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  • hmg-coa reductase The thermal field emission flux becomes su

    2018-10-24

    The thermal field emission flux becomes substantial as the surface temperature reaches a certain value, namely
    The calculations show that the surface roughness reduces the effect of hmg-coa reductase emission, and in fact at a sufficiently high degree of roughness (∼0.8) emission can be neglected ( ≤ 0.325, ≥ 0.822, ≥ 0.956[14]). The proposed technique was used to calculate spatial distributions for the concentrations of charged particles (ions and electrons) in plasma, for the absolute values of ion directed velocity, and for the potential in the region where the plasma was perturbed by the dust particle (Fig. 2). Vertical lines are the coordinates of the boundaries of the perturbed regions for each specific case. The calculations were performed for an isolated particle in a neon discharge without emission taken into account, with , for the values from 0.1 to 10 and in the range from 10–5 to 10–3, which are typical for the discharge conditions. An increase in the collision frequency leads to a decrease in the concentration and the directed velocity of ions, which is due to the growing influence of the collision term in the equation of ion motion. A decrease in ion concentration and velocity means a decrease in ion current density, which in turn leads to a decrease in electron current density (according to the charge balance equation) and, consequently, to an increase in the absolute normalized value of the potential on the surface of the dust particle and in its vicinity. A change in the ionization rate of the isolated particle does not affect the calculated plasma parameters, as the influence of the bulk friction caused by ion-atom collisions by far exceeds the influence of the friction caused by the ionization in the considered range of values ≫ (this effect is not observed in the figures). However, a decrease in the ionization rate leads to an increase in the thickness of the perturbed region. Fig. 3 shows the graphs for the concentration distributions of ions and electrons, and of the absolute values of the potential and the radial velocity of ions, which show the transition from an isolated particle to a dense plasma-dust structure. These graphs were obtained for the parameter values and . Curves 1, corresponding to the distributions for the isolated particle, were obtained for . Curves 2 (/u0= 0.01) and 3 () correspond to the distributions in the Wigner–Seitz cell, with an increased frequency . In this case, the ionization rate for the value (curves 3) is higher than that for the 0.01 value (curves 2); respectively, in the second case, the cell radius 2 is less than in the first one (1). The values of the corresponding normalized radii are given in the caption to Fig. 3.
    Conclusion
    Introduction Acoustic signals of toothed whales are diverse and serve as their primary means for mediating complex coordinated social behavior (foraging, defense against predators, etc.), navigation and communication among dispersed individuals, obtaining information on the environment [1]. We should specifically stress that these signals are the only source of sensory cues for the animals in poor visibility conditions. To date, the general consensus in the scientific literature has been that the toothed whales (Odontoceti) possess a sonar. The sounding signals of the dolphin sonar are clicks lasting about 50µs, with the maximum energy reached at frequencies around 120–130kHz [2]. Most species of dolphins produce two types of sounds, which possibly play the role of communication signals in their social relationships. These are packs of broadband pulses and ‘whistles’ [3]. Several species of dolphins of the Kogiidae, Physeteridae and Phocoenidae families and the Cephalorhynchinae subfamily (Hector\'s dolphin) do not produce whistles and may communicate by pulsed sounds [4–6]. Pulse packs consist of a sequence of broadband pulses that are similar to echolocation clicks but unlike them have very short (0.5–10ms) interpulse intervals [7] and significantly lower sound pressure levels (SPL) [2]. The presence and the function of these packs still remain unclear, even though the hypothesis that dolphins use them for communication has been discussed since the 1960s [6,8,9]. This hypothesis is based on the fact that the above-described signals are recorded when the dolphins are engaged in high social activity and at short distances (2–14m) from them [1], and the interpulse intervals of these signals have a shorter processing time typical for echolocation (15–45ms). It should be noted that the vast majority of the dolphin signals were recorded in the frequency band only up to 20kHz (see, e.g., [8,10]), with few exceptions [6,7].