Mineral chemistry and petrography of basalts from the Kimama drill core recovered by Hotspot: Snake River Scientific Drilling Project, Idaho establish crystallization conditions of these lavas. Twenty-three basalt samples, from 20 individual lava flows were sampled from the upper 1000 m (of the 1912 m drilled) core drilled on the axis of the Snake River Plain, and represent approximately 3 m.y. of volcanism (rocks at the bottom of the hole are ~6 Ma). Rock from the upper 1000 m are typically fresh, while those lower in the core are more altered and are less likely to preserve fresh phenocrysts to analyze. Intratelluric phenocrysts (pre-eruption) are: olivine, plagioclase and Cr-spinel inclusions in olivine and plagioclase; groundmass phases (post-eruption) are: olivine, plagioclase, clinopyroxene, magnetite and ilmenite. Olivine core compositions range from Fo84-68, plagioclase cores range from An80-62, clinopyroxene ranges in composition from Wo47-34, En47-28, Fs30-15, spinel inclusions are Cr (up to 20 wt % Cr2O3) and Al-rich (up to 35 wt % Al2O3) and evolve to lower concentrations of Cr and Al and higher Fe and Ti, chromian titanomagnetite to magnetite, and ilmenite are groundmass oxide phases. Thermobarometry of Kimama core basalts indicates that the phenocryst phases crystallized at temperatures of 1155 to 1255°C at depths of 7 to 17 km, which is within or near the seismically imaged mid-crustal sill. Plagioclase hygrometry suggests that these lavas are relatively anhydrous with less than 0.4 wt % H2O. Groundmass phases crystallized at lower temperatures (<1140°C) after eruption. Oxygen fugacity inferred from Fe-Ti oxide equilibria is at or just below the QFM buffer. The origin of the basaltic rocks of the Snake River Plain has been attributed to a mantle plume or to other, shallow mantle processes. Mineral and whole rock major and trace element geochemistry of the olivine tholeiites from the Kimama core are used to distinguish between these two sources (deep or shallow mantle). Whole rock compositions were corrected for plagioclase and olivine fractionation to calculate primary liquids to estimate mantle potential temperatures. Olivine phenocrysts have the pyroxenite source characteristics of low Mn and Ca, but a peridotite source characteristic of low Ni. Thus, trace element models were used to test whether there is pyroxenite in the source of the Snake River Plain basalts, as hypothesized for Hawaii and other plume-related hotspots (e.g., Sobolev et al., 2005; Herzberg, 2011). Olivine chemistry and trace element models establish that the basalt source is a spinel peridotite, not a pyroxenite. The average mantle potential temperature obtained for these samples is 1577°C, 177°C hotter than ambient mantle, suggesting that the basaltic liquids were derived from a thermal plume. Silica activity barometry shows that melt segregation occurs between 80 and 110 km depth, which is within or very near the spinel stability field, and suggests that the lithosphere has been eroded by the plume to a maximum depth of 80 km, and recent mantle tomography suggests that it may be even thinner.

Today's technical communicators enjoy an increasingly broader role and influence in the workplace, and are often given latitude to use engaging rhetoric and personal touches in many kinds of communications. Historical documents, particularly those that are substantially removed from our own era, can offer fresh approaches and insight into the enduring elements of successful communication. This study explores the technical writings of Benjamin Franklin and Thomas Jefferson and considers their usefulness to professionals today. Although the political writing of Franklin and Jefferson is more familiar, both men frequently wrote about scientific and technical subjects and were well-known in their day for these documents. Franklin created a captivating persona and arguments which carried emotional and logical appeal. Jefferson was a student of ancient rhetoric and applied classical principles of arrangement to guide readers. His fondness for statistical records led to a skill in presenting numerical data and other types of information in creative, efficient ways. By using tone, language, and description, both Franklin and Jefferson created technical narratives that are equally informative and aesthetically pleasing. The contemporary era of technical communication has been shaped by positivism, the plain language movement, and humanism, among other significant trends. Franklin's and Jefferson's approaches to technical communication both support and challenge the guiding philosophies of these movements. Their styles are reviewed in this study against the context of modern approaches. Opportunities for further historical study are also offered, including additional writings of our Founding Fathers and technical writing from the turn of the twentieth century.

The purpose of this essay has been to study the comprehensibility and the plainness of chapter 1 and 2 in “Läroplan, examensmål och gymnasiegemensamma ämnen för gymnasieskola 2011” that is one of the governing documents of Swedish upper secondary school. The Swedish government approved a national language policy in 2005 which involved an aim that the official Swedish language would be refined, easy and comprehensible. Plain language has since the eighties had a prominent place in Swedish research and science and is now a thought-out principle at almost every public authority. This essay has performed a linguistic text analysis, a plain language analysis, a plain language test and a critical discourse analysis on the two chapters from “Läroplan, examensmål och gymnasiegemensamma ämnen för gymnasieskola 2011” that is common for all upper secondary school programs. The chapters are not written in plain language and the comprehensibility of the document is low. There is no usage of a personal pronoun which makes the text harder to read, there are plenty of words that are hard to understand or old-fashioned. The usage of technical terms is also a problem due to the fact that no additional explanations to the terms are being offered. All citizens in Sweden need to be able to read and understand the governing documents of school at some time in their life and it is therefore very disturbing that the document is written in such a way that only a few can read and understand the text in full. This also renders the implementation more difficult and the consequence might be that we have an education that is not equivalent for all. The non-usage of plain language also makes it easier for the elite and more difficult for the non-elite which could help increase the social rifts and bring us back to a class society with huge rifts between classes. The usage of plain language increases democracy and the trust in public authorities; it would therefore have been desirable that the “Läroplan, examensmål och gymnasiegemensamma ämnen för gymnasiskola 2011” had been written in plain language.

Whole-rock and mineral compositions of three eruptive deposits from the Twin Falls caldera, associated with the Yellowstone hotspot, provide a window into melt generation and evolution for hot, dry, A-type rhyolites. Three rhyolitic units were sampled via the Kimberly drill-core as a part of project HOTSPOT, a study focused on mantle plume and continental lithosphere interaction. Previous work has been done to collect high resolution U-Pb zircon ages, and Hf- and O-isotopic compositions. This study examined the geochemistry of apatite and zircon along with host rock compositions in the context of this previous work. The Kimberly core sampled the Shoshone Rhyolite (6.06 Ma, 120 m thick), Kimberly Member (7.70 Ma, 169 m thick), and Castleford Crossing Member (7.96 Ma, >1400 m thick). Apatite compositions more closely reflect the composition of their whole rock hosts than zircons. SiO2 content is higher in apatite of the Kimberly Member at (1.1 ± 0.75 wt.%), vs (0.72 ± 0.47 wt.%) for the Castleford Crossing and (0.84 ± 0.27 wt.%) for the Shoshone Rhyolite. REEs compensate for Si substitution in these apatites, with the Kimberly Member most enriched. Volatile contents in the apatites are typical of metaluminous A-type rhyolites, with very low Cl and high F concentrations. Average Ti-in-zircon crystallization temperatures were highest in the Castleford Crossing Member (847 ± 68°C), followed by the Shoshone Rhyolite (806 ± 78°C), and then the Kimberly Member (804 ± 70°C). Oxygen fugacity calculated from zircons has average ΔQFM values for the Shoshone (0.8), Kimberly (-0.2), and Castleford Crossing (0.2). Hf concentrations and Eu anomalies are comparable in zircons from all three units. REE patterns in zircons are also similar and concentrations of REEs in the Shoshone and Kimberly units are similar even though the whole rock compositions of all three units are distinct. Less than 15% of zircons in the Kimberly and Castleford Crossing rhyolites have CL-dark cores enriched in several REEs, U, and Th. These CL-dark cored zircons are likely xenocrysts entrained from chemically evolved granite and then overgrown with less enriched rims prior to eruption. There are several apatite grains with Si-LREE enriched rims in the Kimberly Member, which serves as further evidence of assimilation of silicic igneous rock by the Kimberly Member before eruption. Principal component analysis of the geochemical data distinguishes between the units using both whole-rock and apatite compositions. However, zircon compositions are not statistically distinguishable using PCA. A global comparison of Ti, U, Th, Yb, and Nb concentrations in zircons show that the zircons in the Central Snake River Plain are similar to zircons in Hawaiian basalts, while younger zircons from Yellowstone formed in cooler more differentiated magma. We propose that the zircon and apatite chemical patterns and trends confirm the A-type origin of Snake River Plain rhyolites and make it unlikely that they represent partial melts of felsic continental crust but are instead derived in large part from partial melts of young mafic crust--the midcrustal sill.

No description available.

No description available.

No description available.

No description available.

The Virginia Runoff Reduction Method (RRM) was adopted in 2014 as a compliance tool for evaluation of stormwater volume and quality, and necessitates use of urban stormwater best management practices (BMPs) to meet regulatory standards. Coastal Virginia is characterized by flat terrain, shallow water tables, and low permeable soils that may limit the application of BMPs as recommended by state regulations. Soil morphological features are often used to estimate the seasonal high water table (SHWT) for initial feasibility, but existing soil data misrepresented expected SHWT depths in the Virginia Beach, VA, study area. A GIS-based methodology relying on perennial surface water elevations and USGS groundwater monitoring data was developed to estimate the SHWT depth in Virginia Beach. The SHWT map was shown to be consistently more reliable than available predictions based on soil morphology, and was used as input to a BMP siting tool. The tool, known as BMP Checker, was developed to explore how flat terrain, shallow water tables, and poor soils influence BMP siting in coastal Virginia. The BMP Checker algorithm was validated on 11 Virginia Beach sites before application on 10,000 ft2 (929 m2) area sections across the city. Citywide application showed that the most widely applicable BMPs in the study area include wet ponds that intercept groundwater and constructed wetlands. Conversely, sheet flow to conservation area and infiltration practices are the least applicable. Because the RRM assigns more credit to infiltration-based practices, sites in Virginia Beach may find it difficult to meet regulatory standards. / Master of Science

The relaxation of restrictions on the type of professions that can report films has resulted in radiographers and other healthcare professionals becoming increasingly involved in image interpretation in areas such as mammography, ultrasound and plain-film radiography. Little attention, however, has been given to sample size determinations concerning film-reading performance characteristics such as sensitivity, specificity and accuracy. Illustrated with hypothetical examples, this paper begins by considering standard errors and confidence intervals for performance characteristics and then discusses methods for determining sample size for studies of film-reading performance. Used appropriately, these approaches should result in studies that produce estimates of film-reading performance with adequate precision and enable investigators to optimize the sample size in their studies for the question they seek to answer.