| 1. |
- Alrutz, Marie, et al.
(författare)
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Projektledning
- 2013
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Bok (populärvet., debatt m.m.)abstract
- Projektledning är ett yrke med egen certifiering. Det pågår en spännande utveckling inom området och det blir allt viktigare att hålla sig ajour med utvecklingen.Det övergripande målet med den här handboken är att vara en ständigt aktuell heltäckande bok om projektarbete. Innehållsmässigt täcker den både frågor som har med struktur och styrning att göra och frågor om ledning av människor och mänskliga processer i grupp. Kompetens inom projekt byggs av både kunskap och erfarenhet. Vi följer kontinuerligt aktuell forskning inom dessa områden och bjuder in intressanta forskare att medverka som författare. Vi skildrar verkliga projekt och låter erfarenheterna få plats, både de bästa erfarenheterna och de utmaningar som man tagit sig igenom.Handboken är levande och det innebär att artiklar tas bort för att ge plats för nya, i takt med att den uppdateras fortlöpande.
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| 2. |
- Friberg, Stina, et al.
(författare)
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Grundutbildade sjuksköterskors upplevelse att börja arbeta på en barnavdelning
- 2016
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Ingår i: Nordisk sygeplejeforskning. - : Scandinavian University Press / Universitetsforlaget AS. - 1892-2678 .- 1892-2686. ; 6:1, s. 20-33
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Tidskriftsartikel (refereegranskat)abstract
- Basic trained nurses experience to start working on a children’s wardThe aim of the study was to describe nurses trained to a basic level experience of starting work on a children's ward. A qualitative study has been conducted with a purposively drawn sample of informants. Semi-structured interviews were conducted with eight basic trained nurses. Data were analyzed using qualitative content analysis. The results showed that respondents felt that the pediatrics course is not preparing for the professional work with children. Most felt that it was through real situations in the workplace that they gained necessary knowledge. Furthermore, it was found that only a few were satisfied with the induction. Spending time with many different supervisors was an important factor for experiencing dissatisfaction with the induction. Good support was received from employees; however the support of the organization was poor. Conclusion: Today's undergraduate education in nursing does not include enough pediatrics to prepare students for professional work with children and adolescents. Actions at individual and workplace levels are needed to increase knowledge of the basic trained nurse. Continuity and support during the induction is important for newly employed nurses to feel competent in their work.
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| 3. |
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| 4. |
- Jansson, Joel, et al.
(författare)
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Targeted (re)-socialization in universities and prisons : a policy study concerning tutor and tutee
- 2015
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Ingår i: Abstract book NERA 2015. ; , s. 1-1
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Konferensbidrag (refereegranskat)abstract
- The paper present a sub-study included in a curriculum theory project on targeted socialization within two institutions of major importance for the Nordic welfare states enculturation, universities and prisons. We compare the relationship between supervisor/doctoral student and correctional contact persons/inmates. There are some apparent differences between these two contexts. Universities are mostly discussed in terms of socialization and learning, prisons more often as institutions where inmates are in need of re-socialization whether they approve or not. Students enter doctoral education as a result of a qualified meritocratic selection process, and success will produce holders of the highest exam possible. Inmates qualify for prison by being convicted for a crime in a court of law, and are deprived of their liberty as they are incarcerated. In addition, prison has a mixed purpose of being about retribution and deterrence, as well as rehabilitation. In this substudy we compare aspects of targeted (re)-socialization processes, from a curriculum theory perspective, regarding the two relationships mentioned above. In other words, the tutoring relationship between tutors and tutees in the contexts of doctoral education and inmate rehabilitation. We pay special attention to the transactions of knowledge, norms, values and identities offered in both cases. The empirical material consists of policy-texts on a national (laws for prisons/ probation, higher education and policy-texts concerning the correctional contact persons)-and a local level (enforcement plans, individual study planes and policy-texts concerning PhD supervision). Preliminary results of this sub-study is that the targeted (re)-socialization process of these two activities have both similarities and difference. This opens up for further research questions on how similarities are played out through the differences between the two institutions in objectives and contents (curriculum), educational forms (pedagogy) and assessment activities (evaluation).
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| 5. |
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| 6. |
- Sahlin, Eva A. U., et al.
(författare)
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Connectivity analyses of valley patterns indicate preservation of a preglacial fluvial valley system in the Dyfi basin, Wales
- 2009
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Ingår i: Proceedings of the Geologists' Association. - : Elsevier BV. - 0016-7878. ; 120, s. 245-255
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Forskningsöversikt (refereegranskat)abstract
- Coastal valleys in the west part of Mid-Wales, such as the Mawddach, Dysynni, Tal-y-Ilyn and Dyfi, acted as corridors for ice which drained the Welsh Ice Cap during the Devensian. Analyses of detailed digital elevation models, and interpretation of satellite images and aerial photographs, show the existence of large variations in the amount of glacial modification between these valleys. Although all the valleys are glacially over-deepened along late Caledonian fault lines, only the Dyfi basin exhibits a dendritic pattern, with V-shaped cross-profiles and valley spurs typical of valleys formed by fluvial processes. Connectivity analysis of the Dyfi basin shows that it exhibits an almost completely dendritic pattern with connectivity alpha and beta values of 0.74 and 1.01, respectively, with little glacial modification of the preglacial fluvial valley pattern in the form of glacial valley breaching. Several examples of glacial meltwater incision into a well-developed pre-existing river valley system, causing river capture across watersheds, have been identified in the Dyfi basin. The degree of preservation of the preglacial fluvial valley system within the Dyfi basin indicates limited modification by glacial processes, despite the area being subjected to glacier activity during the Late Devensian at least. It is possible that major parts of the basin were covered by cold-based or slow-moving ice, close to, or under, a migrating ice-divide, with the major ice drainage Occurring along the weaker zone of the Pennal Fault along which teh Dyfi valley is located, causing minor adjustments to the Surrounding interfluves and uplands. it is proposed here that the general river valley morphology of the Dyfi basin is of a pre-Late Devensian age.
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| 7. |
- Sahlin, Eva A.U. 1971-, et al.
(författare)
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Connectivity analyses of valley patterns reveal Devensian glacial drainage activity in Mid-Wales (poster)
- 2009
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Konferensbidrag (övrigt vetenskapligt/konstnärligt)abstract
- Coastal valleys in the west part of Mid-Wales, such as the Mawddach, Dysynni, Tal-y-llyn and Dyfi, are believed to have acted as corridors for ice which drained the Welsh Ice Cap during the Devensian. Connectivity analyses of valley patterns from detailed digital elevation models, and interpretation of satellite images and aerial photographs show the existence of large variations in the amount of glacial modification between these valleys. Although all the valleys are glacially over-deepened along Silurian fault lines, only the Dyfi basin exhibits a dendritic pattern, with V-shaped cross profiles and valley spurs typical of valleys formed by fluvial processes.The connectivity analyses show that the Dyfi basin exhibits a purely dendritic pattern with little glacial modification of the preglacial fluvial valley pattern in form of valley breaching. It is proposed here that the general river valley morphology of the Dyfi basin is of a pre-Late Devensian age. This suggests a complex glacial drainage history, where cold-based ice was not only confined to the interior uplands, but also covered low-altitude areas previously believed to be a major drainage conduit for the Welsh Ice Cap. This indicates that Late Devensian glacial erosion was not as intense as previously believed and larger areas might have been overlain by cold-based ice.
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| 8. |
- Sahlin, Eva A.U. 1971-, et al.
(författare)
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Evidence for cold-based ice at low altitudes : Preservation of a preglacial fluvial valley system in the Dyfi basin, Wales (poster)
- 2009
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Konferensbidrag (övrigt vetenskapligt/konstnärligt)abstract
- Coastal valleys in the west part of mid-Wales, such as the Mawddach, Dysynni, Tal-y-llyn and Dyfi, are believed to have acted as corridors for ice which drained the Welsh Ice Cap during the Devensian. Analysis of detailed digital elevation models and interpretation of satellite images and aerial photographs show the existence of large variations in the amount of glacial modification between these valleys. Although all the valleys are glacially over-deepened along Silurian fault lines, only the Dyfi basin exhibits a dendritic pattern, with V-shaped cross profiles and valley spurs typical of valleys formed by fluvial processes. Connectivity analysis of the Dyfi basin shows that it exhibits a nearly dendritic pattern with connectivity α and β values of 0.74 and 1.01 respectively, with little glacial modification of the preglacial fluvial valley pattern in the form of valley breaching. It is proposed that the general river valley morphology of the Dyfi basin is of a pre-Late Devensian age. Several examples have been identified of glacial meltwater incision into a well-developed pre-existing river valley system, causing river capture across watersheds. The degree of preservation of the pre-glacial fluvial valley system within the Dyfi basin indicates limited modification by glacial processes, despite the area being subjected to Late Devensian glacier activity. It is possible that major parts of the basin were covered by cold-based or slow-moving ice close to or under a migrating ice divide, with the major ice drainage occurring along the weaker zone of the Pennal Fault, causing minor adjustments to the surrounding interfluves and uplands.
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