Exoskeletons and the Future of Work: Envisioning Power and Control in a Workforce Without Limits

Exoskeletons are an emerging form of technology that combines the skills of both machines and humans to give wearers the ability to complete physically demanding tasks that would be too strenuous for most humans. Exoskeleton adoption has the potential to both enhance and disrupt many aspects of work, including power dynamics in the workplace and the human-machine interactions that take place. Dyadic Power Theory (DPT) is a useful theory for exploring the impacts of exoskeleton adoption. In this conceptual paper, we extend DPT to relationships between humans and machines in organizations, as well as human-human communication where use of an exoskeleton has resulted in shifts of power

The challenges of implementing a spatial ability intervention at secondary level

Spatial skills development has been widely examined throughout the literature, with evidence suggesting many cognitive abilities are malleable and can be improved through targeted solutions. Some previous examples of intervention studies have been shown to reduce the gap between genders, and those of a lower socio-economic status where the training increased spatial ability, as well as in discipline-specific educational performance. These findings align with many national agendas for STEM diversity, which strive to increase participation and performance of such under-represented groups in STEM. With a lot of research being conducted around spatial skill development within a university level setting, or outside of a formal educational context completely, the applicability of such training interventions in a secondary level school context is unclear. With secondary level education aiming to develop many cognitive abilities, including spatial ability as outlined in curriculum documents, the implementation of such an intervention could improve student outcomes and add value to the educational experience of the students. With the time-sensitive nature of secondary level schooling, there are many concerns around the amount of time and effort that needs to be invested to successfully implement such an intervention. Through the piloting of a spatial training intervention, this paper focusses on the development of spatial skills within an upper secondary level setting in Ireland with 358 students aged 14-16 enrolled in the Transition Year programme and their 10 teachers. This paper examines the challenges of implementation of a specific spatial skills intervention, through a variety of lenses, including pedagogy based and performance based, and offers considerations for future research in the area. By looking from both teacher and student perspectives, we explore the issues encountered and offer suggestions to researchers conducting similar studies at secondary level

Implementation and analysis of a spatial skills course for Secondary level STEM education

High spatial skills have been directly linked to enhanced performance in STEM disciplines, with improvements in spatial skills linked to an increase in female retention at the university level. Spatial skills development and direct training are well researched and implemented within university level engineering education but are less defined at earlier stages of education. It is hypothesised that a spatial intervention implemented at the secondary level could be beneficial in order to boost student performance in STEM, where it still influences their interest in subjects and future career paths. The purpose of this paper is to present the implementation process of a spatial intervention in Irish secondary schools and the initial analysis of combined teacher and student data. The intervention was implemented with Transition Year (aged ~15 to 16 years old) students. Fifty teachers undertook a tailored professional development training to prepare them to deliver the spatial skills intervention, some of which then took part in various qualitative data gathering activities. The intervention was delivered to approximately 1500 students. They were administered a range of psychometric tests, including multiple spatial tests and a fluid reasoning test to investigate their development in a variety of cognitive aspects. This paper will focus on investigating the possible relationships between teacher spatial ability and student gains in spatial ability. The findings of the study were positive, indicating the successful implementation of the intervention and showing promise for future iterations

Risk of hospitalisation or death in households with a case of COVID-19 in England: an analysis using the HOSTED dataset

Objective: To determine whether household contacts of confirmed cases of COVID-19 have an increased risk of hospitalisation or death. Methods: We used the HOSTED dataset of index cases of COVID-19 in England between June and November 2020, linked to Secondary Uses Service data on hospital episodes and Office for National Statistics’ mortality data. Multivariable logistic regression models of the odds of household contacts being hospitalised or dying within six weeks of an index case, adjusted for case type, age, sex and calendar month were calculated. Excess risk was determined by comparing the first six weeks after the index case with 6-12 weeks after the index case in a survival analysis framework. Results: Index cases were more likely to be hospitalised or die than either secondary cases or non-cases, having adjusted for age and sex. There was an increased risk of hospitalisation for non-cases (adjusted hazard ratio (aHR) 1.10 (95% CI 1.04, 1.16)) and of death (aHR 1.57 (95% CI 1.14, 2.16)) in the first six weeks after an index case, compared to 6-12 weeks after. Conclusion: Risks of hospitalisation and mortality are predictably higher in cases compared to non-cases. The short-term increase in risks for non-case contacts following diagnosis of the index case may suggest incomplete case ascertainment among contacts, although this was relatively small

Ecological and temperature controls on Mg/Ca ratios of Globigerina bulloides from the southwest Pacific Ocean

We present Mg/Ca data for Globigerina bulloides from 10 core top sites in the southwest Pacific Ocean analyzed by laser ablation inductively coupled plasma mass spectrometry (LA-ICPMS). Mg/Ca values in G. bulloides correlate with observed ocean temperatures (7 degrees C-19 degrees C), and when combined with previously published data, an integrated Mg/Ca-temperature calibration for 7 degrees C-31 degrees C is derived where Mg/Ca (mmol/mol) = 0.955 x e(0.068 x T) (r(2) = 0.95). Significant variability of Mg/Ca values (20%-30%) was found for the four visible chambers of G. bulloides, with the final chamber consistently recording the lowest Mg/Ca and is interpreted, in part, to reflect changes in the depth habitat with ontogeny. Incipient and variable dissolution of the thin and fragile final chamber, and outermost layer concomitantly added to all chambers, caused by different cleaning techniques prior to solution-based ICPMS analyses, may explain the minor differences in previously published Mg/Ca-temperature calibrations for this species. If the lower Mg/Ca of the final chamber reflects changes in depth habitat, then LA-ICPMS of the penultimate (or older) chambers will most sensitively record past changes in near-surface ocean temperatures. Mean size-normalized G. bulloides test weights correlate negatively with ocean temperature (T = 31.8 x e(-30.5xwtN); r(2) = 0.90), suggesting that in the southwest Pacific Ocean, temperature is a prominent control on shell weight in addition to carbonate ion levels

Multi-proxy validation of glacial-interglacial rainfall variations in southwest Sulawesi

Speleothem δ18O is widely used as a proxy for rainfall amount in the tropics on glacial-interglacial to interannual scales. However, uncertainties in the interpretation of this renowned proxy pose a vexing problem in tropical paleoclimatology. Here, we present paired multi-proxy geochemical measurements for stalagmites from southwest Sulawesi, Indonesia, and confirm changes in rainfall amount across ice age terminations. Collectively, the stalagmites span two glacial-interglacial transitions from ~380,000 to 330,000 and 230,000 to 170,000 years ago. Mg/Ca in the slow-growing stalagmites is affected by water moving through the karst and prior calcite precipitation, making it a good proxy for changes in local rainfall. When paired, Mg/Ca and δ18O corroborate prominent shifts from drier glacials to wetter interglacials in the core of the Australasian monsoon domain. These shifts in rainfall occur 4,000-7,000 years later than glacial-interglacial increases in global temperature and the associated response of Sulawesi vegetation, determined by speleothem δ13C

Reassessing the post-Last Glacial Maximum retreat history from the Southwest Ross Sea

Constraining the timing of the retreat of the Last Glacial Maximum (LGM) Antarctic Ice Sheet in the Ross Sea provides insights into the processes controlling marine-based ice sheet retreat. The over-deepened Ross Sea continental shelf is an ideal configuration for marine ice-sheet instability, and this region was thought to be one of the largest Antarctic contributors to post-LGM sea level rise. However, the chronology and pattern of retreat of the LGM ice sheet in the Ross Sea is largely constrained by coastal records along the Transantarctic Mountain front in the Western Ross Sea. Although these offer more reliable dating techniques than marine sediment cores, they may be influenced by local glaciers derived from East Antarctic outlet glaciers. Consequently, these coastal records may be ambiguous in the broader context of retreat in the central regions of the Ross Sea. However, previous studies have inferred that records in this region retreated in a north to south pattern, and was fed by ice sourced from the central Ross Sea – with the implication that broader ice sheet retreat in the central Ross Sea occurred as late as the mid Holocene. We present two lines of evidence that counter this established interpretation of the pattern of retreat in the Ross Sea: 1) a sedimentary facies succession and foraminifera-based radiocarbon chronology from within the Ross Sea embayment that indicates glacial retreat and open marine conditions to the east of Ross Island was already in place before 8.6 cal ka BP, at least 1 kyr earlier than indicated by terrestrial records in McMurdo Sound; and 2) a new multibeam swath bathymetry data that identifies well-preserved glacial features indicating thick (>700m) marine-based ice derived from the East Antarctic Ice Sheet (EAIS) coastal outlet glaciers dominated the ice sheet input into the southwestern Ross Sea during the last phases of glaciation – and thus may have acted independent of any ice in the central Ross Sea embayment. Comparing these data to new modelling experiments, we hypothesize that marine-based ice sheet retreat was triggered by oceanic forcings along most of the Pacific Ocean coastline of Antarctica, but continued early Holocene retreat into the inner shelf region of the Ross Sea occurred primarily as a consequence of marine ice sheet instability. Keywords: Ross Sea, deglaciation, Last Glacial Maximum, Holocen

Sensitivity of the West Antarctic Ice Sheet to +2 °C (SWAIS 2C)

The West Antarctic Ice Sheet (WAIS) presently holds enough ice to raise global sea level by 4.3 m if completely melted. The unknown response of the WAIS to future warming remains a significant challenge for numerical models in quantifying predictions of future sea level rise. Sea level rise is one of the clearest planet-wide signals of human-induced climate change. The Sensitivity of the West Antarctic Ice Sheet to a Warming of 2 ∘C (SWAIS 2C) Project aims to understand past and current drivers and thresholds of WAIS dynamics to improve projections of the rate and size of ice sheet changes under a range of elevated greenhouse gas levels in the atmosphere as well as the associated average global temperature scenarios to and beyond the +2 ∘C target of the Paris Climate Agreement. Despite efforts through previous land and ship-based drilling on and along the Antarctic margin, unequivocal evidence of major WAIS retreat or collapse and its causes has remained elusive. To evaluate and plan for the interdisciplinary scientific opportunities and engineering challenges that an International Continental Drilling Program (ICDP) project along the Siple coast near the grounding zone of the WAIS could offer (Fig. 1), researchers, engineers, and logistics providers representing 10 countries held a virtual workshop in October 2020. This international partnership comprised of geologists, glaciologists, oceanographers, geophysicists, microbiologists, climate and ice sheet modelers, and engineers outlined specific research objectives and logistical challenges associated with the recovery of Neogene and Quaternary geological records from the West Antarctic interior adjacent to the Kamb Ice Stream and at Crary Ice Rise. New geophysical surveys at these locations have identified drilling targets in which new drilling technologies will allow for the recovery of up to 200 m of sediments beneath the ice sheet. Sub-ice-shelf records have so far proven difficult to obtain but are critical to better constrain marine ice sheet sensitivity to past and future increases in global mean surface temperature up to 2 ∘C above pre-industrial levels. Thus, the scientific and technological advances developed through this program will enable us to test whether WAIS collapsed during past intervals of warmth and determine its sensitivity to a +2 ∘C global warming threshold (UNFCCC, 2015)

Spirit, mind and body: the archaeology of monastic healing

Archaeology and material culture are used in this chapter to consider how monastic experience responded to illness, ageing and disability. The approach taken is influenced by the material study of religion, which interrogates how bodies and things engage to construct the sensory experience of religion, and by practice-based approaches in archaeology, which examine the active role of space and material culture in shaping religious agency and embodiment. The archaeology of monastic healing focuses on the full spectrum of healing technologies, from managing the body in order to prevent illness, through to the treatment of the sick and preparation of the corpse for burial

Reducing initial loss to follow up among people with bacteriologically confirmed tuberculosis: LINKEDin, a quasi-experimental study in South Africa

Every person diagnosed with tuberculosis (TB) needs to initiate treatment. The WHO estimated 61% of people who developed TB in 2021 were included in a TB treatment registration system. Initial loss to follow up (ILTFU) is the loss of persons to care between diagnosis and treatment initiation/registration. LINKEDin, a quasi-experimental study, evaluated the effect of two interventions (hospital-recording and an alert-and-response patient management intervention) in six sub-districts across three high-TB burden provinces of South Africa. Using integrated electronic reports, we identified all persons diagnosed with TB (Xpert MTB/RIF positive) in hospital and at primary healthcare facilities. We prospectively determined linkage to care at 30 days after TB diagnosis. We calculated the risk of ILTFU during the baseline and intervention periods and the relative risk reduction in ILTFU between these periods. We found a relative reduction in ILTFU of 42.4% (95%CI:28.5,53.7) in KwaZulu Natal (KZN) and 22.3% (95%CI:13.3,30.4) in the Western Cape (WC) with no significant change in Gauteng. In KZN and the WC, the relative reduction in ILTFU appeared greater in sub-districts where the alert-and-response patient management intervention was implemented; KZN (49.3% (95%CI:32.4,62) vs 32.2% (95%CI:5.4,51.4)); and WC (34.2% (95%CI:20.9,45.3) vs 13.4% (95%CI:0.7,24.4)). We reported a notable reduction in ILTFU in two provinces using existing routine health service data and applying a simple intervention to trace and recall those not linked to care. TB programs need to consider ILTFU as a priority and develop interventions specific to their context to ensure improved linkage to care