Morphology characterization of layer-by-layer films from PAH/MA-co-DR13: the role of film thickness

We report on the use of dynamic scale theory and fractal analyses in the Study of distinct growth stages of layer-by-layer (LBL) films of poly(allylamine hydrochloride) (PAH) and a side-chain-substituted azobenzene copolymer (Ma-co-DR13). The LBL films were adsorbed oil glass substrates and characterized with atomic force microscopy with the Ma-co-DR13 at the top layer. The ganular morphology exhibited by the films allowed the observation of the growth process inside and outside the grains. The growth outside the grains was found to follow the Kardar-Parisi-Zhang model, with fractal dimensions of ca. 2.6. One could expect that inside the grains the morphology would be close to a Euclidian surface with fractal dimension of ca. 2 for any growth stage. The latter, however, was observed only for thicker films containing more than 10 bilayers. For thinner films the morphology was well described by a self-affine fractal. Such dependence of the growth behavior with the film thickness is associated with a more complete coverage of adsorption sites in thicker films due to diffusion of polymer molecules. (c) 2004 Elsevier B.V. All rights reserved.

An image processing method for morphology characterization and pitting corrosion evaluation

A digital image processing and analysis method has been developed to classify shape and evaluate size and morphology parameters of corrosion pits. This method seems to be effective to analyze surfaces with low or high degree of pitting formation. Theoretical geometry data have been compared against experimental data obtained for titanium and aluminum alloys subjected to different corrosion tests. (C) 2002 Elsevier B.V. B.V. All rights reserved.

Morphology, characterization, and distribution of retinal photoreceptors in the Australian lungfish Neoceratodus forsteri (Krefft, 1870)

The Australian lungfish Neoceratodus forsteri (Dipnoi) is an ancient fish that has a unique phylogenetic relationship among the basal Sarcopterygii. Here we examine the ultrastructure, histochemistry, and distribution of the retinal photoreceptors using a combination of light and electron microscopy in order to determine the characteristics of the photoreceptor layer in this living fossil. Similar proportions of rods (53%) and cones (47%) reveal that N. forsteri optimizes both scotopic and photopic sensitivity according to its visual demands. Scotopic sensitivity is optimized by a tapetum lucidum and extremely large rods (18.62 +/- 2.68 mu m ellipsoid diameter). Photopic sensitivity is optimized with a theoretical spatial resolving power of 3.28 +/- 0.66 cycles degree(-1), which is based on the spacing of at least three different cone types: a red cone containing a red oil droplet, a yellow cone containing a yellow ellipsoidal pigment, and a colorless cone containing multiple clear oil droplets. Topographic analysis reveals a heterogeneous distribution of all photoreceptor types, with peak cone densities predominantly found in temporal retina (6,020 rods MM 2, 4,670 red cones mm(-2), 900 yellow cones mm(-2), and 320 colorless cones mm(-2)), but ontogenetic changes in distribution are revealed. Spatial resolving power and the diameter of all photoreceptor types (except yellow cones) increases linearly with growth. The presence of at least three morphological types of cones provides the potential for color vision, which could play a role in the clearer waters of its freshwater environment.

Study on the thermal stability of InN by in-situ laser reflectance system

The thermal stability of InN in the growth environment in metalorganic chemical vapor deposition was systematically investigated in situ by laser reflectance system and ex situ by morphology characterization, X-ray diffraction and X-ray photoelectron spectroscopy. It was found that InN can withstand isothermal annealing at temperature as high as 600 degrees C in NH3 ambient. While in N-2 atmosphere, it will decompose quickly to form In-droplets at least at the temperature around 500 degrees C, and the activation energy of InN decomposition was estimated to be 2.1 +/- 0.1 eV. Thermal stability of InN when annealing in NH3 ambient during temperature altering would be very sensitive to ramping rate and NH3 flow rate, and InN would sustain annealing process at small ramping rate and sufficient supply of reactive nitrogen radicals. Whereas In-droplets formation was found to be the most frequently encountered phenomenon concerning InN decomposition, annealing window for conditions free of In-droplets was worked out and possible reasons related are discussed. In addition, InN will decompose in a uniform way in the annealing window, and the decomposition rate was found to be in the range of 50 and 100 nm/h. Hall measurement shows that annealing treatment in such window will improve the electrical properties of InN. (c) 2005 Elsevier B.V. All rights reserved.

Síntese e impregnação de peneiras moleculares Fe MCM-41 derivada de sílica da casca do arroz

The mesoporous molecular sieves of the MCM-41 and FeMCM-41 type are considered promissory as support for metals used as catalysts in oil-based materials refine processes and as adsorbents for environmental protection proposes. In this work MCM-41 and FeMCM41 were synthesized using rice husk ash - RHA as alternative to the conventional silica source. Hydrothermal synthesis was the method chosen to prepare the materials. Pre-defined synthesis parameters were 100°C for 168 hours, later the precursor was calcinated at 550°C for 2 hours under nitrogen and air flow. The sieves containing different proportions of iron were produced by two routes: introduction of iron salt direct synthesis; and a modification post synthesis consisting in iron salt 1 % and 5% impregnation in the material followed by thermal decomposition. The molecular sieves were characterized by X ray diffraction XRD, Fourier transform infrared spectroscopy FT-IR, X ray fluorescence spectroscopy XFR, scanning electronic microscopy SEM, specific surface area using the BET method, Termogravimetry TG. The kinetic model of Flynn Wall was used with the aim of determining the apparent activation energy of the surfactant remove (CTMABr) in the MCM- 41 porous. The analysis made possible the morphology characterization, identifying the presence of hexagonal structure typical for mesoporous materials, as well as observation of the MCM41 and iron of characteristic bands.

Caracterização morfológica de plantas de rambutan

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Caracterização morfológica da corrosão por pite da liga AL2024 em soluções contendo cloretos e molibdatos

A very new method application for digital image processing and analysis to classify shape and evaluate size and morphology parameters of pit corrosion is used in this paper. This method seems to be very effective to analysis surfaces with low or high degree of pitting formation. Pits formed on 2024 alloy surface by chloride and by chloride + molibdate anions have similar mean area, are found to be widther than deeper and exhibit predominantly conical or near-conical and irregular geometries.

Aplicación de distintas metodologías a la monitorización de la humedad del suelo y al cálculo del balance hídrico diario

Dada la importancia de conocer la humedad del suelo de forma precisa y en tiempo real, se ha realizado este trabajo de investigación cuyo objetivo principal ha sido seleccionar un Balance Hídrico del Suelo (BHS) diario y validar sus estimaciones de humedad del suelo frente a medidas obtenidas “in situ”, aplicándolo a tres emplazamientos seleccionados en la zona centro con características edáficas y climáticas diferentes, y de este modo estimar con cierta precisión la humedad del suelo como Agua Disponible (AD) para las plantas y a su vez permitir la realización de estudios climáticos. Los observatorios meteorológicos seleccionados fueron: Guadalajara/El Serranillo en la zona aluvial del río Henares; Colmenar Viejo/Base Famet en la rampa sur del Guadarrama sobre rocas metamórficas; y Radiosondeo/Madrid(Barajas) en arenas arcósicas de grano grueso. Se realizó una caracterización morfológica y un estudio de las propiedades físicas, químicas e hidrofísicas de los suelos en cada emplazamiento. El suelo de Guadalajara, Xerorthent Típico presenta una secuencia genética de horizontes (Ap-AC-C1-C2) siendo su clase textural entre franco-arenosa a franca, con menos del 2% de elementos gruesos, presencia de caliza a lo largo de todo el perfil, destacando la homogeneidad en vertical y horizontal de sus propiedades. El suelo de Colmenar, Xerorthent Dystrico, presenta una secuencia genética de horizontes (A-C-C/R) apareciendo el horizonte C/R entre 20-30 cm; y la roca aproximadamente a unos 30 cm; destacando en este perfil su acidez y el alto contenido de elementos gruesos. El suelo de Radiosondeo, Haploxeralf Típico, presenta la secuencia normal de horizontes de los alfisoles (A-Bt1-Bt2-C/Bt); destacando su heterogeneidad principalmente en el plano horizontal, con presencia del Bt a diferentes profundidades en un corto espacio longitudinal. En una primera fase de experimentación (2007-2008) se seleccionaron BHS diarios que sólo utilizaban como datos de entrada la información de variables meteorológicas y el valor del Agua Disponible Total (ADT) para cada tipo de suelo y profundidad. Se probaron BHS diarios con agotamiento exponencial y directo de la reserva, utilizando la evapotranspiración de referencia de Penman-Monteith recomendada por FAO. Al mismo tiempo que se disponía de los datos estimados de humedad de suelo mediante diferentes BHS diarios en los tres emplazamientos, también se realizó una monitorización de la humedad del suelo “in situ” mediante el método gravimétrico, con adaptación de dicha metodología a la problemática de cada suelo, para determinar en cada fecha tanto la humedad del suelo como su contenido de AD para una profundidad de 0 a 30 cm. Se tomaron en cada fecha de muestreo 5 muestras para la profundidad 0- 10 cm, otras cinco para 10-20 cm y otras cinco para 20-30 cm, realizándose el correspondiente tratamiento estadístico de los datos. El ADT se calculó a partir de los datos de capacidad de campo y punto de marchitez obtenidos en laboratorio con membrana de Richards. Los resultados de esta primera fase permitieron conocer que el BHS exponencial diario era el que mejor estimaba el AD en Guadalajara considerando la capacidad de campo a una presión de 33 kPa, mientras que en Colmenar se debían considerar para un mejor ajuste, 10 kPa en lugar de 33 kPa. En el observatorio de Radiosondeo debido a que en cada fecha de muestreo la profundidad en la que aparecía el horizonte Bt era diferente, no se pudo demostrar si el BHS exponencial diario tenía un buen comportamiento. En una segunda fase de experimentación (2009-2012) y con el objeto de aminorar los problemas encontrados en Radiosondeo para la medida de humedad del suelo por el método gravimétrico, se procedió a la instalación y utilización de diferentes sensores de medida de humedad de suelo en el mismo observatorio: TDR (time domain reflectometry - TRIME T3 de IMKO); FDR capacitivo (frecuency domain reflectometry - ECH2O EC-20 de DECAGON) y otros. Esta segunda fase de experimentación tuvo una duración de 4 años y se compararon las medidas de humedad de suelo obtenidas a partir de los sensores con las estimadas del BHS exponencial hasta una profundidad de 0 a 85 cm. En laboratorio se realizaron calibraciones específicas de los sensores TDR y FDR para cada uno de los horizontes más diferenciados del Haploxeralf Típico, utilizando diferentes tipos de regresión. Los valores de humedad de suelo con el equipo TDR, corregidos mediante la calibración específica de laboratorio, fueron los que más se ajustaron a las medidas realizadas por método gravimétrico “in situ”, por lo que se utilizó el TDR para las comparaciones con los valores obtenidos del BHS exponencial diario durante los cuatro años de esta segunda fase experimental. Se realizaron diferentes estimaciones del ADT, partiendo de datos de laboratorio y/o de datos procedentes de humedad de los sensores en campo. Los resultados mostraron de nuevo la conveniencia de utilizar el BHS exponencial diario, pero en este caso, con la estimación del ADT realizada a partir de las gráficas de los sensores. Mediante la utilización de los datos de humedad del BHS exponencial diario se han realizado comparaciones con el mismo tipo de balance pero utilizando un periodo semanal o mensual en lugar de diario, para conocer las diferencias. Los valores obtenidos con periodicidad mensual han dado valores de AD inferiores a los balances calculados semanalmente o diariamente. Por último se ha comprobado que los resultados de un BHS exponencial diario pueden complementar la información que se obtiene del Índice de Precipitación Estandarizado (SPI) y pueden mejorar el estudio de la sequía agrícola. ABSTRACT Due to the importance of a better knowledge of soil water at real time and in a more precisely way, this research work has being carried out with the main objective of selecting a daily Soil Water Balance (SWB) to estimate soil water content, and validate it in comparison to “in situ” measurements. Three locations, differing in soil and climate characteristics, were selected in central Spain in order to estimate with certain acuity soil water as plant-Available Water (AW) and to serve as a tool for the climatic studies. The selected places near meteorology stations were: Guadalajara/El Serranillo an alluvium of the Henares watershed; Colmenar Viejo/Base Famet, in the south raised area of the Guadarrama river basin, over metamorphic rocks; and Radiosondeo/Madrid (Barajas) in coarse arkosic sandstone. Morphology characterization, physical, chemical and hydrologic soil properties were studied in each area. In Guadalajara the soil is a Typic Xerorthent with a (Ap-AC-C1- C2) genetic horizon sequence, loam-sandy to loam textural class, less than 2% of rock fragments, presence of equivalent CaCO3 through the whole profile, outstanding the vertical and horizontal homogeneity of the properties. In Colmenar the soil is represented by a Dystric Xerorthent with a (A-C-C/R) genetic horizon sequence, the C/R is 20-30 cm deep where rock outcrops are approximately at 30 cm; a characteristic feature of this profile is its high acidity and high rock fragments content. In Radiosondeo the soil is represented by a Typic Haploxeralf, with the usual alfisol genetic horizon sequence (A-Bt1-Bt2-C/Bt); outstanding its horizontal heterogeneity, “the variability of the Bt (clay enriched horizon) depth in short distances”. In a first experimental stage (2007-2008), the daily SWB chosen was that which only uses as input data the information from the meteorology variables and plant-Total Available Water (TAW) for each soil type and depth. Different daily SWB (with exponential or direct plant-Available Water depletion) were applied, using the Penman- Monteith reference evapotranspiration (ETo) recommended by FAO. At the same time as soil water content was estimated from the different daily SWB at the three locations, also soil water content was being monitored by “in situ” gravimetric methodology, adapting it to each soil characteristic, to determine every time soil water content and AW to a depth of 0 to 30 cm. In each sampling date, 5 samples for each depth were taken: 0-10 cm; 10-20 cm and 20-30 cm and the data were submitted to the corresponding statistical analysis. The TAW was calculated based on field capacity (FC) and permanent wilting point (PWP) data obtained from laboratory by the Richards pressure plate. Results from this first experimental stage show that the daily exponential SWB was the one which better estimated the AW in Guadalajara considering field capacity at -33 kPa, though in Colmenar, field capacity at -10 kPa must be considered instead of -33 kPa for a better estimation. In Radiosondeo due to the fact that the Bt horizon depth varied in different sampling dates, it could not be established if the daily exponential SWB had a good performance. In a second experimental stage (20019-2012) and with the objective of minimizing the problems encountered in Radiosondeo for measuring “in situ” soil water content by the gravimetric method, the installation of different sensors for measuring soil water content were established and used in the same field location: TDR (time domain reflectometry - TRIME T3 from IMKO), capacitance FDR (frecuency domain reflectometry - ECH2O EC-20 from DECAGON) and others. This second experimental stage lasted 4 years in order to compare the soil water measures from the sensors with the estimations by the exponential SWB form 0 to 85 cm soil depths. At laboratory, specific calibrations for TDR and FDR sensors of the Typic Haploxeralf more differentiated horizons were done using different types of regressions. The results showed that soil water data obtained by the TDR equipment, corrected by the specific laboratory calibration, best fitted to “in situ” gravimetric soil water measures. In this way TDR was used for comparing to the daily exponential SWB during the four years of this second experimentation stage. Various estimations for obtaining TAW were tested; based on laboratory data – and/or on the data obtained of the soil water content field sensors. Results confirmed again, the convenience of using the daily exponential SWB, though in this case, with the TAW obtained from the field sensors graphics. Soil water estimated by exponential SWB on daily basis was compared to weekly and monthly periods, in order to know their reliability. The results obtained for a monthly period gave less AW than the ones obtained in a weekly or daily period. Finally it has been proved that the results obtained from the exponential SWB in a daily bases can be used as a useful tool in order to give complementary information to the SPI (Precipitation Standardized Index) and to help in agricultural drought studies.

Síntese e impregnação de peneiras moleculares Fe MCM-41 derivada de sílica da casca do arroz

The mesoporous molecular sieves of the MCM-41 and FeMCM-41 type are considered promissory as support for metals used as catalysts in oil-based materials refine processes and as adsorbents for environmental protection proposes. In this work MCM-41 and FeMCM41 were synthesized using rice husk ash - RHA as alternative to the conventional silica source. Hydrothermal synthesis was the method chosen to prepare the materials. Pre-defined synthesis parameters were 100°C for 168 hours, later the precursor was calcinated at 550°C for 2 hours under nitrogen and air flow. The sieves containing different proportions of iron were produced by two routes: introduction of iron salt direct synthesis; and a modification post synthesis consisting in iron salt 1 % and 5% impregnation in the material followed by thermal decomposition. The molecular sieves were characterized by X ray diffraction XRD, Fourier transform infrared spectroscopy FT-IR, X ray fluorescence spectroscopy XFR, scanning electronic microscopy SEM, specific surface area using the BET method, Termogravimetry TG. The kinetic model of Flynn Wall was used with the aim of determining the apparent activation energy of the surfactant remove (CTMABr) in the MCM- 41 porous. The analysis made possible the morphology characterization, identifying the presence of hexagonal structure typical for mesoporous materials, as well as observation of the MCM41 and iron of characteristic bands.

Morphology-controllable synthesis and characterization of single-crystal molybdenum trioxide

Molybdenum trioxide nanobelts and prism-like particles with good crystallinity and high surface areas have been prepared by a facile hydrothermal method, and the morphology could be controlled by using different inorganic salts, such as KNO3, Ca(NO3)(2), La(NO3)(3), etc. The possible growth mechanism of molybdenum trioxide prism-like particles is discussed on the basis of the presence of HI and the modification of metal cations. The as-prepared nanomaterials are characterized by means of powder X-ray diffraction (PXRD), field-emission scanning electron microscopy (FE-SEM), transmission electron microscopy (TEM), high-resolution TEM (HRTEM), Fourier transformation infrared spectroscopy (FT-IR), X-ray photoelectron spectroscopy (XPS), and ultraviolet and visible spectroscopy (UV-vis). TEM and HRTEM micrographs show that the molybdenum trioxide nanobelts and prism-like particles have a relatively high degree of crystallinity and uniformity. BET specific surface areas of the as-prepared molybdenum trioxide nanocrystals are 67-79 m(2)g(-1). XPS analysis indicates that the hexavalent molybdenum is predominant in the nanocrystals. UV-vis spectra reveal that the direct band gap energy of the annealed molybdenum trioxide prism-like particles shows a pronounced blue shift compared to that of bulk MoO3 powder.

CHARACTERIZATION, MORPHOLOGY AND THERMAL-PROPERTIES OF ETHYLENE PROPYLENE BLOCK COPOLYMERS

Characterization, morphology and thermal properties of commercial ethylene-propylene block copolymers have been studied by C-13 nuclear magnetic resonance (n.m.r.) spectroscopy, differential scanning calorimetry (d.s.c.), dynamic mechanical analysis (d.m.a.) and scanning electron microscopy (SEM). The results obtained show that there exists some ethylene-propylene random copolymer in the block copolymers extractable by n-heptane. The possibility of forming PP-b-PE diblock copolymer is questionable on the basis of the effects of residual propene and the chain-transfer reaction in the sequential copolymerization. A difference in the thermal properties between commercial ethylene-propylene block copolymers and PP/PE blends was noticed, which cannot be used to identify PP-b-PE diblock copolymer. The multiphase structure has been confirmed by d.m.a. and SEM, with ethylene-propylene random copolymer and polyethylene forming the domains in the matrix of polypropylene.

Surface morphology and optical characterization of OC1 OC6-PPV films

We report optical and morphological properties of poly(2-methoxy-5-hexyloxy-p-phenylenevinylene) (OC1OC6-PPV) films processed by casting, spin-coating (SC) and Langmuir-Blodgett (LB) techniques. The absorption spectra are practically the same, with an absorption maximum at approximately at 500 nm. For the photoluminescence (PL) spectra at low temperature (T=10K), a small but significant difference was noted in the cast film, in comparison with the LB and SC films. The zero-phonon transition shifted from 609 nm for the LB film to 615 and 621 nm for the SC and cast films, respectively. At room temperature, the PL spectra are similar for all films, and blue shifted by ca. 25 nm in comparison with the spectra at low temperature due to thermal disorder. Using atomic force microscopy (AFM) we inferred that the distinctive behavior of the cast film, probably associated with structural defects, is related to the large thickness of this film. The surface roughness, which was surprisingly higher for the LB film, apparently played no role in the emission properties of OC1OC6-PPV films.

Nanostructured films from phthalocyanine and carbon nanotubes: Surface morphology and electrical characterization

Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq)