Miḳraʾot gedolot : ʻim 32 perushim = Mikraet gedalet, t.e., Sv. Pisanı̄e s kommentarı̄i︠a︡mi.

Vols. 2-6, 8 published by V. b. Z. Yaʻbets and Y. L. Shṭain, v. 7 published by N. Shrifṭgiser, v. 12 printed by Y. Goldman.

Midrash Shoḥer ṭov ʻal Tehilim = Midrash Tegilim : s komentarʹem ; Midrash Shoḥer ṭov ʻal Shemuʾel u-Mishle = Midrash shokher tovʹ : s komentarı̄i /

Mode of access: Internet.

Augusti Pfeiferi D. Critica sacra, : de sacri codicis partitione, editionibus variis, lingvis originalibus & illibatâ puritate fontium, interpretatione scripturae legitima, nec non ejusdem : Translatione in lingvas totius universi de Masora & Kabbala, Talmude deniq; & Alcorano. : Accessere, suisq locis inserti, Tractatus qvatuor, I. De antiqvis ritibus Ebraeorum. II. De natura, usu & subsidiis lingvarum orientalium omnium. III. De compendiaria ratione legendi scripta rabbinico-talmudica. IV. De accentuatione tàm prosaica qvàm metrica facilè discenda.

Includes index.

Opīsanie rukopiseĭ biblīoteki Viḟanskoĭ dukhovnoĭ seminarīi. (S prilozhenīi︠a︡mi)

The supplements contain congratulatory poems and correspondence between members of the imperial family and the metropolitans Platon and Augustin.

The great commentary of Cornelius à Lapide /

[v. 1] S. Matthew's gospel--chaps. I-IX -- [v. 2] S. Matthew's gospel-- chaps. X to XXI -- [v. 3] S. Matthew's gospel--chaps. XXII to XXVIII. S. Mark's gospel--complete -- [v. 4] S. Luke's gospel -- [v. 5] S. John's gospel--chaps. I to XI -- [v. 6] S. John's gospel--chaps. XII to XXI and epistles I, II, and III.

La "Lectura ordinaria super sacram scripturam," attribuʹee à Henri de Gand. Introductio generalis ad sacram scripturam. Introductio generalis ad genesim. Expositio trium primorum capitulorum genesis.

"Attribution de lo̕uvrage à Henri de Gand dans le MS. Paris, Nat. lat. 15355, au f. 251v." Cf. also L. Delisle. Inventaire . . . Sorbonne, 1870.

Ksįega pamįatkow XI

Mode of access: Internet.

Na 1 Nachlass Max Horkheimer, 803 - "Dialektik der Aufklärung" von Max Horkheimer und Theodor W. Adorno (p. XI 6.43 - XI 6.106)

43. - 62. Sammlung B: "Konzepte als Zugabe zur Festschrift für Friedrich Pollock" [GS 12, S. 250 - 295]. 64 Blatt; 43. "Zum Problem der Bedürfnisse". Typoskript, 6 Blatt; 44. "Dichtung und Moral". Typoskript, 5 Blatt; 45. "Geschichte der amerikanischen Arbeiterschaft". Typoskript, 1 Blatt; 46. "Kein Weg zur Wahrheit". Typoskript, 1 Blatt; 47. "Zur Rechtsphilosophie". Typoskript mit eigenen Korrekturen, 2 Blatt; 48. "Strafgefangene". Typoskript, 1 Blatt; 49. "Jüdischer Charakter". Typoskript, 1 Blatt; 50. "Solidarität". Typoskript, 2 Blatt; 51. "Unmöglichkeit der Dichtung". Typoskript, 1 Blatt; 52. "Theorie des Verbrechers". Typoskript, 14 Blatt; 53. "Erbsünde und Kopula". Typoskript, 2 Blatt; 54. "Feind". Typoskript, 2 Blatt; 55. "Haupt- und Nebensatz". Typoskript, 3 Blatt; 56. "Bewußtsein". Typoskript, 1 Blatt; 57. "Kampf und Gewaltlosigkeit". Typoskript, 6 Blatt; 58. "Umschlag der idealistischen Dialektik". Typoskript, 1 Blatt; 59. "Die Rackets und der Geist". Typoskript, 7 Blatt; 60. "Altmodische Probleme". Typoskript mit eigenen Korrekturen, 2 Blatt; 61. "Physiognomik". Typoskript, 1 Blatt; 62. "Religionspsychologie". Typoskript, 2 Blatt; 63. - 106. Sammlung C: "New Yorker Notizen [I]"; 63. "Dialektik der Aufklärung Nr. 7". Typoskript mit eigenen Korrekturen, 12 Blatt; 64. Aus der "Dialektik der Aufklärung"; Kapitel: "Elemente des Antisemitismus", Abschitt VII:; 64a) Typoskript mit eigenen Korrekturen, 11 Blatt; 64b) Teilstück, Typoskript, 2 Blatt; 64c) Teilstück, Typoskript, 1 Blatt; 64d) Teilstück, Typoskript, 1 Blatt; 65. "Bemerkungen zu These VII" [zu: 64]; Über Antisemitismus und Stalinismus, [von Theodor W. Adorno]. Typoskript, 3 Blatt; 66. "Verwandlung der Idee in Gesinnung":; 66a) Typoskript, 5 Blatt; 66b) Typoskript mit eigenen Korrekturen, 4 Blatt; 66c) Typoskript, 5 Blatt; 67. "Zum Problem der Bedürfnisse". Typoskript mit eigenen Korrekturen, 6 Blatt; 68. "Dichtung und Moral":; 68a) Typoskript, 5 Blatt; 68b) Typoskript mit eigenen Korrekturen, 4 Blatt; 68c) Typoskript mit eigenen Korrekturen, 4 Blatt; 68d) Typoskript mit eigenen Korrekturen, 5 Blatt; 69. "Geschichte der amerikanischen Arbeiterschaft":; 69a) Typoskript, 1 Blatt; 69b) Typoskript; 1 Blatt; 70. "Straftheorie. Zur Rechtsphilosophie":; 70a) Typoskript mit eigenen Korrekturen, 3 Blatt; 70b) Typoskript mit eigenen Korrekturen, 3 Blatt; 70c) Typoskript mit eigenen Korrekturen, 3 Blatt; 70d) Typoskript, 3 Blatt; 71. "Jüdischer Charakter". Typoskript, 1 Blatt; 72. "Solidarität". Typoskript, 2 Blatt; 73. "Theorie des Verbrechens". Typoskript mit eigenen Korrekturen, 17 Blatt; 74. "Erbsünde und Copula":; 74a) Typoskript, 2 Blatt; 74b) Typoskript mit eigenen Korrekturen, 3 Blatt; 75. "Geschichtsphilosophischer Exkurs zur Odysee" [von Theodor W. Adorno ?]. Teilstück, Typoskript, 1 Blatt; 76. "Feind":; 76a) Typoskript, 2 Blatt; 76b) Typoskript, 2 Blatt; 76c) Typoskript, 2 Blatt; 76d) Entwurf, englisch, Typoskript mit eigenen Korrekturen, 2 Blatt; 77. "Haupt- und Nebensatz":; 77a) Typoskript, 2 Blatt; 77b) Typoskript mit eigenen Korrekturen, 2 Blatt; 77c) Typoskript mit eigenen Korrekturen, 2 Blatt; 77d) Typoskript mit eigenen Korrekturen, 3 Blatt; 78. "Bewußtsein":; 78a) Typoskript, 1 Blatt; 78b) Typoskript mit eigenen Korrekturen, 1 Blatt; 79. "Kampf und Gewaltlosigkeit":; 79a) Typoskript, 6 Blatt; 79b) Typoskript, 6 Blatt; 79c) Teilstücke, Typoskript mit eigenen Korrekturen, 6 Blatt; 79d) Typoskript mit eigenen Korrekturen, 5 Blatt; 79e) Typoskript, 5 Blatt; 79f) Teilstück, Typoskript mit eigenen Korrekturen, 2 Blatt; 80. "Die Rackets und der Geist":; 80a) Typoskript mit eigenen Korrekturen, 2 Blatt; 80b) Typoskript mit eigenen Korrekturen, 6 Blatt; 81. "Altmodisches Problem". Typoskript, 2 Blatt; 82. "Physiognomik". Typoskript, 1 Blatt; 83. "Religionspsychologie":; 83a) Typoskript mit eigenen Korrekturen, 2 Blatt; 83b) Typoskript mit eigenen Korrekturen, 2 Blatt; 84. "Leeres Erschrecken":; 84a) Typoskript mit eigenen Korrekturen, 2 Blatt; 84b) Typoskript, 2 Blatt; 84c) Typoskript mit eigenen Korrekturen, 2 Blatt; 85. "Philosophie und Arbeitsteilung":; 85a) Typoskript mit eigenen Korrekturen, 3 Blatt; 85b) Typoskript mit eigenen Korrekturen, 3 Blatt; 85c) Typoskript, 3 Blatt; 85d) Typoskript mit handschriftlichen Korrekturen, 3 Blatt; 86. "Vorrede" zur Dialektik der Aufklärung. Typoskript mit eigenen Korrekturen, 11 Blatt; 87. ["Umschlag der idealistischen Dialektik"] Typoskript, 1 Blatt; 88. Über Erkenntnis und Sprache. Typoskript mit eigenen Korrekturen, 1 Blatt; 89. "Zur Kritik der Geschichtsphilosophie". Typoskript mit eigenen Korrekturen, 3 Blatt; 90. "Mensch und Tier":; 90a) Typoskript mit eigenen und handschriftlichen Korrekturen, 12 Blatt; 90b) Typoskript mit eigenen Korrekturen, 3 Blatt; 90c) Typoskript mit eigenen Korrekturen, 4 Blatt; 90d) Typoskript mit eigenen Korrekturen, 3 Blatt; 90e) Typoskript mit eigenen Korrekturen, 10 Blatt; 91. "Massengesellschaft". Typoskript, 1 Blatt; 92. "Zwei Welten". Typoskript, 2 Blatt; 93. "Zur Theorie der Gespenster":; 93a) Typoskript, 1 Blatt; 93b) Typoskript mit eigenen Korrekturen, 1 Blatt; 94. "Interesse am Körper":; 94a) Typoskript mit eigenen Korrekturen, 6 Blatt; 94b) Typoskript mit eigenen Korrekturen, 7 Blatt; 94c) Typoskript, 2 Blatt; 94d) Typoskript, 6 Blatt; 95. "Unmöglichkeit der Dichtung". Typoskript, 1 Blatt; 96. "Die Einseitigkeit der Negativität":; 96a) Typoskript, 2 Blatt; 96b) Typoskript mit eigenen Korrekturen, 2 Blatt; 96c) Typoskript, 2 Blatt; 97. "Widersprüche":; 97a) Typoskript, 4 Blatt; 97b) Typoskript mit eigenen Korrekturen, 4 Blatt; 98. "Zur Theorie der Dummheit":; 98a) Typoskript, 3 Blatt; 98b) Typoskript mit eigenen Korrekturen, 3 Blatt.; 99. "Gezeichnet". Typoskript, 2 Blatt; 100. "Quand-même":; 100a) Typoskript, 2 Blatt; 100b) Typoskript mit eigenen Korrekturen, 2 Blatt; 101. "Isolierung durch Verkehr":; 101a) Typoskript mit eigenen Korrekturen, 1 Blatt; 101b) Typoskript, 1 Blatt; 102. "Gegen Gescheitheit". Typoskript mit eigenen Korrekturen, 1 Blatt; 103. "Propaganda":; 103a) Typoskript mit eigenen Korrekturen, 2 Blatt; 103b) Typoskript, 2 Blatt; 103c) Typoskript mit eigenen Korrekturen, 2 Blatt; 104. "Der Gedanke". Typoskript mit eigenen Korrekturen, 1 Blatt; 105. Fragment aus der "Dialektik der Aufklärung", Exkurs II. Typoskript mit eigenen Korrekturen, 3 Blatt; 106. Zum Begriff des Individuums bei Leibniz und Hegel [GS 12, S. 314 - 315]. Typoskript mit eigenen Korrekturen, 2 Blatt;

A CFD study of biomass pyrolysis in a downer reactor equipped with a novel gas-solid separator - I:hydrodynamic performance

This study presents the first part of a CFD study on the performance of a downer reactor for biomass pyrolysis. The reactor was equipped with a novel gas-solid separation method, developed by the co-authors from the ICFAR (Canada). The separator, which was designed to allow for fast separation of clean pyrolysis gas, consisted of a cone deflector and a gas exit pipe installed inside the downer reactor. A multi-fluid model (Eulerian-Eulerian) with constitutive relations adopted from the kinetic theory of granular flow was used to simulate the multiphase flow. The effects of the various parameters including operation conditions, separator geometry and particle properties on the overall hydrodynamics and separation efficiency were investigated. The model prediction of the separator efficiency was compared with experimental measurements. The results revealed distinct hydrodynamic features around the cone separator, allowing for up to 100% separation efficiency. The developed model provided a platform for the second part of the study, where the biomass pyrolysis is simulated and the product quality as a function of operating conditions is analyzed. Crown Copyright © 2014 Published by Elsevier B.V. All rights reserved.

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

Compilation of planktonic foraminiferal census counts from the Southern Hemisphere Oceans

We present an improved database of planktonic foraminiferal census counts from the Southern Hemisphere Oceans (SHO) from 15°S to 64°S. The SHO database combines 3 existing databases. Using this SHO database, we investigated dissolution biases that might affect faunal census counts. We suggest a depth/[DCO3]2- threshold of ~3800 m/[DCO3]2- = ~-10 to -5 µmol/kg for the Pacific and Indian Oceans, and ~4000 m/[DCO3]2- = ~0 to 10 µmol/kg for the Atlantic Ocean, under which core-top assemblages can be affected by dissolution and are less reliable for paleo-sea surface temperature (SST) reconstructions. We removed all core-tops beyond these thresholds from the SHO database. This database has 598 core-tops and is able to reconstruct past SST variations from 2° to 25.5°C, with a root mean square error of 1.00°C, for annual temperatures. To inspect dissolution affects SST reconstruction quality, we tested the data base with two "leave-one-out" tests, with and without the deep core-tops. We used this database to reconstruct Summer SST (SSST) over the last 20 ka, using the Modern Analog Technique method, on the Southeast Pacific core MD07-3100. This was compared to the SSST reconstructed using the 3 databases used to compile the SHO database. Thus showing that the reconstruction using the SHO database is more reliable, as its dissimilarity values are the lowest. The most important aspect here is the importance of a bias-free, geographic-rich, database. We leave this dataset open-ended to future additions; the new core-tops must be carefully selected, with their chronological frameworks, and evidence of dissolution assessed.

Role of metalliferous mudstones and graphitic shales in the location, genesis, and paleoenvironment

The Cambrian Tally Pond volcanic belt in central Newfoundland contains numerous volcanogenic massive sulphide (VMS) deposits, prospects, and showings that are locally associated with metalliferous mudstones and/or graphitic shales. Deposits in the belt are bimodal felsic-type VMS that are both base metal- (e.g., Duck Pond, Boundary) and precious metal-enriched (e.g., Lemarchant). At the Lemarchant deposit metalliferous mudstones are genetically and spatially associated with mineralization, whereas the relationship of other mudstones and shales to massive sulphide mineralization is more intricate and remains not fully understood. Metalliferous mudstones represent a hiatus in the volcanic activity where the deposition of hydrothermal products dominated over the abiogenic background sedimentation and/or dilution by volcaniclastic-epiclastic material. Lithogeochemical signatures allow one to distinguish between predominantly hydrothermally or detritally (i.e., non-hydrothermal) derived material. Metalliferous mudstones with a significant hydrothermal component, like those at Lemarchant, have elevated Fe/Al and base-metal contents, compared to detrital shales, and shale-normalized negative Ce and positive Eu anomalies, indicative of deposition from high temperature (>250°C) hydrothermal fluids within an oxygenated water column. Mudstones and shales sampled from other locations in the Tally Pond volcanic belt have more variable signatures ranging from hydrothermal (signatures as above) to non-hydrothermal (no positive Eu-anomalies, flat REE patterns), with some that have mixed (hydrothermal and detrital) signatures. Both S and Pb isotopic compositions indicate that proximal sulphides hosted in mudstones immediately associated with massive sulphide mineralization within the Lemarchant deposit contain a higher proportion of sulphur derived from hydrothermal sources and processes, and have more juvenile lead contributions, when compared to sulphides distal (not associated with massive sulphides) from mineralization. Lead and Nd isotopic compositions of both whole rock and minerals in the Lemarchant mudstones indicate involvement of underlying crustal basement during massive sulphide formation and throughout the evolution of the Tally Pond belt. Metalliferous mudstones precipitated early in the massive sulphide depositional history, but also have undergone syn- and post-ore-forming processes and have a larger lateral extent than the mineralization. Using lithogeochemistry, whole rock and in situ stable and radiogenic isotopes it is possible to distinguish prospective vent proximal (immediately associated with massive sulphide mineralization) from less prospective distal (not associated with massive sulphides) depositional environments and to reconstruct the paleotectonic setting on a deposit- to regional-scale for the Lemarchant deposit and other mudstone-associated prospects in the Tally Pond volcanic belt.

Genesis and character of thin-bedded turbidites associated with submarine channels

Acknowledgements We acknowledge the support of the PRACSS Joint Industry Project at University of Aberdeen, funded by BG Group, BP, DONG, RWE Dea, Petrochina, Statoil and Tullow Oil. We also acknowledge the entire crew of the Urania Research vessel which was used to acquire the CHIRP lines, bathymetric data and gravity cores from the Tyrrhenian Sea, Italy. Our colleagues Michal Janocko and Mike Mayall are thanked for the discussions and comments. Our colleagues Pan Li, Amanda Santa Catharina, Guilherme Bozetti and Matheus Silveira Sobiesiak are thanked for their assistance during field work where some of the ideas in this paper were synthesized. Finally we thank one anonymous reviewer and Brian Romans for their invaluable feedback which made some of the ideas introduced in this review much more succinct.