Rapid upskilling about COVID-19 vaccines: an evaluation of a novel interprofessional education workshop

Background: An inter-professional education (IPE) workshop centred around newly approved COVID-19 vaccination was attended by 77 nursing and pharmacy students. Aim: To embed and evaluate the implementation of a virtual IPE workshop, and to upskill undergraduate nursing and pharmacy students about the COVID-19 vaccination. Methods: The workshop was evaluated using a questionnaire completed by participants from both disciplines. A focus group was conducted with the IPE facilitators. Results: 77 students out of a potential 400 attended the workshop (19% attendance). Of the 77 participants, 44 (23 nursing, 21 pharmacy) completed the questionnaire (57%), rating the content highly. There was overall positivity toward working interprofessionally, and there was no evidence of significant differences between how the two groups of students rated the workshop. Qualitative findings from students and facilitators corroborated the supposition that the workshop would enhance professional development. Thus, the workshop was successful in facilitating interprofessional interactions, with students all working collaboratively toward the same goal, the ultimate purpose of IPE. It was agreed that such an event should be included as part of the student curricula.Conclusion: Implementing an IPE event that includes real-time healthcare priorities can contribute to optimising students' healthcare education. More high-quality longitudinal research is needed to understand the impact of such sessions on students' competence and confidence

Considering Soil Potassium Pools with Dissimilar Plant Availability

Soil potassium (K) has traditionally been portrayed as residing in four functional pools: solution K, exchangeable K, interlayer (sometimes referred to as “fixed” or “nonexchangeable”) K, and structural K in primary minerals. However, this four-pool model and associated terminology have created confusion in understanding the dynamics of K supply to plants and the fate of K returned to the soil in fertilizers, residues, or waste products. This chapter presents an alternative framework to depict soil K pools. The framework distinguishes between micas and feldspars as K-bearing primary minerals, based on the presence of K in interlayer positions or three-dimensional framework structures, respectively; identifies a pool of K in neoformed secondary minerals that can include fertilizer reaction products; and replaces the “exchangeable” K pool with a pool defined as “surface-adsorbed” K, identifying where the K is located and the mechanism by which it is held rather than identification based on particular soil testing procedures. In this chapter, we discuss these K pools and their behavior in relation to plant K acquisition and soil K dynamics

Soil mineral weathering/ Editor: J.A. Kittrick

xiii, 271 hal.; 25 cm

Factors influencing the transport of actinides in the groundwater environment. Final report

This report summarizes investigations of factors that significantly influence the transport of actinide cations in the groundwater environment. Briefly, measurements of diffusion coefficients for Am(III), Cm(III), and Np(V) in moist US soils indicated that diffusion is negligible compared to mass transport in flowing groundwater. Diffusion coefficients do, however, indicate that, in the absence of flowing water, actinide elements will migrate only a few centimeters in a thousand years. The remaining investigations were devoted to the determination of distribution ratios (K/sub d/s) for representative US soils, factors influencing them, and chemical and physical processes related to transport of actinides in groundwaters. The computer code GARD was modified to include complex formation to test the importance of humic acid complexing on the rate of transport of actinides in groundwaters. Use of the formation constant and a range of humic acid, even at rather low concentrations of 10/sup -5/ to 10/sup -6/ molar, significantly increases the actinide transport rate in a flowing aquifer. These computer calculations show that any strong complexing agent will have a similar effect on actinide transport in the groundwater environment. 32 references, 9 figures