Estudio de seis tratamientos nitrogenados bajo riego por goteo de 3.6 litros de agua por metro lineal por día en la producción de chilote en el cultivo del maíz (Zea mays L.), variedad NB-S, a una densidad de 62 500 ptas/ha

El presente trabajo de investigación se estableció entre los meses de febrero–mayo del año 2012, bajo sistema de riego por goteo en los terrenos propiedad de la Universidad Nacional Agraria (UNA), ubicada en el km 12 1/2 carretera norte, municipio de Managua con las coordenadas 12°08 ́36” latitud norte y 86°09 ́49” longitud oeste a una alturade 56 msnm. Con el objetivo de estudiar seis tratamientos nitrogenados (A=50 kg ha-1 de N aplicada 100% a los 21 ddg; B = 50 kg ha-1 de N; Aplicada 50% a los 21dds y 50 % a los 42 ddg; C=50 kg ha-1 de N aplicada 100% a los 42 ddg; D= 100 kg ha-1 de N; Aplicada 100% a los 21 ddg; E= 100 kg ha-1 de N; Aplicada 50% a los 21 ddg y 50 % a los 42 ddg; F=100 kg ha-1 de N; Aplicado 100% a los 42 ddg) ) se estableció un experimento unifactorial en bloques completos al azar, para evaluar el efecto de los mismos sobre el crecimiento del maíz y rendimiento del chilote. Las variables evaluadas fueron durante el desarrollo de la planta: altura de planta, diámetro de tallo, número de hojas. A la cosecha: Altura de la 1era y 2da inserción del chilote (cm),peso del chilote con brácteas y sin brácteas (kg),longitud del chilote con brácteas y sin brácteas (cm), diámetro del chilote con brácteas y sin brácteas (cm) y rendimiento del chilote (kg/ha). La evaluación estadística a los datos de estas variables, se realizó por medio del Análisis de Varianza y separación de medias por Duncan al 5 % de confiabilidad. De los seis tratamientos evaluados, el tratamiento. E indujo al mayor rendimiento de chilote con una producción de 2,265.63 kg ha-1,con un beneficio neto de C$ 12,493.03 córdobas ha-1 y una tasa de retorno marginal del 201.49%

Efecto de seis tratamientos bajo riego localizado en la producción de chilote en el cultivo del maíz (Zea mays L.), variedad NB-S, a una densidad de 62 500 ptas/ha

El presente trabajo de investigación se estableció en época seca entre los meses de marzo mayo 2012, bajo sistema de riego por goteo, el experimento se realizó en los terrenos de la Universidad Nacional Agraria, la cual se encuentra ubicada en el km 12 ½ carretera norte, Managua. Sus coordenadas corresponden 12º 08’ latitud norte y 86º 10’ latitud oeste y a una altura de 56 m.s.n.m. Con el objetivo de obtener información acerca del mejoramiento de rendimiento del chilote en el cultivo del maíz a una densidad de 62500 ptas. ha-1, se estudiaron la aplicación seis tratamientos nitrogenados(A=50 kg/ha de nitrógeno aplicado 100% en la dosis a los 21 ddg; B = 50 kg/ha de nitrógeno aplicando la dosis el 50% a los 21dds y 50 % a los 42 ddg;C=50 kg/ha de nitrógeno aplicando la dosis 100% a los 42 ddg, D=100 kg/ha de nitrógeno, aplicando la dosis 100% a los 21 ddg, E=100 kg/ha de nitrógeno, Aplicando el 50% de la dosis a los 21 ddg y 50 % de la dosis a los 42 ddg y el F=100 kg/ha de nitrógeno aplicado el 100% de la dosis a los 42 ddg ), establecidos en un diseño de bloques completamente al azar. Las variables evaluadas durante el crecimiento del cultivo fueron: altura de planta, numero de hojas y diámetro de tallo; y las variables del rendimiento de chilote y sus principales componentes fueron: altura de primera y segunda inserción, longitud del chilote con y sin bráctea, diámetro del chilote con y sin bráctea, peso del chilote con y sin bráctea y el rendimiento del chilote en kg/ha.El mayor rendimiento se obtuvo con el tratamiento E,con 3744.58 kg ha-1 de chilote, obteniendo un beneficio neto de 34879.56 C$ ha-1 y una tasa de retorno marginal del 733.01 por ciento.

Estudio de diferentes láminas de riego por goteo y aplicación fraccionada de 150kg.ha-1 de nitrógeno, sobre el cultivo del maíz (Zea mays L.) en su rendimiento de chilote a una densidad de 62,500.00 plantas por hectáreas

En la Universidad Nacional Agraria (U.N.A) Ubicada en el km 12 1⁄2 Carretera Norte, cuyas coordenadas geográficas corresponden 12° 8' 56.52" latitud norte y 86° 9' 36.02" longitud oeste a una altura de 56 m.s.n.m, se estableció un ensayo en la época seca comprendido en el período durante los meses de Marzo-Mayo del 2012, se estableció un estudio del Efecto de diferentes láminas de riego por goteo y la aplicación fraccionada dela dosis de 150 kg. ha-1 de N, sobre el crecimiento del cultivo del maíz (Zea mays L.) y el rendimiento del chilote, en la variedad mejorada de Maíz NB-S a una densidad de 62,500.00 plantas/ha-1. Se estableció un ensayo bifactorial 3 x 3, utilizando un arreglo de parcelas divididas, en bloques completos al azar, con cuatro repeticiones y nueve tratamientos. Los Factores en estudio fueron: Factor A (Lámina riego /goteo) y Factor B (Momentos de aplicación de la dosis a raz ón de 150 kg. ha -1 de N) recolectando los datos en la etapa de campo a los 14, 35, 48 ddg y la cosecha a 60 ddg. Las variables evaluadas durante el crecimiento del cultivo fueron: Altura de planta (cm), Diámetro del tallo (cm) y Número de hoja por planta. A los 60 ddg se realizó la cosecha del chilote y se procedió a medir las siguientes variables: altura de la primera y segunda inserción del chilote en (cm), Peso del chilote con brácteas y sin brácteas (gr), Longitud del chilote con brácteas y sin brácteas (cm), Diámetro del chilote con brácteas y sin brácteas (cm), Rendimiento del chilote (kg. ha-1). Los datos recolectados se sometieron a un análisis estadístico de análisis de varianza, y de medias por rangos múltiples de Duncan (α=0.05). Para los 3 niveles evaluados del Factor A (Laminas de riego por goteo), el nivel al indujo al mayor rendimiento de chilote con una producción de 1,291.22 kg.ha -1; de los 3 niveles evaluados del Factor B (Fraccionamiento de la dosis de 150 kg.ha -1 de nitrógeno), el nivel b2 indujo al mayor rendimiento de chilote con una producción de 1,122.94 kg.ha-1. De los nueve tratamientos evaluados, la interacción a 1 b 2 ( 4.5 lt de agua/m/día; 150 kg.ha - 1 de N aplicado (Urea) el 50 % de la dosis a los 21 ddg y 50 % a los 42 ddg.) indujo al mayor rendimiento de chilote con una producción de 1,329.16 kg. ha - 1

Sapientia, 1963, Vol. XVIII, nº 67 (número completo)

Contenido: Multiplicidad material y unidad espiritual / Octavio N. Derisi – Para una filosofía de la Universidad / Alberto Caturelli – La moral existencialista y la regulación racional tomista / José Ignacio Alcorta – La cultura y las culturas / Octavio N. Derisi – Notas y comentarios -- Bibliografía

Aperfeiçoamentos no DL nº 167/67 : emolumentos extrajudiciais e garantias reais em Cédulas de Crédito Rural-CCR e em Cédulas de Crédito Bancário-CCB

Consultoria de Orçamento e Fiscalização Financeira.

Legislação processual aplicável aos prefeitos e o Decreto-Lei nº 201/67

Consultoria Legislativa - Área I - Direito Constitucional, Eleitoral, Municipal, Direito Administrativo, Processo Legislativo e Poder Judiciário.

Diário da Constituinte [gravação de vídeo] : [programa n. 500 ]

O sindicato dos artistas mantem contato diário com os constituintes. Eles querem que a Constituinte garanta alguns direitos e traga avanços para cultura do país. Eles pedem a aprovação de várias emendas dentre as quais, a do deputado Roberto D’ Ávila que cria obrigatoriedade de produção regional na área artística e cultural e outra que suprime o artigo que impede empresas culturais com fins lucrativos de utilizar verbas do governo. Será Realizado um seminário cujos participantes serão deputados estaduais e funcionários. O objetivo do seminário será a troca de experiências que contribuirão na elaboração das constituintes estaduais. O presidente da Assembleia apresentou um novo cronograma para encerrar o primeiro turno em quarenta sessões. Foi apresentada também outra proposta para apressar a Constituinte que consiste em realizar algumas fusões que facilitarão a votação de pontos polêmicos além da diminuição da exigência de quórum. Ainda não está definida a definida a punição para os faltosos. Começa a discussão sobre as emendas que aperfeiçoam o presidencialismo, já aprovadas. Ficou mantido o quórum para a moção de censura aos ministros de Estado. A votação avançou por causa de acordo feito entre as lideranças, no qual foi aprovada a fusão de três emendas. O candidato à vice-presidente será registrado junto com o presidente da república e se nenhum candidato alcançar maioria absoluta na primeira votação haverá nova eleição trinta dias depois entre os dois candidatos mais votados. O presidente da república poderá vetar projetos de lei total ou parcialmente.

Shoreline erosion due to extreme storms and sea level rise

A summary is presented of research conducted on beach erosion associated with extreme storms and sea level rise. These results were developed by the author and graduate students under sponsorship of the University of Delaware Sea Grant Program. Various shoreline response problems of engineering interest are examined. The basis for the approach is a monotonic equilibrium profile of the form h = Ax2 /3 in which h is water depth at a distance x from the shoreline and A is a scale parameter depending primarily on sediment characteristics and secondarily on wave characteristics. This form is shown to be consistent with uniform wave energy dissipation per unit volume. The dependency of A on sediment size is quantified through laboratory and field data. Quasi-static beach response is examined to represent the effect of sea level rise. Cases considered include natural and seawalled profiles. To represent response to storms of realistic durations, a model is proposed in which the offshore transport is proportional to the "excess" energy dissipation per unit volume. The single rate constant in this model was evaluated based on large scale wave tank tests and confirmed with Hurricane Eloise pre- and post-storm surveys. It is shown that most hurricanes only cause 10% to 25% of the erosion potential associated with the peak storm tide and wave conditions. Additional applications include profile response employing a fairly realistic breaking model in which longshore bars are formed and long-term (500 years) Monte Carlo simulation including the contributions due to sea level rise and random storm occurrences. (PDF has 67 pages.)

Cruise Report 67-S-1 Crab

(PDF contains 6 pages.)

Cruise Report 67-S-2 Shrimp

(PDF contains 4 pages.)

Cruise Report 67-S-3 (Bottomfish Extension)

(PDF contains 1 page.)

Cruise Report 67-S-4 - Albacore

(PDF contains 3 pages.)

Cruise Report 67-S-5

(PDF contains 4 pages.)

Distribution of Atlantic menhaden, Brevoortia tyrannus, purse-seine sets and catches from southern New England to North Carolina, 1985-96

Sets and catches of Atlantic menhaden, Brevoortia tyrannus, made in 1985-96 by purse-seine vessels from Virginia and North Carolina were studied by digitizing and analyzing Captain's Daily Fishing Reports (CDFR's), daily logs of fishing activities completed by captains of menhaden vessels. 33,674 CDFR's were processed, representing 125,858 purse-seine sets. On average, the fleet made 10,488 sets annually. Virginia vessels made at least one purse-seine set on 67%-83% of available fishing days between May and December. In most years, five was the median number of sets attempted each fishing day. Mean set duration ranged from 34 to 43 minutes, and median catch per set ranged from 15 to 30 metric tons (t). Spotter aircraft assisted in over 83% of sets overall. Average annual catch in Chesapeake Bay (149,500 t) surpassed all other fishing areas, and accounted for 52% of the fleet's catch. Annual catch from North Carolina waters (49,100 t) ranked a distant second. Fishing activity in ocean waters clustered off the Mid-Atlantic states in June-September, and off North Carolina in November-January. Delaware Bay and the New Jersey coast were important alternate fishing grounds during summer. Across all ocean fishing areas, most sets and catch occurred within 3 mi. of shore, but in Chesapeake Bay about half of all fishing activity occurred farther offshore. In Virginia, areas adjacent to fish factories tended to be heavily fished. Recent regulatory initiatives in various coastal states threaten the Atlantic menhaden fleet's access to traditional nearshore fishing grounds. (PDF file contains 26 pages.)

Part I. A study of the velocity structure of the earth by the use of core phases. Part II. The 1971 San Fernando earthquake series focal mechanisms and tectonics

The initial objective of Part I was to determine the nature of upper mantle discontinuities, the average velocities through the mantle, and differences between mantle structure under continents and oceans by the use of P'dP', the seismic core phase P'P' (PKPPKP) that reflects at depth d in the mantle. In order to accomplish this, it was found necessary to also investigate core phases themselves and their inferences on core structure. P'dP' at both single stations and at the LASA array in Montana indicates that the following zones are candidates for discontinuities with varying degrees of confidence: 800-950 km, weak; 630-670 km, strongest; 500-600 km, strong but interpretation in doubt; 350-415 km, fair; 280-300 km, strong, varying in depth; 100-200 km, strong, varying in depth, may be the bottom of the low-velocity zone. It is estimated that a single station cannot easily discriminate between asymmetric P'P' and P'dP' for lead times of about 30 sec from the main P'P' phase, but the LASA array reduces this uncertainty range to less than 10 sec. The problems of scatter of P'P' main-phase times, mainly due to asymmetric P'P', incorrect identification of the branch, and lack of the proper velocity structure at the velocity point, are avoided and the analysis shows that one-way travel of P waves through oceanic mantle is delayed by 0.65 to 0.95 sec relative to United States mid-continental mantle.

A new P-wave velocity core model is constructed from observed times, dt/dΔ's, and relative amplitudes of P'; the observed times of SKS, SKKS, and PKiKP; and a new mantle-velocity determination by Jordan and Anderson. The new core model is smooth except for a discontinuity at the inner-core boundary determined to be at a radius of 1215 km. Short-period amplitude data do not require the inner core Q to be significantly lower than that of the outer core. Several lines of evidence show that most, if not all, of the arrivals preceding the DF branch of P' at distances shorter than 143° are due to scattering as proposed by Haddon and not due to spherically symmetric discontinuities just above the inner core as previously believed. Calculation of the travel-time distribution of scattered phases and comparison with published data show that the strongest scattering takes place at or near the core-mantle boundary close to the seismic station.

In Part II, the largest events in the San Fernando earthquake series, initiated by the main shock at 14 00 41.8 GMT on February 9, 1971, were chosen for analysis from the first three months of activity, 87 events in all. The initial rupture location coincides with the lower, northernmost edge of the main north-dipping thrust fault and the aftershock distribution. The best focal mechanism fit to the main shock P-wave first motions constrains the fault plane parameters to: strike, N 67° (± 6°) W; dip, 52° (± 3°) NE; rake, 72° (67°-95°) left lateral. Focal mechanisms of the aftershocks clearly outline a downstep of the western edge of the main thrust fault surface along a northeast-trending flexure. Faulting on this downstep is left-lateral strike-slip and dominates the strain release of the aftershock series, which indicates that the downstep limited the main event rupture on the west. The main thrust fault surface dips at about 35° to the northeast at shallow depths and probably steepens to 50° below a depth of 8 km. This steep dip at depth is a characteristic of other thrust faults in the Transverse Ranges and indicates the presence at depth of laterally-varying vertical forces that are probably due to buckling or overriding that causes some upward redirection of a dominant north-south horizontal compression. Two sets of events exhibit normal dip-slip motion with shallow hypocenters and correlate with areas of ground subsidence deduced from gravity data. Several lines of evidence indicate that a horizontal compressional stress in a north or north-northwest direction was added to the stresses in the aftershock area 12 days after the main shock. After this change, events were contained in bursts along the downstep and sequencing within the bursts provides evidence for an earthquake-triggering phenomenon that propagates with speeds of 5 to 15 km/day. Seismicity before the San Fernando series and the mapped structure of the area suggest that the downstep of the main fault surface is not a localized discontinuity but is part of a zone of weakness extending from Point Dume, near Malibu, to Palmdale on the San Andreas fault. This zone is interpreted as a decoupling boundary between crustal blocks that permits them to deform separately in the prevalent crustal-shortening mode of the Transverse Ranges region.