Supervisory Working Alliance as a Predictor for Counselor Burnout: The Potential Mediating Role of Supervisee Nondisclosure

Clinical supervision sometimes lacks the elements necessary for a rigorous, helpful, and meaningful experience for the supervisee. The purpose of this study was to examine the relationships between the supervisory working alliance, supervisee nondisclosure (i.e., when a supervisee does not communicate information that would otherwise be shared with the supervisor), and counselor burnout, specifically in a sample of counselors, social workers, and psychologists pursuing their original state licenses. Nondisclosure was examined to determine if it was a mediator of the relationship between the supervisory working alliance and burnout. Participants (n = 288) completed a demographic questionnaire, the supervisee form of the Working Alliance Inventory (Bahrick, 1989), the Disclosure in Supervision Scale (Gunn & Pistole, 2012), and the Maslach Burnout Inventory-Human Services Survey (Maslach, Jackson, & Leiter, 1997). Final analyses showed that supervisee nondisclosure did not mediate the relationship between the supervisory working alliance and burnout. However, the supervisory working alliance predicted nondisclosure (b = -.73, p \u3c .001) and burnout (b = -.41, p \u3c .001). Other major findings involving the various subscales of working alliance and burnout are reported and discussed; these have implications for future research, clinical supervision, and training. Limitations are also discussed. The supervisory working alliance seemed to be of utmost importance to developing counselors’ experiences as they pursued their state licenses

Budding Nationalism in the Black Garden; Nagorno Karabakh and the Role of Conflict in Developing Azerbaijani National Identity

Azerbaijan\u27s war with Armenia in late 2020, was dubbed the Patriotic War by Azerbaijani President Ilham Aliyev and his supporters. Emphasizing the nature of conflict with Armenia as the greatest possible expression of Azerbaijani nationalism, the Aliyev cabinet has utilized the conflict to generate popular support for the authoritarian government. This paper delves into the history of Azerbaijan to flesh out the roots of the conflict and better understand how Azerbaijanis understand their own national identity

Hungarian Historical Hysteria

This paper analyzes the deployment of Hungary\u27s historical memory of national movements by Viktor Orban and FIDESZ. This deployment is designed to cement Orban\u27s authoritarian grip over Hungary, as historical threats to Hungarian nationalism are invoked to legitimize Orban\u27s goal of an illiberal democracy

Carbon Doping of MgB2 by Toluene and Malic-Acid-in-Toluene

The decomposition of malic acid in the presence of Mg and B was studied using Differential Scanning Calorimetry (DSC) and Thermogravimetric Analysis (TGA) which revealed that malic acid reacted with Mg but not B. Also, the addition of toluene to dissolve malic acid followed by subsequent drying resulted in no reaction with Mg, indicating that the malic acid had decomposed during the dissolution/drying stage. The total carbon contributed by toluene versus a toluene/5 wt% malic acid mixture was measured using a LECO CS600 carbon analyzer. The toluene sample contained ~0.4 wt% C while the toluene/malic acid mixture had ~1.5 wt% C, demonstrating that the toluene contributed a significant amount of carbon to the final product. Resistivity measurements on powder-in-tube MgB2 monofilamentary wires established that the toluene/malic acid doped sample had the highest Bc2. However, the toluene-only sample had the highest transport Jc over most of the magnetic field range (0-9 T), equaled only by that of toluene/malic acid sample in fields above 9 T.Comment: 17 pages, 6 figures, 1 tabl

The Commons: Volume 3, Issue 1

Table of Contents Letter From the EditorsLILA BERNARDIN AND HANNAH WILLIAMS Who Sent the Devil Down to Georgia?KRIS BOHNENSTIEHL The Dehumanizing Gaze: Race in the Context of Academic TourismLEONA DERANGO Balancing Populations of Electoral DistrictsETHAN STERN-ELLI

Frequency-magnitude distribution of microearthquakes beneath the 9°50′N region of the East Pacific Rise, October 2003 through April 2004

Relocated hypocentral data from a 7-month deployment (October 2003 to April 2004) of ocean bottom seismometers provide an opportunity to map microearthquake frequency-magnitude distributions (FMDs) along the 9°49–52′N region on the East Pacific Rise. These analyses, which incorporate more than 9000 earthquakes, represent the first investigation of the 3-D spatial and temporal patterns of FMDs along any mid-ocean ridge spreading center. The data are described well by a Gutenberg-Richter model, indicating a power law or fractal relationship between earthquake size and frequency. The scaling exponent, or b value, shows significant spatial variability, exceeding a value of 2.0 at the shallowest depths on axis and dropping below 1.0 away from the axial trough. This spatial pattern is consistent with an inverse relationship between b value and ambient stress conditions, with the lowest stress levels at shallow depths and relatively high stress levels (or low pore pressures) observed away from the axial zone. Intermediate b values are observed on-axis above the ridge system's melt lens; however, within this region there also exists significant spatial variability. This indicates that stress conditions and/or structural heterogeneity may vary at subkilometer scales within the hydrothermal circulation cell. Although the observational period is characterized by increasing seismicity rates, building toward an eruptive episode in January 2006, the first-order spatial pattern of b values is sustained, with no overall temporal trend. As a byproduct of this b value analysis, the detection capabilities of the array are assessed empirically

Soundscape manipulation enhances larval recruitment of a reef-building mollusk

© The Author(s), 2015. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in PeerJ 3 (2015): e999, doi:10.7717/peerj.999.Marine seafloor ecosystems, and efforts to restore them, depend critically on the influx and settlement of larvae following their pelagic dispersal period. Larval dispersal and settlement patterns are driven by a combination of physical oceanography and behavioral responses of larvae to a suite of sensory cues both in the water column and at settlement sites. There is growing evidence that the biological and physical sounds associated with adult habitats (i.e., the “soundscape”) influence larval settlement and habitat selection; however, the significance of acoustic cues is rarely tested. Here we show in a field experiment that the free-swimming larvae of an estuarine invertebrate, the eastern oyster, respond to the addition of replayed habitat-related sounds. Oyster larval recruitment was significantly higher on larval collectors exposed to oyster reef sounds compared to no-sound controls. These results provide the first field evidence that soundscape cues may attract the larval settlers of a reef-building estuarine invertebrate.Funding was provided by the National Science Foundation (Grants OCE-1234688 & ISO-1210292). Additional support for experimental materials came from a PADI Foundation Grant (#5145) and a National Shellfisheries Association Melbourne R. Carriker Student Research Grant to AL

Hydroacoustic monitoring of oceanic spreading centers : past, present, and future

Author Posting. © The Oceanography Society, 2012. This article is posted here by permission of The Oceanography Society for personal use, not for redistribution. The definitive version was published in Oceanography 25, no. 1 (2012): 116–127, doi:10.5670/oceanog.2012.10.Mid-ocean ridge volcanism and extensional faulting are the fundamental processes that lead to the creation and rifting of oceanic crust, yet these events go largely undetected in the deep ocean. Currently, the only means available to observe seafloor-spreading events in real time is via the remote detection of the seismicity generated during faulting or intrusion of magma into brittle oceanic crust. Hydrophones moored in the ocean provide an effective means for detecting these small-magnitude earthquakes, and the use of this technology during the last two decades has facilitated the real-time detection of mid-ocean ridge seafloor eruptions and confirmation of subseafloor microbial ecosystems. As technology evolves and mid-ocean ridge studies move into a new era, we anticipate an expanding network of seismo-acoustic sensors integrated into seafloor fiber-optic cabled observatories, satellite-telemetered surface buoys, and autonomous vehicle platforms.SOSUS studies discussed in this paper were supported by the NOAA Vents Program and during 2006–2009 by the National Science Foundation, Grant OCE-0623649

Seafloor seismicity, Antarctic ice-sounds, cetacean vocalizations and long-term ambient sound in the Indian Ocean basin

International audienceThis paper presents the results from the Deflo-hydroacoustic experiment in the Southern Indian Ocean using three autonomous underwater hydrophones, complemented by two permanent hydroacoustic stations. The array monitored for 14 months, from November 2006 to December 2007, a 3000 x 3000 km wide area, encompassing large segments of the three Indian spreading ridges that meet at the Indian Triple Junction. A catalogue of 11 105 acoustic events is derived from the recorded data, of which 55 per cent are located from three hydrophones, 38 per cent from 4, 6 per cent from five and less than 1 per cent by six hydrophones. From a comparison with land-based seismic catalogues, the smallest detected earthquakes are m(b) 2.6 in size, the range of recorded magnitudes is about twice that of land-based networks and the number of detected events is 5-16 times larger. Seismicity patterns vary between the three spreading ridges, with activity mainly focused on transform faults along the fast spreading Southeast Indian Ridge and more evenly distributed along spreading segments and transforms on the slow spreading Central and ultra-slow spreading Southwest Indian ridges; the Central Indian Ridge is the most active of the three with an average of 1.9 events/100 km/month. Along the Sunda Trench, acoustic events mostly radiate from the inner wall of the trench and show a 200-km-long seismic gap between 2 degrees S and the Equator. The array also detected more than 3600 cryogenic events, with different seasonal trends observed for events from the Antarctic margin, compared to those from drifting icebergs at lower (up to 50 degrees S) latitudes. Vocalizations of five species and subspecies of large baleen whales were also observed and exhibit clear seasonal variability. On the three autonomous hydrophones, whale vocalizations dominate sound levels in the 20-30 and 100 Hz frequency bands, whereas earthquakes and ice tremor are a dominant source of ambient sound at frequencies < 20 Hz