8,716 research outputs found

    Cemetery Board

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    Cemetery Board

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    Cemetery Board

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    Smoking and intention to quit in deprived areas of Glasgow: is it related to housing improvements and neighbourhood regeneration because of improved mental health?

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    Background: People living in areas of multiple deprivation are more likely to smoke and less likely to quit smoking. This study examines the effect on smoking and intention to quit smoking for those who have experienced housing improvements (HI) in deprived areas of Glasgow, UK, and investigates whether such effects can be explained by improved mental health. Methods: Quasi-experimental, 2-year longitudinal study, comparing residents’ smoking and intention to quit smoking for HI group (n=545) with non-HI group (n=517), adjusting for baseline (2006) sociodemographic factors and smoking status. SF-12 mental health scores were used to assess mental health, along with self-reported experience of, and General Practitioner (GP) consultations for, anxiety and depression in the last 12 months. Results: There was no relationship between smoking and HI, adjusting for baseline rates (OR=0.97, 95% CI 0.57 to 1.67, p=0.918). We found an association between intention to quit and HI, which remained significant after adjusting for sociodemographics and previous intention to quit (OR 2.16, 95% CI 1.12 to 4.16, p=0.022). We found no consistent evidence that this association was attenuated by improvement in our three mental health measures. Conclusions: Providing residents in disadvantaged areas with better housing may prompt them to consider quitting smoking. However, few people actually quit, indicating that residential improvements or changes to the physical environment may not be sufficient drivers of personal behavioural change. It would make sense to link health services to housing regeneration projects to support changes in health behaviours at a time when environmental change appears to make behavioural change more likely

    Open Futures: an enquiry- and skills- based educational programme developed for primary education and its use in tertiary education

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    Open Futures is a transforming enquiry-based and skills-based system for education that is central to the curriculum, linking learning and life. It was developed to help children discover and develop practical skills, personal interests and values, which will contribute to their education and help to enhance their adult lives. Open Futures works in partnership with groups of schools in local clusters to develop a bespoke training programme, which extends the existing curriculum and nurtures independent learning through pupil-led approaches to personal learning. Schools benefit from the experience, knowledge and support of like-minded education professionals locally, nationally and internationally. Working with schools and their communities in the UK and India, Open Futures has been running with widespread success for 9 years. It now reaches more than 30,000 children in the UK. There is a body of independent evidence from primary and secondary education showing that both individual strands, as well as the complete Open Futures programme, significantly improve learner outcomes. We now wished to move Open Futures into the tertiary education sector. It was felt that an Open Futures approach to learning and teaching, particularly involving askit, would be beneficial to the community of learners at Central Bedfordshire Further Education College, rated Grade 2 by Ofsted in October 2013. Training has been in three areas so far: Construction, Public Services and Pathways (i.e. Learners with learning difficulties and disabilities). In all cases, there were significant positive impacts for learners and for teachers. As experience with Open Futures develops in the College, it should become clear how such a central enquiry-based and skills-based approach will help learners, and provide evidence for the use of Open Futures in tertiary education that could be used in other tertiary educational institutions

    Nature and dynamics of late Miocene/early Pliocene Ice-Sheet grounding events on the Pacific margin of the Antarctic Pennisula outer continental shelf

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    Package-3 unconformities identified by Bart and Anderson (1995) were mapped to evaluate their glacial unconformity interpretation using a regional grid of single channel seismic data from the Antarctic Peninsula outer continental shelf. Detailed correlations show many crosscutting relationships within Package 3 such that the unconformities and units they bound are not regionally continuous across the margin. Comparison of Package-3 unconformities with the modern bathymetry reveals that cross-shelf trough and bank morphology is absent, which indicates that ice streams probably did not exist on the shelf during Package-3 time. On the continental shelf, only the middle part of Package 3 is sampled at ODP Leg 178 sites (1097 and 1103 on the southern and northern sectors of the margin, respectively.) Although mapping results do not uniquely require/preclude ice sheet grounding, taken together, the diamict lithology and crosscutting supports the interpretation of waxing and waning of grounded ice on the outer continental shelf. Chronostratigraphic resolution at Leg 178 sites on the continental shelf is too coarse to allow unconformity-to-unconformity correlations between Package-3 strata sampled at the two shelf drill sites. At most, fifteen (15) Package-3 glacial unconformities are found at any one location, and this represents the most conservative estimate of the maximum number of grounding events from the perspective of regional shelf stratigraphy. Basinward of the continental shelf, coeval section sampled on continental-rise drift 6 at ODP site 1095 exhibits distinct meter-scale bioturbation events, capping thick (up to 20 m) unbioturbated section, interpreted to result from \u3e30 glacial episodes. The large difference between the minimum estimate of shelf grounding events (15) and the number of glacial cycles deduced from drift lithology (30) suggests either 1) amalgamation of shelf glacial unconformities, or 2) lithologic alternations on the rise reflect phenomena unrelated to grounding events. Chlorite-smectite covariance at drift 6, interpreted to represent ~16 glacial episodes, shows much better correspondence to the minimum number of Package-3 glacial unconformities. However, the poor covariance between the two drift-derived proxies (bioturbation and clay mineralogy) demonstrates that one or both may be recording something other than grounding events on the adjacent shelf
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