1,007 research outputs found

    Beyond Metaphysics:Gianni Vattimo and the meaning of hermeneutics for political theory

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    This article examines Gianni Vattimo’s contribution to the recent ontological turn in political theory. Drawing on Nietzsche and Heidegger, Vattimo offers a ‘philosophy of history’ in which strong metaphysical claims are presented as gradually being weakened, but in which the irrationalism he thinks characteristic of many anti-foundationalist theorists is also avoided. This philosophy is said to provide for new understandings of ethical and political life which have the acceptance of pluralism as their aim. The article argues that Vattimo’s attempt to identify a position beyond metaphysics on the one hand and relativism on the other is unsuccessful, and that he ought to join in with the thoroughgoing anti-foundationalism that marks the work of writers such as Rorty and Derrida. It suggests further that awareness of our historical situation need not weaken the confidence with which our beliefs are held, and does not support any particular political programme. </jats:p

    Applications of PB-210/RA-226 and PO-210/PB-210 disequilibria in the study of marine geochemical processes

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    Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution November, 1975The distribution of Pb-210 and Po-210 in dissolved (0.4 micron) phases has been measured at ten stations in the tropical and eastern North Atlantic and at two stations in the Pacific. Both radionuclides occur principally in the dissolved phase. Unsupported Pb-210 activities, maintained by flux from the atmosphere, are present in the surface mixed layer and penetrate into the thermocline to depths of about 500 m. Dissolved Po-210 is ordinarily present in the mixed layer at less than equilibrium concentrations, suggesting rapid biological removal of this nuclide. Particulate matter is enriched in Po-210, with Po-210/Pb-210 activity ratios greater than 1.0, similar to those reported for phytoplankton. Box-model calculations yield a 2-y residence time for Pb-210 and a 0.6-y residence time for Po-210 in the mixed layer. These residence times are considerably longer than the time calculated for turnover of particles in the mixed layer (about 0.1 y). At depths of 100-300 m, Po-210 maxima occur and unsupported Po-210 is frequently present. Calculations indicate that at least 50% of the Po-210 removed from the mixed layer is recycled within the thermocline. Similar calculations for Pb-210 suggest much lower recycling efficiencies. Comparison of the Pb-210 distribution with the reported distribution of Ra-226 at nearby GEOSECS. stations has confirmed the widespread existence of a Pb-210/Ra-226 disequilibrium in the deep sea. Vertical profiles of particulate Pb-210 were used to test the hypothesis that Pb-210 is removed from deepwater by in situ scavenging. With the exception of one profile taken near the Mid-Atlantic Ridge, significant vertical gradients in particulate Pb-210 concentration were not observed, and it is necessary to invoke exceptionally high particle sinking velocities (>10 m/d) to account for the inferred Pb-210 flux. It is proposed that an additional sink for Pb-210 in the deep sea must be sought. Estimates of the dissolved Pb-210/Ra-226 activity ratio at depths greater than 1,000 m range from 0.2 to 0.8 and reveal a systematic increase, in both vertical and horizontal directions, with increasing distance from the sea floor. This observation implies rapid scavenging of Pb-210 at the sediment-water interface and is consistent with a horizontal eddy diffusivity of 3-6 x 107 cm2/s. The more reactive element Po, on the other hand, shows evidence of rapid in situ scavenging. In filtered sea water, Po-210 is deficient, on the average, by ca. 10% relative to Pb-210; a corresponding enrichment is found in the particulate phase. Total inventories of Pb-210 and Po-210 over the entire water column, however, show no significant departure from secular equilibrium, and reliable estimates of particle sinking rates cannot be made.Prepared under National Science Foundation Grant GA-41061 and U.S.A.E.C. Contract AT(11-1)

    Deconstructing the ivory tower: identifying challenges of university-industry ecosystem partnerships

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    Collaboration between industry and academia necessitates the management of entrepreneurial dynamics within ecosystem contexts. However, such partnerships perpetuate numerous challenges that, without effective management, can impact upon the ecosystem as a whole. Limited research to date has addressed the challenges affecting these university-industry partnerships and ascertained their impact upon ecosystem management. This study identifies the challenges pervading university-industry partnerships across entrepreneurial ecosystems, with a view that through an exposition of such challenges, more specific strategies could be implemented to address them. Questionnaires were distributed to key ecosystem stakeholders, requesting their perceptions of the key challenges affecting their collaborative relationships. Empirical data was analysed utilising fuzzy-set qualitative comparative analysis to deduce the configurational nature of the conditions. Results reveal mutually exclusive solutions grounded upon distinct combinations of conditions, constituting distinct pathways to ineffective ecosystem management. Theoretical and practical implications are discussed, as well as acknowledged limitations of this study and suggestions for future research

    Coarse embeddings of graphs into Hilbert space

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    In this paper, we study coarse embeddings of graphs into Hilbert space. For a graph &Gamma expressible as an infinite union of coarsely embeddable subgraphs, &Gammai, we prove that if the nerve of the covering of &Gamma by the &Gammai is a tree and any nonempty intersections of the subgraphs have universally bounded diameter then &Gamma is coarsely embeddable into a Hilbert space

    2,6-Diacetylpyridine-resorcinol (1/1)

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    The title co-crystal, C9H9NO2·C6H6O2, is composed of one 2,6-diacetylpyridine molecule and one resorcinol molecule as the asymmetric unit. In the 2,6-diacetylpyridine molecule, the two carbonyl groups are antiperiplanar to the pyridine N atom. In the crystal, the 2,6-diacetylpyridine and resorcinol molecules are connected by two O-H...O hydrogen bonds, forming planar chains of alternating components running along [120]

    Density mapping with weak lensing and phase information

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    The available probes of the large scale structure in the Universe have distinct properties: galaxies are a high resolution but biased tracer of mass, while weak lensing avoids such biases but, due to low signal-to-noise ratio, has poor resolution. We investigate reconstructing the projected density field using the complementarity of weak lensing and galaxy positions. We propose a maximum-probability reconstruction of the 2D lensing convergence with a likelihood term for shear data and a prior on the Fourier phases constructed from the galaxy positions. By considering only the phases of the galaxy field, we evade the unknown value of the bias and allow it to be calibrated by lensing on a mode-by-mode basis. By applying this method to a realistic simulated galaxy shear catalogue, we find that a weak prior on phases provides a good quality reconstruction down to scales beyond l=1000, far into the noise domain of the lensing signal alone.Comment: 11 pages, 9 figures, published in MNRA
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