CONTEXTUALIZING SELF-DETERMINATION WITHIN A MENTAL HEALTH RECOVERY ORIENTED SERVICE AND SUPPORT SYSTEM In consultation with fellow research team members

Abstract There is increasing convergence of defining mental health recovery as the ongoing, interactional process/personal journey and outcome of restoring a positive sense of self and meaningful sense of belonging while actively self-managing psychiatric disorder and rebuilding a life within the community

Estimated payments to employment service providers for persons with mental illness in the Ticket to Work program

OBJECTIVE: The Ticket to Work and Work Incentives Improvement Act of 1999 removes work disincentives and promotes access to vocational services for people with disabilities. This study calculated the amount of payments that would have been made to employment service providers if study participants had been enrolled in the Ticket program. METHODS: Data were from 450 Social Security Disability Insurance beneficiaries with psychiatric disabilities enrolled in a multisite study of supported employment. Earnings over two years were used to calculate provider payments under two reimbursement formulas used in the Ticket program. RESULTS: Only a quarter of service recipients (26 percent) reached earnings levels that would have triggered provider payments under the first reimbursement formula. Only 4 percent would have completed their trial work period and left the rolls, generating payments under the second formula. CONCLUSIONS: The current provider payment systems of the Ticket to Work program do not reflect the reality of rehabilitation for individuals with severe mental illness. Reforms should take into account outcomes of return-to-work services for this population

Terminal Pleistocene to early Holocene volcanic eruptions at Zuni Salt Lake, west-central New Mexico, USA

Zuni Salt Lake (ZSL) is a large maar in the Red Hill-Quemado volcanic field located in west-central New Mexico in the southwestern USA. Stratigraphic analysis of sections in and around the maar, coupled with optically stimulated luminescence (OSL) and accelerator mass spectrometry (AMS) C-14 dating, indicate that ZSL volcanic activity occurred between similar to 13.4 and 9.9 ka and was most likely confined to a <= 500-year interval sometime between similar to 12.3 and 11.0 ka. The basal volcanic unit consists of locally widespread basaltic ash fallout interpreted to represent a violent or wind-aided strombolian eruption tentatively attributed to Cerro Pomo, a scoria cone similar to 10 km south of ZSL. Subsequent eruptions emanated from vents near or within the present-day ZSL maar crater. Strombolian eruptions of multiple spatter and scoria cones produced basaltic lava and scoria lapilli fallout. Next, a phreatomagmatic eruption created the maar crater and surrounding tephra rim and apron. ZSL eruptions ended with strombolian eruptions that formed three scoria cones on the crater floor. The revised age range of ZSL is younger and more precise than the 190-24 ka 2-sigma age range derived from previous argon dating. This implies that other morphologically youthful, argon-dated volcanoes on the southern margin of the Colorado Plateau might be substantially younger than previously reported.National Science Foundation IGERT Fellowship in Archaeological Science from the University of Arizona; Geological Society of America Graduate Student Research Grant [10716-14]; P.E.O. Scholar Award; Department of Geosciences, University of Arizona12 month embargo; First Online: 04 January 2017This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at [email protected]

A search for long-timescale, low-frequency radio transients

This article has been accepted for publication in Monthly Notices of the Royal Astronomical Society. © 2017 The Author(s). Published by Oxford University Press on behalf of the Royal Astronomical Society. All rights reserved.We present a search for transient and highly variable sources at low radio frequencies (150-200 MHz) that explores long timescales of 1-3 years. We conducted this search by comparing the TIFR GMRT Sky Survey Alternative Data Release 1 (TGSS ADR1) and the GaLactic and Extragalactic All-sky Murchison Widefield Array (GLEAM) survey catalogues. To account for the different completeness thresholds in the individual surveys, we searched for compact GLEAM sources above a flux density limit of 100 mJy that were not present in the TGSS ADR1; and also for compact TGSS ADR1 sources above a flux density limit of 200 mJy that had no counterpart in GLEAM. From a total sample of 234 333 GLEAM sources and 275 612 TGSS ADR1 sources in the overlap region between the two surveys, there were 99658 GLEAM sources and 38 978 TGSS ADR sources that passed our flux density cutoff and compactness criteria. Analysis of these sources resulted in three candidate transient sources. Further analysis ruled out two candidates as imaging artefacts. We analyse the third candidate and show it is likely to be real, with a flux density of 182 +/- 26 mJy at 147.5 MHz. This gives a transient surface density of rho = (6.2 +/- 6) x 10-5 deg-2 . We present initial follow-up observations and discuss possible causes for this candidate. The small number of spurious sources from this search demonstrates the high reliability of these two new low-frequency radio catalogues.Peer reviewe