Public perceptions of recycled water: a survey of visitors to the London 2012 Olympic Park

The Old Ford Water Recycling Plant, operated by Thames Water, was used to supply non-potable recycled blackwater to some of the venues at the London 2012 Games. In an effort to learn from this experience, Thames Water commissioned a survey of visitors to the Olympic Park during the Games to explore public responses to the water recycling project. Results show a very high level of support for using non-potable recycled blackwater, both in public venues and in homes. Such findings may indicate a growing receptivity towards this technology, and show that Thames Water (and other private water companies) are well placed to encourage and even lead public discussion around the role of water reuse in the future of urban water supplies

Multi-physics ensemble snow modelling in the western Himalaya

Combining multiple data sources with multi-physics simulation frameworks offers new potential to extend snow model inter-comparison efforts to the Himalaya. As such, this study evaluates the sensitivity of simulated regional snow cover and runoff dynamics to different snowpack process representations. The evaluation is based on a spatially distributed version of the Factorial Snowpack Model (FSM) set up for the Astore catchment in the upper Indus basin. The FSM multi-physics model was driven by climate fields from the High Asia Refined Analysis (HAR) dynamical downscaling product. Ensemble performance was evaluated primarily using MODIS remote sensing of snow-covered area, albedo and land surface temperature. In line with previous snow model inter-comparisons, no single FSM configuration performs best in all of the years simulated. However, the results demonstrate that performance variation in this case is at least partly related to inaccuracies in the sequencing of inter-annual variation in HAR climate inputs, not just FSM model limitations. Ensemble spread is dominated by interactions between parameterisations of albedo, snowpack hydrology and atmospheric stability effects on turbulent heat fluxes. The resulting ensemble structure is similar in different years, which leads to systematic divergence in ablation and mass balance at high elevations. While ensemble spread and errors are notably lower when viewed as anomalies, FSM configurations show important differences in their absolute sensitivity to climate variation. Comparison with observations suggests that a subset of the ensemble should be retained for climate change projections, namely those members including prognostic albedo and liquid water retention, refreezing and drainage processes

Stability of hexagonal solidification patterns

We investigate the dynamics of cellular solidification patterns using three-dimensional phase-field simulations. The cells can organize into stable hexagonal patterns or exhibit unsteady evolutions. We identify the relevant secondary instabilities of regular hexagonal arrays and find that the stability boundaries depend significantly on the strength of crystalline anisotropy. We also find multiplet states that can be reached by applying well-defined perturbations to a pre-existing hexagonal array.Comment: Minor changes, mainly in introduction and conclusion, one reference adde

Grain Boundary Loops in Graphene

Topological defects can affect the physical properties of graphene in unexpected ways. Harnessing their influence may lead to enhanced control of both material strength and electrical properties. Here we present a new class of topological defects in graphene composed of a rotating sequence of dislocations that close on themselves, forming grain boundary loops that either conserve the number of atoms in the hexagonal lattice or accommodate vacancy/interstitial reconstruction, while leaving no unsatisfied bonds. One grain boundary loop is observed as a "flower" pattern in scanning tunneling microscopy (STM) studies of epitaxial graphene grown on SiC(0001). We show that the flower defect has the lowest energy per dislocation core of any known topological defect in graphene, providing a natural explanation for its growth via the coalescence of mobile dislocations.Comment: 23 pages, 7 figures. Revised title; expanded; updated reference

Pleistocene Stratigraphy of the Athabasca River Valley Region, Rocky Mountains, Alberta

The Pleistocene stratigraphy of the central Canadian Rocky Mountains is described from a region where few studies of Late Quaternary deposits have been conducted. Six informal lithostratigraphic units are recognized from newly mapped exposures in Jasper National Park. The oldest deposits are interpreted as paleofan deposits (Unit 1) and they are overlain by glaciofluvial gravels and sands (Unit 2), glaciolacustrine sediments (Unit 3) and by a glacigenic diamicton sequence (Unit 4) that includes basal till, supraglacial deposits and ice-marginal debris flow sediments. Proximal glaciofluvial gravels, debris flow deposits and minor glaciolacustrine sediments (Unit 5) and paragiacial fan deposits and loess (Unit 6) cap the stratigraphic sequence. Limited chronologic control suggests that nonglacial fluvial and alluvial fan sedimentation began prior to 48 ka and continued throughout the Middle Wisconsinan. Braided stream deposits were accumulating in the Athabasca River valley near Jasper townsite about 29 ka. In the Late Wisconsinan, Rocky Mountain and Cordilleran glaciers advanced through the area, initially damming lakes in a number of Front Range tributary valleys. During déglaciation, ice-marginal glaciofluvial activity and paragiacial debris flows dominated sedimentation. Glacial lakes were limited in extent. A radiocarbon date on shells from one small ice-marginal lake indicates that glaciers were well in retreat by about 12 ka. Alpine glaciers in the region were at or near their present limits by 10 ka.On a reconnu six unités lithostratigraphiques informelles à partir d'affleurements récemment cartographies dans le parc national de Jasper. Les dépôts les plus anciens ont été interprétés comme étant d'anciens cônes de déjection (unité n°1), surmontés par des graviers et des sables fluvioglaciaires (unité n° 2), des sédiments glaciolacustres (unité n° 3) et par une séquence de diamictons (unité n° 4) qui comprend du till de fond, des dépôts supraglaciaires et des sédiments provenant de coulées boueuses de marge glaciaire. Des graviers fluvioglaciaires proximaux, des dépôts de coulée boueuse et des sédiments glaciolacustres (unité n° 5) ainsi que des dépôts de cône de déjection « paraglaciaires » et des loess (unité n° 6) complètent la séquence. L'imprécision chronologique découle du fait que la sédimentation non glaciaire de type fluviatile et alluvionnaire en cône de déjection a commencé avant 48 ka et s'est poursuivie tout au long du Wisconsinien moyen. Les dépôts de cours d'eau anastomosés se sont accumulés dans la vallée de l'Athabasca, près de Jasper, vers 29 ka. Au cours du Wisconsinien supérieur, les glaciers des Rocheuses et de la Cordillère ont couvert la région, édifiant d'abord des barrages dans un bon nombre de vallées tributaires du Front Range. À la déglaciation, l'activité fluvioglaciaire de marge glaciaire et les coulées boueuses « paraglaciaires » étaient les principales formes de sédimentation. Les lacs glaciaires étaient peu étendus. Une date au radiocarbone de coquillages recueillis dans un petit lac de marge glaciaire montre que le retrait glaciaire était en bonne voie vers 12 ka. Les glaciers alpins avaient dès 10 ka atteint à peu près leur limite actuelle.Die Stratigraphie der zentralen kanadischen Rocky Mountains im Pleistozàn wird fur eine Region beschrieben, fur die wenige Studien uber Ablagerungen im spàten Quaternar durchgefuhrt worden sind. Man hat inneu kartographierten Aufschlussen im Jasper Nationalpark sechs informelle lithostrati-graphische Einheiten identifiziert. Die àltesten Ablagerungen werden als Palàoschwemmfâcher gedeutet (Einheit l),und bie sind von glazifluvialem Kies und Sand uberlagert (Einheit 2), glaziallimnischen Sedimenten (Einheit 3) und einer glazigenen Diamiktit-Sequenz (Einheit 4), die Grundtill, supraglaziale Ablagerungen und Sedimente vom SchuttfluB am Eisrand enthàlt. Proximaler glazifluvialer Kies, SchuttfluBablagerungen und geringere glaziallimnische Sedimente (Einheit 5) sowie paraglaziale Schwemmfàcherablagerungen und LoB (Einheit 6) beschlieBen die stratigraphische Sequenz. Die begrenzte chronologische Kontrolle IaBt annehmen, daB die nichtglaziale fluviatile und Schwemmfàcher-Sedimentierung vor 48 ka begann und durch das ganze mittlere Wisconsinium fortdauerte. Verwilderte Stromablagerungen sammelten sich im AthabaskafluBtal in der Nâhe der Stadt Jasper urn etwa 29 ka an. Im spàten Wisconsinium ruckten die Gletscher der Rocky Mountains und der Kordilleren durch das Gebiet voran und dâmmten Seen in einer Reihe von tributàren Tàlern des Front Range. Wàhrend der Enteisung haben glazifluviale Eisrandaktivitàt und paraglazialer SchuttfluB die Sedimentierung beherrscht. Glaziale Seen waren in ihrer Ausdehnung begrenzt. Eine Radiokarbondatierung von Muscheln von einem kleinen Eisrandsee zeigt, daB der Gletscherruckzug urn etwa 12 ka schon eingetreten war. Alpine Gletscher des Gebiets befanden sich urn 10ka an Oder nahe bei ihren heutigen Grenzen

MgB2 conductors for dc and ac applications

The paper presents discussion on up to date results on MgB2 conductors from the point of view of their future dc and ac applications. Basic physical parameters of MgB2 compound relevant to conductors are introduced. Different conductor preparation methods and conductor architectures are presented and attainable critical current densities discussed. Some numerical results on critical currents and ac losses of future multifilamentary MgB2 conductors with magnetic cladding of their filaments are given. Recently observed anomalous decrease of ac susceptibility at 50 K in copper clad Powder-in-tube, PIT, MgB2 wires is presented.Comment: Paper presented at EUCAS'01 conference, Copenhagen, 26-30 August 200

The impact of repetitive unclamped inductive switching on the electrical parameters of low-voltage trench power nMOSFETs

The impact of hot-carrier injection (HCI) due to repetitive unclamped inductive switching (UIS) on the electrical performance of low-voltage trench power n-type MOSFETs (nMOSFETs) is assessed. Trench power nMOSFETs with 20- and 30-V breakdown voltage ratings in TO-220 packages have been fabricated and subjected to over 100 million cycles of repetitive UIS with different avalanche currents IAV at a mounting base temperature TMB of 150°C. Impact ionization during avalanche conduction in the channel causes hot-hole injection into the gate dielectric, which results in a reduction of the threshold voltage VGSTX, as the number of avalanche cycles N increases. The experimental data reveal a power-law relationship between the change in the threshold voltage ΔVGSTX and N. The results show that the power-law prefactor is directly proportional to the avalanche current. After 100 million cycles, it was observed in the 20-V rated MOSFETs that the power-law prefactor increased by 30% when IAV was increased from 160 to 225 A, thereby approximating a linear relationship. A stable subthreshold slope with avalanche cycling indicates that interface trap generation may not be an active degradation mechanism. The impact of the cell pitch on avalanche ruggedness is also investigated by testing 2.5- and 4- m cell-pitch 30-V rated MOSFETs. Measurements showed that the power-law prefactor reduced by 40% when the cell pitch was reduced by 37.5%. The improved VGSTX stability with the smaller cell-pitch MOSFETs is attributed to a lower avalanche current per unit cell resulting in less hot-hole injection and, hence, smaller VGSTX shift. The 2.5-m cell-pitch MOSFETs also show 25% improved on -state resistance RDSON, better RDSON stability, and 20% less subthreshold slope compared with the 4-m cell-pitch MOSFETs, although with 100% higher initial IDSS and less IDSS stability with avalanche cycling. These results are important for manufacturers of automotive MOSFETs where multiple avalanche occurrences over the lifetime of the MOSFET are expected

On Resilient Behaviors in Computational Systems and Environments

The present article introduces a reference framework for discussing resilience of computational systems. Rather than a property that may or may not be exhibited by a system, resilience is interpreted here as the emerging result of a dynamic process. Said process represents the dynamic interplay between the behaviors exercised by a system and those of the environment it is set to operate in. As a result of this interpretation, coherent definitions of several aspects of resilience can be derived and proposed, including elasticity, change tolerance, and antifragility. Definitions are also provided for measures of the risk of unresilience as well as for the optimal match of a given resilient design with respect to the current environmental conditions. Finally, a resilience strategy based on our model is exemplified through a simple scenario.Comment: The final publication is available at Springer via http://dx.doi.org/10.1007/s40860-015-0002-6 The paper considerably extends the results of two conference papers that are available at http://ow.ly/KWfkj and http://ow.ly/KWfgO. Text and formalism in those papers has been used or adapted in the herewith submitted pape