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Managing the Boundaries of Taste: Culture, Valuation, and Computational Social Science* Ryan Light University of Oregon Colin Od
Managing the Boundaries of Taste: Culture, Valuation, and Computational Social Science* Ryan Light University of Oregon Colin Odden Ohio State University Ohio Colleges of Medicine This is a pre-copyedited, author-produced version of an article accepted for publication in Social Forces following peer review. The version of record is available online at: https://doi.org/10.1093/sf/sox055. *Please direct all correspondence to Ryan Light, [email protected]. The authors thank James Moody, Jill Ann Harrison, Matthew Norton, Brandon Stewart, Achim Edelmann, Clare Rosenfeld Evans, Jordan Besek, and Brian Ott for their helpful comments on earlier drafts of this paper. Managing the Boundaries of Taste: Culture, Valuation, and Computational Social Science Abstract The proliferation of cultural objects, such as music, books, film and websites, has created a new problem: How do consumers determine the value of cultural objects in an age of information glut? Crowd-sourcing – paralleling word-of-mouth recommendations – has taken center stage, yet expert opinion has also assumed renewed importance. Prior work on the valuation of artworks and other cultural artifacts identifies ways critics establish and maintain classificatory boundaries, such as genre. We extend this research by offering a theoretical approach emphasizing the dynamics of critics’ valuation and classification. Empirically, this analysis turns to Pitchfork.com, an influential music review website, to examine the relationship between classification and valuation. Using topic models of fourteen years of Pitchfork.com album reviews (n=14,495), we model the dynamics of valuation through genre and additional factors predictive of positive reviews and cultural consecration. We use gold record awards to study the relationship between valuation processes and commercial outcomes. -
Ice Ic” Werner F
Extent and relevance of stacking disorder in “ice Ic” Werner F. Kuhsa,1, Christian Sippela,b, Andrzej Falentya, and Thomas C. Hansenb aGeoZentrumGöttingen Abteilung Kristallographie (GZG Abt. Kristallographie), Universität Göttingen, 37077 Göttingen, Germany; and bInstitut Laue-Langevin, 38000 Grenoble, France Edited by Russell J. Hemley, Carnegie Institution of Washington, Washington, DC, and approved November 15, 2012 (received for review June 16, 2012) “ ” “ ” A solid water phase commonly known as cubic ice or ice Ic is perfectly cubic ice Ic, as manifested in the diffraction pattern, in frequently encountered in various transitions between the solid, terms of stacking faults. Other authors took up the idea and liquid, and gaseous phases of the water substance. It may form, attempted to quantify the stacking disorder (7, 8). The most e.g., by water freezing or vapor deposition in the Earth’s atmo- general approach to stacking disorder so far has been proposed by sphere or in extraterrestrial environments, and plays a central role Hansen et al. (9, 10), who defined hexagonal (H) and cubic in various cryopreservation techniques; its formation is observed stacking (K) and considered interactions beyond next-nearest over a wide temperature range from about 120 K up to the melt- H-orK sequences. We shall discuss which interaction range ing point of ice. There was multiple and compelling evidence in the needs to be considered for a proper description of the various past that this phase is not truly cubic but composed of disordered forms of “ice Ic” encountered. cubic and hexagonal stacking sequences. The complexity of the König identified what he called cubic ice 70 y ago (11) by stacking disorder, however, appears to have been largely over- condensing water vapor to a cold support in the electron mi- looked in most of the literature. -
A Primer on Ice
A Primer on Ice L. Ridgway Scott University of Chicago Release 0.3 DO NOT DISTRIBUTE February 22, 2012 Contents 1 Introduction to ice 1 1.1 Lattices in R3 ....................................... 2 1.2 Crystals in R3 ....................................... 3 1.3 Comparingcrystals ............................... ..... 4 1.3.1 Quotientgraph ................................. 4 1.3.2 Radialdistributionfunction . ....... 5 1.3.3 Localgraphstructure. .... 6 2 Ice I structures 9 2.1 IceIh........................................... 9 2.2 IceIc........................................... 12 2.3 SecondviewoftheIccrystalstructure . .......... 14 2.4 AlternatingIh/Iclayeredstructures . ........... 16 3 Ice II structure 17 Draft: February 22, 2012, do not distribute i CONTENTS CONTENTS Draft: February 22, 2012, do not distribute ii Chapter 1 Introduction to ice Water forms many different crystal structures in its solid form. These provide insight into the potential structures of ice even in its liquid phase, and they can be used to calibrate pair potentials used for simulation of water [9, 14, 15]. In crowded biological environments, water may behave more like ice that bulk water. The different ice structures have different dielectric properties [16]. There are many crystal structures of ice that are topologically tetrahedral [1], that is, each water molecule makes four hydrogen bonds with other water molecules, even though the basic structure of water is trigonal [3]. Two of these crystal structures (Ih and Ic) are based on the same exact local tetrahedral structure, as shown in Figure 1.1. Thus a subtle understanding of structure is required to differentiate them. We refer to the tetrahedral structure depicted in Figure 1.1 as an exact tetrahedral structure. In this case, one water molecule is in the center of a square cube (of side length two), and it is hydrogen bonded to four water molecules at four corners of the cube. -
Table of Contents (Online, Part 1)
TM PERIODICALS PHYSICALREVIEWE Postmaster send address changes to: For editorial and subscription correspondence, please see inside front cover APS Subscription Services (ISSN: 2470-0045) P.O. Box 41 Annapolis Junction, MD 20701 THIRD SERIES, VOLUME 101, NUMBER 5 CONTENTS MAY 2020 PARTS A AND B The Table of Contents is a total listing of Parts A and B. Part A consists of pages 050101(R)–052320, and Part B pages 052401–059902(E). PART A RAPID COMMUNICATIONS Statistical Physics Measurability of nonequilibrium thermodynamics in terms of the Hamiltonian of mean force (6 pages) ......... 050101(R) Philipp Strasberg and Massimiliano Esposito Nonlinear Dynamics and Chaos Observation of accelerating solitary wavepackets (6 pages) ............................................... 050201(R) Georgi Gary Rozenman, Lev Shemer, and Ady Arie Networks and Complex Systems Kinetic roughening of the urban skyline (5 pages) ....................................................... 050301(R) Sara Najem, Alaa Krayem, Tapio Ala-Nissila, and Martin Grant Liquid Crystals Phase transitions of heliconical smectic-C and heliconical nematic phases in banana-shaped liquid crystals (4 pages) ................................................................................... 050701(R) Akihiko Matsuyama Granular Materials Two mechanisms of momentum transfer in granular flows (5 pages) ........................................ 050901(R) Matthew Macaulay and Pierre Rognon Direct measurement of force configurational entropy in jamming (5 pages) .................................. 050902(R) James D. Sartor and Eric I. Corwin Plasma Physics X-ray heating and electron temperature of laboratory photoionized plasmas (6 pages)......................... 051201(R) R. C. Mancini, T. E. Lockard, D. C. Mayes, I. M. Hall, G. P. Loisel, J. E. Bailey, G. A. Rochau, J. Abdallah, Jr., I. E. Golovkin, and D. Liedahl Copyright 2020 by American Physical Society (Continued) 2470-0045(202005)101:5:A;1-8 The editors and referees of PRE find these papers to be of particular interest, importance, or clarity. -
Arxiv:2004.08465V2 [Cond-Mat.Stat-Mech] 11 May 2020
Phase equilibrium of liquid water and hexagonal ice from enhanced sampling molecular dynamics simulations Pablo M. Piaggi1 and Roberto Car2 1)Department of Chemistry, Princeton University, Princeton, NJ 08544, USA a) 2)Department of Chemistry and Department of Physics, Princeton University, Princeton, NJ 08544, USA (Dated: 13 May 2020) We study the phase equilibrium between liquid water and ice Ih modeled by the TIP4P/Ice interatomic potential using enhanced sampling molecular dynamics simulations. Our approach is based on the calculation of ice Ih-liquid free energy differences from simulations that visit reversibly both phases. The reversible interconversion is achieved by introducing a static bias potential as a function of an order parameter. The order parameter was tailored to crystallize the hexagonal diamond structure of oxygen in ice Ih. We analyze the effect of the system size on the ice Ih-liquid free energy differences and we obtain a melting temperature of 270 K in the thermodynamic limit. This result is in agreement with estimates from thermodynamic integration (272 K) and coexistence simulations (270 K). Since the order parameter does not include information about the coordinates of the protons, the spontaneously formed solid configurations contain proton disorder as expected for ice Ih. I. INTRODUCTION ture forms in an orientation compatible with the simulation box9. The study of phase equilibria using computer simulations is of central importance to understand the behavior of a given model. However, finding the thermodynamic condition at II. CRYSTAL STRUCTURE OF ICE Ih which two or more phases coexist is particularly hard in the presence of first order phase transitions. -
Indiana Glaciers.PM6
How the Ice Age Shaped Indiana Jerry Wilson Published by Wilstar Media, www.wilstar.com Indianapolis, Indiana 1 Previiously published as The Topography of Indiana: Ice Age Legacy, © 1988 by Jerry Wilson. Second Edition Copyright © 2008 by Jerry Wilson ALL RIGHTS RESERVED 2 For Aaron and Shana and In Memory of Donna 3 Introduction During the time that I have been a science teacher I have tried to enlist in my students the desire to understand and the ability to reason. Logical reasoning is the surest way to overcome the unknown. The best aid to reasoning effectively is having the knowledge and an understanding of the things that have previ- ously been determined or discovered by others. Having an understanding of the reasons things are the way they are and how they got that way can help an individual to utilize his or her resources more effectively. I want my students to realize that changes that have taken place on the earth in the past have had an effect on them. Why are some towns in Indiana subject to flooding, whereas others are not? Why are cemeteries built on old beach fronts in Northwest Indiana? Why would it be easier to dig a basement in Valparaiso than in Bloomington? These things are a direct result of the glaciers that advanced southward over Indiana during the last Ice Age. The history of the land upon which we live is fascinating. Why are there large granite boulders nested in some of the fields of northern Indiana since Indiana has no granite bedrock? They are known as glacial erratics, or dropstones, and were formed in Canada or the upper Midwest hundreds of millions of years ago. -
LAZ Update Request Nonteks 7-2020
Request to Update Content Not Reviewed and Approved by the State Review Panel Proclamation Year: 2019 Publisher: Learning A-Z, LLC Subject Area /Course: English Language Arts and Reading Program Information: Program Title: Raz-Plus ELL Texas Edition Program Title: 9 7 8 0 6 9 2 1 9 6 5 4 0 Identical Raz-Plus ELL Texas Edition Program Title: Identical 9 7 8 0 6 9 2 1 9 6 5 4 0 Program ISBN: Component Information You must submit a separate form for each component title and ISBN. Component Raz Plus ELL Texas Edition Title: Component 9 7 8 0 6 9 2 1 9 6 5 4 0 ISBN: Identical component Raz-Plus ELL Texas Edition Title: Identical Component 9 7 8 0 6 9 2 1 9 6 5 4 0 ISBN: Request to Update Content Not Reviewed and Approved by the State Review Panel Access Information Use the table below to provide access information to the adopted version of the instructional materials and the proposed new content. URL Username Password Adopted www.raz-plus.com TXREV2 RAZPLUS2 content: New content: www.raz-plus.com txadoption Learning123 Publisher’s rationale for the update The updates provide minor updates and corrections, additional leveled text, passages, and resources to expand the program’s content library. See the attached spreadsheet for a list of all new material. Side-by-side comparison: Any content that has been changed in the component listed on the previous page should be documented in this side-by-side comparison. You must submit a separate request for each component. -
1000 Klassiekers 2019
1000 Klassiekers © 2019 RADIO 2 / www.radio2.be Deze lijst is alleen voor persoonlijk gebruik. Deze lijst mag gepubliceerd worden op het internet of in een ander medium, mits een verwijzing naar www.radio2.be. Herbeluister onze lijst op Spotify: Radio 2 | 1000 Klassiekers | 2019 Wat betekenen de icoontjes? w Nieuw in de 1000 Klassiekers vanaf dit jaar p Gestegen in de 1000 Klassiekers in vergelijking met vorig jaar q Gedaald in de 1000 Klassiekers in vergelijking met vorig jaar F Ex-aequo in de lijst in vergelijking met de 1000 Klassiekers van vorig jaar P Dit nummer stond eerder reeds in de 1000 Klassiekers, maar vorig jaar niet. Dit jaar komt het nummer opnieuw binnen. Nr. UitzendingARTIEST TITEL 1000 q 26/12 6-7 10 CC The Wall Street shuffle 999 w 26/12 6-7 DORIS DAY Whatever will be, will be 998 q 26/12 6-7 ALPHAVILLE Big in Japan 997 q 26/12 6-7 ARMAND Ben ik te min 996 P 26/12 6-7 CLIFF RICHARD We don't talk anymore 995 P 26/12 6-7 3 DOORS DOWN Kryptonite 994 q 26/12 6-7 BOB DYLAN Sara 993 q 26/12 6-7 BRAM VERMEULEN Rode Wijn 992 q 26/12 6-7 ABBA Knowing me, knowing you 991 q 26/12 6-7 DAVE BERRY This strange effect 990 q 26/12 6-7 BLONDIE Atomic 989 q 26/12 6-7 SMOKIE Lay back in the arms of someone 988 w 26/12 6-7 BELLE PEREZ Que viva la vida 987 q 26/12 6-7 BARRY WHITE Let the music play 986 q 26/12 6-7 BOUDEWIJN DE GROOT Als de rook om je hoofd is verdwenen 985 q 26/12 7-8 CLIFF RICHARD & THE YOUNG ONES Living doll 984 q 26/12 7-8 CHICAGO If you leave me now 983 q 26/12 7-8 BRYAN ADAMS Please forgive me 982 q 26/12 7-8 DAVID BOWIE Life on Mars 981 q 26/12 7-8 ENYA Orinoco flow 980 q 26/12 7-8 V.O.F. -
Genesis and Geographical Aspects of Glaciers - Vladimir M
HYDROLOGICAL CYCLE – Vol. IV - Genesis and Geographical Aspects of Glaciers - Vladimir M. Kotlyakov GENESIS AND GEOGRAPHICAL ASPECTS OF GLACIERS Vladimir M. Kotlyakov Institute of Geography, Russian Academy of Sciences, Moscow, Russia Keywords: Chionosphere, cryosphere, equilibrium line, firn line, glacial climate, glacier, glacierization, glaciosphere, ice, seasonal snow line, snow line, snow-patch Contents 1. Introduction 2. Properties of natural ice 3. Cryosphere, glaciosphere, chionosphere 4. Snow-patches and glaciers 5. Basic boundary levels of snow and ice 6. Measures of glacierization 7. Occurrence of glaciers 8. Present-day glacierization of the Arctic Glossary Bibliography Biographical Sketch Summary There exist ten crystal variants of ice and one amorphous form in Nature, however only one form ice-1 is distributed on the Earth. Ten other ice variants steadily exist only under a certain combinations of pressure, specific volume and temperature of medium, and those are not typical for our planet. The ice density is less than that of water by 9%, and owing to this water reservoirs are never totally frozen., Thus life is sustained in them during the winter time. As a rule, ice is much cleaner than water, and specific gas-ice compounds called as crystalline hydrates are found in ice. Among the different spheres surrounding our globe there are cryosphere (sphere of the cold), glaciosphere (sphere of snow and ice) and chionosphere (that part of the troposphere where the annual amount of solid precipitation exceeds their losses). The chionosphere envelopes the Earth with a shell 3 to 5 km in thickness. In the present epoch, snow and ice cover 14.2% of the planet’s surface and more than half of the land surface. -
Liquid Pre-Freezing Percolation Transition to Equilibrium Crystal-In-Liquid Mesophase
http://www.scirp.org/journal/ns Natural Science, 2018, Vol. 10, (No. 7), pp: 247-262 Liquid Pre-Freezing Percolation Transition to Equilibrium Crystal-in-Liquid Mesophase Leslie V. Woodcock Department of Physics, University of Algarve, Faro, Portugal Correspondence to: Leslie V. Woodcock, Keywords: Liquid State, Percolation, Phase Transition, Pre-Freezing Mesophase Received: May 25, 2018 Accepted: June 23, 2018 Published: July 23, 2018 Copyright © 2018 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY 4.0). http://creativecommons.org/licenses/by/4.0/ Open Access ABSTRACT Pre-freezing anomalies are explained by a percolation transition that delineates the exis- tence of a pure equilibrium liquid state above the temperature of 1st-order freezing to the stable crystal phase. The precursor to percolation transitions are hetero-phase fluctuations that give rise to molecular clusters of an otherwise unstable state in the stable host phase. In-keeping with the Ostwald’s step rule, clusters of a crystalline state, closest in stability to the liquid, are the predominant structures in pre-freezing hetero-phase fluctuations. Evi- dence from changes in properties that depend upon density and energy fluctuations suggests embryonic nano-crystallites diverge in size and space at a percolation threshold, whence a colloidal-like equilibrium is stabilized by negative surface tension. Below this transition temperature, both crystal and liquid states percolate the phase volume in an equilibrium state of dispersed coexistence. We obtain a preliminary estimate of the prefreezing percola- tion line for water determined from higher-order discontinuities in Gibbs energy that de- rivatives the isothermal rigidity [(dp/dρ)T] and isochoric heat capacity [(dU/dT)v] respec- tively. -
O X Fo Rd Reading Cir C
7 SECOND EDITION EADIN R G D C R I O R F C L X E O N H I C G H R O U L B A S S R H O O H R R E S B A I U R G H • C L Teaching Guide 1 Contents Introduction iv 1. The Secret of Seaview Cottage 1 2. Cat 8 3. Meet Tom Sawyer 13 4. The Tide Rises, the Tide Falls 20 5. A Drive in the Motor Car 25 6. Nicholas Nye 33 7. My Big Brother 38 8. Ode to Autumn 46 9. A Little Princess 52 10. An Ode to the Rain 60 11. The Long Exile 66 12. English is Tough 72 13. The Valley Of Spiders 77 14. Night Mail 83 15. The Yellow Face 90 16. Matilda who Told lies 97 17. The £1,000,000 Banknote 102 18. Bees 108 19. Piano 113 20. Oliver Twist 117 21. The Beggar and the King 124 iii 1 Introduction The Teaching Guides of Oxford Reading Circle provide some guidelines for the help of the teacher in the classroom. This Teaching Guide includes: • an introduction on how to use Oxford Reading Circle in class. • suggestions for pre-reading tasks or warm-ups to the main lesson. • suggestions for while reading tasks with in-text questions. • suggestions for post-reading activities, based on basic concepts of literature presented progressively with respect to difficulty level within and across each grade. • suggested answers and hints to the exercises in the book. • additional questions related to the text. -
When the Hotter Cools More Quickly: Mpemba Effect in Granular Fluids
week ending PRL 119, 148001 (2017) PHYSICAL REVIEW LETTERS 6 OCTOBER 2017 When the Hotter Cools More Quickly: Mpemba Effect in Granular Fluids Antonio Lasanta,1,2 Francisco Vega Reyes,2 Antonio Prados,3 and Andrés Santos2 1Gregorio Millán Institute of Fluid Dynamics, Nanoscience and Industrial Mathematics, Department of Materials Science and Engineering and Chemical Engineering, Universidad Carlos III de Madrid, 28911 Leganés, Spain 2Departamento de Física and Instituto de Computación Científica Avanzada (ICCAEx), Universidad de Extremadura, 06006 Badajoz, Spain 3Física Teórica, Universidad de Sevilla, Apartado de Correos 1065, 41080 Sevilla, Spain (Received 16 November 2016; revised manuscript received 20 March 2017; published 4 October 2017) Under certain conditions, two samples of fluid at different initial temperatures present a counterintuitive behavior known as the Mpemba effect: it is the hotter system that cools sooner. Here, we show that the Mpemba effect is present in granular fluids, both in uniformly heated and in freely cooling systems. In both cases, the system remains homogeneous, and no phase transition is present. Analytical quantitative predictions are given for how differently the system must be initially prepared to observe the Mpemba effect, the theoretical predictions being confirmed by both molecular dynamics and Monte Carlo simulations. Possible implications of our analysis for other systems are also discussed. DOI: 10.1103/PhysRevLett.119.148001 Let us consider two identical beakers of water, initially at In a general physical system, the study of the ME implies two different temperatures, put in contact with a thermal finding those additional variables that control the temper- reservoir at subzero (on the Celsius scale) temperature.