Development of a counselling and psychotherapy supervision training program within an Australian educational context.

Although supervision has been a significant component of counselling and psychotherapy practice since the days of Freud, it appears that only since the professionalisation of this industry has supervision become a requirement for ongoing practice. Indeed, it can be argued that supervision is becoming a profession in its own right as it is increasingly recognised that not only does the supervisee benefit in a multitude of ways, but ultimately it is the welfare of the client that is of prime concern. In Australia, the registration process only began in 1999 and as such, is still defining its role amongst the 'helping* professions and government bodies. Although there are clear statements regarding the amount of supervision hours required for both training and ongoing professional practice for counsellors and psychotherapists, there is still work to be achieved in both defining supervisor qualifications and designing an ethical code of practice. At the macro level, a motivation behind this project was my desire for greater personal lucidity about the nature of supervision and the characteristics that determine a good supervisor within the strictures of an educational establishment. One of the possible outcomes was to contribute to the registration definitions. More specifically, the intent was to design a training program for supervisors that was congruent with the needs of supervisees and was cross-theoretical in orientation to allow potential supervisors to develop their own personal model of working. This project documents the phenomenological research I undertook with recently graduated Master of Counselling participants. One of the principle intentions was to explore each individuals underlying meaning and intent towards supervision. Equally, the aim was to develop increased clarity about the nature of supervision itself. The results of this research in combination with other materials were used to develop a supervision training program that was run over 12 weeks in March 2003 and then evaluated for future developments. In the course of this research, a framework of supervision emerged which I have defined as the 'Wheel of Supervision', which has the potential for further evolution in terms of future training and further publications. This 'Wheel of Supervision’ is a new and different way of viewing supervision from both the supervisor and supervise e perspective

The Uniform Environmental Covenants Act: Why, How, and Whether

With contaminated land, it sometimes makes sense to do a partial cleanup, rather than a complete one, and combine the cleanup with land use restrictions and continuing obligations to monitor the land. The Uniform Environmental Covenants Act creates a new state law property interest to make these restrictions and obligations permanent and enforceable. It addresses issues created by traditional common law doctrines that were hostile to permanent land restrictions, as well as more contemporary problems presented by tax liens, eminent domain, and adverse possession. This Article reviews the Act’s legal infrastructure for creating, enforcing, and modifying the terms of the land use restrictions and monitoring obligations. The Article argues that the Act’s legal infrastructure provides parties with the legal certainty needed to encourage future cleanups, while also protecting against environmental risks that the residual contamination could otherwise pose. These cleanups, often financed as part of the property’s redevelopment, are particularly useful because they are a way to return blighted properties to the stream of commerce. The Act has drawn some criticism, primarily for not going further with its protections, and these are reviewed at the end of the Article

Hydrogen safety Progress report no. 6, 1 Apr. - 30 Jun. 1965

Hydrogen safety hazards, storage, and handling - Hydrogen plume studies to determine quantity-distance criteria and guidelines for optimum placement of hydrogen detector

Hydrogen safety Progress report no. 7 1 Jul. - 30 Sep. 1965

Performance characteristics of two console-type hydrogen gas detectors sampling by diffusion and convectio

Metapopulation dynamics of the softshell clam, Mya arenaria

Submitted in partial fulfillment of the requirements for the degree of Doctor of Philosophy at the Massachusetts Institute of Technology and the Woods Hole Oceanographic Institution June 2008In this dissertation, I explored metapopulation dynamics and population connectivity, with a focus on the softshell clam, Mya arenaria. I first worked towards developing a method for using elemental signatures retained in the larval shell as a tag of natal habitat. I designed and implemented an experiment to determine whether existing methods commonly used for fishes would be applicable to bivalves. I found that the instrumentation and setup I used were not able to isolate and measure the first larval shell of M. arenaria. In concert with developing this method for bivalves, I reared larval M. arenaria in the laboratory under controlled conditions to understand the environmental and biological factors that may influence elemental signatures in shell. My results show that growth rate and age have significant effects on juvenile shell composition, and that temperature and salinity affect larval and juvenile shell composition in variable ways depending on the element evaluated. I also examined the regional patterns of diversity over the current distribution of M. arenaria using the mitochondrial gene, cytochrome oxidase I (COI). I found minimal variability across all populations sampled, suggesting a recent population expansion in the Northwest Atlantic. Finally, I employed theoretical approaches to understand patch dynamics in a two-patch metapopulation when one patch is of high quality and the other low quality. I developed a matrix metapopulation model and compared growth rate elasticity to patch parameters under variable migration scenarios. I then expanded the model to include stochastic disturbance. I found that in many cases, the spatial distribution of individuals within the metapopulation affects whether growth rate is most elastic to parameters in the good or bad patch.Financial support was provided by the National Defense Science and Engineer- ing Graduate Fellowship; the WHOI Academic Programs O±ce; NSF grants OCE- 0326734, OCE-0215905, OCE-0349177, DEB-0235692, DMS-0532378, and ATM-0428122; and by NOAA National Sea Grant College Program O±ce, Department of Commerce, under Grant No. NA86RG0075 (Woods Hole Oceanographic Institution Sea Grant Project No. R/0-32), and Grant No. NA16RG2273 (WHOI Sea Grant Project No. R/0-35)

Carbonate Sedimentation Rates Today and in the Past: Holocene of Florida Bay, Bahamas, and Bermuda vs. Upper Jurassic and Lower Cretaceous of the Jura Mountains (Switzerland and France)

Lagoonal to intertidal sediments from the Holocene in Florida Bay, on the Bahamas, and in Bermuda are compared to similar facies in the Kimmeridgian and Berriasian of the Swiss and French Jura Mountains. Dating by 14C permits the estimation of sediment accumulation rates in the Holocene. In the ancient outcrops, the timing is given by cyclostratigraphic analysis. Elementary depositional sequences formed in tune with the 20-ka precession cycle, although much of this time may have been spent in non-deposition and/or erosion. After decompaction of the ancient sequences, their accumulation rates can be evaluated. It is suggested that the studied Holocene sediments accumulated over the past 6000 years with rates of 0.3 to 3 mm/a, whereas the Kimmeridgian and Berriasian facies show somewhat lower rates of 0.07 to 0.6 mm/a. This difference may be due to metho­dological errors, but also to variable carbonate production. In shallow carbonate systems, much of the sediment produced may be redistributed over the platform or exported. Furthermore, basin morpho­logy and currents can strongly influence facies and thickness of the accumulated sediment. Finally, the accumulated sediment may suffer further erosion before it is preserved in the sedimentary record. Consequently, when estimating sedimentation rates in ancient sequences, it is important to do this with the highest time resolution possible, and only after having decompacted the sediment and evaluated the time lost in hiatuses or condensed intervals