SwePub
Sök i SwePub databas

  Utökad sökning

Träfflista för sökning "WFRF:(Ren D) ;mspu:(publicationother)"

Sökning: WFRF:(Ren D) > Annan publikation

  • Resultat 1-3 av 3
Sortera/gruppera träfflistan
   
NumreringReferensOmslagsbildHitta
1.
  • Baumgartner, D., et al. (författare)
  • INFLUENCE OF HEAD ROTATIONAL ACCELERATION PULSE SHAPE ON BRAIN TISSUE STRAINS
  • 2014
  • Ingår i: Journal of Neurotrauma. - 0897-7151. ; 31:12
  • Annan publikation (övrigt vetenskapligt/konstnärligt)abstract
    • Brain tolerance to rotational acceleration is relevant for understanding injury thresholds and development of injury mitigation techniques for automobiles and sporting events. This computational-modeling study outlined effects of head rotational acceleration pulse shape on strains within brain tissues. A detailed finite element model of the human skull and brain was developed and validated previously. The model was exercised using realistic rotational accelerations with different magnitude and duration characteristics, and the principal strain re- sponse was extracted for parietal cortex, hippocampus, thalamus, and hypothalamus. Rotational acceleration magnitude was varied to three levels: 3.6krad/s 2 (M1), 5.3krad/s 2 (M2), and 6.6krad/s 2 (M3). Duration was varied to 9msec (D1), 18msec (D2), and 27msec (D3). Hippocampus and hypothalamus sustained more strain than cortex and thalamus. With increasing acceleration magnitude from M1 to M2 and M2 to M3, strain in all brain regions was uniformly increased by 42% and 80%. However, strains demonstrated regionally dependent chan- ges with increasing duration (D1 to D3): 68%, 37%, 33% and 14% in parietal cortex, hippocampus, thalamus and hypothalamus, respec- tively. The trend was consistent for all acceleration magnitudes. This study demonstrated differing and independent effects of rotational acceleration magnitude and duration on strains within brain tissues during rotational acceleration. Magnitude has long been a correlate of injury severity and this study supports that finding in that increased acceleration magnitudes led to uniformly higher brain tissue strains (higher injury risk). However, rotational acceleration duration chan- ged the strain distribution within the brain, resulting in different injury risks in different brain regions. This finding is significant as changing strain distribution with different durations can manifest as different injury distributions within the brain and different neuropsychological outcomes following exposure to head rotational acceleration.
  •  
2.
  • Angelopoulus, M., et al. (författare)
  • Physical properties of sea ice cores from site MCS_FYI measured on legs 1 to 3 of the MOSAiC expedition.
  • 2022
  • Ingår i: PANGAEA.
  • Annan publikation (övrigt vetenskapligt/konstnärligt)abstract
    • We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
  •  
3.
  • Angelopoulus, M., et al. (författare)
  • Physical properties of sea ice cores from site MCS-SYI measured on legs 1 to 3 of the MOSAiC expedition
  • 2022
  • Ingår i: PANGAEA.
  • Annan publikation (övrigt vetenskapligt/konstnärligt)abstract
    • We present sea ice temperature and salinity data from first-year ice (FYI) and second-year ice (SYI) relevant to the temporal development of sea ice permeability and brine drainage efficiency from the early growth phase in October 2019 to the onset of spring warming in May 2020. Our dataset was collected in the central Arctic Ocean during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC) Expedition in 2019 to 2020. MOSAiC was an international transpolar drift expedition in which the German icebreaker RV Polarstern anchored into an ice floe to gain new insights into Arctic climate over a full annual cycle. In October 2019, RV Polarstern moored to an ice floe in the Siberian sector of the Arctic at 85 degrees north and 137 degrees east to begin the drift towards the North Pole and the Fram Strait via the Transpolar Drift Stream. The data presented here were collected during the first three legs of the expedition, so all the coring activities took place on the same floe. The end dates of legs 1, 2, and 3 were 13 December, 24 February, and 4 June, respectively. The dataset contributed to a baseline study entitled, Deciphering the properties of different Arctic ice types during the growth phase of the MOSAiC floes: Implications for future studies. The study highlights downward directed gas pathways in FYI and SYI by inferring sea ice permeability and potential brine release from several time series of temperature and salinity measurements. The physical properties presented in this paper lay the foundation for subsequent analyses on actual gas contents measured in the ice cores, as well as air-ice and ice-ocean gas fluxes. Sea ice cores were collected with a Kovacs Mark II 9 cm diameter corer. To measure ice temperatures, about 4.5 cm deep holes were drilled into the core (intervals varied by site and leg) . The temperatures were measured by a digital thermometer within minutes after the cores were retrieved. The ice cores were placed into pre-labelled plastic sleeves sealed at the bottom end. The ice cores were transported to RV Polarstern and stored in a -20 degrees Celsius freezer. Each of the cores was sub-sampled, melted at room temperature, and processed for salinity within one or two days. The practical salinity was estimated by measuring the electrical conductivity and temperature of the melted samples using a WTW Cond 3151 salinometer equipped with a Tetra-Con 325 four-electrode conductivity cell. The practical salinity represents the the salinity estimated from the electrical conductivity of the solution. The dataset also contains derived variables, including sea ice density, brine volume fraction, and the Rayleigh number.
  •  
Skapa referenser, mejla, bekava och länka
  • Resultat 1-3 av 3

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy