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  • 1
    Online Resource
    Online Resource
    World Scientific Pub Co Pte Ltd ; 2020
    In:  Journal of Mechanics in Medicine and Biology Vol. 20, No. 08 ( 2020-10), p. 2030001-
    In: Journal of Mechanics in Medicine and Biology, World Scientific Pub Co Pte Ltd, Vol. 20, No. 08 ( 2020-10), p. 2030001-
    Abstract: In this paper, problems concerning the uniaxial experimental investigation of the human abdominal aortic aneurysm (AAA) biomechanical characteristics, concomitant values of the associated Cauchy stress, failure (ultimate) stress in AAA, and the constitutive modeling of AAA are considered. The aim of this paper is to review and compare the disposable experimental data, to reveal the reasons for the high dissipation of the results between studies, and to propound some unification criteria. We examined 22 literature sources published between 1994 and 2017 and compared their results, including our own results. The experiments in the reviewed literature have been designed to obtain the stress–strain characteristics and the failure (ultimate) stress and strain of the aneurysmal tissue. A variety of forms of the strain–energy function (SEF) have been applied in the considered studies to model the biomechanical behavior of the aneurysmal wall. The specimen condition and physical parameters, the experimental protocols, the failure stress and strain, and SEFs differ between studies, contributing to the differences between the final results. We propound some criteria and suggestions for the unification of the experiments leading to the comparable results.
    Type of Medium: Online Resource
    ISSN: 0219-5194 , 1793-6810
    Language: English
    Publisher: World Scientific Pub Co Pte Ltd
    Publication Date: 2020
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  • 2
    Online Resource
    Online Resource
    Peytchinski Publishing Ltd. ; 2021
    In:  Journal of IMAB - Annual Proceeding (Scientific Papers) Vol. 27, No. 1 ( 2021-03-25), p. 3643-3651
    In: Journal of IMAB - Annual Proceeding (Scientific Papers), Peytchinski Publishing Ltd., Vol. 27, No. 1 ( 2021-03-25), p. 3643-3651
    Abstract: Purpose: The aim of the study was to establish the socio-demographic and professional characteristics of the sample of dental assistants and their contributions to the efficiency of dental teamwork. Material and methods: An anonymous inquiry was conducted among 108 dental assistants working in dental offices in 4 Bulgarian cities. The questionnaire consisted of 18 questions about socio-demographic and professional characteristics of the sample and their opinion about obligations, positives and negatives in the workplace, and efficiency of teamwork. The methods used in the survey were sociological (poll) and statistical (alternative analysis). Results: The socio-demographic and professional characteristics of the surveyed dental assistants were established, such as: gender and age distribution, work in active working age/pension, types of working places, location of practices, types of education and number of dentists working with over the period of their work experience. All respondents reported that they assisted the physicians in the treatment process and the majorityf them (70.37- 85.19%) cleaned, disinfected and sterilized the instruments, the workplace and the premises of the practice. Only 4.6% dealt financialelations with the patients and worked directly in their mouths. The opinion of the respondents for building a well-functioning dental team was that both the personal and professional qualities of the team members were essential. Conclusions: Dental assistants were convinced of the benefits of their assistance; between 79.6% and 58.3% of them believed that they had contributed for quicker and better job of the doctor and to patient'somfort.
    Type of Medium: Online Resource
    ISSN: 1312-773X
    URL: Issue
    Language: Unknown
    Publisher: Peytchinski Publishing Ltd.
    Publication Date: 2021
    detail.hit.zdb_id: 2724123-3
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  • 3
    Online Resource
    Online Resource
    Peytchinski Publishing Ltd. ; 2021
    In:  Journal of IMAB - Annual Proceeding (Scientific Papers) Vol. 27, No. 2 ( 2021-04-01), p. 3663-3667
    In: Journal of IMAB - Annual Proceeding (Scientific Papers), Peytchinski Publishing Ltd., Vol. 27, No. 2 ( 2021-04-01), p. 3663-3667
    Abstract: PURPOSE: To compare the opinion of dentists and dental assistants about the advantagesf teamwork. MATERIAL AND METHODS: We conducted an anonymous survey of 110 dental practitioners and 108 dental assistants in four cities in Bulgaria. The questionnaires for the two groups include several identical questions that allow the respondents' opinions to be compared. The methods used are sociological (poll) and statistical (alternative analysis). RESULTS: The majority of dental assistants - 75% are convinced that every dentist should work with an assistant, while 58.6% of the doctors are of the same opinion. Almost the same number of surveyed doctors and dental assistants - mentioned as a strength of the teamwork a relief of the doctor's work (80.90 and 79.63%), an increase in the volume (68.18 and 57.40%) and quality (53.63 and 54.62%) of the medical activity and a reduction in working time (54.54 and 55.62 %). For dentists, the most important factors for creating a goodeam are observing rights and obligations (68.5%), mutual respect (67.6 %) and a relaxedork atmosphere (56.8%). For dental assistants, the most important factors for effective teamwork are mutual respect (74.1%) and the professionalualities of the dentist (72.2%). CONCLUSION: The results show a positive attitude of dental doctors and assistants to teamwork, albeit with varying degrees of conviction.
    Type of Medium: Online Resource
    ISSN: 1312-773X
    URL: Issue
    Language: Unknown
    Publisher: Peytchinski Publishing Ltd.
    Publication Date: 2021
    detail.hit.zdb_id: 2724123-3
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  • 4
    Online Resource
    Online Resource
    Elsevier BV ; 2016
    In:  Remote Sensing of Environment Vol. 182 ( 2016-09), p. 169-191
    In: Remote Sensing of Environment, Elsevier BV, Vol. 182 ( 2016-09), p. 169-191
    Type of Medium: Online Resource
    ISSN: 0034-4257
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2016
    detail.hit.zdb_id: 1498713-2
    SSG: 11
    SSG: 14
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  • 5
    In: Global Change Biology, Wiley, Vol. 24, No. 9 ( 2018-09), p. 3976-3989
    Abstract: Waterbodies in the arctic permafrost zone are considered a major source of the greenhouse gas methane ( CH 4 ) in addition to CH 4 emissions from arctic wetlands. However, the spatio‐temporal variability of CH 4 fluxes from waterbodies complicates spatial extrapolation of CH 4 measurements from single waterbodies. Therefore, their contribution to the CH 4 budget of the arctic permafrost zone is not yet well understood. Using the example of two study areas of 1,000 km² each in the Mackenzie Delta, Canada, we approach this issue (i) by analyzing correlations on the landscape scale between numerous waterbodies and CH 4 fluxes and (ii) by analyzing the influence of the spatial resolution of CH 4 flux data on the detected relationships. A CH 4 flux map with a resolution of 100 m was derived from two aircraft eddy‐covariance campaigns in the summers of 2012 and 2013. We combined the CH 4 flux map with high spatial resolution (2.5 m) waterbody maps from the Permafrost Region Pond and Lake Database and classified the waterbody depth based on Sentinel‐1 SAR backscatter data. Subsequently, we reduced the resolution of the CH 4 flux map to analyze if different spatial resolutions of CH 4 flux data affected the detectability of relationships between waterbody coverage, number, depth, or size and the CH 4 flux. We did not find consistent correlations between waterbody characteristics and the CH 4 flux in the two study areas across the different resolutions. Our results indicate that waterbodies in permafrost landscapes, even if they seem to be emission hot spots on an individual basis or contain zones of above average emissions, do currently not necessarily translate into significant CH 4 emission hot spots on a regional scale, but their role might change in a warmer climate.
    Type of Medium: Online Resource
    ISSN: 1354-1013 , 1365-2486
    URL: Issue
    Language: English
    Publisher: Wiley
    Publication Date: 2018
    detail.hit.zdb_id: 2020313-5
    SSG: 12
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  • 6
    Online Resource
    Online Resource
    Elsevier BV ; 2015
    In:  Procedia Engineering Vol. 123 ( 2015), p. 41-49
    In: Procedia Engineering, Elsevier BV, Vol. 123 ( 2015), p. 41-49
    Type of Medium: Online Resource
    ISSN: 1877-7058
    Language: English
    Publisher: Elsevier BV
    Publication Date: 2015
    detail.hit.zdb_id: 2509658-8
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  • 7
    In: Remote Sensing, MDPI AG, Vol. 8, No. 11 ( 2016-11-03), p. 903-
    Type of Medium: Online Resource
    ISSN: 2072-4292
    Language: English
    Publisher: MDPI AG
    Publication Date: 2016
    detail.hit.zdb_id: 2513863-7
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  • 8
    In: Earth System Science Data, Copernicus GmbH, Vol. 15, No. 4 ( 2023-04-13), p. 1617-1653
    Abstract: Abstract. Climate warming and related drivers of soil thermal change in the Arctic are expected to modify the distribution and dynamics of carbon contained in perennially frozen grounds. Thawing of permafrost in the Mackenzie River watershed of northwestern Canada, coupled with increases in river discharge and coastal erosion, triggers the release of terrestrial organic matter (OMt) from the largest Arctic drainage basin in North America into the Arctic Ocean. While this process is ongoing and its rate is accelerating, the fate of the newly mobilized organic matter as it transits from the watershed through the delta and into the marine system remains poorly understood. In the framework of the European Horizon 2020 Nunataryuk programme, and as part of the Work Package 4 (WP4) Coastal Waters theme, four field expeditions were conducted in the Mackenzie Delta region and southern Beaufort Sea from April to September 2019. The temporal sampling design allowed the survey of ambient conditions in the coastal waters under full ice cover prior to the spring freshet, during ice breakup in summer, and anterior to the freeze-up period in fall. To capture the fluvial–marine transition zone, and with distinct challenges related to shallow waters and changing seasonal and meteorological conditions, the field sampling was conducted in close partnership with members of the communities of Aklavik, Inuvik and Tuktoyaktuk, using several platforms, namely helicopters, snowmobiles, and small boats. Water column profiles of physical and optical variables were measured in situ, while surface water, groundwater, and sediment samples were collected and preserved for the determination of the composition and sources of OMt, including particulate and dissolved organic carbon (POC and DOC), and colored dissolved organic matter (CDOM), as well as a suite of physical, chemical, and biological variables. Here we present an overview of the standardized datasets, including hydrographic profiles, remote sensing reflectance, temperature and salinity, particle absorption, nutrients, dissolved organic carbon, particulate organic carbon, particulate organic nitrogen, CDOM absorption, fluorescent dissolved organic matter intensity, suspended particulate matter, total particulate carbon, total particulate nitrogen, stable water isotopes, radon in water, bacterial abundance, and a string of phytoplankton pigments including total chlorophyll. Datasets and related metadata can be found in Juhls et al. (2021) (https://doi.org/10.1594/PANGAEA.937587).
    Type of Medium: Online Resource
    ISSN: 1866-3516
    Language: English
    Publisher: Copernicus GmbH
    Publication Date: 2023
    detail.hit.zdb_id: 2475469-9
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  • 9
    In: Remote Sensing, MDPI AG, Vol. 10, No. 4 ( 2018-03-21), p. 494-
    Abstract: In permafrost areas, seasonal freeze-thaw cycles result in upward and downward movements of the ground. For some permafrost areas, long-term downward movements were reported during the last decade. We measured seasonal and multi-year ground movements in a yedoma region of the Lena River Delta, Siberia, in 2013–2017, using reference rods installed deep in the permafrost. The seasonal subsidence was 1.7 ± 1.5 cm in the cold summer of 2013 and 4.8 ± 2 cm in the warm summer of 2014. Furthermore, we measured a pronounced multi-year net subsidence of 9.3 ± 5.7 cm from spring 2013 to the end of summer 2017. Importantly, we observed a high spatial variability of subsidence of up to 6 cm across a sub-meter horizontal scale. In summer 2013, we accompanied our field measurements with Differential Synthetic Aperture Radar Interferometry (DInSAR) on repeat-pass TerraSAR-X (TSX) data from the summer of 2013 to detect summer thaw subsidence over the same study area. Interferometry was strongly affected by a fast phase coherence loss, atmospheric artifacts, and possibly the choice of reference point. A cumulative ground movement map, built from a continuous interferogram stack, did not reveal a subsidence on the upland but showed a distinct subsidence of up to 2 cm in most of the thermokarst basins. There, the spatial pattern of DInSAR-measured subsidence corresponded well with relative surface wetness identified with the near infra-red band of a high-resolution optical image. Our study suggests that (i) although X-band SAR has serious limitations for ground movement monitoring in permafrost landscapes, it can provide valuable information for specific environments like thermokarst basins, and (ii) due to the high sub-pixel spatial variability of ground movements, a validation scheme needs to be developed and implemented for future DInSAR studies in permafrost environments.
    Type of Medium: Online Resource
    ISSN: 2072-4292
    Language: English
    Publisher: MDPI AG
    Publication Date: 2018
    detail.hit.zdb_id: 2513863-7
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  • 10
    Online Resource
    Online Resource
    Frontiers Media SA ; 2021
    In:  Frontiers in Earth Science Vol. 9 ( 2021-7-6)
    In: Frontiers in Earth Science, Frontiers Media SA, Vol. 9 ( 2021-7-6)
    Abstract: Arctic deltas and their river channels are characterized by three components of the cryosphere: snow, river ice, and permafrost, making them especially sensitive to ongoing climate change. Thinning river ice and rising river water temperatures may affect the thermal state of permafrost beneath the riverbed, with consequences for delta hydrology, erosion, and sediment transport. In this study, we use optical and radar remote sensing to map ice frozen to the riverbed (bedfast ice) vs. ice, resting on top of the unfrozen water layer (floating or so-called serpentine ice) within the Arctic’s largest delta, the Lena River Delta. The optical data is used to differentiate elevated floating ice from bedfast ice, which is flooded ice during the spring melt, while radar data is used to differentiate floating from bedfast ice during the winter months. We use numerical modeling and geophysical field surveys to investigate the temperature field and sediment properties beneath the riverbed. Our results show that the serpentine ice identified with both types of remote sensing spatially coincides with the location of thawed riverbed sediment observed with in situ geoelectrical measurements and as simulated with the thermal model. Besides insight into sub-river thermal properties, our study shows the potential of remote sensing for identifying river channels with active sub-ice flow during winter vs. channels, presumably disconnected for winter water flow. Furthermore, our results provide viable information for the summer navigation for shallow-draught vessels.
    Type of Medium: Online Resource
    ISSN: 2296-6463
    Language: Unknown
    Publisher: Frontiers Media SA
    Publication Date: 2021
    detail.hit.zdb_id: 2741235-0
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