Miracle-dz/UniFAR-FTUs huggingface dataset:
Marble quarrying: an energy and waste intensive activity in the production of building materials

Marble represents an important component of Italian buildings, where it is often utilized as a covering for bottom surfaces, despite its relatively high price. Moreover, it characterizes several public buildings, for which it is by far the most important decorative material, also because of its structural features and its long durability. Unfortunately, marble quarrying is an energy intensive activity that requires relevant amounts of electric and thermal energy sources; in addition, the extraction of the marble blocks from the mountain sides does involve a noticeable quantity of explosives, particularly in sites where traditional working methods are utilized. Another important feature of the marble mining is represented by the high level of waste materials released during the quarrying process. Both these elements call for careful attention to the production of this material, aiming for a suitable reduction of the environmental impact exerted by the current working procedures. An energy audit analysis, moreover, could allow the singling out of the steps of the whole process where it would be possible to reach improved efficiency, in this way properly cutting the energy resources involved in the production of the functional unit of this natural stone. The feasibility of such considerations is verified by means of an application to a marble quarry in Sicily, the region where an important rate of the Italian domestic production is realized. The field energy audit, other than suggesting a general approach to the problem, does indicate the high inefficiencies actually present in the working chain of the Sicilian marble.
Apparent Coincidences in the Life-history of the Moine Schists

Abstract A review of the progress of knowledge concerning the Moine Schists shows that, whereas about twenty years ago many geologists supported Horne's contention that the Moine sediments were pre-Torridonian, there has been recently a marked swing towards Peach's view that they are the equivalents of the Torridonian. The interpretation of the structural petrology of these schists in the light of this change of opinion is then discussed.
Scattered P′P′ Waves Observed at Short Distances

We detect previously unreported 1 Hz scattered waves at epicentral dis- tances between 30° and 50° and at times between 2300 and 2450 s after the earthquake origin. These waves likely result from off-azimuth scattering of PKPbc to PKPbc in the upper mantle and crust and provide a new tool for mapping variations in fine-scale (10 km) mantle heterogeneity. Array beams from the Large Aperture Seismic Array (LASA) clearly image the scattered energy gradually emerging from the noise and reaching its peak amplitude about 80 s later, and returning to the noise level after 150 s. Stacks of transverse versus radial slowness (ρt, ρr) show two peaks at about (2, � 2) and �� 2; � 2� s=°, indicating the waves arrive along the major arc path (180° to 360°) and significantly off azimuth. We propose a mantle and surface PKPbc to PKPbc scattering mechanism for these observations because (1) it agrees with the initiation time and distinctive slowness signature of the scattered waves and (2) it follows a scattering path analogous to previously observed deep-mantle PKKPscat- tering (Chang and Cleary, 1981). The observed upper-mantle scattered waves and PKKP waves fit into a broader set of scattered waves that we call P 0 dP 0 , which can scatter from any depth, d, in the mantle.
Characteristics of soil moisture in permafrost observed in East Siberian taiga with stable isotopes of water

Soil moisture and its isotopic composition were observed at Spasskaya Pad experimental forest near Yakutsk, Russia, during summer in 1998, 1999, and 2000. The amount of soil water (plus ice) was estimated from volumetric soil water content obtained with time domain reflectometry. Soil moisture and its δ18O showed large interannual variation depending on the amount of summer rainfall. The soil water δ18O decreased with soil moisture during a dry summer (1998), indicating that ice meltwater from a deeper soil layer was transported upward. On the other hand, during a wet summer (1999), the δ18O of soil water increased due to percolation of summer rain with high δ18O values.
Oceanographic observations on the Scotian Shelf during CASP

Abstract Winter‐time (1985–86) observations of sea‐level, surface waves, currents, bottom pressure, and water properties were made on the Scotian Shelf as part of the Canadian Atlantic Storms Program (CASP). The purpose of the field program and the locations, instrument systems, and sampling schemes are described. Statistics on the observed currents are presented, and monthly estimates of the longshore transport of the Nova Scotian Current are given for four months spanning the winter season (December to March). The 1985–86 transports are compared with previous estimates of the baroclinic transport made using the dynamic method. Cross‐shelf temperature and salinity distributions corresponding to the beginning and end of the field program are described and compared with the climatological means. The autospectra of the observed currents exhibit energy concentrations at frequencies of 0.2–0.5, 1.0, 1.4 and 2.0 cycles per day (cpd). Coastal‐trapped wave motions account for significant portions of the energy i.
Borehole Stoneley wave propagation across permeable structures

This study investigates the propagation of borehole Stoneley waves across permeable structures. By modeling the structure as a zone intersecting the borehole, a simple 1D theory is formulated to treat the interaction of the Stoneley wave with the structure. This is possible because the Stoneley wave is a guided wave, with no geometric spreading as it propagates along the borehole. The interaction occurs because the zone and the surrounding formation possess different Stoneley wavenumbers. Given appropriate representations of the wavenumber, the theory can be applied to treat a variety of structures, including a fluid-filled fracture. Of special interest are the cases of permeable porous zones and fracture zones. The results show that, while Stoneley wave reflections are generated, strong Stoneley wave attenuation is produced across a very permeable zone. This result is particularly important in explaining the observed strong Stoneley wave attenuation at major fractures where it has been difficult to explain the attenuation in terms of the single planar fracture theory. In addition, by using a simple and sufficiently accurate theory to model the effects of the permeable zone, a fast and efficient method is developed to characterize the fluid transport properties of a permeable fracture zone.
Experiments on Wedge-Shaped Deep Sea Sedimentary Deposits in Minibasins and/or on Channel Levees Emplaced by Turbidity Currents. Part II. Morphodynamic Evolution of the Wedge and of the Associated Bedforms

Rapidly decelerating sediment-laden flows typically emplace confined sedimentary deposits. In the fluvial environment, when sediment-laden rivers reach lakes the decelerating flow emplaces a subaerial delta with distinctive topset, foreset, and bottomset deposits. In the submarine environment, turbidity currents undergoing rapid deceleration commonly emplace sedimentary wedges (i.e., deposits thinning in the downstream direction). Froude-supercritical turbidity currents have an intrinsic self-regulating mechanism for deceleration, in that the faster they flow, the more they incorporate ambient sea water through mixing at their interface. In addition, special topographic configurations, such as the entrance into a zone of much lower slope and/or lateral confinement, or the passage into a confined minibasin, may trigger sudden flow deceleration by forcing a transition to subcritical flow through an internal hydraulic jump. The present paper and its companion present experiments on a generic configuration aimed at studying the emplacement of wedge-shaped sedimentary deposits by continuous supercritical density currents. The deceleration is achieved both by natural entrainment of ambient water and by the presence of an obstructing barrier downstream. Lightweight plastic sediment was used as an analog for sand, and was transported mostly as bedload, but with some suspension, by a saline underflow. The saline underflow served as a surrogate for a turbidity current driven by fine mud that does not easily settle out. The companion paper is focused on the flow patterns associated with the decelerating current. The present paper focuses on the depositional sequences. The decelerating supercritical flows produced a wedge with a distinct pattern of aggradation and progradation. In addition, a foreset-like structure is attributed to the presence of an internal hydraulic jump forced by the downstream barrier. Although they do not reproduce any specific field-scale setting, the experiments are deemed a good generic model for several wedge-shaped submarine deposits in various settings, from slope aprons to deposits in minibasins or on the external flanks of channel levees. The paper also documents the regimes of bedforms associated with the diverse flow regions. It provides the first evidence for the formation of trains of the upstream-migrating sediment waves known as cyclic steps, similar to those commonly observed on channel levees and also along the thalwegs of some steep canyons. In addition, the experiments provide convincing evidence for the formation of downstream-migrating antidunes as well.
Bridging the research gap

While there is a rich history of studies involving robots and individuals with autism spectrum disorders (ASD), few of these studies have made substantial impact in the clinical research community. In this paper we first examine how differences in approach, study design, evaluation, and publication practices have hindered uptake of these research results. Based on ten years of collaboration, we suggest a set of design principles that satisfy the needs (both academic and cultural) of both the robotics and clinical autism research communities. Using these principles, we present a study that demonstrates a quantitatively measured improvement in human-human social interaction for children with ASD, effected by interaction with a robot.
Environmental Influences on the Development of Endometriosis

Purpose Several environmental toxicants (ETs), including dioxins and dioxin-like compounds (DLCs), perfluorochemicals, organochlorine pesticides, phthalates, and heavy metals (especially cadmium with its estrogen-like properties in animal models) have been investigated as possibly being related to endometriosis. Methods Systematic review of pertinent literature. Results DLCs have been the most investigated ETs. DLCs are persistent organic pollutants with highly toxic potential and include three types of compounds: polychlorinated dibenzo-p-dioxins (PCDDs), polychlorinated dibenzofurans (PCDFs) or furans, and polychlorinated biphenyls (PCBs). The most toxic is 2, 3, 7, 8- tetrachlorodibenzo-p-dioxin (TCDD). The connection mechanism between dioxins and endometriosis is still unclear. However, dioxins and DLCs are endocrine-disrupting compounds that can affect the pathobiology of endometriosis at multiple levels. Part of the dioxin and DLCs toxic effects can be accounted for by their interaction with the aryl hydrocarbon receptor (AhR). It has been proposed that dioxin can initiate or promote endometriosis by means of interaction with estrogen receptors or by suppressing the expression of progesterone receptors. Furthermore, TCDD alters the expression of cytokines and growth factors, remodeling enzymes and cytochrome P450 expression and activity. Conclusions Studies in rhesus models have revealed a correlation between dioxin exposure and endometriosis. However, evidence from epidemiologic studies is inconclusive.
Simulation of upscale error growth with a stochastic convection scheme

By directly comparing the results of a recent convection‐permitting upscale error growth study with simulations on coarser grids, we assessed the ability of two different convection schemes to represent convective uncertainty and propagate it upscale. It is found that the widely used Tiedtke convection scheme shows significantly reduced upscale error growth and hence leads to an overconfidence of the model. In contrast it is found that the stochastic convection scheme of Plant and Craig is able to better reproduce the high‐resolution results. Evidence is presented that this improved uncertainty evolution can be related to the representation of (unpredictable) convective variability near the grid scale.
The application of remote sensing to seagrass ecosystems: an overview and future research prospects

This review evaluates various methods employed to produce seagrass habitat maps using optical and acoustic remote-sensing (RS) techniques coupled with in situ sampling to highlight recent advances and to define areas where potential future research should be focused in the application of RS technologies. A critical review of 195 studies revealed that, in the past four decades, advances in the application of RS methods, notably using Landsat imagery, are identified for seagrass detection, assessment of areal coverage, distribution and abundance mapping, and the detection of extent and biomass changes, as illustrated in peer-reviewed literature. Rapid technological and methodological advances have occurred in the acquisition and interpretation of optical and acoustic data for the mapping of seagrass habitats. The methods have been tested to segment, classify, and combine RS data with biological field or ground truth sample data. There is no single technology or approach that is suitable for and capable of measuring all seagrass parameters (presence/absence, cover, species, and biomass) and assessing change. Integration of field, imagery, and mapping approaches is therefore required. Further research is required for continued improvements in understanding of theoretical and methodological aspects of seagrass RS.
Tropical cyclone size in observations and in radiative-convective equilibrium

Tropical cyclone size remains an unsolved problem in tropical meteorology, yet size plays a significant role in the damage caused by tropical cyclones due to wind, storm surge, and inland freshwater flooding. This work explores size, defined as the radius of vanishing wind, in observations and at equilibrium in an idealized numerical model. First, a climatology of size is created from the QuikSCAT database of near-surface wind vectors for the years 1999-2008. Globally, the distribution of the outer radius is found to be log-normal, with statistically significant variation across ocean basins, but with minimal correlation with various dynamic and thermodynamic parameters. Second, the sensitivity of the structure of a numerically-simulated axisymmetric tropical cyclone at statistical equilibrium to the set of relevant model, initial, and environmental external parameters is explored. The analysis is performed in a highly-idealized state of radiative-convective equilibrium (RCE). The non-dimensional equilibrium radial wind profile is found to be modulated primarily by a single nondimensional parameter given by the ratio of the storm radial length scale to the parameterized eddy radial length scale. The relevant storm length scale is shown to be the ratio of the potential intensity to the Coriolis parameter, matching the prediction for the "natural" storm length scale in prevailing axisymmetric tropical cyclone theory. The outer storm circulation is further modulated by a second non-dimensional parameter that represents the non-dimensional Ekman suction rate. Third, size is explored in three-dimensional "tropical cyclone world" simulations, with preliminary results confirming the relevant length scale obtained in axisymmetry. Ultimately, the results of the equilibrium storm analysis are insufficient to explain the observed distribution of tropical cyclone size, but they provide the first steps toward a more fundamental understanding of the dynamics of size. Thesis Supervisor: Kerry A. Emanuel Title: Cecil & Ida Green Professor of Atmospheric Science
The Role of Landmark Information in Intelligent Navigation Displays

Advanced Traveler Information Systems (ATIS) are advanced communication and navigation systems that use computer-based in-vehicle systems to provide navigation and travel-related information to drivers. To help drivers navigate effectively and get to their destinations quickly and safely, navigational information must be effectively communicated to the driver. Landmarks are important environmental and navigational cues that help drivers to get to their destinations. This paper describes a study that tested the influence of landmark information in route guidance displays on navigation performance in a simulated driving environment. Forty-eight participants drove in a high-fidelity simulator and navigated using route guidance displays with and without landmark icons. The results indicated that landmarks were beneficial as a navigation aid; they helped drivers make turning decisions more quickly, especially in reduced visibility conditions (i.e., foggy conditions). Landmarks were particularly beneficial to older drivers by improving their turning accuracy and turn signal accuracy, especially in the fog.
Mortalidade por acidentes de motocicleta no Brasil: análise de tendência temporal, 1996-2009

OBJECTIVE To analyze motorcycle accidents mortality trends in Brazil. METHODS A descriptive time series study of mortality from motorcycle accidents in Brazil between 1996 and 2009 according to state and age group. The data on mortality were obtained from the National Mortality Information System of Ministry of Health and the population data from the Brazilian Institute of Geography and Statistics. Standardized mortality rates were calculated for the entire period for the country as a whole and for each state. Annual variability in mortality rates was estimated using Prais-Winsten generalized linear correlation. RESULTS Between 1996 and 2009 the mortality rate increased from 0.5 to 4.5 per 100.000 habitants (an increase of 800.0% in mortality rates during the period studied and an average annual increase of 19.0%). High mortality rates in 2009 were observed in the states of Piaui, Sergipe and Mato Grosso. The largest increases were observed in states in the North, Northeast and Midwest of Brazil. CONCLUSIONS There was a significant increase in motorcycle accident mortality rates for the country as a whole during the studied period, mainly in states in the Northeast.
Infiltration capacity of disturbed soils: temporal change and lithologic control

The hydrologic character and response of disturbed land is controlled, to a large degree,by soil infiltration characteristics. Reconstructed soils on surface mines (mine soils) of different age (1 to 4 years old) are used to investigate infiltration rates on disturbed landscapes. The data consist of soil/surface properties and runoff volumes fit to the Horton infiltration equation. Infiltration rates on newly reclaimed mine soils are an order of magnitude lower than adjacent, undisturbed soil. Few significant correlations exist between soil/surface properties and infiltration parameters for newly reclaimed soils. However, the correlation between infiltration and mine soil characteristics increases with soil age. Multiple regressions are used to explore relationships between infiltration parameters and soil/surface properties for each soil age. Regression models of 30-min infiltration volume and the steady-state rate consistently include the percent silt and clay, slope, bulk density, and vegetation. Mean infiltration volumes at different mines are equal in the first year following reclamation, but become significantly different with surface age. The magnitude of the increase is controlled by the soil texture, vegetation, slope, and bulk density. Soil characteristics are determined ultimately by the overburden lithology and its effect on mineralogy and grain size during physical redistribution of soil particles andmore » initial weathering. « less
The nutritional footprint: an innovative management approach for the food sector.

The food and nutrition sector accounts for huge environmental impacts caused by production, processing, final consumption and waste treatment in private households or in out of home catering settings. Further, the field of nutrition inextricably links environmental and health aspects to each other. Thus, the domain of nutrition has to be considered intensively if environmental aspects and health considerations should be further investigated. However, a healthy and environmentally friendly diet is a criterion which remains quite abstract to the consumer. Against this background, the following research question is addressed: “How can environmental and health indicators be linked to each other? ” For that reason a comprehensive concept is developed in this paper, the so-called nutritional footprint. The model is based on conceptual frameworks, such as the Hot Spot Analysis. Within a data assortment, relevant and available environmental data (e.g. material footprint or water consumption within the life cycle) is set in relation to available nutrition data (e.g. nutrient density or the classical calorie specifications). The paper shows that a nutritional footprint – as an assessment instrument – presents a way to communicate environmental and health issues together and provides a comprehensive and integrated perspective on quantitative and qualitative data. The concept developed in this paper is also available and useful for companies to expand their internal data and their external communication performance. Nonetheless, the current paper presents a first version on this concept, which has to be refined in cooperation with a leading fast food company in order to integrate the approach in their business.
Caribbean coral tracks Atlantic Multidecadal Oscillation and past hurricane activity

It is highly debated whether global warming contributed to the strong hurricane activity observed during the last decade. The crux of the recent debate is the limited length of the reliable instrumental record that exacerbates the detection of possible long-term changes in hurricane activity, which naturally exhibits strong multidecadal variations that are associated with the Atlantic Multidecadal Oscillation (AMO). The AMO, itself a major mode of climate variability, remains also poorly understood because of limited data. Here, we present the first coral-based proxy record (δ18O) that clearly captures multidecadal variations in the AMO and the hurricane activity. Our record, obtained from a brain coral situated in the Atlantic hurricane domain, is equally sensitive to variations in sea surface temperature (SST) and seawater δ18O, with the latter being strongly linked to precipitation, by this means amplifying large-scale climate signals in coral δ18O. The SST and precipitation signals in the coral provide the longest, thus far, continuous proxy-based record of hurricane activity that interestingly exhibits a long-term increase over the last century. As multidecadal SST variations in this region are closely related to the AMO, this study raises new possibilities to extend the limited observations and to gain new insights into the mechanisms underlying the AMO and long-term hurricane variations.