hartmann — although respecting the role of reason — understands personhood particularly as participation in a shared spiritual sphere called Objektiver Geist (objective spirit), which includes various intersubjective phenomena as languages, religion, moral, arts, and the
sciences. Being part of this sphere seems to be more fundamental than having distinct rational properties, which requests a spiritual frame to be exerted. Further it is shown that Hartmann’s ontology of person also includes a notion of being affected by the existential weight of situations and other person’s actions — an idea often maintained by phenomenological positions. By regarding rational, intersubjective and affective aspects, Hartmann’s philosophy of person succeeds in offering a broad articulation of our self-understanding and may also be seen as providing a background to understand certain phenomena that are part of the personal situation.
Above and underground hydrological processes depend on soil moisture (SM) variability, driven by different environmental factors that seldom are well-monitored, leading to a misunderstanding of soil water temporal patterns. This study investigated the stability of the SM temporal dynamics to different monitoring temporal resolutions around the border between two soil types in a tropical watershed. Four locations were instrumented in a small-scale watershed (5.84 km(2)) within the tropical coast of Northeast Brazil, encompassing different soil types (Espodossolo Humiluvico or Carbic Podzol, and Argissolo Vermelho-Amarelo or Haplic Acrisol), land covers (Atlantic Forest, bush vegetation, and grassland) and topographies (flat and moderate slope). The SM was monitored at a temporal resolution of one hour along the 2013-2014 hydrological year and then resampled a resolutions of 6 h, 12 h, 1 day, 2 days, 4 days, 7 days, and 15 days. Descriptive statistics, temporal variability, time-stability ranking, and hierarchical clustering revealed uneven associations among SM time components. The results show that the time-invariant component ruled SM temporal variability over the time-varying parcel, either at high or low temporal resolutions. Time-steps longer than 2 days affected the mean statistical metrics of the SM time-variant parcel. Additionally, SM at downstream and upstream sites behaved differently, suggesting that the temporal mean was regulated by steady soil properties (slope, restrictive layer, and soil texture), whereas their temporal anomalies were driven by climate (rainfall) and hydrogeological (groundwater level) factors. Therefore, it is concluded that around the border between tropical soil types, the distinct behaviour of time-variant and time-invariant components of SM time series reflects different combinations of their soil properties.
This study explores the theoretical and political potentials of Édouard Glissant’s philosophy of relation and its approach to the issues of borders, migration, and the setup of political communities as proposed by his pensée nouvelle de la frontière (new border thought), against the background of the German migration crisis of 2015. The main argument of this article is that Glissant’s work offers an alternative epistemological and normative framework through which the contemporary political issues arising around the phenomenon of repressive border regimes can be studied. To demonstrate this point, this article works with Glissant’s border thought as an analytical lens and proposes a pathway for studying the contemporary German border regime. Particular emphasis is placed on the identification of potential areas where a Glissantian politics of relation could intervene with the goal of transforming borders from impermeable walls into points of passage. By exploring the political implications of his border thought, as well as the larger philosophical context from which it emerges, while using a transdisciplinary approach that borrows from literary and political studies, this work contributes to ongoing debates in postcolonial studies on borders and borderlessness, as well as Glissant’s political legacy in the twenty-first century.
There is an ongoing discussion in the literature whether the series of sentences ‘It’s not α that did P. α and β did P.’ is acceptable or not. Whereas the homogeneity approach in Büring & Križ 2013, Križ 2016, and Križ 2017 predicts these sentences to be unacceptable, the alternative-based approach predicts acceptability depending on the predicate being interpreted distributively or non- distributively (among others, Horn 1981, Velleman et al. 2012, Renans 2016a,b). We report on three experiments testing the predictions of both types of approaches. These studies provide empirical data that not only bears on these approaches, but also allows us to distinguish between different accounts of cleft exhaustivity that might otherwise make the same predictions. The results of the three studies reported here suggest that the acceptability of clefts depends on the interpretation of the predicate, thereby posing a serious challenge to the homogeneity approach, and contributing to the ongoing discussion on the semantics of it-clefts.
Groundwater travel time distributions (TTDs) provide a robust description of the subsurface mixing behavior and hydrological response of a subsurface system. Lagrangian particle tracking is often used to derive the groundwater TTDs. The reliability of this approach is subjected to the uncertainty of external forcings, internal hydraulic properties, and the interplay between them. Here, we evaluate the uncertainty of catchment groundwater TTDs in an agricultural catchment using a 3-D groundwater model with an overall focus on revealing the relationship between external forcing, internal hydraulic properties, and TTD predictions. Eight recharge realizations are sampled from a high-resolution dataset of land surface fluxes and states. Calibration-constrained hydraulic conductivity fields (Ks fields) are stochastically generated using the null-space Monte Carlo (NSMC) method for each recharge realization. The random walk particle tracking (RWPT) method is used to track the pathways of particles and compute travel times. Moreover, an analytical model under the random sampling (RS) assumption is fit against the numerical solutions, serving as a reference for the mixing behavior of the model domain. The StorAge Selection (SAS) function is used to interpret the results in terms of quantifying the systematic preference for discharging young/old water. The simulation results reveal the primary effect of recharge on the predicted mean travel time (MTT). The different realizations of calibration-constrained Ks fields moderately magnify or attenuate the predicted MTTs. The analytical model does not properly replicate the numerical solution, and it underestimates the mean travel time. Simulated SAS functions indicate an overall preference for young water for all realizations. The spatial pattern of recharge controls the shape and breadth of simulated TTDs and SAS functions by changing the spatial distribution of particles' pathways. In conclusion, overlooking the spatial nonuniformity and uncertainty of input (forcing) will result in biased travel time predictions. We also highlight the worth of reliable observations in reducing predictive uncertainty and the good interpretability of SAS functions in terms of understanding catchment transport processes.