Source of the tsunami generated by the 1650 AD eruption of Kolumbo submarine volcano (Aegean Sea, Greece)

The 1650 AD explosive eruption of Kolumbo submarine volcano (Aegean Sea, Greece) generated a destructive tsunami. In this paper we propose a source mechanism of this poorly documented tsunami using both geological investigations and numerical simulations. Sedimentary evidence of the 1650 AD tsunami was found along the coast of Santorini Island at maximum altitudes ranging between 3.5 m a.s.l. (Perissa, southern coast) and 20 m a.s.l. (Monolithos, eastern coast), corresponding to a minimum inundation of 360 and 630 m respectively. Tsunami deposits consist of an irregular 5 to 30 cm thick layer of dark grey sand that overlies pumiceous deposits erupted during the Minoan eruption and are found at depths of 30–50 cm below the surface. Composition of the tsunami sand is similar to the composition of the present-day beach sand but differs from the pumiceous gravelly deposits on which it rests. The spatial distribution of the tsunami deposits was compared to available historical records and to the results of numerical simulations of tsunami inundation. Different source mechanisms were tested: earthquakes, underwater explosions, caldera collapse, and pyroclastic flows. The most probable source of the 1650 AD Kolumbo tsunami is a 250 m high water surface displacement generated by underwater explosion with an energy of ~ 2 × 1016 J at water depths between 20 and 150 m. The tsunamigenic explosion(s) occurred on September 29, 1650 during the transition between submarine and subaerial phases of the eruption. Caldera subsidence is not an efficient tsunami source mechanism as short (and probably unrealistic) collapse durations (< 5 min) are needed. Pyroclastic flows cannot be discarded, but the required flux (106 to 107 m3 · s− 1) is exceptionally high compared to the magnitude of the eruption

Structural and dielectric properties of Sr2_{2}TiO4_{4} from first principles

We have investigated the structural and dielectric properties of Sr$_{2}$TiO$_{4}$,the first member of the Sr$_{n+1}$Ti$_{n}$O$_{3n+1}$ Ruddlesden-Popper series, within density functional theory. Motivated by recent work in which thin films of Sr$_{2}$TiO$_{4}$ were grown by molecular beam epitaxy (MBE) on SrTiO$_{3}$ substrates, the in-plane lattice parameter was fixed to the theoretically optimized lattice constant of cubic SrTiO$_{3}$ (n=$\infty$), while the out-of-plane lattice parameter and the internal structural parameters were relaxed. The fully relaxed structure was also investigated. Density functional perturbation theory was used to calculate the zone-center phonon frequencies, Born effective charges, and the electronic dielectric permittivity tensor. A detailed study of the contribution of individual infrared-active modes to the static dielectric permittivity tensor was performed. The calculated Raman and infrared phonon frequencies were found to be in agreement with experiment where available. Comparisons of the calculated static dielectric permittivity with experiments on both ceramic powders and epitaxial thin films are discussed.Comment: 11 pages, 1 figure, 8 tables, submitted to Phys. Rev.

Source of the tsunami generated by the 1650 AD eruption of Kolumbo submarine volcano (Aegean Sea, Greece)

The 1650 AD explosive eruption of Kolumbo submarine volcano (Aegean Sea, Greece) generated a destructive tsunami. In this paper we propose a source mechanism of this poorly documented tsunami using both geological investigations and numerical simulations. Sedimentary evidence of the 1650 AD tsunami was found along the coast of Santorini Island at maximum altitudes ranging between 3.5 m a.s.l. (Perissa, southern coast) and 20 m a.s.l. (Monolithos, eastern coast), corresponding to a minimum inundation of 360 and 630 m respectively. Tsunami deposits consist of an irregular 5 to 30 cm thick layer of dark grey sand that overlies pumiceous deposits erupted during the Minoan eruption and are found at depths of 30-50 cm below the surface. Composition of the tsunami sand is similar to the composition of the present-day beach sand but differs from the pumiceous gravelly deposits on which it rests. The spatial distribution of the tsunami deposits was compared to available historical records and to the results of numerical simulations of tsunami inundation. Different source mechanisms were tested: earthquakes, underwater explosions, caldera collapse, and pyroclastic flows. The most probable source of the 1650 AD Kolumbo tsunami is a 250 m high water surface displacement generated by underwater explosion with an energy of ~2 × 1016 J at water depths between 20 and 150 m. The tsunamigenic explosion(s) occurred on September 29, 1650 during the transition between submarine and subaerial phases of the eruption. Caldera subsidence is not an efficient tsunami source mechanism as short (and probably unrealistic) collapse durations (&amp;lt;5 min) are needed. Pyroclastic flows cannot be discarded, but the required flux (106 to 107 m3 · s-1) is exceptionally high compared to the magnitude of the eruption. © 2016 Elsevier B.V

Imunidade passiva, ingestão de colostro e mortalidade em cabritos Moxotó criados em sistemas extensivo e intensivo Passive immunity, colostrum ingestion, and mortality of Moxotó kids raised under extensive and intensive breeding systems

Dosou-se a proteína sérica total para avaliar a aquisição de imunidade passiva em cabritos Moxotó. Para tal, formaram-se quatro grupos experimentais, sendo dois sistemas de criação, extensivo e intensivo, e dois manejos de colostro, ingestão natural e artificial. Tanto no sistema intensivo quanto no extensivo, os teores de proteína no soro foram significativamente mais altos nos animais com ingestão natural de colostro, 7,11±0,2g/dL, do que nos com ingestão artificial, 6,35±0,17g/dL. Independentemente da forma de ingestão de colostro, os cabritos do sistema intensivo tiveram teores de proteína sérica total, 7,21±0,19g/dL, mais elevados que os do sistema extensivo, 6,25±0,18g/dL, no entanto a imunidade passiva foi satisfatória nos dois grupos de animais. Ocorreu alta mortalidade de crias no sistema extensivo, 37%, devido ao complexo hipotermia/inanição em decorrência dos baixos níveis de colostro ingeridos. No sistema intensivo de criação não ocorreu mortalidade de cabritos. A produção de colostro das cabras criadas intensivamente, 163,5±14,71mL, foi mais alta que das cabras criadas extensivamente, 53,75±19,12mL. O peso total dos cabritos foi semelhante nos dois sistemas de criação, 2881±252,78g no sistema extensivo, e 2297±194,59g no sistema intensivo. Conclui-se que a ingestão de colostro nos dois sistemas de produção permitiu adequada aquisição de imunidade em cabritos, porém o sistema extensivo determinou severa deficiência nutricional nas mães, com baixa produção de colostro e graves perdas de neonatos.<br>The acquisition of passive immunity in Moxotó kids was determined by dosages of total serum proteins. Four experimental groups were formed in two breeding systems - extensive and intensive - and two managements of colostrum intake - suckling from the mother or supplying in bottles. In both breeding systems, the serum protein levels were significantly higher in kids with natural ingestion of colostrum, 7.11±0.2g/dL, than in kids with artificial ingestion, 6.35±0.17g/dL. The kids of the intensive system had levels of total serum protein of 7.21±0.19 g/dL which was higher than the one of the extensive breeding system, 6.25±0.18g/dL. However, the passive immunity was satisfactory in all groups. There was high mortality of kids, 37%, due to starvation/hypothermia, in the extensive breeding system. This mortality was apparently due to the low levels of colostrum ingestion, 55.83±8.7mL. The production of colostrum by does from intensive breeding sistem, 163.5±14.71mL, was significantly higher than those from extensive breeding system, 53.75±19.12mL. The total weight of the kids born in the extensive breeding system, 2,881±252.78g, was similar to those born in the intensive breeding system, 2,297±194.59g. The colostrum ingestion allowed appropriate immunity acquisition by kid raised under both systems. However, the extensive breeding system determined a severe nutritional deficiency in the does with low colostrum production and high neonatal losses