Building an Institutional Repository: Managing Faculty Publication and Author Rights Workflow in the Wyoming Scholars Repository

Wyoming Scholar’s Repository (WySR), is an initiative by the University of Wyoming Libraries to support our scholars and provide a Green Open Access solution. WySR (http://repository.uwyo.edu/) disseminates a wide variety of scholarship, including faculty papers, student scholarship, conference proceedings, and journals. The Digital Collections office and the Scholarly Communication Librarian have been implementing and managing WySR by searching our purchased electronic materials, relying on the SHERPA/RoMEO database of publisher policies, and communicating with faculty to seek permissions to bring their scholarly publications into the repository. This presentation will discuss the differences among four colleges at the University of Wyoming: College of Business, College of Education, College of Engineering, and the Department of History in the College of Arts and Sciences with respect to the number of journal articles in the publisher PDF version (known as the version of record) that have been ingested into WySR. The workflow will be addressed in detail and includes copyrights and accession policies for deposit into WySR with SHERPA/RoMEO and a process of seeking permission from publishers to deposit the publisher PDF version on the author’s behalf. This workflow uncovered disciplinary differences with regard to Green Open Access and surrounding issues affecting the practices of self-archiving, copyrights, accession policies, faculty participation and the strategy for outreach to our colleagues across the academy

Student Success: Open Access Repository Work Impacts University Libraries\u27 Student Employees

This presentation will identify new methods for in the libraries student employment program related to Open Access repository work. The hands on learning opportunities are focused on publishing production workflows, including: CV checking; author rights and permissions for depositing faculty papers in the UTA’s institutional repository; and creating a research metrics report to provide alternative impact measurements of the faculty’s publications in support of tenure and promotion packet of materials. Additional production processes include learning layout design and project management in publishing monographs and journals through a variety of publishing tools, such as: Open Journal Systems (OJS), Pressbooks, and InDesign. The student work experience enhances the educational development and growth of students by providing training through a variety of library engagement. For example, shadowing the librarian, attending individual consultation with a faculty, or discussing ways to enhance the workflow. Scholarly Communication System learning outcomes for the student employees include understanding the research and publishing cycles, basic copyright issues, Memorandum of Understanding (MOU), publication process and timeline, author agreements, publisher policies, and other practices in OA publishing. When students have a detailed knowledge in OA their contributions to the Libraries increases and builds their confidence and sense of belonging that they will carry with them into their bright futures. We will share additional details of student roles and related workflows, how their experiences translate to marketable skills in the workforce, and how they are more knowledgeable of rights management through the lens of Open Access repository work

Modelling of the LTDE-SD radionuclide diffusion experiment in crystalline rock at the Aspo Hard Rock Laboratory (Sweden)

This study shows a comparison and analysis of results from a modelling exercise concerning a field experiment involving the transport and retention of different radionuclide tracers in crystalline rock. This exercise was performed within the Swedish Nuclear Fuel and Waste Management Company (SKB) Task Force on Modelling of Groundwater Flow and Transport of Solutes (Task Force GWFTS). Task 9B of the Task Force GWFTS was the second subtask within Task 9 and focused on the modelling of experimental results from the Long Term Sorption Diffusion Experiment in situ tracer test. The test had been performed at a depth of about 410m in the Aspo Hard Rock Laboratory. Synthetic groundwater containing a cocktail of radionuclide tracers was circulated for 198 days on the natural surface of a fracture and in a narrow slim hole drilled in unaltered rock matrix. Overcoring of the rock after the end of the test allowed for the measurement of tracer distribution profiles in the rock from the fracture surface (A cores) and also from the slim hole (D cores). The measured tracer activities in the rock samples showed long profiles (several cm) for non-or weakly-sorbing tracers (Cl-36, Na-22), but also for many of the more strongly-sorbing radionuclides. The understanding of this unexpected feature was one of the main motivations for this modelling exercise. However, re-evaluation and revision of the data during the course of Task 9B provided evidence that the anomalous long tails at low activities for strongly sorbing tracers were artefacts due to cross-contamination during rock sample preparation. A few data points remained for Cs-137, Ba-133, Ni-63 and Cd-109, but most measurements at long distances from the tracer source (>10mm) were now below the reported detection limits. Ten different modelling teams provided results for this exercise, using different concepts and codes. The tracers that were finally considered were Na-22, Cl-36, Co-57, Ni-63, Ba-133, Cs-137, Cd-109, Ra-226 and Np-237. Three main types of models were used: i) analytical solutions to the transport-retention equations, ii) continuum -porous-medium numerical models, and iii) microstructure-based models accounting for small-scale heterogeneity (i.e. mineral grains, porosities and/or microfracture distributions) and potential centimetre-scale fractures. The modelling by the different teams led to some important conclusions, concerning for instance the presence of a disturbed zone (a few mm in thickness) next to the fracture surface and to the wall of the slim hole and the role of micro-fractures and cm-scale fractures in the transport of weakly sorbing tracers. These conclusions could be reached after the re-evaluation and revision of the experimental data (tracer profiles in the rock) and the analysis of the different sets of model results provided by the different teams.Peer reviewe