989 resultados para NaY zeolite


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Dissertação para obtenção do Grau de Mestre em Engenharia Química e Bioquímica

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Dissertação para obtenção do Grau de Mestre em Engenharia Química e Bioquímica

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Dissertação de mestrado em Biofísica e Bionanossistemas

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Dissertação de mestrado em Bioengenharia

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Dairy sludge generated at Glanbia Ingredients Ltd., Kilkenny has up until now been landspread. This study investigated the feasibility of using earthworms to vermicompost the sludge as an alternative method of treatment. It was found that high levels of ammonia in the sludge led to earthworm fatality but that by manually aerating the sludge the ammonia could be volatilised or by adding zeolite the ammonia could be absorbed, thus solving the problem. In a medium scale trial, the earthworm species Dendrobaena veneta and Eisenia fetida dominated the polyculture. Earthworms grew and generated cocoons during vermicomposting. During vermicomposting no leachate was generated. Nutrient changes took place during vermicomposting. There were high levels of nitrate, increased calcium and sulphate in the vermicomposted dairy sludge. The amount of magnesium, potassium and chloride did not change, while phosphate was undetectable after vermicomposting. The levels of nitrate and phosphate were good indicators of the extent of vermicomposting. The vermicomposted dairy sludge provided improved growth and yields of radishes and barley compared to the dairy sludge and control. Compared to the vermicompost, the dairy sludge provided heavier ryegrass yields and more marigolds with larger flower diameters. Generally, it is the amount of phosphate in dairy sludge that dictates how much can be applied as a fertiliser on land. Vermicomposting reduced the amount of phosphate to an undetectable level but on the other hand created a problem of high nitrate levels. In a pot trial with grass grown in vermicompost the nitrate leached from the vermicompost. In field conditions the leaching of nitrate might occur and could cause an increased risk of contamination of groundwater and watercourses.

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To make a diagnostic of cancer in a young adult (15-30 years of age) has important physical, psychological and social implications. The most frequent cancers seen at this age are cancer of the thyroid, testicular germ cell tumours, 'melanoma, Hodgkin's lymphoma, non-Hodgkin lymphoma, leukaemia, cerebral tumours and sarcomas. Even if the prognostic of most of these cancers is excellent, treatments are difficult and often associated with long-term side effects. A multidisciplinary approach of these patients is essential. A long-term follow-up by a general practicioner or an oncologist is indispensable.

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The 24-km diameter Ries crater, Germany, exhibits well-preserved crater filling and surficial melt-rich breccia deposits that are believed to have been altered by post-impact hydrothermal fluids. The alteration mineralogy of the crater filling breccias is characterized by clay (smectite, chlorite) and a zeolite assemblage, and secondary clay phases (smectite, minor halloysite) in surficial melt-bearing breccia deposits. Using stable isotope analysis of secondary smectitic clay fractions, evidence of significant hydrous alteration of impactites at large water/rock ratios was found. The estimated fluid temperatures, using data derived by delta(18)O and delta D fractionation, suggest smectite precipitation in surficial breccias in equilibrium with meteoric fluids at temperatures 16 +/- 5 degrees C in agreement with the long-term variation of modern precipitation in the area. The stable isotope composition of smectite in crater-fill breccia, however, suggests a trend of monotonously increasing temperatures from 43 to 112 degrees C. with increasing depth through the breccia sequence. This demonstrates a different origin of alteration and temperature distribution for the surficial and crater filling melt-bearing impact breccias in the Ries crater. Our results suggest that the inverted structure of hydrothermal systems observed in some terrestrial impact craters, including the Ries crater, could indicate the initial configuration of a thermal anomaly in the crater filling sequence, but which is replaced with a normal hydrothermal convection in crater proper, during the course of post-impact cooling. (C) 2010 Elsevier B.V. All rights reserved.

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Buts de la revue: Les Médulloblastomes sont des tumeurs rares chez l'adulte. Le traitement habituel comprend une radiothérapie de tout l'axe cranio-spinal avec ou sans chimiothérapie. Beaucoup d'efforts sont actuellement entrepris pour mieux comprendre la biologie tumorale, afin de mieux stratifier les patients en différents groupes à risques et de les traiter en fonction. Cette revue discute les nouveaux facteurs de risques cliniques et moléculaires qui peuvent aider à optimiser le traitement des patients adultes avec des médulloblastomes. Découvertes récentes: Jusqu'à présent les patients étaient divisés en groupes à bas risque ou à haut risque sur la base de facteurs cliniques (âge, maladie résiduelle après chirurgie, dissémination dans le système nerveux central et l'histologie). Cette classification devrait être complétée par des facteurs pronostics moléculaires. Le profilage de l'expression des gènes a permis d'identifier six sous-groupes moléculaires de médulloblastomes. Le WNT sous-groupe montre une activation des gènes de la voie de signalisation WNT/wingless avec des mutations fréquentes du gène CNNTB1, une perte du chromosome 6 et une accumulation de β-catenine nucléaire. Ce sous-groupe est rencontré le plus souvent chez les enfants avec des médulloblastomes avec une histologie classique. Ils ont un bon pronostic. Une activation de la voie de signalisation du sonic hedgehog montre des mutations fréquentes des gènes PTCH et SUFU, une perte du 9q et une positivité pour GLI1 et SFRP1 et est rencontré plus fréquemment chez les enfants de moins de 3 ans et chez les adultes. Ce sous-groupe est souvent associé à une histologie de type desmoplastique. D'autre sous-groupes sont moins bien délimités et présentent des caractéristiques qui se chevauchent. Cependant une amplification MYC/MYCN, un gain du 17p et une histologie de type grandes cellules/anaplasique sont des facteurs de mauvais pronostic. Résumé: Des nouveaux sous-groupes moléculaires vont dorénavant aider à mieux adapter les traitements aux différents groupes de risque et permettront à développer de nouvelles thérapies ciblées. Des études prospectives et si possibles randomisées devraient être effectuées comprenant une stratification dans des sous-groupes moléculaires, afin d'identifier au mieux le meilleur traitement pour chaque groupe à risque.

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The Cretaceous Mont Saint-Hilaire complex (Quebec, Canada) comprises three major rock units that were emplaced in the following sequence: (I) gabbros; (II) diorites; (III) diverse partly agpaitic foid syenites. The major element compositions of the rock-forming minerals, age-corrected Nd and oxygen isotope data for mineral separates and trace element data of Fe-Mg silicates from the various lithologies imply a common source for all units. The distribution of the rare earth elements in clinopyroxene from the gabbros indicates an ocean island basalt type composition for the parental magma. Gabbros record temperatures of 1200 to 800 degrees C, variable silica activities between 0 center dot 7 and 0 center dot 3, and f(O2) values between -0 center dot 5 and +0 center dot 7 (log delta FMQ, where FMQ is fayalite-magnetite-quartz). The diorites crystallized under uniform a(SiO2) (a(SiO2) = 0 center dot 4-0 center dot 5) and more reduced f(O2) conditions (log delta FMQ similar to-1) between similar to 1100 and similar to 800 degrees C. Phase equilibria in various foid syenites indicate that silica activities decrease from 0 center dot 6-0 center dot 3 at similar to 1000 degrees C to < 0 center dot 3 at similar to 550 degrees C. Release of an aqueous fluid during the transition to the hydrothermal stage caused a(SiO2) to drop to very low values, which results from reduced SiO(2) solubilities in aqueous fluids compared with silicate melts. During the hydrothermal stage, high water activities stabilized zeolite-group minerals. Fluid inclusions record a complex post-magmatic history, which includes trapping of an aqueous fluid that unmixed from the restitic foid syenitic magma. Cogenetic aqueous and carbonic fluid inclusions reflect heterogeneous trapping of coexisting immiscible external fluids in the latest evolutionary stage. The O and C isotope characteristics of fluid-inclusion hosted CO(2) and late-stage carbonates imply that the surrounding limestones were the source of the external fluids. The mineral-rich syenitic rocks at Mont Saint-Hilaire evolved as follows: first, alkalis, high field strength and large ion lithophile elements were pre-enriched in the (late) magmatic and subsequent hydrothermal stages; second, percolation of external fluids in equilibrium with the carbonate host-rocks and mixing processes with internal fluids as well as fluid-rock interaction governed dissolution of pre-existing minerals, element transport and precipitation of mineral assemblages determined by locally variable parameters. It is this hydrothermal interplay between internal and external fluids that is responsible for the mineral wealth found at Mont Saint-Hilaire.

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BACKGROUND: Uveal metastasis is the most common intraocular malignancy. METHODS: This was a retrospective study of all patients with uveal metastases referred to the Liverpool Ocular Oncology Centre between January 2007 and December 2012. Biopsy was performed as a primary investigation if the clinical examination suggested metastasis with no evidence of any extraocular metastases. RESULTS: Ninety-six patients (109 eyes) were included. Breast and lung carcinomas were the most common primary malignancies, affecting 41 and 27 patients, respectively. The median time interval between detection of primary cancer and uveal metastasis was 24 months (range 1-288 months). Thirty-nine patients underwent ocular biopsy, confirming the diagnosis in all patients. The biopsy indicated the site of origin in 24 out of the 27 without a known primary tumour. In 7 of these 27 cases, previous systemic investigations had failed to identify the primary tumour. Seventy-three patients received external beam irradiation; two patients received photodynamic therapy; and two patients had Ru-106 plaque radiotherapy. The visual acuity was stable or improved in 75.5% of the cases. CONCLUSIONS: Immediate biopsy provides a quick diagnosis that may expedite treatment and improve any opportunities for conserving vision while facilitating the general oncologic management on these patients.

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Baïn muoán coù moät vieäc laøm. Vaø baïn cuõng coù caoem giaùctin raèng ôoe moät nôi naøo ñoù coù moätngöôøi chuoechuû nhaân ñang caàn moät ngöôøi laømchính xaùc coâng vieäc baïn muoán - moät coâng vieäcñoøi hooei ñuùng kieán thöùc vaø caùc khaoe naêng cuoea baïn, cuõng nhö ñöa ra nhöõng thaùch thöùc vaø côhoäi thaêng tieán. Ñeå tìm ñöôïc coâng vieäc aáy, baïn caàn phaoei laäpkeá hoaïch tìm vieäc moät caùch kyõ caøng vaø thöïc hieän ñuùng keá hoaïch ñoù. Baïn coù theå baùn ñi moätthöù - ñoù laøcoi nhöõng kieán thöùc, kyõ naêng, vaøkinh nghieäm cuoea baïn - töùc - laø chính baïn! - nhölaø moät saûn phaåm caàn “baùn” cho caùc chuû nhaân!.Ñieàu baïn caàn bieát laø laøm theá naøo ñeå chöùng tooenaêng löïc cuoea mình moät caùch coù hieäu quaoe nhaát. Cho duø baïn môùi ra tröôøng hay vaø ñang chuaånbò baét ñaàu moätböôùc ñaàu trong söï nghieäp cuûa mình hay ñang tìm moät coâng vieäc môùi sau 20naêm kinh nghieäm, moät soá phöông phaùp ñöôïctrình baøy trong taäp thoâng tin naøy coù theå giuùpích cho baïn. NOTE: Vietnamese Translation

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In Brazilian agriculture, urea is the most commonly used nitrogen (N) source, in spite of having the disadvantage of losing considerable amounts of N by ammonia-N volatilization. The objectives of this study were to evaluate: N lossby ammonia volatilization from: [urea coated with copper sulfate and boric acid], [urea coated with zeolite], [urea+ammonium sulfate], [urea coated with copper sulfate and boric acid+ammonium sulfate], [common urea] and [ammonium nitrate]; and the effect of these N source son the maize yield in terms of amount and quality. The treatments were applied to the surface of a soil under no-tillage maize, in two growing seasons. The first season (2009/2010) was after a maize crop (maize straw left on the soil surface) and the second cycle (2012/2011) after a soybean crop. Due to the weather conditions during the experiments, the volatilization of ammonia-N was highest in the first four days after application of the N sources. Of all urea sources, under volatilization-favorable conditions, the loss of ammonia from urea coated with copper sulfate and boric acid was lowest, while under high rainfall, the losses from the different urea sources was similar, i.e., an adequate rainfall was favorablet o reduce volatilization. The ammonia volatilization losses were greatest in the first four days after application. Maize grain yield differed due to N application and in the treatments, but this was only observed with cultivation of maize crop residues in 2009/2010. The combination of ammonium+urea coated with copper sulfate and boric acid optimized grain yield compared to the other urea treatments. The crude protein concentration in maize was not influenced by the technologies of urea coating.

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The approaches of comparative studies and profile measurements, often used in order to detect post-depositional alterations of ceramics, have been applied simultaneously to two sets of Roman pottery, both of which include altered individuals. As analytical techniques, Neutron Activation Analysis and X-Ray Diffraction have been used. Both approaches lead to substantially different results. This shows that they detect different levels of alteration and should complement each other rather than being used exclusively. For the special process of a glassy phase decomposition followed by a crystallization of the Na-zeolite analcime, the results suggest that it changes high-fired calcareous pottery rapidly, and so fundamentally that the results of various archaeometric techniques can be severely disturbed.