Improving Teacher Job Satisfaction: The Roles of Social Capital, Teacher Efficacy, and Support

In this study, we examine how social capital, teacher efficacy, and organizational support increase teacher job satisfaction. Research suggests that teachers worldwide are exceedingly dissatisfied with their jobs and have significantly higher levels of turnover than their counterparts in other professions. We investigate this phenomenon using a sample of 122 elementary school teachers. We found that teachers’ centrality position, or each teacher’s relationship with every other teacher, in their school’s trust network and the density of a teacher’s academic advice ego-network predicted the development of teacher job satisfaction. Additionally, we found that teacher efficacy mediated the relationship between teacher’s trust and academic advice relationships and job satisfaction, and perceived organizational support strengthened the relationship between teacher efficacy and job satisfaction. The article concludes by offering implications of the findings for both administrators and teachers as well as for the social capital, teaching efficacy, and teacher job satisfaction literatures

What’s in Your Gifted Education Online Teacher Professional Development? Incorporating Theory- and Practice-Based Elements of Instructional Learning Design

This paper examined six theory- and practice-based elements of instructional learning design in online teacher professional development (oTPD), how these elements were implemented into Edinger’s (2017) PACKaGE model of gifted education oTPD, and how teachers evaluated each element. Elements were based on Berge’s (1995) instructor roles model theory and gifted education research. Each element was evaluated by teachers (N=184) who completed oTPD designed from the PACKaGE model. Self-report survey findings suggest that teachers considered most elements, such as asynchronous discussion board and article review assignments, to be useful to a great extent to their gifted education learning and pedagogy. However, teachers reported less usefulness for the online group project element. This finding directly contrasts with researchers’ suggestions for oTPD. These findings may encourage teachers to choose theory- and research-based oTPD. PD designers can investigate and implement oTPD elements that satisfy instructional design model needs for optimal teacher learning and gifted education pedagogy

Online Teacher Professional Development for Gifted Education: Examining the Impact of a New Pedagogical Model

This paper theoretically develops and examines the outcomes of a pilot study that evaluates the PACKaGE Model of online Teacher Professional Development (the Model). The Model was created to facilitate positive pedagogical change within gifted education teachers’ practice, attitude, collaboration, content knowledge, and goal effectiveness. Kirkpatrick and Kirkpatrick’s (2006) model of training evaluation suggests that trainees should evaluate the training for satisfaction at the time the training is completed, as well as six months after, to evaluate for behavior change. Applying Kirkpatrick and Kirkpatrick’s (2006) model, findings indicate that teachers were immediately satisfied with the Model’s effectiveness, adequacy and overall quality. Six months after the online teacher professional development, teachers indicated a strong positive change in each of the five gifted education pedagogical components. Overall, these preliminary findings suggest that the use of the Model creates a positive change within teachers’ gifted education pedagogy

Saturn 5/Voyager load relief study Final report

Load relief control system to improve launch probability of Saturn 5 booster with Voyager payloa

Placenta-Derived Mesenchymal Stromal Cells: Modulation of Immunity and Inflammation

As an organ generally discarded after a normal full-term birth, the placenta is one of the most studied organs from the cellular standpoint. The placenta contains large numbers of immune cells, stem cells, and stromal cells. These cell types spurred the field of regenerative medicine by catalyzing the establishment of cord blood banks and hematopoietic stem cell reconstitution in the treatment of many diseases including cancer. Previously, many scientific articles and reviews have focused on the production, phenotype, and functional characterization of bone marrow-derived mesenchymal stromal cells. In this chapter, the focus will be solely on the biology, phenotype, and functional characterization of placenta-derived stromal cells. Modulation of the immune response, including T cell proliferation, dendritic cell maturation, and monocyte differentiation by placenta-derived stromal cells, will be discussed. This chapter will span in vitro functional analyses, animal models highlighting the in vitro data culminating in a summary of current clinical activity

Saturn 5/Voyager load relief study Data base report

Saturn 5/Voyager load relief control syste

Ariel - Volume 4 Number 6

Editors David A. Jacoby Eugenia Miller Tom Williams Associate Editors Paul Bialas Terry Burt Michael Leo Gail Tenikat Editor Emeritus and Business Manager Richard J. Bonnano Movie Editor Robert Breckenridge Staff Richard Blutstein Mary F. Buechler J.D. Kanofsky Rocket Weber David Maye

Arctic sea-ice decline archived by multicentury annual-resolution record from crustose coralline algal proxy

Northern Hemisphere sea ice has been declining sharply over the past decades and 2012 exhibited the lowest Arctic summer sea-ice cover in historic times. Whereas ongoing changes are closely monitored through satellite observations, we have only limited data of past Arctic sea-ice cover derived from short historical records, indirect terrestrial proxies, and low-resolution marine sediment cores. A multicentury time series from extremely long-lived annual increment-forming crustose coralline algal buildups now provides the first high-resolution in situ marine proxy for sea-ice cover. Growth and Mg/Ca ratios of these Arctic-wide occurring calcified algae are sensitive to changes in both temperature and solar radiation. Growth sharply declines with increasing sea-ice blockage of light from the benthic algal habitat. The 646-y multisite record from the Canadian Arctic indicates that during the Little Ice Age, sea ice was extensive but highly variable on subdecadal time scales and coincided with an expansion of ice-dependent Thule/Labrador Inuit sea mammal hunters in the region. The past 150 y instead have been characterized by sea ice exhibiting multidecadal variability with a long-term decline distinctly steeper than at any time since the 14th century

Enigmatic deep-water mounds on the Orphan Knoll, Labrador Sea

Deep-sea mounds can have a variety of origins and may provide hard-substrate features in depths that are normally dominated by mud. Orphan Knoll, a 2 km high bedrock horst off northeast Newfoundland, hosts more than 200 mounds, or mound complexes, of unknown composition, in water depths of 1720–2500 m. Most mounds are 10–600 m high, with average mound height 187 m, and 1–3 km wide. The study objective was to characterize the size, shape, orientation, and composition of the enigmatic Orphan Knoll mounds, in order to determine their age and origin. Archival ship-based side-scan sonar, multibeam sonar, airgun, high-resolution sparker and 3.5 kHz acoustic sub-bottom profiling, and newly acquired ship-based multibeam sonar, video transects by remotely operated vehicle (ROV), rock samples, and near-bottom multibeam sonar data were analyzed. Four mounds were studied during two ROV dives. Archival sidescan sonar data show > 200 mounds. Sparker profiles show that the mound crests are covered by condensed stratified Quaternary sediment and airgun seismic data show faults reaching near the seafloor. New multibeam sonar data show mounds are dominantly conical to elliptical in shape, but without preferred orientation or alignment. Remotely operated vehicle (ROV) transects and near-bottom multibeam showed that three mounds were rounded and symmetrically arranged, while a fourth was more asymmetrical, with steep faces on the southwestern and southeastern flanks, where finely bedded to massive sedimentary bedrock outcropped dipping 15–45°SW. Rock samples from the mounds include Eocene calcareous ooze and mid-Miocene bedded pelagic limestone. Thick ferromanganese crusts were found on many surfaces, obscuring possible outcrops from physical sampling. Polymetallic nodules were found on the slope of one mound. Ice-rafted detritus, including igneous and metamorphic rocks and Paleozoic limestone and dolostone, was common in the sediments immediately surrounding the mounds. Quaternary sub-fossil solitary scleractinian corals accumulated over a span of at least 0.18 Ma at the base of one mound. The presence of uplifted condensed Eocene-Miocene rocks on the mounds and faulting in seismic profiles suggest uplift during reactivation of old rift-related faults during the Neogene, with seabed mass wasting creating residual mounds, which were then draped by Quaternary proglacial muds. Sculpting of hemipelagic Quaternary sediment by bottom currents probably contributed to mound morphology