Effectiveness of house dust mite acaricide tri-n-butyl tin maleate on carpets, fabrics and mattress foam: a standardization of methodology

The aim of this study was to determine the effectiveness of the acaricide tri-n-butyl tin maleate, industrially applied to samples of carpets, mattress foam, and fabrics used for furniture upholstery, soft toys and shoe uppers. Approximately 100 adult house dust mites of the species Dermatophagoides pteronyssinus were inoculated into a Petri dish containing the sample (a piece of carpet, mattress foam, or fabric), treated with the acaricide, randomly collected. Mite-maintenance culture medium was added on top of each sample. After one, two, three, seven and 30 days of incubation at 25 ºC and 75% relative humidity, each dish was examined using a 40X stereoscopic microscope (40X). One hundred percent acaricide effectiveness was obtained in treated materials by the end of the 30th-day postinoculation period, under optimal conditions for mite maintenance.

Foam-forming properties of Ilex paraguariensis (mate) saponin: foamability and foam lifetime analysis by Weibull equation

Saponins are natural soaplike foam-forming compounds widely used in foods, cosmetic and pharmaceutical preparations. In this work foamability and foam lifetime of foams obtained from Ilex paraguariensis unripe fruits were analyzed. Polysorbate 80 and sodium dodecyl sulfate were used as reference surfactants. Aiming a better data understanding a linearized 4-parameters Weibull function was proposed. The mate hydroethanolic extract (ME) and a mate saponin enriched fraction (MSF) afforded foamability and foam lifetime comparable to the synthetic surfactants. The linearization of the Weibull equation allowed the statistical comparison of foam decay curves, improving former mathematical approaches.

Estudos histológico, histoquímico e ultra-estrutural de fígados e linfonodos de bovinos com presença de macrófagos espumosos ("foam cells")

Foram examinadas amostras de fígado, rins, baço e linfonodos hepáticos, mesentéricos, retro-mandibulares, pré-escapulares e mediastínicos de 12 lotes em um total de 120 animais, envolvendo diferentes faixas etárias, todos oriundos do Estado de Mato Grosso. Os animais haviam sido mantidos em pastos onde Brachiaria decumbens e Brachiaria brizantha eram as forrageiras predominantes. Macroscopicamente o fígado desses animais mostrava coloração amarelada, mais evidente após 24 horas de fixação em formol a 10%. Nos linfonodos hepáticos e mesentéricos foram evidenciadas, na superfície de corte, estriações esbranquiçadas de forma radiada na cortical e medular com pequenas áreas brancas nodulares multifocais principalmente na medular. Em muitos casos, associado com essas áreas foram vistos focos de aspecto hemorrágico. Microscopicamente foram encontradas, no fígado, linfonodos hepáticos e mesentéricos, células com citoplasma espumoso, muitas das quais multinucleadas. Nos linfonodos hepáticos e mesentéricos estes infiltrados estavam associados a áreas de necrose e hemorragia. No fígado, as células de citoplasma espumoso estavam presentes em todo parênquima, de forma irregular, geralmente formando nódulos ao redor da veia centrolobular. Estas células não se coravam pelo ácido periódico de Schiff (PAS) e apenas fracamente na coloração de gordura pelo Oil Red O. Na ultra-estrutura as células de citoplasma espumoso apresentavam fendas, parcial ou totalmente delimitadas por membrana, que representam a imagem negativa de cristais, presentes também no citoplasma dos hepatócitos.

Relação entre macrófagos espumosos ("foam cells") no fígado de bovinos e ingestão de Brachiaria spp no Brasil

Com o objetivo de estabelecer uma relação etiológica e caracterizar, cronologicamente, o aparecimento de macrófagos espumosos (foam cells), comuns em fígados de bovinos oriundos das regiões de clima tropical do Brasil, foram reexaminados cortes histológicos de fígado de bovinos dos arquivos do Setor de Anatomia Patológica da Embrapa-Projeto Sanidade Animal, RJ. O material utilizado provinha de investigações sobre causas de mortandades em bovinos nas regiões Norte, Centro-Oeste e Sudeste do Brasil, realizadas de 1970 a 1991. Foram estudados 55 fígados de bovinos afetados por enfermidades variadas. Somente foram usados casos em que o tipo de pastagem era conhecido. Essa alteração não foi encontrada de 1970 até o final de 1975, embora 40 amostras (72,7%) tenham sido coletadas nesse período. A presença de macrófagos espumosos, observada a partir de 1976, coincidiu com a introdução da gramínea Brachiaria decumbens var. australiana no Brasil. Algumas amostras eram provenientes de bovinos que apresentaram histórico de fotossensibilização, na época atribuída ao fungo Pithomyces chartarum. Os achados indicam que essas alterações hepáticas são relacionadas com a ingestão de Brachiaria spp.

DESIDRATAÇÃO DA POLPA DE ACEROLA (Malpighia emarginata D.C.) PELO PROCESSO "FOAM-MAT"

Foi elaborado um suplemento alimentar em pó, a partir da desidratação da polpa de frutos de acerola utilizando o método "FOAM-MAT". Vários testes utilizando diferentes agentes químicos, que favorecem à formação da espuma, foram realizados, tendo sido escolhido o experimento que mais se ajustou ao parâmetro de densidade recomendado como ideal (0,1 a 0,6). Na condição experimental definida, a polpa foi formulada e desidratrada em estufa de secagem com circulação de ar, a uma temperatura de 60 a 70°C, por 90 minutos, obtendo-se um produto em pó, com umidade final de 7,2%. Em paralelo ao experimento, foi efetuada uma caracterização química da polpa de acerola. O produto em pó obtido, foi embalado em sacos metalizados de 25 gramas e submetido a um estudo de estabilidade por 3 meses. Os resultados encontrados, mostraram que o produto elaborado apresentou elevado teor de vitamina C, em um nível 10 vezes maior do que na polpa integral.

Diffuse panbronchiolitis: an underdiagnosed disease? Study of 4 cases in Brazil

BACKGROUND: Diffuse panbronchiolitis is a clinical pathologic condition characterized by chronic inflammation of respiratory bronchioles, with clinical features that position it as a differential diagnosis among the sinopulmonary syndromes. METHODS AND RESULTS: We present 4 cases (1 Black, 2 Japanese descendants, and 1 Japanese), living in Brazil, in which the diagnosis was made by the clinical and radiological features and confirmed by transbronchial biopsy. The clinical findings included chronic sinusitis, productive cough, rhonchi, and wheezes. The pulmonary function tests showed an obstructive pattern. High resolution computerized tomography showed a diffuse nodular pattern, airway ectasia, and airway wall thickening. The biopsy showed interstitial accumulation of foam cells and lymphoid cells in the walls of respiratory bronchioles: 2 of our cases had bronchus-associated lymphoid tissue hyperplasia. We searched for the HLA Bw54 in all of our patients, but only 1 was positive. A low dose macrolide treatment was introduced, resulting in with clinical and functional improvement. A score that rated the extent of nodules, airway ectasia, mucus plugging, and airway wall thickening was applied on pre- and post-treatment High resolution computerized tomography results, revealing an improvement in tomographic pattern related to that observed in the pulmonary function tests. CONCLUSION: We conclude that diffuse panbronchiolitis is a systemic disease that is not exclusive to the Asian population, whose clinical and radiological features should be better known by occidental pulmonary physicians.

Determinação do ciclo estral em catetos Pecari tajacu: aspectos colpocitológicos e clínicos

Este trabalho teve por objetivo estudar o ciclo estral do cateto, aplicando a colpocitologia como método diagnóstico. As amostras da citologia vaginal foram coletadas em dez fêmeas adultas, durante três vezes na semana, por seis meses. Verificou-se que a duração média do ciclo estral para esta espécie foi de 28,45 ± 5,45 dias. Observou-se diferença estatística (p<0,01) em relação à frequência dos diferentes tipos celulares na mesma fase do ciclo estral. No proestro foi verificado o aumento de células intermediárias e superficiais. A fase de estro caracterizou-se pela elevação significativa de células superficiais em relação aos demais tipos celulares e pela ausência de leucócitos. Durante este período, a genitália externa estava hiperêmica, edemaciada e com muco. No metaestro houve um decréscimo de células superficiais, quando comparado com o proestro e com o estro, e uma elevação significativa de células intermediárias, presença de leucócitos, de células de metaestro e de foam. Na fase de diestro, houve um aumento de células intermediárias, e um decréscimo no número de leucócitos. Conclui-se que, por meio da colpocitologia, é possível diferenciar as fases do ciclo estral em catetos.

Reproductive behavior of Leptodactylus mystacinus (Anura, Leptodactylidae) with notes on courtship call of other Leptodactylus species

Here we present data on the reproductive behavior of Leptodactylus mystacinus (Burmeister, 1861), including details on courtship behavior. We also describe and compared the courtship calls of L. mystacinus, L. furnarius Sazima & Bokermann, 1978 and Leptodactylus sp. (L. aff. andreae). Field works were conducted in Uberlândia (central Brazil). During courtship, a female approaches a calling male and is led to a previously excavated chamber; a female can approach a silent male that beat his hands and/or feet on the ground as well. The courtship call of L. mystacinus consists of one single arch-shaped note (duration = 0.04 s) repeated 258 times per minute; the courtship calls of L. furnarius (0.06 s, 84 times per minute) and Leptodactylus sp. (0.15 s, 5 times per minute) also are arch-shaped. The courtship behavior of L. mystacinus is similar to that of other species of the L. fuscus (Schneider, 1799) group; unique to it is that males can beat his hands and/or feet on the ground while courting. The male behavior of conducting the female to a previously excavates chamber and the arch-shaped courtship call may represent other shared derived features of members of the L. fuscus group, including the former Adenomera species.

Paleogenetic and taphonomic analysis of human bones from Moa, Beirada, and Zé Espinho Sambaquis, Rio de Janeiro, Brazil

The present paper discusses mtDNA and taphonomy of human remains from Moa, Beirada, and Zé Espinho sambaquis of Saquarema, state of Rio de Janeiro, Brazil. New human bone dating by 14C-AMS for Moa archeological site (3810+50 BP - GX-31826-AMS) is included. Preservation of microscopic lamellae and DNA is not related to the macroscopic integrity of the bones. Results here suggest that the preservation of amplifiable DNA fragments may have relation to the preservation of the lamellar arrangement as indicated by optical microscopic examination (polarized light). In 13 human bone fragments from Moa, Beirada, and Zé Espinho it was possible to sequence mtDNA from the 3 individuals of Moa, and from 1 of 4 individuals of Beirada, whose bones also show extensive areas with preserved lamellar structures. The 6 human bone fragments of Zé Espinho and 3 of the 4 fragments of Beirada showed extensive destruction of cortical microstructure represented by cavities, intrusive minerals, and agglomerated microscopic bodies of fungi and bacteria; it was not possible to extract mtDNA from these samples. The results support the hypothesis that the preservation of the microscopic osteon organization is a good predictor for DNA preservation. It was also confirmed the C haplogroup antiquity in Brazil.

Genesis and classification of Oxisols in a highland toposequence of the upper Jequitinhonha Valley (MG)

The Brazilian System of Soil Classification (SiBCS) is a taxonomic system, open and in permanent construction, as new knowledge on Brazilian soils is obtained. The objective of this study was to characterize the chemical, physical, morphological, micro-morphological and mineralogical properties of four pedons of Oxisols in a highland toposequence in the upper Jequitinhonha Valley, emphasizing aspects of their genesis, classification and landscape development. The pedons occupy the following slope positions: summit - Red Oxisol (LV), mid slope (upper third) - Yellow-Red Oxisol (LVA), lower slope (middle third)- Yellow Oxisol (LA) and bottom of the valley (lowest third) - "Gray Oxisol" ("LAC"). These pedons were described and sampled for characterization in chemical and physical routine analyses. The total Fe, Al and Mn contents were determined by sulfuric attack and the Fe, Al and Mn oxides in dithionite-citrate-bicarbonate and oxalate extraction. The mineralogy of silicate clays was identified by X ray diffraction and the Fe oxides were detected by differential X ray diffraction. Total Ti, Ga and Zr contents were determined by X ray fluorescence spectrometry. The "LAC" is gray-colored and contains significant fragments of structure units in the form of a dense paste, characteristic of a gleysoil, in the horizons A and BA. All pedons are very clayey, dystrophic and have low contents of available P and a pH of around 5. The soil color was related to the Fe oxide content, which decreased along the slope. The decrease of crystalline and low- crystalline Fe along the slope confirmed the loss of Fe from the "LAC". Total Si increased along the slope and total Al remained constant. The clay fraction in all pedons was dominated by kaolinite and gibbsite. Hematite and goethite were identified in LV, low-intensity hematite and goethite in LVA, goethite in LA. In the "LAC", no hematite peaks and goethite were detected by differential X ray diffraction. The micro-morphology indicated prevalence of granular microstructure and porosity with complex stacking patterns.. The soil properties in the toposequence converged to a single soil class, the Oxisols, derived from the same source material. The landscape evolution and genesis of Oxisols of the highlands in the upper Jequitinhonha Valley are related to the evolution of the drainage system and the activity of excavating fauna.

Quantificação e utilização das frações húmicas como característica diferencial em horizontes diagnósticos de solos Brasileiros

As informações obtidas pela distribuição das frações húmicas podem ser utilizadas em estudos pedológicos brasileiros como atributo diagnóstico ou característica diferencial e, assim, contribuir para a evolução do Sistema Brasileiro de Classificação de Solos (SiBCS). Os objetivos deste trabalho foam quantificar o C orgânico das frações húmicas de horizontes diagnósticos superficiais e subsuperficiais de solos e propor a utilização no Sistema Brasileiro de Classificação de Solos. Foram utilizados 169 horizontes diagnósticos distribuídos entre O hístico, H hístico, A chernozêmico, A húmico e B espódico. Eles foram avaliados quanto à composição química e física. Quantificaram-se os teores de C orgânico nas frações: ácidos fúlvicos (C-FAF), ácidos húmicos (C-FAH) e humina (C-HUM). Foram calculadas as relações C-FAH/C-FAF, C-EA/C-HUM e C-EA/COT (C-EA = C-FAF + C-FAH) e o percentual de cada fração em relação a C orgânico total (COT), %FAF, %FAH, %HUM e %EA (extrato alcalino). Os horizontes O e H hístico apresentaram predomínio do C-HUM, seguido do C-FAH; o A chernozêmico, dominância absoluta do C-HUM; o A húmico, predomínio da C-HUM, seguido do C-FAH; e o B espódico, maior expressividade de C-FAH ou do C-FAF. Com base na avaliação da distribuição das frações húmicas, propõe-se o uso das seguintes características diferenciais para os níveis de família e série do SiBCS: matéria orgânica estável (horizontes minerais superficiais) - C-EA/C-HUM (< 0,5); matéria orgânica iluvial (horizontes minerais subsuperficiais) - C-EA/C-HUM (> 2,0); e potencial de lixiviação (sistema ou solo) - C-FAH/C-FAF e C-EA/C-HUM (> 1,0).

New methods to quantify NH3 volatilization from fertilized surface soil with urea

Gaseous N losses from soil are considerable, resulting mostly from ammonia volatilization linked to agricultural activities such as pasture fertilization. The use of simple and accessible measurement methods of such losses is fundamental in the evaluation of the N cycle in agricultural systems. The purpose of this study was to evaluate quantification methods of NH3 volatilization from fertilized surface soil with urea, with minimal influence on the volatilization processes. The greenhouse experiment was arranged in a completely randomized design with 13 treatments and five replications, with the following treatments: (1) Polyurethane foam (density 20 kg m-3) with phosphoric acid solution absorber (foam absorber), installed 1, 5, 10 and 20 cm above the soil surface; (2) Paper filter with sulfuric acid solution absorber (paper absorber, 1, 5, 10 and 20 cm above the soil surface); (3) Sulfuric acid solution absorber (1, 5 and 10 cm above the soil surface); (4) Semi-open static collector; (5) 15N balance (control). The foam absorber placed 1 cm above the soil surface estimated the real daily rate of loss and accumulated loss of NH3N and proved efficient in capturing NH3 volatized from urea-treated soil. The estimates based on acid absorbers 1, 5 and 10 cm above the soil surface and paper absorbers 1 and 5 cm above the soil surface were only realistic for accumulated N-NH3 losses. Foam absorbers can be indicated to quantify accumulated and daily rates of NH3 volatilization losses similarly to an open static chamber, making calibration equations or correction factors unnecessary.

Highlands of the upper Jequitinhonha valley, Brazil: II - mineralogy, micromorphology, and landscape evolution¹

Palm swanp formations, the so-called veredas, typically occur in the Brazilian biome known as "Cerrado" (savanna-like vegetation), especially on flattened areas or tablelands (chapadas). The aim of this study was to characterize the mineralogy and micromorphology of soil materials from a representative toposequence of the watershed of the vereda Lagoa do Leandro, located in Minas Novas, state of Minas Gerais, Brazil, on plains in the region of the upper Jequitinhonha valley, emphasizing essential aspects of their genesis and landscape evolution. The toposequence is underlain by rocks of the Macaúbas group and covered with detrital and metamorphic rocks (schists of Proterozoic diamictites). The soil profiles were first pedologically described; samples of the disturbed and undisturbed soils were collected from all horizons for further micromorphological and mineralogical analyses. The mineralogical analysis was mainly based on powder X ray diffractometry (XRD) and micromorphological descriptions of thin sections under a petrographic microscope. The soils from the bottom to the top of this toposequence were classified as: Typic Albaquult (GXbd), Xanthic Haplustox, gray color, here called "Gray Haplustox" ("LAC"), Xanthic Haplustox (LA) and Typic Haplustox (LVA). The clay mineralogy of all soils was found to be dominated by kaolinite. In soil of LA and LVA, the occurrence of goethite, gibbsite, and anatase was evidenced; "LAC" also contained anatase and the GXbd, illite, anatase, and traces of vermiculite. The micromorphological analyses of the LVA, LA and "LAC" soils showed the prevalence of a microaggregate-like or granular microstructure, and aggregate porosity has a stacked/packed structure, which is typical of Oxisols. A massive structure was observed in GXbd material, with the presence of illuviation cutans of clay minerals and iron compounds. Paleogleissolos, which are strongly weathered, due to the action of the excavating fauna , and resulted in the present "LAC". The GXbd at the base of the vereda preserved the physical, mineralogical and micromorphological properties that are typical of a pedogenesis with a strong influence of long dry periods.

MORPHOLOGICAL AND MICROMORPHOLOGICAL CHANGES IN THE STRUCTURE OF A RHODIC HAPLUDOX AS A RESULT OF AGRICULTURAL MANAGEMENT

In evaluation of soil quality for agricultural use, soil structure is one of the most important properties, which is influenced not only by climate, biological activity, and management practices but also by mechanical and physico-chemical forces acting in the soil. The purpose of this study was to evaluate the influence of conventional agricultural management on the structure and microstructure of a Latossolo Vermelho distroférrico típico (Rhodic Hapludox) in an experimental area planted to maize. Soil morphology was described using the crop profile method by identifying the distinct structural volumes called Morphologically Homogeneous Units (MHUs). For comparison, we also described a profile in an adjacent area without agricultural use and under natural regrowth referred to as Memory. We took undisturbed samples from the main MHUs so as to form thin sections and blocks of soil for micromorphological and micromorphometrical analyses. Results from the application of the crop profile method showed the occurrence of the following structural types: loose (L), fragmented (F) and continuous (C) in both profiles analyzed. In the Memory soil profile, the fragmented structures were classified as Fptμ∆+tf and Fmt∆μ, whose micromorphology shows an enaulic-porphyric (porous) relative distribution with a great deal of biological activity as indicated by the presence of vughs and channels. Lower down, from 0.20 to 0.35 m, there was a continuous soil volume (sub-type C∆μ), with a subangular block microstructure and an enaulic-porphyric relative distribution, though in this case more compact and with aggregate coalescence and less biological activity. The micromorphometrical study of the soil of the Memory Plot showed the predominance of complex pores in NAM (15.03 %), Fmt∆μ (11.72 %), and Fptμ∆+tf (7.73 %), and rounded pores in C∆μ (8.21 %). In the soil under conventional agricultural management, we observed fragmented structures similar to the Memory Plot from 0.02 to 0.20 m, followed by a volume with a compact continuous structure (C∆μ), without visible porosity and with few roots. In the MHUs under conventional management, reduction in the packing pores (40 %) was observed, mainly in the continuous units (C). The microstructure had well-defined blocks, with the occurrence of planar pores and less evidence of biological activity. In conclusion, the morphological and micromorphological analyses of the soil profiles studied offered complementary information regarding soil structural quality, especially concerning the changes in pore types as result of mechanical stress undergone by the soil.

Discrepancies over the onset of surfactant monomer aggregation interpreted by fluorescence, conductivity and surface tension methods

Molecular probe techniques have made important contributions to the determination of microstructure of surfactant assemblies such as size, stability, micropolarity and conformation. Conductivity and surface tension were used to determine the critical aggregation concentration (cac) of polymer-surfactant complexes and the critical micellar concentration (cmc) of aqueous micellar aggregates. The results are compared with those of fluorescent techniques. Several surfactant systems were examined, 1-butanol-sodium dodecylsulfate (SDS) mixtures, solutions containing poly(ethylene oxide)-SDS, poly(vinylpyrrolidone)-SDS and poly(acrylic acid)-alkyltrimethylammonium bromide complexes. We found differences between the cac and cmc values obtained by conductivity or surface tension and those obtained by techniques which use hydrophobic probe.