Record of wells in Volusia County, Florida

A detailed study of the geology and ground-water resources of Volusia County, on the eastern coast of Florida (fig. 1), was made during the period 1953-57 by the U. S. Geological Survey in cooperation with the Florida Geological Survey and the cities of Daytona Beach, New Smyrna Beach, and Port Orange. The results of this study have been published by the Florida Geological Survey in the following reports: Information Circular No. 8, entitled "Interim Report on Ground-Water Resources of Northeastern Part of Volusia County, Florida, " by Granville G. Wyrickand Willard P. Leutze;, and Report of Investigations No. 22, entitled "Ground-Water Resources of Volusia County, Florida, " by Granville G. Wyrick. This report contains a table of well records that was compiled from data collected during that investigation. longitude. (PDF contains 100 pages.)

Distribution of Temperature in GlidArc Discharge Plasma

The GlidArc discharge is one of the main generation methods of non-equilibrium plasma near atmospheric pressures. In general, Gliding Arc discharge is driven by gas flow [1] in axial direction or by magnetic field in circumferential direction. [2] In this paper, a GlidArc discharge driven by rotating-gas-flow in circumferential direction is presented. The principle of the plasma generator is analyzed. The distribution of the temperature in axial direction is measured by a digital thermometer for three different gases. The experimental set-up of the GlidArc plasma is shown in Fig.1. It consists of a center electrode, an outside electrode, a power supply and a gas supply. The shortest distance between the electrodes is 2-3 mm. When a power supply with 10000 volts is attached to the electrodes, the arc will be ignited at the shortest distance. The small plasma column is rotated by the rotating gas flow in circumferential direction and then the rotating arc is driven towards the exit of the setup by the gas flow.

La observación sistemática aplicada a la evaluación de la gimnasia rítmica

Oidui Usabiaga; Julen Castellano y Joseba Etxebeste (editores).

Cruise Report NOAA Ship McARTHUR II Cruise AR-04-04: Leg 2 (June 1-12, 2004): A pilot survey of deepwater coral/sponge assemblages and their susceptibility to fishing/harvest impacts at the Olympic Coast National Marine Sanctuary (OCNMS)

Summary: The offshore shelf and canyon habitats of the OCNMS (Fig. 1) are areas of high primary productivity and biodiversity that support extensive groundfish fisheries. Recent acoustic surveys conducted in these waters have indicated the presence of hard-bottom substrates believed to harbor unique deep-sea coral and sponge assemblages. Such fauna are often associated with shallow tropical waters, however an increasing number of studies around the world have recorded them in deeper, cold-water habitats in both northern and southern latitudes. These habitats are of tremendous value as sites of recruitment for commercially important fishes. Yet, ironically, studies have shown how the gear used in offshore demersal fishing, as well as other commercial operations on the seafloor, can cause severe physical disturbances to resident benthic fauna. Due to their exposed structure, slow growth and recruitment rates, and long life spans, deep-sea corals and sponges may be especially vulnerable to such disturbances, requiring very long periods to recover. Potential effects of fishing and other commercial operations in such critical habitats, and the need to define appropriate strategies for the protection of these resources, have been identified as a high-priority management issue for the sanctuary. To begin addressing this issue, an initial pilot survey was conducted June 1-12, 2004 at six sites in offshore waters of the OCNMS (Fig. 2, average depths of 147-265 m) to explore for the presence of deep-sea coral/sponge assemblages and to look for evidence of potential anthropogenic impacts in these critical habitats. The survey was conducted on the NOAA Ship McARTHUR-II using the Navy’s Phantom DHD2+2 remotely operated vehicle (ROV), which was equipped with a video camera, lasers, and a manipulator arm for the collection of voucher specimens. At each site, a 0.1-m2 grab sampler also was used to collect samples of sediments for the analysis of macroinfauna (> 1.0 mm), total organic carbon (TOC), grain size, and chemical contaminants. Vertical profiles of salinity, dissolved oxygen (DO), temperature, and pressure were recorded at each site with a small SeaCat conductivity-temperature-depth (CTD) profiler. Niskin bottles attached to the CTD also obtained near-bottom water samples in support of a companion study of microbial indicators of coral health and general ecological condition across these sites. All samples except the sediment-contaminant samples are being analyzed with present project funds. Original cruise plans included a total of 12 candidate stations to investigate (Fig. 3). However, inclement weather and equipment failures restricted the sampling to half of these sites. In spite of the limited sampling, the work completed was sufficient to address key project objectives and included several significant scientific observations. Foremost, the cruise was successful in demonstrating the presence of target deepwater coral species in these waters. Patches of the rare stony coral Lophelia pertusa, more characteristic of deepwater coral/sponge assemblages in the North Atlantic, were observed for the first time in OCNMS at a site in 271 meters of water. A large proportion of these corals consisted of dead and broken skeletal remains, and a broken gorgonian (soft coral) also was observed nearby. The source of these disturbances is not known. However, observations from several sites included evidence of bottom trawl marks in the sediment and derelict fishing gear (long lines). Preliminary results also support the view that these areas are important reservoirs of marine biodiversity and of value as habitat for demersal fishes. For example, onboard examination of 18 bottom-sediment grabs revealed benthic infaunal species representative of 14 different invertebrate phyla. Twenty-eight species of fishes from 11 families, including 11 (possibly 12) species of ommercially important rockfishes, also were identified from ROV video footage. These initial discoveries have sparked considerable interests in follow-up studies to learn more about the spatial extent of these assemblages and magnitude of potential impacts from commercial-fishing and other anthropogenic activities in the area. It is essential to expand our knowledge of these deep-sea communities and their vulnerability to potential environmental risks in order to determine the most appropriate management strategies. The survey was conducted under a partnership between NOAA’s National Centers for Coastal Ocean Science (NCCOS) and National Marine Sanctuary Program (NMSP) and included scientists from NCCOS, OCNMS, and several other west-coast State, academic, private, and tribal research institutions (see Section 4 for a complete listing of participating scientists). (PDF contains 20 pages)

Oceanographic results during VERTEX particle interceptor trap experiment 17 August to 8 September 1980

This report presents oceanographic data supporting the detailed chemical studies in the VERTEX Particle Interceptor Trap (PIT) experiment off the central California coast. Prior to the deployment of the PITs, an oceanographic survey of the intended study area was made on R/V CAYUSE from 17 to 21 August 1980. During this cruise, twenty CTD stations (Fig. 1) were occupied in a grid centered about the PIT site selected earlier based on archival oceanographic data. During the second leg of the VERTEX experiment from 25 August to 3 September, CTO profiles were taken as time permitted. In addition, a short survey near the PITs was made on 2 September. The intent of the pre-deployment cruise was to obtain data characterizing the vertical and horizontal variability of physical and chemical properties and to map the geostrophic flow field. Toward this end, vertical profiles of salinity, temperature and dissolved oxygen were made using a Plessey 9040 CTOa profiler. Considerable effort was expended to make vertical beam attenuation profiles to

Oceanographic Profiling Observations from the MOCE-3 Cruise: 27 October to 15 November 1994

This report contains results from the third cruise of the Marine Optical Characterization Experiment (Fig. 1). A variety of spectroradiometric observations of the upper water column and atmosphere were made by investigators from the University of Miami, NOAA, CHORS and MLML. Data presented here were obtained by oceanographic CTD profiler: salinity, temperatllre, dissolved oxygen, beam attenuation and chlorophyll-a fluorescence; and by water samplers: total suspended matter and suspended organic carbon and nitrogen, salinity, and dissolved oxygen.

Studies on hymenopteran parasitism of Drosophila

Studies on Hymenopteran Parasitism of Drosophila

Flies of the genus Drosophila are subject to attack by a number of parasitic forms. Sturtevant (1921) has listed records of parasitism by protozoa (Leptomonas), fungi (Muiaria and Stigmatomyces), nematodes, mites and v~rious hymenoptera. According to Sturtevant, Perkins (1913) has bred at least five species of hymenoptera, belonging to the proctotrupoid, cynipoid and chalcidoid groups, upon Drosophiline flies. H.S. Smith has bred an unidentified proctotrupoid and a chalcidoid, Pachy crepoideus dubius Ashmead* from both Drosophila melanogaster ani D. hydei. Kieffer ( 1913) has described three species of hymenoptera from Africa collected by Silvestri and stated by him to be parasitic on Drosophila, species not given. They are Trichopria (Planopria) rhopalica (Diapriidae), Ashmeadopria drosophilae (Diapriidae), and the insect which forms the subject matter of the present investigation, Eucoila drosophilae (Figitidae).

There are in addition a number of predacious enemies among wasps, spiders, flies and beetles.

The present account is concerned with parasitism of various species of Drosophila by Eucoila drosophilae Kieff. The wasps were found b y Dr. w. P. Spencer who exposed traps in an effort to collect Drosophila at Long Lake, Ohio, in Sept. 1934 . Drosophila larvae from the trap gave a large number of pupae from which wasps emerged in considerable proportions. Since that time stock s have been maintained in culture on Drosophila melanogaster.

I. Fundamental limitations in microelectronics. II. Power Schottky diode design and comparison with the junction diode. III. Permittivity of strontium titanate

Part I

The physical phenomena which will ultimately limit the packing density of planar bipolar and MOS integrated circuits are examined. The maximum packing density is obtained by minimizing the supply voltage and the size of the devices. The minimum size of a bipolar transistor is determined by junction breakdown, punch-through and doping fluctuations. The minimum size of a MOS transistor is determined by gate oxide breakdown and drain-source punch-through. The packing density of fully active bipolar or static non-complementary MOS circuits becomes limited by power dissipation. The packing density of circuits which are not fully active such as read-only memories, becomes limited by the area occupied by the devices, and the frequency is limited by the circuit time constants and by metal migration. The packing density of fully active dynamic or complementary MOS circuits is limited by the area occupied by the devices, and the frequency is limited by power dissipation and metal migration. It is concluded that read-only memories will reach approximately the same performance and packing density with MOS and bipolar technologies, while fully active circuits will reach the highest levels of integration with dynamic MOS or complementary MOS technologies.

Part II

Because the Schottky diode is a one-carrier device, it has both advantages and disadvantages with respect to the junction diode which is a two-carrier device. The advantage is that there are practically no excess minority carriers which must be swept out before the diode blocks current in the reverse direction, i.e. a much faster recovery time. The disadvantage of the Schottky diode is that for a high voltage device it is not possible to use conductivity modulation as in the p i n diode; since charge carriers are of one sign, no charge cancellation can occur and current becomes space charge limited. The Schottky diode design is developed in Section 2 and the characteristics of an optimally designed silicon Schottky diode are summarized in Fig. 9. Design criteria and quantitative comparison of junction and Schottky diodes is given in Table 1 and Fig. 10. Although somewhat approximate, the treatment allows a systematic quantitative comparison of the devices for any given application.

Part III

We interpret measurements of permittivity of perovskite strontium titanate as a function of orientation, temperature, electric field and frequency performed by Dr. Richard Neville. The free energy of the crystal is calculated as a function of polarization. The Curie-Weiss law and the LST relation are verified. A generalized LST relation is used to calculate the permittivity of strontium titanate from zero to optic frequencies. Two active optic modes are important. The lower frequency mode is attributed mainly to motion of the strontium ions with respect to the rest of the lattice, while the higher frequency active mode is attributed to motion of the titanium ions with respect to the oxygen lattice. An anomalous resonance which multi-domain strontium titanate crystals exhibit below 65°K is described and a plausible mechanism which explains the phenomenon is presented.

Interpretación litoestratigráfica y paleogeográfica del Jurásico marino del este Cantabria-oeste de Vizcaya en base a diagrafías de sondeo y su correlación con series tipo

Este trabajo se centra en el estudio del Jurásico marino (Lías y Dogger) de un área de la parte central de La Cuenca Vasco-Cantábrica situada en el este de Cantabria y oeste de Vizcaya donde sus afloramientos son muy escasos pero se dispone de datos de sondeos de exploración petrolífera (Fig 1A y B), poniendo especial interés en la localización y distribución lateral de los niveles de rocas madre de hidrocarburos (black shales) y de potenciales almacenes (unidades carbonatadas fracturadas o dolomitizadas). La sucesión del Jurásico de la Cuenca Vasco-Cantábrica (CVC) está formada por dos unidades diferenciadas por edad y ambiente sedimentario. Por una parte tenemos los materiales del “Jurásico marino” (Robles et al., 1989) que representan la mayor parte de la sucesión (Lías y Dogger) y por otro lado, tenemos los materiales del “Jurásico continental” pertenecientes exclusivamente al Tithoniense Superior y que se engloban en las facies Purbeck que abarcan hasta el Berriasiense (Rat 1962).

Ecologia de Tropidurus torquatus (Wied, 1820) (Squamata, Tropiduridae) no Costão de Itacoatiara, Parque Estadual da Serra da Tiririca, municípios de Niterói e Maricá, RJ

O lagarto Tropidurus torquatus (Wied, 1820) possui ampla distribuição geográfica e é encontrado em abundância nas áreas onde ocorre, sendo considerada uma espécie apropriada para estudos ecológicos. No presente estudo nós analisamos o período de atividade, o uso do microhabitat, a intensidade de forrageamento, a dieta e a ecologia térmica de uma população de T. torquatus do Costão de Itacoatiara, no Parque Estadual da Serra da Tiririca, situado nos municípios de Niterói e Maricá, RJ. Os dados foram coletados em dois períodos: entre julho de 2004 e janeiro de 2008 para estudo do período de atividade, uso do microhabitat e intensidade de forrageamento, e entre julho e agosto de 2010 para estudo da ecologia térmica e dieta. Todos os indivíduos coletados eram adultos, com comprimento rostro-cloacal médio de 66,2 12,0mm para machos (n = 11) e 64,1 8,0mm para fêmeas (n = 03). O período de atividade de T. torquatus no Costão de Itacoatiara durou de 12 a 14 horas. Teve um padrão unimodal na estação seca, com pico de atividade entre 09:00h e 13:00h, durante as horas mais quentes do dia. Na estação chuvosa o padrão de atividade foi bimodal, com um pico entre 8:00h e 9:00h e outro entre 16:00h e 17:00h, ambos associados aos horários de temperaturas ambientais mais amenas. O período de atividade não diferiu entre as estações, o que pode ser explicado pelo extenso pico de atividade dos lagartos na estação seca. Os microhabitats mais utilizados foram o substrato rochoso do Costão e a bromélia, refletindo a disponibilidade destes na área. A intensidade de forrageamento não diferiu sazonalmente e o tempo médio que os lagartos ficaram parados foi maior do que o tempo médio em deslocamento. A dieta foi onívora e esteve composta por artrópodes, principalmente insetos, e material vegetal, principalmente frutos. Os principais insetos consumidos foram Formicidae, Coleoptera e Hymenoptera não-Formicidae como pequenas vespas e abelhas. Os frutos, as sementes e as flores consumidos pertenciam às cactáceas Rhipsalis cereoides e Coleocephalocereus fluminensis, para as quais T. torquatus pode ser um potencial agente dispersor de sementes na área. Lagartos maiores consumiram itens maiores, mas em menor número, indicando um balanço energético positivo. O consumo de material vegetal variou de acordo com o tamanho dos lagartos, aumentando sua proporção nos indivíduos mais velhos. A temperatura média em atividade de T. torquatus foi de 34,3 2,5C, estando na faixa de temperatura corpórea média encontrada para outras populações e para outros Tropidurus. O substrato foi a fonte de calor ambiental com maior importância relativa para a termorregulação dos lagartos durante a estação seca, explicando cerca de 48% da variação na temperatura corpórea da população. Os lagartos termorregularam de forma passiva, principalmente em relação à temperatura do substrato.

Estudio biologíco pesquero del camaron Artemesia longinaris Bate de Mar del Plata

This consisted on the examination of approximately 31.000 specimens obtained from the commercial fishery in the region of Mar del Plata, between Cabo Corrientes and Punta Mogotes (Fig.3) and some complementary material of this area and its vicinities was also included. Living adult animals were also obtained and larvae and postlarvae of this species were separated from the plakton collected during several trips carried on by boats of coastal fleet. These trips allowed the study of the conditions of catches, and the selectivity of both net and fisherman. The aims of this work were to study the migrations, growth, sexual cycle, nutrition, behaviour, mortality and fishing of this important crustacean of commercial interest.

Stations cotières et station hydrologique cotière d'Abidjan années 1977, 1978 et 1979

On tables 1 to 12, daily beach surface temperatures are presented. These temperatures are also ploted on figures 2 to 5 in daily values and in 7, 15, 30 days means. Salinity variations are less important than these of temperature (Fig. 6, 7). It follows that during upwelling period, variations of dynamic height anomaly are closely correlated with temperature (Fig. 6 and 8).

Brincadeira e arte: patrimônio, formação cultural e samba de coco em Pernambuco

Esta proposta de estudo aborda questões relativas a políticas públicas de cultura. Tem por referente o samba de coco nas comunidades afrodescendentes de Castainho e Atoleiros, situadas nos municípios de Garanhuns e Caetés, do agreste de Pernambuco, região que se constitui parcela de território do antigo quilombo dos Palmares, um dos principais focos de resistência dos escravos negros do Brasil colonial, que se manteve incólume durante quase um século. Na região atribuída à existência do antigo quilombo estão vários grupos autointitulados remanescentes, que fazem dos ideais de força e resistência quilombola sua própria vida. O título do estudo é Brincadeira e arte: patrimônio, formação cultural e samba de coco em Pernambuco. O objetivo geral é relacionar o processo de criação em manifestações artísticas populares com as políticas institucionais empreendidas, numa perspectiva intercultural e transdisciplinar, tomando como referencial empírico a brincadeira de samba de coco nos municípios de Garanhuns e Caetés, em Pernambuco, respectivamente nas comunidades Sítio Castainho e Sítio Atoleiros, através da Banda Folclore Verde do Castainho e do Samba de Coco Santa Luzia. A ideia é viabilizar um estudo que se reporta ao conceito de patrimônio cultural étnico brasileiro, percebendo cultura como uma construção histórica da humanidade e compreendendo a manifestação artística como patrimônio imaterial. Trata-se de uma análise sobre grupos brincantes do chamado samba de coco como manifestação plural, de características diversificadas, que ambiciona influenciar políticas públicas destinadas a artistas populares ligados à música, ao canto, à dança e à literatura popular, encarnada em letras de canções, cujo conteúdo é repassado às novas gerações através da oralidade ou por ações de formação cultural, como iniciativas do poder público. Políticas públicas de cultura, patrimônio e formação cultural para preservação são as palavras-chave para identificação das condições atuais da relação entre artistas e gestão pública, considerando a perspectiva de educação não formal, no sentido atribuído pela UNESCO, referenciando-se em depoimentos como principal fonte. Conhecer algumas dimensões do imaginário mítico-simbólico que envolve produtores e gestores, é fundamento para o estudo, que se constitui a partir do levantamento, caracterização e análise da relação entre artistas e instituições de cultura, em diversas instâncias, considerando ideais de modernidade, permanências e transformações observadas no exercício, difusão e gestão da brincadeira. Os produtores do Povoado Atoleiros são criadores do samba de coco, brincadeira de adultos que se traduz em espaço de confraternização e comunhão e recebe interferência do poder público municipal, em Caetés, um dos municípios do entorno de Garanhuns, na periferia do qual está também o Sítio Castainho. Este, a partir de formas diversas de articulação, é contemplado por ações das gestões públicas municipal, estadual e federal, especificamente dentro do Festival de Inverno de Garanhuns FIG. A abordagem contempla a situação das duas comunidades, mas não elimina o reconhecimento de outros locais para a brincadeira do samba de coco e ações de preservação a ela direcionadas, como partes de um processo cultural que é também e necessariamente educativo e, em suas possibilidades de rupturas e continuidades, forma gerações.

Description of embryonic development of Atka mackerel (Pleurogrammus monopterygius)

Atka mackerel (Pleurogrammus monopterygius) is hexagrammid fish that inhabits the temperate and subarctic North Pacific Ocean and neighboring seas (Fig. 1). This highly abundant fish is a critically important prey species (Sinclair and Zeppelin, 2002; Zenger, 2004) that supports a directed commercial trawl fishery (Lowe et al., 2006). Atka mackerel is a demersal spawner and males provide parental care to eggs (Zolotov, 1993). During breeding periods, sexually mature males aggregate on the bottom at nesting sites where they establish territories (Lauth et al., in press). Sexually mature females periodically visit male nesting territories from July to October to spawn batches of demersal egg masses (McDermott and Lowe, 1997; McDermott et al., 2007). Individual nests may consist of multiple egg masses deposited by different females, and males defend nesting territories for a protracted period lasting from the time territories are being established until all eggs within the territory are completely hatched (Lauth et al., 2007). Knowledge about the timing of the reproductive cycle and the use of spawning habitat are important for understanding population structure and the dynamics of stock recruitment, which in turn are important factors in the management of Atka mackerel populations.

Hatching date, nursery grounds, and early growth of juvenile walleye pollock (Theragra chalcogramma) off northern Japan*

Walleye pollock (Theragra chalcogramma) is widely distributed in the North Pacific Ocean and plays an important role in coastal subarctic ecosystems. The Japanese Pacific population of this species is one of the most important demersal fishes for commercial fisheries in northern Japan. The population is distributed along the Pacific coast of Hokkaido and the Tohoku area (Fig. 1), which is the southern limit of distribution of the species in the western North Pacific. In Funka Bay, the main spawning ground for this population, pollock spawn from December to March (Kendall and Nakatani, 1992). Planktonic eggs and larvae are transported into the bay, where juveniles usually remain until late July when they reach 60−85 mm in total length (Hayashi et al., 1968; Nakatani and Maeda, 1987). These juvenile pollock then migrate from Funka Bay eastward to the Doto area off southeastern Hokkaido (Honda et al., 2004). Many studies on eggs, larvae, and juveniles of the species have been conducted in or near Funka Bay, but little information is available on the ecology of the early life stages in the Tohoku area. Hashimoto and Ishito (1991) suggested that eggs are transported from Funka Bay southward to the Tohoku area by the coastal branch of the Oyashio Current, but there has been no study to verify this hypothesis.