Quantum phase transitions in rotating nuclei

We extend the classical Landau theory for rotating nuclei and show that the backbending in 162Yb, that comes about as a result of the two-quasiparticle alignment, is identified with the second order phase transition. We found that the backbending in 156Dy, caused by the instability of $\gamma$-vibrations in the rotating frame, corresponds to the first order phase transition.Comment: 4 pages, 2 figure

Approaches Toward Improving the Prognosis of Pediatric Patients With Glioma: Pursuing Mutant Drug Targets With Emerging Small Molecules

Gliomas represent approximately 70% of all pediatric brain tumors and most of these are of astrocytic lineage, furthermore, malignant or high-grade astrocytoma account for approximately 20% of pediatric astrocytoma. Treatment options for pediatric glioma patients are limited. Although low-grade astrocytoma are relatively slow-growing tumors which can often be cured through surgical resection, a significant proportion of cases will recur, as such new treatments are desperately needed. This review covers the various approaches that are currently being made towards improving the prognosis of pediatric glioma patients by pursuing pediatric-selective mutant drug targets with emerging small molecules

The emotional geography of prison life

Accounts of prison life consistently describe a culture of mutual mistrust, fear, aggression and barely submerged violence. Often too, they explain how prisoners adapt to this environment—in men’s prisons, at least—by putting on emotional ‘masks’ or ‘fronts’ of masculine bravado which hide their vulnerabilities and deter the aggression of their peers. This article does not contest the truth of such descriptions, but argues that they provide a partial account of the prison’s emotional world. Most importantly, for current purposes, they fail to describe the way in which prisons have a distinctive kind of emotional geography, with zones in which certain kinds of emotional feelings and displays are more or less acceptable. In this article, we argue that these ‘emotion zones’, which cannot be characterized either as ‘frontstage’ or ‘backstage’ domains, enable the display of a wider range of feelings than elsewhere in the prison. Their existence represents a challenge to depictions of prisons as environments that are unwaveringly sterile, unfailingly aggressive or emotionally undifferentiated. This is the accepted manuscript. The final version is available from Sage at http://tcr.sagepub.com/content/18/1/56

The energy flux into a fluidized granular medium at a vibrating wall

We study the power input of a vibrating wall into a fluidized granular medium, using event driven simulations of a model granular system. The system consists of inelastic hard disks contained between a stationary and a vibrating elastic wall, in the absence of gravity. Two scaling relations for the power input are found, both involving the pressure. The transition between the two occurs when waves generated at the moving wall can propagate across the system. Choosing an appropriate waveform for the vibrating wall removes one of these scalings and renders the second very simple.Comment: 5 pages, revtex, 7 postscript figure

STUDENT ENGAGEMENT THROUGH DATA MAPPING IN AN UNDERGRADUATE ENVIRONMENTAL CHEMISTRY LABORATORY

We are all too familiar with the map visualisations in media depicting the spread and severity of COVID-19 across the world. The representation of statistical data on a map is a powerful tool that can effectively convey factors such as magnitude, density and spatial variations. Analysing data in this format can help identify trends (eg “hotspots”, “patient zero”) from large datasets. Whilst students outside the discipline of geosciences may be familiar with analysing a data map; constructing one would be a rare experience. In our undergraduate environmental chemistry laboratory, students analyse the metal ion content and hardness of water samples collected on campus. We have used Google Maps Application Programming Interface (API)1 to allow students to geotag their results on a Google Map. The resulting bubble map is live and continually updated as students complete the lab and submit their results.2 This map is shared with the cohort so students can view the evolution of data, their contribution to the “project” and generate their own hypotheses as to why certain concentrations may be linked to certain locales (eg. age of building). This approach offers rich context-based learning that could be modified to address other datasets/contexts, locations, and disciplines

Determining noble gas partitioning within a CO2–H2O system at elevated temperatures and pressures

Quantifying the distribution of noble gases between phases is essential for using these inert trace gases to track the processes controlling multi-phase subsurface systems. Here we present experimental data that defines noble gas partitioning for two phase CO2–water systems. These are at the pressure and temperature range relevant for engineered systems used for anthropogenic carbon capture and geological storage (CCS) technologies, and CO2-rich natural gas reservoirs (CO2 density range 169–656 kg/m3 at 323–377 K and 89–134 bar). The new partitioning data are compared to predictions of noble gas partitioning determined in low-pressure, pure noble gas–water systems for all noble gases except neon and radon. At low CO2 density there was no difference between measured noble gas partitioning and that predicted in pure noble gas–water systems. At high CO2 density, however, partition coefficients express significant deviation from pure noble gas–water systems. At 656 kg/m3, these deviations are −35%, 74%, 113% and 319% for helium, argon, krypton and xenon, respectively. A second order polynomial fit to the data for each noble gas describes the deviation from the pure noble gas–water system as a function of CO2 density. We argue that the difference between pure noble gas–water systems and the high density CO2–water system is due to an enhanced degree of molecular interactions occurring within the dense CO2 phase due to the combined effect of inductive and dispersive forces acting on the noble gases. As the magnitude of these forces are related to the size and polarisability of each noble gas, xenon followed by krypton and argon become significantly more soluble within dense CO2. In the case of helium repulsive forces dominate and so it becomes less soluble as a function of CO2 density

The Indian Ocean tsunami: socio-economic impacts in Thailand

On the morning of 26 December 2004 large areas of coastal southern Thailand were transformed when a tsunami, generated by a powerful submarine earthquake in the Indian Ocean, swept ashore. Officially, there were 5395 confirmed deaths in Thailand with another 2932 people listed as missing. In February 2005 a team led by Dr Ben Horton of the University of Pennsylvania was awarded an SGER grant by the National Science Foundation to undertake exploratory research on the tsunami in Malaysia and Thailand. This report summarizes the preliminary conclusions of the social science element of the Thai fieldwork. The team undertook fieldwork in three main sites during July 2005: Koh Lanta, Koh Phi Phi and Khao Lak. We chose Koh Phi Phi as a small, tourist (backpacker)-oriented island economy with high levels of damage and casualties; Koh Lanta as a site with a significant population of fisherfolk with a long presence in the area; and Khao Lak as a mainland site with the highest number of casualties in Thailand and with a mixed tourism-fishing economy