1,336 research outputs found

    Symmetry of re-entrant tetragonal phase in Ba1-xNaxFe2As2: Magnetic versus orbital ordering mechanism

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    Magneto-structural phase transitions in Ba1-xAxFe2As2 (A = K, Na) materials are discussed for both magnetically and orbitally driven mechanisms, using a symmetry analysis formulated within the Landau theory of phase transitions. Both mechanisms predict identical orthorhombic space-group symmetries for the nematic and magnetic phases observed over much of the phase diagram, but they predict different tetragonal space-group symmetries for the newly discovered re-entrant tetragonal phase in Ba1-xNaxFe2As2 (x ~ 0.24-0.28). In a magnetic scenario, magnetic order with moments along the c-axis, as found experimentally, does not allow any type of orbital order, but in an orbital scenario, we have determined two possible orbital patterns, specified by P4/mnc1' and I4221' space groups, which do not require atomic displacements relative to the parent I4/mmm1' symmetry and, in consequence, are indistinguishable in conventional diffraction experiments. We demonstrate that the three possible space groups are however, distinct in resonant X-ray Bragg diffraction patterns created by Templeton & Templeton scattering. This provides an experimental method of distinguishing between magnetic and orbital models

    What women know: Perceptions of seven female superintendents

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    An anomalous concentration of female superintendents in mostly rural South Texas prompted this inquiry. South Texas faces critical shortages in personnel due to impending retirement and turnover of existing school administrators and superintendents (Wesson & Marshall, 2012). It is difficult to recruit and retain the best talent necessary to solve tough school improvement challenges—high dropout rates, high poverty, low student achievement, and complex multi-cultural issues—in high needs, Hispanic majority, primarily rural school districts (Trevino Jr., Braley, Brown, & Slate, 2008; Wesson & Marshall, 2012). Krüger (2008) stated women are stronger educational leaders than men. Females seek and obtain leadership credentials for the express purpose of impacting education for students (Young & McLeod, 2001). Schools of all sizes and levels with female administrators achieved higher student success than schools with male administrators, according to a 7000 campus Texas study, in the 2006-2007 academic year (Roser, Brown, & Kelsey, 2009). In every ethnic group, women earn more doctoral degrees in education than men; women earn bachelors and masters degrees in education in proportion to their representation in the field; and women have more years of teaching experience than men (Shakeshaft, Brown, Irby, Grogan, & Ballenger, 2007). Women also outnumber men in education administration preparation programs (Petrie & Lindauer, 2001). Yet women are not ascending to the superintendency in proportion to their representation in the education profession (Shakeshaft et al., 2007). This naturalistic study of seven female superintendents in South Texas, including leaders in large and small rural districts, illuminated perceptions and experiences of female school leadership through portraiture and lent insight into common themes of aspiration and motivation

    The Effects of Oxidation on the Refractive Index of Uranium Thin Films in the Extreme Ultraviolet

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    We measured the transmittance and reflectance of two samples in the extreme ultraviolet (XUV) at the Advanced Light Source at Lawrence Berkeley National Laboratory. The samples were prepared with approximately 20 nm of UOx with one reactively sputtered onto a diode, and one allowed to oxidize naturally on an identical diode. Fitting the reflectance data to the Parratt model yielded a more precise thickness of the UOx film. This thickness combined with a simple analysis of the transmission measurements provides estimates for the imaginary part of the index of refraction for UOx at approximately every tenth of a nanometer from about 3 nm to 30 nm with emphasis in the 12- to 13-nm range. Using these values, a first approximation for the real part of the refractive index has also been calculated. These values provide researchers with information for modeling, design, and fabrication of optical systems in the extreme ultraviolet

    Anisotropic Hc2H_{c2} determined up to 92 T and the signature of multi-band superconductivity in Ca10_{10}(Pt4_{4}As8_{8})((Fe1x_{1-x}Ptx_{x})2_{2}As2_{2})5_{5} superconductor

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    The upper critical fields, Hc2H_{c2}(TT), of single crystals of the superconductor Ca10_{10}(Pt4δ_{4-\delta}As8_{8})((Fe0.97_{0.97}Pt0.03_{0.03})2_{2}As2_{2})5_{5} (δ\delta \approx 0.246) are determined over a wide range of temperatures down to TT = 1.42 K and magnetic fields of up to μ0H\mu_{0}H \simeq 92 T. The measurements of anisotropic Hc2H_{c2}(TT) curves are performed in pulsed magnetic fields using radio-frequency contactless penetration depth measurements for magnetic field applied both parallel and perpendicular to the \textbf{ab}-plane. Whereas a clear upward curvature in Hc2cH_{c2}^{\parallel\textbf{c}}(TT) along \textbf{H}\parallel\textbf{c} is observed with decreasing temperature, the Hc2abH_{c2}^{\parallel\textbf{ab}}(TT) along \textbf{H}\parallel\textbf{ab} shows a flattening at low temperatures. The rapid increase of the Hc2cH_{c2}^{\parallel\textbf{c}}(TT) at low temperatures suggests that the superconductivity can be described by two dominating bands. The anisotropy parameter, γH\gamma_{H} \equiv Hc2ab/Hc2cH_{c2}^{\parallel\textbf{ab}}/H_{c2}^{\parallel\textbf{c}}, is \sim7 close to TcT_{c} and decreases considerably to \sim1 with decreasing temperature, showing rather weak anisotropy at low temperatures.Comment: 4pages, 3figures, accepted PRB Rapid Communicatio

    Bi2Te1.6S1.4 - a Topological Insulator in the Tetradymite Family

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    We describe the crystal growth, crystal structure, and basic electrical properties of Bi2Te1.6S1.4, which incorporates both S and Te in its Tetradymite quintuple layers in the motif -[Te0.8S0.2]-Bi-S-Bi-[Te0.8S0.2]-. This material differs from other Tetradymites studied as topological insulators due to the increased ionic character that arises from its significant S content. Bi2Te1.6S1.4 forms high quality crystals from the melt and is the S-rich limit of the ternary Bi-Te-S {\gamma}-Tetradymite phase at the melting point. The native material is n-type with a low resistivity; Sb substitution, with adjustment of the Te to S ratio, results in a crossover to p-type and resistive behavior at low temperatures. Angle resolved photoemission study shows that topological surface states are present, with the Dirac point more exposed than it is in Bi2Te3 and similar to that seen in Bi2Te2Se. Single crystal structure determination indicates that the S in the outer chalcogen layers is closer to the Bi than the Te, and therefore that the layers supporting the surface states are corrugated on the atomic scale.Comment: To be published in Physical Review B Rapid Communications 16 douuble spaced pages. 4 figures 1 tabl

    Ungulate preference for burned patches reveals strength of fire–grazing interaction

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    The interactions between fire and grazing are widespread throughout fire-dependent landscapes. The utilization of burned areas by grazing animals establishes the fire–grazing interaction, but the preference for recently burned areas relative to other influences (water, topography, etc.) is unknown. In this study, we determine the strength of the fire–grazing interaction by quantifying the influence of fire on ungulate site selection. We compare the preference for recently burned patches relative to the influence of other environmental factors that contribute to site selection; compare that preference between native and introduced ungulates; test relationships between area burned and herbivore preference; and determine forage quality and quantity as mechanisms of site selection. We used two large ungulate species at two grassland locations within the southern Great Plains, USA. At each location, spatially distinct patches were burned within larger areas through time, allowing animals to select among burned and unburned areas. Using fine scale ungulate location data, we estimated resource selection functions to examine environmental factors in site selection. Ungulates preferred recently burned areas and avoided areas with greater time since fire, regardless of the size of landscape, herbivore species, or proportion of area burned. Forage quality was inversely related to time since fire, while forage quantity was positively related. We show that fire is an important component of large ungulate behavior with a strong influence on site selection that drives the fire–grazing interaction. This interaction is an ecosystem process that supersedes fire and grazing as separate factors, shaping grassland landscapes. Inclusion of the fire–grazing interaction into ecological studies and conservation practices of fire-prone systems will aid in better understanding and managing these systems

    Analysis and Modeling of Two Flare Loops Observed by AIA and EIS

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    We analyze and model an M1.0 flare observed by SDO/AIA and Hinode/EIS to investigate how flare loops are heated and evolve subsequently. The flare is composed of two distinctive loop systems observed in EUV images. The UV 1600 \AA emission at the feet of these loops exhibits a rapid rise, followed by enhanced emission in different EUV channels observed by AIA and EIS. Such behavior is indicative of impulsive energy deposit and the subsequent response in overlying coronal loops that evolve through different temperatures. Using the method we recently developed, we infer empirical heating functions from the rapid rise of the UV light curves for the two loop systems, respectively, treating them as two big loops of cross-sectional area 5\arcsec by 5\arcsec, and compute the plasma evolution in the loops using the EBTEL model (Klimchuk et al. 2008). We compute the synthetic EUV light curves, which, with the limitation of the model, reasonably agree with observed light curves obtained in multiple AIA channels and EIS lines: they show the same evolution trend and their magnitudes are comparable by within a factor of two. Furthermore, we also compare the computed mean enthalpy flow velocity with the Doppler shift measurements by EIS during the decay phase of the two loops. Our results suggest that the two different loops with different heating functions as inferred from their footpoint UV emission, combined with their different lengths as measured from imaging observations, give rise to different coronal plasma evolution patterns captured both in the model and observations.Comment: Accepted for publication in Ap

    Properties of the Fractured Glacial Till at the Madison County, Ohio, Field Workshop Pit Site

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    Author Institution: USDA/ARS, Soil Drainage Research Unit ; School of Natural Resources, The Ohio State University ; Department of Food, Agricultural and Biological Engineering, The Ohio State UniversityWater and contaminants obviously do move through the so-called impermeable glacial tills in Ohio. This study was conducted to illustrate the extensive presence of fractures in the till and to quantify the differences in hydraulic conductivity and physical and chemical properties between the fractureaffected zones and the till matrix. In situ measurements of the saturated hydraulic conductivity were made in small boreholes positioned either in the matrix or intersecting the fractures. Soil samples from both the fracture faces and the matrix were analyzed for particle size distribution, clay mineralogy, calcite, dolomite, and iron content. Hydraulic conductivity measured in boreholes intersecting fractures was 1.25 x 105 cm/sec (0.018 in/hr), one order of magnitude greater than in boreholes in the matrix. Particle size distribution was the same for the fracture faces and the matrix. The fracture faces showed no significant change in total clay content and a slight increase in expandable clay. Calcite content was 62% greater, dolomite content was 6% lower, and iron content was 73% lower on the fracture faces as compared to the matrix. The fractures affected approximately 7% of the soil volume
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