Influence of Wind and Grain Size on Migration of Asymmetric Sand Waves

Large parts of shallow seas are covered by regular seabed patterns and sand wave is one kind of these patterns. The instability of the sedimentary structures may hazard pipelines and the foundations of offshore structures. In the last decade or so, it's a focus for engineers to investigate the movement mechanism of sand waves. Previous theoretical studies of the subject have developed a general model to predict the growth and migration of sand waves, which is based on the two-dimensional vertical shallow water equations and the bed-form deformation equations. Although the relation between wave-current flow and sand bed deformation has been established, the topographic influence has not been considered in the model. In this paper some special patterns, which are asymmetric and close to the reality, are represent as the perturbed seabed and the evolution of sand waves is calculated. The combination of a steady flow induced by wind and a sinusoidal tidal flow is considered as the basic flow. Finally the relations of some parameters (grain size, etc.) and sand waves' growth and migration are discussed, and the growth rate and migration speeds of asymmetric sand waves are carried out.

Bowhead and white whale migration, distribution, and abundance in the Bering, Chukchi, and Beaufort Seas, 1975-78

From September 1975 to September 1977 we conducted field research on bowhead, Balaena mysticetus, and white, Delphinapterus leucas, whales in the U.S. Bering, Chukchi, and Beaufort Seas. The objectives were to determine the general distribution and migration of these whales in spring and autumn and to estimate abundance. We also surveyed the literature beginning in June 1975 through March 1978 to augment our empirical results. (PDF contains 48 pages)

Novel mechanisms for regulation of cell survival and migration by ceramide 1-phosphate

201 p. : gráf.

Suspension mechanics: I. Inertial and non-Newtonian migration of neutrally buoyant rigid spheres in two-dimensional unidirectional flows; II. The effect of viscoelasticity on the creeping motion of a train of neutrally buoyant Newtonian drops through a circular tube

The lateral migration of neutrally buoyant rigid spheres in two-dimensional unidirectional flows was studied theoretically. The cases of both inertia-induced migration in a Newtonian fluid and normal stress-induced migration in a second-order fluid were considered. Analytical results for the lateral velocities were obtained, and the equilibrium positions and trajectories of the spheres compared favorably with the experimental data available in the literature. The effective viscosity was obtained for a dilute suspension of spheres which were simultaneously undergoing inertia-induced migration and translational Brownian motion in a plane Poiseuille flow. The migration of spheres suspended in a second-order fluid inside a screw extruder was also considered.

The creeping motion of neutrally buoyant concentrically located Newtonian drops through a circular tube was studied experimentally for drops which have an undeformed radius comparable to that of the tube. Both a Newtonian and a viscoelastic suspending fluid were used in order to determine the influence of viscoelasticity. The extra pressure drop due to the presence of the suspended drops, the shape and velocity of the drops, and the streamlines of the flow were obtained for various viscosity ratios, total flow rates, and drop sizes. The results were compared with existing theoretical and experimental data.

Caracterização geológica da ocorrência de óleo na Formação Rio Bonito associada a um modelo não convencional de geração

O trabalho teve como escopo a caracterização geológica, em termos estruturais e estratigráficos, do sistema petrolífero responsável pela ocorrência de óleos encontrados na Formação Rio Bonito, na região carbonífera de Santa Catarina. Atualmente, especula-se que a assinatura geoquímica destes óleos relaciona-se à Formação Irati associado a um modelo não convencional de geração, vinculando a maturação térmica à intrusão de diabásio, devido a um soterramento insuficiente da rocha geradora. Como a Formação Irati encontra-se posicionada estratigraficamente acima da Formação Rio Bonito, o sistema está associado a um forte controle estrutural para o modelo de migração. A preparação de um mapa geológico integrado para a área de estudo envolvendo dados geológicos de campo, dados aeromagnetométricos e informações de furos de sondagem permitiu um entendimento mais aprofundado do arcabouço tectônico-estratigráfico da região. Seções geológicas mostraram a presença de falhas de grandes rejeitos que promoveram um sistema de Horsts e Grabens relacionados às NE-SW e secundariamente a falhas E-W, que permitiram a colocação da Formação Irati em contato lateral ou em um posicionamento abaixo da Formação Rio Bonito. A partir das seções cronoestratigráficas elaboradas foi possível reconhecer prováveis selos, trapas estratigráficos e estruturais, associados ao sistema petrolífero Irati-Rio Bonito. A análise geoquímica (isótopos e biomarcadores) dos óleos coletados na Formação Rio Bonito apontaram que os mesmos estão associadas aos folhelhos do Membro Assistência da Formação Irati, por possuírem uma razão pristano/fitano menor que 1, gamacerano, e a presença de isoprenóides pentametileicosano (i-25) e esqualano (i-30). A partir de análises geoquímicas realizadas em extratos orgânicos extraídos de folhelhos da Formação Irati intrudidos por diabásio, obteve-se valores da relação entre biomarcadores correspondentes e valores de Ro que indicam que foi alcançado o pico de geração de óleo. Contudo, não há registro na área de estudo de um soterramento suficiente que favorecesse essa situação, levando-nos, assim, a acreditar em um modelo de geração não convencional, por meio da intrusão de diabásio nas rochas geradoras. O arcabouço estrutural e os óleos estudados na região sugerem um processo migratório de sudoeste para o nordeste, ao longo de um sistema de falhas NE-SW, encontradas na região, que foram geradas anteriormente ou concomitantemente ao derrame basáltico associado à Formação Serra Geral.

Investigations on the vertical migration of planktonic Crustacea in the Bodensee-Obersee. [Translation from: Schriften des Vereins fur Geschichte des Bodensees und seiner Umgebung, 87, 177-187, 1969.]

The vertical zoning of the planktonic Crustacea in a lake is the expression of a complex set of different factors. Besides the measurable, external influences such as light, temperature, acid and C02 stratification, a particularly large part is played by internal factors, which co-ordinate a specific reaction in each species depending on state of development, age and sex. Supporting this extensive, predictable, annual course of diurnal depths and the daily vertical migrations, whose extent is again dependent on external conditions, primarily of course on the amount of light. The individual factors mentioned, however, are here also of great significance. Within the scope of a long-term study of the planktonic Copepoda of Lake Constance, some day and night series were in 1963 also carried out in the Obersee, in order to obtain at least volumetric data on the extent of the daily migrations of these creatures.

On drift and diel vertical migration of bottom invertebrates of the Amur. [Translation from: Zoologicheskie Zhurnal 42 1601-1612, 1963.]

Planktobenthos was sampled in 1957-58 in the river Amur. A determination of the kind of organisms drifting in the mass of water of the Amur was carried out. Of special interest for the authors was the activity of drifting of benthic larvae.

Bird migration and the spread of Crustacea. [Translation from: Verhandlungen der Deutschen Zoologischen Gesellschaft 27, 311-316, 1963.]

The passive spread of a high percentage of freshwater organisms is one of the most important requirements in short-lived and insular communities for species to attai n and survive - and consequently to balance the lack of a topographical continuity of most inland waters. Unfortunately hardly anything is known about the amounts of seed material typical for any lake into which it is carried. The causes of passive dissemination - wind, water and animals as well as man - are confirmed by many examples. It has been assumed now for at least a hundered years that , among animals, birds play a prominent role, although also disappointingly few facts are at hand. The passage and spread through birds' intestines has up to now been supported only by some limited data. This paper reports on experimental research where the eggs of Daphnia magna, Triops cancriformis, Artemia salina, Diaptomus spinosus and Cypris pubera were introduced by means of gelatine capsules into the oesophagus of a drake. The bird's excrements were inspected under a microscope for eggs and resting stages, and these were transferred into corresponding cultures.

Representação Social da Igreja Universal do Reino de Deus por evangélicos dela egressos

A Igreja Universal do Reino de Deus (IURD) foi fundada há trinta e quatro anos e tem forte influência social e política. Sua capilaridade religiosa se expressa através da sua inserção em diversas mídias, como TV, rádio, jornal etc. e da participação política evidenciada pelas "bancadas evangélicas" nos diferentes parlamentos, onde predominam autoridades da IURD. Também se faz presente através dos milhares de templos construídos e espalhados por mais de 180 países. Sua estratégia de proselitismo religioso é baseada na conversão de adeptos de outras religiões. Sua hierarquia: obreiros, pastores e bispos, define a igreja como o maior "pronto-socorro" espiritual do Brasil. Caracterizada pelo oferecimento de solução de problemas imediatos e de natureza espiritual. Após algum tempo, conversos da IURD migram para outras igrejas evangélicas. O objetivo desta pesquisa foi identificar as Representações Sociais da IURD segundo evangélicos dela egressos. Para tanto, foram entrevistados vinte indivíduos adultos, na Cidade do Rio de Janeiro, egressos da IURD. Como instrumento, utilizamos um questionário para entrevista semi-estruturada, composto por questões acerca da IURD e dados pessoais do entrevistado. O material resultante foi analisado a partir da análise de conteúdo. As entrevistas foram gravadas, com a autorização dos entrevistados e o comprometimento na manutenção do anonimato dos participantes. Dentre os resultados da pesquisa, confirmando o que é dito por seus líderes, encontramos a IURD como um pronto socorro, não só espiritual, como emocional e de saúde física. A migração da IURD para outras denominações cristãs está associada a três grandes categorias: a) o sujeito não tem mais necessidade do pronto-socorro; b) crítica às cobranças sistemáticas por bens espirituais; c) a necessidade de aprofundamento religioso. Neste aspecto, a IURD caracteriza-se por ser uma Igreja de transição, de início de vida espiritual cristã e de proselitismo voltado quase que exclusivamente para a conversão.

Biologie de Penaeus duorarum (Burkenroad) en Côte d'Ivoire: 2 - ponte et migration

The pink shrimp Penaeus duorarum spawns from 25 to 60m, mostly in summer (October to June). Size at first sexual maturity is 31 mm (carapace length). The observed difference with the Caribbean pink shrimp is analysed. Immature shrimps migrate all year round but a peak migration occurs from January to March (in summer) and is associated with maximum salinities. A secondary peak migration occurs in October corresponding to minimum salinity and maximum river discharge. The action of salinity on migration is discussed and a preponderant action of currents in the process is also suggested. Migration is also related to moon phase, tide and day-night cycles. Migration intensity as expressed by catch per unit of effort is maximum at night, during ebb tide, on new and full moon. Seasonal variation of mean migration size and abundance are related by a negative linear correlation on a logarithmic plot (R = 0.776). This phenomenon is perhaps related to competition for food.

Prediction and confirmation of seasonal migration of Pacific sardine (Sardinops sagax) in the California Current Ecosystem

During the last century, the population of Pacific sardine (Sardinops sagax) in the California Current Ecosystem has exhibited large fluctuations in abundance and migration behavior. From approximately 1900 to 1940, the abundance of sardine reached 3.6 million metric tons and the “northern stock” migrated from offshore of California in the spring to the coastal areas near Oregon, Washington, and Vancouver Island in the summer. In the 1940s, the sardine stock collapsed and the few remaining sardine schools concentrated in the coastal region off southern California, year-round, for the next 50 years. The stock gradually recovered in the late 1980s and resumed its seasonal migration between regions off southern California and Canada. Recently, a model was developed which predicts the potential habitat for the northern stock of Pacific sardine and its seasonal dynamics. The habitat predictions were successfully validated using data from sardine surveys using the daily egg production method; scientific trawl surveys off the Columbia River mouth; and commercial sardine landings off Oregon, Washington, and Vancouver Island. Here, the predictions of the potential habitat and seasonal migration of the northern stock of sardine are validated using data from “acoustic–trawl” surveys of the entire west coast of the United States during the spring and summer of 2008. The estimates of sardine biomass and lengths from the two surveys are not significantly different between spring and summer, indicating that they are representative of the entire stock. The results also confirm that the model of potential sardine habitat can be used to optimally apply survey effort and thus minimize random and systematic sampling error in the biomass estimates. Furthermore, the acoustic–trawl survey data are useful to estimate concurrently the distributions and abundances of other pelagic fishes.