Comparación de calidad en la producción de carbón vegetal en la Finca El Plantel, Masaya

La presente investigación tuvo como objetivo comparar la producción de calidad de carbón vegetal entre la fosa de tierra y el horno de ladrillo utilizando Eucalyptus camaldulensis, se seleccionaron árboles con diámetros entre 20-30 cm y mayores de 30 cm. Por cada categoría diamétrica se emplearon cinco árboles para un total de diez individuos, se tumbaron los árboles con la técnica de tala dirigida, con hacha a partir de 30 cm del suelo. Se procedió a medir la longitud de la troza en metros empleando una cinta métrica para la medición del diámetro medio. Se calculó el volumen del fuste limpio utilizando la fórmula de Smalian, posteriormente se trasladó trozas y ramas al sitio de carbonización, se depositaron por clase diamétrica donde se calculó el volumen empleando la fórmula de Huber, para la cubicación de las ramas se empleó el método de metro estéreo. Para la clase diamétrica de 20 a 30 cm se utilizó un volumen de 4.48 m3 y para mayor de 30 cm, 6.55 m3 -. Finalizado el proceso de carbonización se obtuvieron ocho sacos en la fosa de tierra, equivalente a 0.217 m3, en el horno de ladrillo se obtuvieron 18 sacos lo que representa 0.496 m3. . Comparando los estándares de calidad de la FAO, con los obtenidos en este estudio, son aceptables, se concluye que el método de producción de horno de ladrillos usando arboles mayores de 30 cm es el mejor método para la producción de carbón vegetal.

Non-die explosive forming of spherical pressure-vessels

This paper presents a newly developed method of manufacturing spherical pressure vessels based on the technology of non-die explosive forming. Compared with the traditional method, this technology does not need any dies and pressing equipment, so that the cost of the production process can be greatly reduced, especially for vessels of less than 100 m3 capacity.

Magnetic properties of sintered sm2fe17ny magnets

Sintered magnets of Sm2Fe17Ny nitrides, with a density of 6.0-7.4 g/cm3, have been prepared by using an explosion technique. Both crystalline structure and the magnetic properties of Sm2Fe17Ny nitrides were retained in the process. The sintered magnet had a remanence B(r)=0.83 T, an intrinsic coercivity mu(0i)H(c)=0.57 T and an energy product (BH)max=88 kJ/m3. The temperature dependence of coercivity and remanence were also measured. The temperature coefficients alpha of remanence and beta of coercivity are -0.076%/degrees-C and -0.51%/degrees-C, respectively.

Reproducción de Tarjeta de visita de Eliodoro de la Torre.

Fecha: s.f. (>1970 reproducción) / Unidad de instalación: Carpeta 25 - Expediente 23-5 / Nº de pág.: 1 (mecanografiada)

Niveles de nutrientes y pigmentos fotosintéticos en el Río de la Plata interior (55°-59°W 34°-36°S)

The "Río de la Plata" River is one of the less studied systems of the basin with respect to its biological and ecological aspects. Twenty four and twenty seven surface stations were sample on September 22-23 and November 22-23, 1982, respectively. The section studied is part of the zone called inner "Río de la Plata" River. The discharge was 29.000 m3/s in September and 45.200 m3/s in November. Total phosphorus (PT), total organic nitrogen (NOT), chemical oxygen demad (COT) and total cholrophyll were measured. Dissolved oxygen (DO), turbidity (TURB), pH and electrical conductivity (K20) were also measured at the surface with a HORIBA U7 sensor on November 1982. PT was 72-208 mg/m3 and 66-205 mg/m3 in September and November repectively; the higher values were near the Argentinian coast and the outer zone. NOT was 33-106 µM and 49-117 µM and CHL was 1.4-5.8 mg/m3 and 1.3-9.4 mg/m3. TURB was between 44 and 240 NTU in November; the maximun value were obseved in the central zone. Steep K20 gradients were found near both coast. The reduced organic carbon load into the lower and external part of the "Río de la Plata" River was estimated. (Document contains 40 pages.)

Faunas locales argentinas. I. Lista de los pescados recogidos en los alrededores de La Plata (prov. de Bs. As.), durante el año 1894 y conservados en las colecciones del Museo de La Plata.

Publicación de la lista de materiales depositados en la Colección de la Sección Zoológica del Museo de La Plata y sus localidades. (PDF tiene 13 paginas.)

Manual do subdito fiel [pseud.], ou, Cartas de um lavrador a sua Magestade o Imperador sobre a questão do elemento servil

A campanha abolicionista já entrava em sua reta final e um dos documentos jurídicos mais claros e esclarecedores a seu favor foi redigido pelo deputado da Bahia, Ruy Barbosa, em parecer apresentado às Comissões de Orçamento e Justiça Civil, em 4 de agosto de 1884.

Recent Oyster researches on Chesapeake Bay in Maryland

At one time Maryland produced more oysters annually than the rest of the world combined, including all species used for food. This document shows the decline in production to one sixth of the 1884 yield in 1929-1930. Observations over the course of the last decade have indicated two major factors responsible for the decline in oyster production. Reduction of brood stock stands first, while failing to provide clutch (shells) for the setting purposes has been a close second. (PDF contains 29 pages)

Atlas dos itinerarios, perfis longitudinaes e da zona demarcada = Atlas des itinéraires, des profils longitudinaux et de la zône démarquée publicado por L. Cruls

Referenciado por : Blake, Sacramento. Diccionario bibliographico brazileiro. Rio de Janeiro: Imprensa Nacional, 1883-1902. v. 4, p. 386-388

Limites entre o Brazil e a Bolivia : relatorio apresentado ao Exmo. Sr. Dr. Olyntho de Magalhaes Ministro das Relaçoes Exteriores

Louis Cruls nasceu em Diest, Bélgica, em 1848, e morreu em Paris, em 1908. Formado em Engenharia Civil, desenvolveu notáveis trabalhos nos campos da geografia, geologia, meteorologia e astronomia. Em 1874, mudou-se para o Brail, onde participou de diversas expedições cientìficas, especialmente, pela região do Planalto Central. Foi engenheiro da Comissão da Carta-Geral do Império. Em 1876, foi admitido como voluntário no observatório astronomico do Rio de Janeiro, e em 1884 tornou-se diretor ao suceder o frances E. Liais. Planejou e integrou diversas comissões, entre as quais a de exploração do Planalto Central do Brasil, em 1892, cuja finalidade era identificar e escolher o melhor local para a implantação da futura capital do País.

A video method for quantifying size distribution, density, and three-dimensional spatial structure of reef fish spawning aggregations

There is a clear need to develop fisheries independent methods to quantify individual sizes, density, and three dimensional characteristics of reef fish spawning aggregations for use in population assessments and to provide critical baseline data on reproductive life history of exploited populations. We designed, constructed, calibrated, and applied an underwater stereo-video system to estimate individual sizes and three dimensional (3D) positions of Nassau grouper (Epinephelus striatus) at a spawning aggregation site located on a reef promontory on the western edge of Little Cayman Island, Cayman Islands, BWI, on 23 January 2003. The system consists of two free-running camcorders mounted on a meter-long bar and supported by a SCUBA diver. Paired video “stills” were captured, and nose and tail of individual fish observed in the field of view of both cameras were digitized using image analysis software. Conversion of these two dimensional screen coordinates to 3D coordinates was achieved through a matrix inversion algorithm and calibration data. Our estimate of mean total length (58.5 cm, n = 29) was in close agreement with estimated lengths from a hydroacoustic survey and from direct measures of fish size using visual census techniques. We discovered a possible bias in length measures using the video method, most likely arising from some fish orientations that were not perpendicular with respect to the optical axis of the camera system. We observed 40 individuals occupying a volume of 33.3 m3, resulting in a concentration of 1.2 individuals m–3 with a mean (SD) nearest neighbor distance of 70.0 (29.7) cm. We promote the use of roving diver stereo-videography as a method to assess the size distribution, density, and 3D spatial structure of fish spawning aggregations.

Seasonal, horizontal, and vertical distribution of phytoplankton chlorophyll a in the Northeast U.S. Continental Shelf Ecosystem

The broad scale features in the horizontal, vertical, and seasonal distribution of phytoplankton chlorophyll a on the northeast U.S. continental shelf are described based on 57,088 measurements made during 78 oceanographic surveys from 1977 through 1988. Highest mean water column chlorophyll concentration (Chlw,) is usually observed in nearshore areas adjacent to the mouths of the estuaries in the Middle Atlantic Bight (MAB), over the shallow water on Georges Bank, and a small area sampled along the southeast edge of Nantucket Shoals. Lowest Chlw «0.125 ug l-1) is usually restricted to the most seaward stations sampled along the shelf-break and the central deep waters in the Gulf of Maine. There is at least a twofold seasonal variation in phytoplankton biomass in all areas, with highest phytoplankton concentrations (m3) and highest integrated standing stocks (m2) occurring during the winter-spring (WS) bloom, and the lowest during summer, when vertical density stratification is maximal. In most regions, a secondary phytoplankton biomass pulse is evident during convective destratification in fall, usually in October. Fall bloom in some areas of Georges Bank approaches the magnitude of the WS-bloom, but Georges Bank and Middle Atlantic Bight fall blooms are clearly subordinate to WS-blooms. Measurements of chlorophyll in two size-fractions of the phytoplankton, netplankton (>20 um) and nanoplankton «20 um), revealed that the smaller nanoplankton are responsible for most of the phytoplankton biomass on the northeast U.S. shelf. Netplankton tend to be more abundant in nearshore areas of the MAB and shallow water on Georges Bank, where chlorophyll a is usually high; nanoplankton dominate deeper water at the shelf-break and deep water in the Gulf of Maine, where Chlw is usually low. As a general rule, the percent of phytoplankton in the netplankton size-fraction increases with increasing depth below surface and decreases proceeding offshore. There are distinct seasonal and regional patterns in the vertical distribution of chlorophyll a and percent netplankton, as revealed in composite vertical profiles of chlorophyll a constructed for 11 layers of the water column. Subsurface chlorophyll a maxima are ubiquitous during summer in stratified water. Chlorophyll a in the subsurface maximum layer is generally 2-8 times the concentration in the overlying and underlying water and approaches 50 to 75% of the levels observed in surface water during WS-bloom. The distribution of the ratio of the subsurface maximum chlorophyll a to surface chlorophyll a (SSR) during summer parallels the shelfwide pattern for stability, indexed as the difference in density (sigma-t) between 40 m and surface (stability 40. The weakest stability and lowest SSR's are found in shallow tidally-mixed water on Georges Bank; the greatest stability and highest SSR's (8-12:1) are along the mid and outer MAB shelf, over the winter residual water known as the "cold band." On Georges Bank, the distribution of SSR and the stability40 are roughly congruent with the pattern for maximum surface tidal current velocity, with values above 50 cms-1 defining SSR's less than 2:1 and the well-mixed area. Physical factors (bathymetry, vertical mixing by strong tidal currents, and seasonal and regional differences in the intensity and duration of vertical stratification) appear to explain much of the variability in phytoplankton chlorophyll a throughout this ecosystem. (PDF file contains 126 pages.)

Historia patria : o Brazil de 1831 a 1840

História cronológica do período da Minoridade, com detalhes sobre suas conspirações e lutas.

Reflexões sobre a metaphysica do calculo infinitesimal

Referência: Diccionario Bibliographico Portuguez / Innocencio Francisco da Silva, 1884 v. 6, p. 8