357 research outputs found

    School Psychology Shortages in West Virginia

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    The United States continues to experience a shortage of school psychologists nationwide which has been found to impact both students and school psychologists in negative ways. There is a broad scope of practice that school psychologists are competently able to provide but are physically unable to deliver because of their need to focus on required assessments and testing. Overwhelming workloads can create stress and lead to burnout. However, little research has been done to understand the shortage of school psychologists in the country, including the state of West Virginia. To better understand West Virginia’s shortage problem, this researcher conducted a survey successfully completed by one participant from 47 of the 55 counties in West Virginia. It was found that 33 of 47 counties currently had a ratio of students to school psychologists higher than the nation’s average ratio of students to school psychologists (1:1,381). Only 4 counties met the NASP recommended ratio of no more than 1,000 students per school psychologist. Ratios did not vary by size or location of the county. Common reasons believed by participants for shortages include inadequate numbers of students produced by graduate programs, lack of interest due to salary, and lack of awareness about the profession. Common strategies to address the shortages include utilizing contract psychologists and advertising positions. Recommendations for future studies include expanding the current study to have a wider population by surveying contracted school psychologists and special education teachers

    The effects of interdisciplinary team size on student achievement, behavior, attendance, and student perceptions about community

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    This study explored the impact of interdisciplinary team size on student achievement, behavior, attendance, and perceptions about community in an affluent Midwestern suburban middle school. Interdisciplinary teams were divided up in to three-, four- and five-teacher configurations. Data were gathered through the use of the district\u27s School Information and Management System (SIMS) as well as the School Ethical Climate Index (SECI) (Schulte et al., 2002). The dependent variables were (a) academic achievement, (b) student behavior, (c) student attendance, and (d) student perceptions about community. Independent variables were the interdisciplinary team and grade level. All four research questions were answered using the two-way analysis of variance conducted at the .01 level to control for Type I errors. A total of 210 out of 213 students (98.6%) participated in the study

    Brittle Fracture of Dental Amalgam

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    Peer Reviewedhttp://deepblue.lib.umich.edu/bitstream/2027.42/67331/2/10.1177_00220345650440053801.pd

    Making a Place for the Next Generation of Geoscientists

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    Early-career scientists from the AGU Mentoring Network discuss how the global pandemic has exacerbated long-standing issues with the availability of positions in and the diversity of the geosciences.</jats:p

    The fate of sediment, wood and organic carbon eroded during an extreme flood, Colorado Front Range, USA

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    Identifying and quantifying the dominant processes of erosion and tracking the fate of sediment, wood, and carbon eroded during floods is important for understanding channel response to floods, downstream sediment and carbon loading, and the influence of extreme events on landscapes and the terrestrial carbon cycle. We quantify sediment, wood, and organic carbon (OC) from source to local sink following an extreme flood in the tectonically quiescent, semi-arid Colorado (USA) Front Range. Erosion of >500,000 m3 or as much as ~115 yr of weathering products occurred through landsliding and channel erosion during September 2013 flooding. More than half of the eroded sediment was deposited at the inlet and delta of a water supply reservoir, resulting in the equivalent of 100 yr of reservoir sedimentation and 2% loss in water storage capacity. The flood discharged 28 Mg C/km2, producing an event OC flux equivalent to humid, tectonically active areas. Post-flood remobilization resulted in a further ~100 yr of reservoir sedimentation plus export of an additional 1.3 Mg C/km2 of wood, demonstrating the ongoing impact of the flood on reservoir capacity and carbon cycling. Pronounced channel widening during the flood created accommodation space for 40% of flood sediment and storage of wood and eroded carbon. We conclude that confined channels, normally dismissed as transport reaches, can store and export substantial amounts of flood constituents

    Luminescence Dating Without Sand Lenses: an Application of Osl to Coarse-grained Alluvial Fan Deposits of the Lost River Range, Idaho, USA

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    Optically stimulated luminescence (OSL) dating is increasingly used to estimate the age of fluvial deposits. A significant limitation, however, has been that conventional techniques of sampling and dose rate estimation are suitable only for thick (\u3e60 cm) layers consisting of sand size or finer grains. Application of OSL dating to deposits lacking such layers remains a significant challenge. Alluvial fans along the western front of the Lost River Range in east-central Idaho, USA are one example. Deposits are typically pebble to cobble sheetflood gravels with a sandy matrix but thin to absent sand lenses. As a result, the majority of samples for this project were collected by excavating matrix material from gravelly deposits under light-safe tarps or at night. To examine the contributions of different grain-size fractions to calculated dose-rates, multiple grain-size fractions were analyzed using ICP–MS, high resolution gamma spectrometry and XRF. Dose rates from bulk sediment samples were 0.4–40% (mean of 18%) lower than dose-rate estimates from the sand-size fractions alone, illustrating the importance of representative sampling for dose rate determination. We attribute the difference to the low dose-rate contribution from radio-nuclide poor carbonate pebbles and cobbles that occur disproportionately in clast sizes larger than sand. Where possible, dose rates were based on bulk sediment samples since they integrate the dose-rate contribution from all grain sizes. Equivalent dose distributions showed little evidence for partial bleaching. However, many samples had significant kurtosis and/or overdispersion, possibly due to grain-size related microdosimetry effects, accumulation of pedogenic carbonate or post-depositional sediment mixing. Our OSL age estimates range from 4 to 120 ka, preserve stratigraphic and geomorphic order, and show good agreement with independent ages from tephra correlation and U-series dating of pedogenic carbonate. Furthermore, multiple samples from the same deposit produced ages in good agreement. This study demonstrates that with modified sampling methods and careful consideration of the dose rate, OSL dating can be successfully applied to coarse-grained deposits of climatic and tectonic significance that may be difficult to date by other methods
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