The impact of vatinoxan on microcirculation after intramuscular coadministration with medetomidine in Beagle dogs – a blinded cross-over study

Author(s):  
L. Niemann ◽  
A.P.N. Kutter ◽  
F.B. Joerger ◽  
M.L. Wieser ◽  
S. Hartnack ◽  
...  
Keyword(s):  
2015 ◽  
Vol 163 (3-4) ◽  
pp. 174-182 ◽  
Author(s):  
Berenice C. Bastien ◽  
Avinash Patil ◽  
Ebenezer Satyaraj

2019 ◽  
Author(s):  
Jiangbei CAO ◽  
Yongyi ZHANG ◽  
Wei WANG ◽  
Hao LI ◽  
Weidong MI

Abstract Background: When an airway is difficult to manage during surgery, it can be fatal. Thus, peritoneum oxygenation may be theoretically feasible as an alternative route to supply oxygen. The objective of this study is to investigate whether artificial oxygen pneumoperitoneum combined with abdominal lifting and compression is effective in systemic oxygenation and hypoxia tolerance in a beagle dog model of asphyxia. Methods: Latin Square design was adopted. Eight adult female beagle dogs were divided into four subgroups; they received four treatments in sequence in four sessions at 1-week intervals. The pre-treatment procedures included general anesthesia and a pause in ventilation to establish an asphyxia model. Each subgroup was subjected to the treatments as follows: negative control(A), artificial oxygen pneumoperitoneum(B), artificial oxygen pneumoperitoneum combined with abdominal lifting and compression from the 1st minute after asphyxia(C), or the same as C but starting the method from the 5th minute(D). Vital signs, important organ functions, and arterial blood gas were monitored. Hypoxia tolerance was assessed by the asphyxia time (from pause to restoration of ventilation) and PaO2 levels at 0, 6, 7, 8, 9, and 10 minutes after asphyxia onset. Results: The physiological status of the beagles was approximately identical before each experiment and the treatments did not aggravate the impact of hypoxia. The asphyxia time for treatments A, B, C, and D were 9.65 ± 1.10 min, 11.18± 0.50min, 11.45 ± 0.79min, and 11.70 ± 0.99min, respectively; the time was lengthened in treatments B, C, and D, compared with that in treatment A (P<0.01). Moreover, PaO2 levels at 9 and 10 min were higher in treatments B, C, and D than in treatment A (P<0.01). Conclusions: Artificial oxygen pneumoperitoneum combined with abdominal lifting and compression appears safe and effective and may improve systemic oxygenation and enhance hypoxia tolerance.


1996 ◽  
Vol 13 (1) ◽  
pp. 27-30 ◽  
Author(s):  
George K. Stookey ◽  
Janice M. Warrick ◽  
Linda L. Miller ◽  
Barry P. Katz

We conducted a clinical trial in beagle dogs to determine the impact of a popular snack-type biscuit and an experimental biscuit coated with 0.6% sodium hexametaphosphate (HMP) upon calculus formation. The study used a crossover design evaluating each dog on each regimen with 4-week test periods, each of which began with a dental prophylaxis (scaling and polishing). The dogs were provided a single daily feeding of dry chow followed 4 hours later by either no snack or a snack comprised of two or four conventional biscuits, or two HMP-coated biscuits. As compared to the no-snack regimen, feeding two or four conventional bone-shaped biscuits exerted no significant effect upon calculus formation, while the similar feeding of two HMP-coated biscuits significantly reduced calculus formation by 46%.


1962 ◽  
Vol 14 ◽  
pp. 415-418
Author(s):  
K. P. Stanyukovich ◽  
V. A. Bronshten

The phenomena accompanying the impact of large meteorites on the surface of the Moon or of the Earth can be examined on the basis of the theory of explosive phenomena if we assume that, instead of an exploding meteorite moving inside the rock, we have an explosive charge (equivalent in energy), situated at a certain distance under the surface.


1962 ◽  
Vol 14 ◽  
pp. 169-257 ◽  
Author(s):  
J. Green

The term geo-sciences has been used here to include the disciplines geology, geophysics and geochemistry. However, in order to apply geophysics and geochemistry effectively one must begin with a geological model. Therefore, the science of geology should be used as the basis for lunar exploration. From an astronomical point of view, a lunar terrain heavily impacted with meteors appears the more reasonable; although from a geological standpoint, volcanism seems the more probable mechanism. A surface liberally marked with volcanic features has been advocated by such geologists as Bülow, Dana, Suess, von Wolff, Shaler, Spurr, and Kuno. In this paper, both the impact and volcanic hypotheses are considered in the application of the geo-sciences to manned lunar exploration. However, more emphasis is placed on the volcanic, or more correctly the defluidization, hypothesis to account for lunar surface features.


1997 ◽  
Vol 161 ◽  
pp. 197-201 ◽  
Author(s):  
Duncan Steel

AbstractWhilst lithopanspermia depends upon massive impacts occurring at a speed above some limit, the intact delivery of organic chemicals or other volatiles to a planet requires the impact speed to be below some other limit such that a significant fraction of that material escapes destruction. Thus the two opposite ends of the impact speed distributions are the regions of interest in the bioastronomical context, whereas much modelling work on impacts delivers, or makes use of, only the mean speed. Here the probability distributions of impact speeds upon Mars are calculated for (i) the orbital distribution of known asteroids; and (ii) the expected distribution of near-parabolic cometary orbits. It is found that cometary impacts are far more likely to eject rocks from Mars (over 99 percent of the cometary impacts are at speeds above 20 km/sec, but at most 5 percent of the asteroidal impacts); paradoxically, the objects impacting at speeds low enough to make organic/volatile survival possible (the asteroids) are those which are depleted in such species.


1997 ◽  
Vol 161 ◽  
pp. 189-195
Author(s):  
Cesare Guaita ◽  
Roberto Crippa ◽  
Federico Manzini

AbstractA large amount of CO has been detected above many SL9/Jupiter impacts. This gas was never detected before the collision. So, in our opinion, CO was released from a parent compound during the collision. We identify this compound as POM (polyoxymethylene), a formaldehyde (HCHO) polymer that, when suddenly heated, reformes monomeric HCHO. At temperatures higher than 1200°K HCHO cannot exist in molecular form and the most probable result of its decomposition is the formation of CO. At lower temperatures, HCHO can react with NH3 and/or HCN to form high UV-absorbing polymeric material. In our opinion, this kind of material has also to be taken in to account to explain the complex evolution of some SL9 impacts that we observed in CCD images taken with a blue filter.


1997 ◽  
Vol 161 ◽  
pp. 179-187
Author(s):  
Clifford N. Matthews ◽  
Rose A. Pesce-Rodriguez ◽  
Shirley A. Liebman

AbstractHydrogen cyanide polymers – heterogeneous solids ranging in color from yellow to orange to brown to black – may be among the organic macromolecules most readily formed within the Solar System. The non-volatile black crust of comet Halley, for example, as well as the extensive orangebrown streaks in the atmosphere of Jupiter, might consist largely of such polymers synthesized from HCN formed by photolysis of methane and ammonia, the color observed depending on the concentration of HCN involved. Laboratory studies of these ubiquitous compounds point to the presence of polyamidine structures synthesized directly from hydrogen cyanide. These would be converted by water to polypeptides which can be further hydrolyzed to α-amino acids. Black polymers and multimers with conjugated ladder structures derived from HCN could also be formed and might well be the source of the many nitrogen heterocycles, adenine included, observed after pyrolysis. The dark brown color arising from the impacts of comet P/Shoemaker-Levy 9 on Jupiter might therefore be mainly caused by the presence of HCN polymers, whether originally present, deposited by the impactor or synthesized directly from HCN. Spectroscopic detection of these predicted macromolecules and their hydrolytic and pyrolytic by-products would strengthen significantly the hypothesis that cyanide polymerization is a preferred pathway for prebiotic and extraterrestrial chemistry.


Author(s):  
R. F. Bils ◽  
W. F. Diller ◽  
F. Huth

Phosgene still plays an important role as a toxic substance in the chemical industry. Thiess (1968) recently reported observations on numerous cases of phosgene poisoning. A serious difficulty in the clinical handling of phosgene poisoning cases is a relatively long latent period, up to 12 hours, with no obvious signs of severity. At about 12 hours heavy lung edema appears suddenly, however changes can be seen in routine X-rays taken after only a few hours' exposure (Diller et al., 1969). This study was undertaken to correlate these early changes seen by the roengenologist with morphological alterations in the lungs seen in the'light and electron microscopes.Forty-two adult male and female Beagle dogs were selected for these exposure experiments. Treated animals were exposed to 94.5-107-5 ppm phosgene for 10 min. in a 15 m3 chamber. Roentgenograms were made of the thorax of each animal before and after exposure, up to 24 hrs.


Author(s):  
Lucien F. Trueb

Crushed and statically compressed Madagascar graphite that was explosively shocked at 425 kb by means of a planar flyer-plate is characterized by a black zone extending for 2 to 3 nun below the impact plane of the driver. Beyond this point, the material assumes the normal gray color of graphite. The thickness of the black zone is identical with the distance taken by the relaxation wave to overtake the compression wave.The main mechanical characteristic of the black material is its great hardness; steel scalpels and razor blades are readily blunted during attempts to cut it. An average microhardness value of 95-3 DPHN was obtained with a 10 kg load. This figure is a minimum because the indentations were usually cracked; 14.8 DPHN was measured in the gray zone.


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