Novel metallo-porphyrin based colourimetric amine sensors and their processing via plasma enhanced chemical vapour deposition at atmospheric pressure : synthesis, characterisation and mechanistic studies

Volatile amines are prominent indicators of food freshness, as they are produced during many microbiological food degradation processes. Monitoring and indicating the volatile amine concentration within the food package by intelligent packaging solutions might therefore be a simple yet powerful way to control food safety throughout the distribution chain.rnrnIn this context, this work aims to the formation of colourimetric amine sensing surfaces on different substrates, especially transparent PET packaging foil. The colour change of the deposited layers should ideally be discernible by the human eye to facilitate the determination by the end-user. rnrnDifferent tailored zinc(II) and chromium(III) metalloporphyrins have been used as chromophores for the colourimetric detection of volatile amines. A new concept to increase the porphyrins absorbance change upon exposure to amines is introduced. Moreover, the novel porphyrins’ processability during the deposition process is increased by their enhanced solubility in non-polar solvents.rnrnThe porphyrin chromophores have successfully been incorporated into polysiloxane matrices on different substrates via a dielectric barrier discharge enhanced chemical vapour deposition. This process allows the use of nitrogen as a cheap and abundant plasma gas, produces minor amounts of waste and by-products and can be easily introduced into (existing) roll-to-roll production lines. The formed hybrid sensing layers tightly incorporate the porphyrins and moreover form a porous structure to facilitate the amines diffusion to and interaction with the chromophores.rnrnThe work is completed with the thorough analysis of the porphyrins’ amine sensing performance in solution as well as in the hybrid coatings . To reveal the underlying interaction mechanisms, the experimental results are supported by DFT calculations. The deposited layers could be used for the detection of NEt3 concentrations below 10 ppm in the gas phase. Moreover, the coated foils have been tested in preliminary food storage experiments. rnrnThe mechanistic investigations on the interaction of amines with chromium(III) porphyrins revealed a novel pathway to the formation of chromium(IV) oxido porphyrins. This has been used for electrochemical epoxidation reactions with dioxygen as the formal terminal oxidant.rn

Ottimizzazione di un sistema manometrico per la misura dell'assorbimento di idrogeno nei metalli

Nel presente lavoro viene descritto come è stata ottimizzata, a livello software e hardware, la procedura di controllo della pressione in uno strumento manometrico utilizzato per la misura della quantità di idrogeno assorbita e desorbita da parte di metalli. Dopo una breve introduzione sulle caratteristiche dell'idrogeno che lo rendono così appetibile dal punto di vista energetico, viene esposta la teoria alla base del processo di formazione di idruri metallici. Vengono dunque descritte le due principali tecniche di caratterizzazione di questi sistemi, ovvero le cinetiche e le isoterme pressione-composizione (PCI), e il metodo di misura adottato, ovvero quello volumetrico. Successivamente si passa alla descrizione delle componenti hardware del sistema, per poi soffermarsi sull'analisi dettagliata dell'algoritmo del software implementato, spiegando i problemi affrontati e le soluzioni adottate, riportando anche alcune formule utili ricorrenti. Infine, vengono esposti i risultati ottenuti da misure di cinetiche e PCI per il sistema MgH2 (idruro di magnesio).

Studio di nuovi processi di sintesi di anidride maleica in fase gas

Oggi il mercato mondiale dell'anidride maleica (AM) è in continua espansione grazie ad un numero sempre crescente di applicazioni finali e sviluppo di nuove tecnologie industriali. La AM viene impiegata nella produzione di resine poliestere insature e resine alchidiche e nella produzione di chemicals a più alto valore aggiunto. Il processo di sintesi è tutt’ora basato sull'ossidazione selettiva del benzene e del n-butano. Con l’aumento delle emissione di gas serra, legate all’impiego di materie di origine fossile e la loro continua diminuzione, si stanno studiando nuovi processi basati su materie derivanti da fonti rinnovali. Tra i vari processi studiati vi è quello per la sintesi di AM, i quali utilizzano come molecola di furfurale, 5-idrossimetilfurfurale e 1-butanolo; tutte queste presentano però il problema di un costo superiore rispetto alle molecole tutt’ora usate. Ad oggi una delle molecole ottenibili da fonti rinnovabili avente un costo competitivo alle materie derivanti da fonti fossili è il bio-etanolo. Essendo nota la possibilità di trasformare dell’etanolo in composti a 4 atomi di carbonio (C4) come 1-butanolo (reazione di Guerbet) e in 1,3- butadiene (processo Lebedev) su ossidi misti Mg/Si e la loro trasformazioni in AM, è’ dunque possibile ipotizzare un processo operante in fase gas che accoppi entrambi i processi. Lo scopo di questo lavoro di tesi è stato quello di effettuare uno studio su sistemi catalitici mediante differenti approcci impiantistici. Il primo ha previsto l’impiego di un sistema detto “a cascata” nel quale è stato accoppiato il sistema misto a base di Mg/Si/O, per la trasformazione dell’etanolo a C4, e il pirofosfato di vanadile (VPP), per l’ossidazione selettiva di quest’ultimi in AM. Il secondo approccio ha previsto l’impiego di un unico sistema multifunzionale in grado di catalizzare tutti gli step necessari. In quest’ultimo caso, i sistemi studiati sono stati il Mg2P2O7 ed un sistema costituito da VPP DuPont sul quale è stato depositato MgO. I catalizzatori sono stati caratterizzati mediante diffrattometria a raggi X, spettroscopia Raman e analisi dell’area superficiale mediante metodo BET, mentre i test catalitici sono stati condotti su un impianto di laboratorio con un reattore assimilabile ad un modello di tipo PFR.

Sintesi di nanoparticelle composite con morfologia avanzata mediante condensazione in atmosfera inerte o reattiva

Uno dei concetti chiave dell'impiego della nanotecnologia è quello dell'ingegnerizzazione dei materiali alla nano-scala. Si procede così alla realizzazione di materiali aventi morfologia, struttura e composizione ottimizzate per migliorarne specifiche proprietà in maniera controllata. In questo lavoro sono stati realizzati campioni nanoparticellari a base di magnesio con la tecnica (R-)IGC (Reactive or Inert Gas Condensation) allo scopo di studiare come l'atmosfera nella quale vengono sintetizzati ne influenzi le proprietà morfologiche e strutturali, al fine di poterne controllare la crescita per impieghi specifici. In particolare, si sono voluti analizzare i risultati ottenuti in diverse situazioni: nel caso in cui la sintesi avvenga in un'atmosfera contenente una piccola concentrazione di ossigeno e nel caso della coevaporazione di magnesio e titanio in atmosfera inerte o contenente idrogeno. I campioni sono poi stati analizzati dal punto di vista morfologico, composizionale e strutturale mediante microscopia a scansione elettronica e diffrazione a raggi X. E' stato mostrato che la presenza controllata di ossigeno durante la sintesi permette di realizzare strutture core-shell di dimensione media 40nm e che la co-evaporazione di magnesio e titanio permette la sintesi di nanoparticelle di dimensioni medie anche inferiori ai 12nm. La presenza di idrogeno durante l'evaporazione permette inoltre di crescere nanoparticelle contenenti idruro di titanio senza dover ricorrere ad una idrurazione successiva. Le proprietà termodinamiche e cinetiche di (de)-idrurazione dei campioni sintetizzati sono state misurate utilizzando sia un apparato barometrico Sievert, sia effettuando un'analisi direttamente nel sito di crescita. I campioni realizzati non mostrano una termodinamica significativamente diversa da quella del magnesio bulk, mentre le cinetiche dei processi di assorbimento e desorbimento risultano notevolmente più rapide.

Electroencephalographic changes after pediatric cardiac surgery with cardiopulmonary bypass: is slow wave activity unfavorable?

Pediatric cardiac surgery with cardiopulmonary bypass (CPB) is frequently associated with neurologic deficits. We describe the postoperative EEG changes, assess their possible causes, and evaluate their relevance to neurologic outcome. Thirty-one children and five neonates with congenital heart disease were included. EEG recording started after intubation and continued until 22-96 h after CPB. In addition to conventional analysis, spectral analysis was performed for occipital and frontal electrodes, and differences between pre- and postoperative delta power (delta-deltaP) were calculated. Maximum values of occipital delta-deltaP that occurred within 48 h after CPB were correlated with clinical variables and with perioperative markers of oxidative stress and inflammation. Occipital delta-deltaP correlated with frontal delta-deltaP, and maximum delta-deltaP correlated with conventional rating. Distinct rise of deltaP was detected in 18 of 21 children without any acute or long-term neurologic deficits but only in five of 10 children with temporary or permanent neurologic deficits. Furthermore, maximally registered delta-deltaP was inversely associated with duration of CPB and postoperative ventilation. Maximal delta-deltaP was also inversely associated with the loss of plasma ascorbate (as an index of oxidative stress) and plasma levels of IL-6 and IL-8. Slow wave activity frequently occurs within 48 h after CPB. However, our data do not support the notion that EEG slowing is associated with adverse neurologic outcome. This is supported by the fact that EEG slowing was associated with less oxido-inflammatory stress.

Caracterización química de efluentes de bodegas, Mendoza (Argentina)

La industria vitivinícola genera efluentes sólidos y líquidos en cantidad apreciable. Los sólidos son aprovechados en distintas aplicaciones e inclusive tienen valor comercial. En cambio, los líquidos pueden originar problemas cuando es necesario decidir cómo desecharlos o transformarlos en desechables. En Mendoza (Argentina), es común enviarlos después de su decantación a cauces y campos abiertos. En ambos casos aparece un serio riesgo de contaminación. Visto que generalmente se desconoce la composición de tales efluentes, este trabajo pretende caracterizarlos físico-químicamente en el período de elaboración de vinos, determinando: pH, conductividad eléctrica, DBO, DQO, cloruros, sulfatos, carbonatos y bicarbonatos, calcio, magnesio, sodio y potasio. La calidad de los efluentes varía notablemente con el agua empleada en los lavados, que aporta mayoritariamente aniones y cationes. Cuando el agua de lavado es abundante, los valores de pH, DBO y DQO de los efluentes permiten su eliminación junto con otros residuos cloacales o en campo abierto.

Determinación de la actividad de la óxido nítrico sintetasa endotelial y del factor NF-kB, en la piel del paciente con pseudoangiomatosis eruptiva : informe preliminar

La pseudoangiomatosis eruptiva se caracteriza por la aparición brusca de múltiples pápulas eritematosas, asintomáticas, rodeadas de un halo blanquecino, con remisión espontánea. Histológicamente se observa dilatación vascular con escaso infiltrado inflamatorio. Su etiología permanece incierta a pesar de ser relacionada con virus o picaduras de insectos. Basados en el compromiso vascular, el objetivo del trabajo fue investigar la actividad de la enzima endotelial oxido nítrico sintetasa (eNOS) y la expresión del factor NF-kB por inmunohistoquimica en un intento de esclarecer su patogenia. Material y métodos: Se estudiaron diez pacientes con diagnóstico clínico de pseudoangiomatosis eruptiva (PAE) que presentaron la dermatosis en forma epidémica. Se realizaron biopsias teñidas con Hematoxilina-Eosina y Tricrómico de Masson. Se efectuó estudio virológico de los pacientes Nª 4, 9 y 10 mediante determinaciones serológicas para echovirus, enterovirus, citomegalovirus, parvovirus B19 y hepatitis A, B y C. En cinco pacientes se obtuvo material para determinación de eNOS y NF-kB. Resultados: Todos los pacientes, 5 hombres y 5 mujeres presentaron pápulas eritematosas rodeadas por un halo blanquecino, especialmente en las extremidades, alrededor de las rodillas. Histológicamente mostraron vasos dilatados y células endoteliales prominentes con un infiltrado discreto perivascular. Todos los estudios serológicos fueron negativos. La actividad de eNOS fue significativamente menor comparada con la piel normal (p= 0,002) y la expresión de NF- ĸB fue fuertemente positiva en los vasos de la dermis papilar y reticular. Conclusiones: Todos los pacientes fueron afectados en verano, por lo que la picadura del mosquito debe ser considerada como un factor etiológico. La baja expresión de eNOS está relacionada con la vasodilatación y la expresión aumentada de NF-ĸB confirma que el proceso es de tipo inflamatorio.

Comparación del poder de neutralización de enmiendas calcáreo-magnésicas en suelos de la Pampa llana santafesina

El objetivo de este trabajo fue comparar el poder de neutralización de enmiendas calcáreo- magnésicas y evaluar su efecto sobre el complejo de intercambio catiónico en suelos de la pampa llana santafesina. Para ello, se aplicaron tres enmiendas (caliza, dolomita y enmienda mezcla) a dos dosis (neutralización del 100% y 150% del hidrógeno de intercambio). Se evaluó: pH actual, pH potencial, hidrógeno, calcio y magnesio intercambiable luego de 60 días de incubación. El pH actual no mostró diferencias entre dosis, mientras que el incremento de pH de las enmiendas fue caliza > dolomita > mezcla. El pH potencial fue más sensible al tipo de enmienda y dosis. Todos los tratamientos redujeron el nivel de insaturación, aunque ninguno neutralizó la totalidad del hidrógeno intercambiable. En relación con el calcio intercambiable, todos los tratamientos produjeron aumentos y la mayor saturación cálcica se obtuvo con la aplicación de caliza o enmienda mezcla con la dosis necesaria para neutralizar 1,5 veces el hidrógeno intercambiable. En cuanto al magnesio, las enmiendas dolomita y mezcla aumentaron significativamente el contenido independientemente de la dosis. La información aquí presentada es de utilidad para la prescripción de enmiendas calcáreo- magnésica en los suelos de la Pampa llana santafesina.

Geochemistry of ODP Leg 125 peridotites

Trace element analyses (first-series transition elements, Ti, Rb, Sr, Zr, Y, Nb, and REE) were carried out on whole rocks and minerals from 10 peridotite samples from both Conical Seamount in the Mariana forearc and Torishima Forearc Seamount in the Izu-Bonin forearc using a combination of XRF, ID-MS, ICP-MS, and ion microprobe. The concentrations of incompatible trace elements are generally low, reflecting the highly residual nature of the peridotites and their low clinopyroxene content (<2%). Chondrite-normalized REE patterns show extreme U shapes with (La/Sm)n ratios in the range of 5.03-250.0 and (Sm/Yb)n ratios in the range of 0.05-0.25; several samples show possible small positive Eu anomalies. LREE enrichment is common to both seamounts, although the peridotites from Conical Seamount have higher (La/Ce)n ratios on extended chondrite-normalized plots, in which both REEs and other trace elements are organized according to their incompatibility with respect to a harzburgitic mantle. Comparison with abyssal peridotite patterns suggests that the LREEs, Rb, Nb, Sr, Sm, and Eu are all enriched in the Leg 125 peridotites, but Ti and the HREEs exhibit no obvious enrichment. The peridotites also give positive anomalies for Zr and Sr relative to their neighboring REEs. Covariation diagrams based on clinopyroxene data show that Ti and the HREEs plot on an extension of an abyssal peridotite trend to more residual compositions. However, the LREEs, Rb, Sr, Sm, and Eu are displaced off this trend toward higher values, suggesting that these elements were introduced during an enrichment event. The axis of dispersion on these plots further suggests that enrichment took place during or after melting and thus was not a characteristic of the lithosphere before subduction. Compared with boninites sampled from the Izu-Bonin-Mariana forearc, the peridotites are significantly more enriched in LREEs. Modeling of the melting process indicates that if they represent the most depleted residues of the melting events that generated forearc boninites they must have experienced subsolidus enrichment in these elements, as well as in Rb, Sr, Zr, Nb, Sm, and Eu. The lack of any correlation with the degree of serpentinization suggests that low-temperature fluids were not the prime cause of enrichment. The enrichment in the high-field-strength elements also suggests that at least some of this enrichment may have involved melts rather than aqueous fluids. Moreover, the presence of the hydrous minerals magnesio-hornblende and tremolite and the common resorption of orthopyroxene indicate that this high-temperature peridotite-fluid interaction may have taken place in a water-rich environment in the forearc following the melting event that produced the boninites. The peridotites from Leg 125 may therefore contain a record of an important flux of elements into the mantle wedge during the initial formation of forearc lithosphere. Ophiolitic peridotites with these characteristics have not yet been reported, perhaps because the precise equivalents to the serpentinite seamounts have not been analyzed.

Heavy minerals from Paleogene sediments at DSDP Leg 81 Holes

Five heavy mineral associations occur in the Paleocene and Eocene sediments recovered during Leg 81 of the Deep Sea Drilling Project (DSDP) in the SW Rockall area. Association 1, consisting of augite, iddingsite, and olivine, was derived from the basaltic rocks of the northern part of the Rockall Plateau. Association 2 consists of epidote group minerals, including piedmontite, and amphiboles of actinolite, actinolitic hornblende, and magnesio-hornblende compositions, and was derived from the metamorphic basement of south Greenland. Association 3 comprises garnet, augite, apatite, and edenitic and pargasitic amphiboles and has a provenance in the southern Rockall Plateau. Associations 4 (garnet, apatite, edenitic/pargasitic amphiboles) and 5 (garnet, apatite) are intrastratal solution derivatives of Association 3, with successive removal of first pyroxene and then amphibole with increasing depth of burial. Throughout the SW Rockall Plateau area there is a significant change in the spectrum of the above assemblages in the lower part of the Eocene. This change has been noted at Sites 403, 404, 553, and 555 and is defined by the last appearance of Association 2. This level therefore marks the cessation of sediment supply from southern Greenland and is the result of the final separation of Rockall and Greenland immediately prior to magnetic Anomaly 24.

Petrography and mineral compositions of gabbros at DSDP Leg 60 Holes

The compositions, mineralogies, and textures of gabbros recovered in polymict breccias in Hole 453 indicate that they are the cumulus assemblages of calc-alkalic crystal fractional on that occurred beneath the West Mariana Ridge. They are among a class of gabbros known only from other calc-alkalic associations (e.g., the Lesser Antilles and the Peninsular Ranges batholith of Southern California) and differ from gabbros of stratiform complexes, ophiolites, and the ocean crust. Particularly abundant in the Hole 453 breccias are olivine-bearing gabbros with extremely calcic Plagioclase (An94-97) but with fairly iron-rich olivines (Fo76-77). Other gabbros contain biotite and amphibole and occur in breccias with fairly high-grade greenschist facies (amphibole-chlorite-stilpnomelane) metabasalts. One unusual gabbro has experienced almost complete subsolidus recrystallization to an assemblage of aluminous magnesio-hornblende, anorthite, and green hercynitic spinel. This reaction, the extremely calcic Plagioclase, the occurrence of biotite and amphibole, and the association with greenschist facies metamorphic rocks suggest that crystallization of the gabbros occurred at elevated P(H2O). Comparisons with other calc-alkalic gabbro suites suggest pressures in excess of 4 kbar (about 12 km depth). The gabbros were exposed by the early stages of opening of the Mariana Trough and imply that considerable uplift may have attended rifting. They were also subjected to hydrothermal alteration after breccia formation, resulting in formation of chlorite, epidote, actinolite, and prehnite. Temperatures of at least 200°C - and probably 350°C - were reached, and most likely could not have been attained without extrusion or intrusion of magmas nearby, even though no such rocks were cored.

Chemistry of secondary minerals from the deep sheeted dike complex of ODP Holes 137-504B and 140-504B

Dolerites sampled from the lower sheeted dikes from Hole 504B during Ocean Drilling Program Legs 137 and 140, between 1562.4 and 2000.4 mbsf, were examined to document the mineralogy, petrography, and mineral parageneses associated with secondary alteration, to constrain the thermal history and composition of hydrothermal fluids. The main methods used were mineral chemical analyses by electron microprobe, X-ray diffraction, and cathodoluminescence microscopy. Temperatures of alteration were estimated on the basis of single and/or coexisting mineral chemistry. Permeability is important in controlling the type and extent of alteration in the studied dike section. At the meter-scale, intervals of weakly altered dolerites containing fresh olivine are interpreted as having experienced restricted exposure to hydrothermal fluids. At the centimeter- or millimeter-scale, alteration patches and extensively altered halos adjacent to veins reflect the permeability related to intergranular primary porosity and cracks. Most of the sheeted dike alteration in this case resulted from non-focused, pervasive fluid-rock interaction. This study confirms and extends the previous model for hydrothermal alteration at Hole 504B: hydrothermal alteration at the ridge axis followed by seawater recharge and off-axis alteration. The major new discoveries, all related to higher temperatures of alteration, are: (1) the presence of hydrothermal plagioclase (An80-95), (2) the presence of deuteric and/or hydrothermal diopside, and (3) the general increasing proportion of amphiboles, and particularly magnesio-hornblende with depth. We propose that the dolerites at Hole 504B were altered in five stages. Stage 1 occurred at high temperatures (less than 500° to 700°C) and involved late-magmatic formation of Na- and Ti-rich diopside, the hydrothermal formation of Na, Ti-poor diopside and the hydrothermal formation of an assemblage of An-rich plagioclase + hornblende. Stage 2 occurred at lower temperatures (250°-320°C) and is characterized by the appearance of actinolite, chlorite, chlorite-smectite, and/or talc (in low permeability zones) and albite. During Stage 3, quartz and epidote precipitated from evolved hydrothermal fluids at temperatures between 310° and 320°C. Anhydrite appeared during Stage 4 and likely precipitated directly from heated seawater. Stage 5 occurred off-axis at low temperatures (250°C) with laumontite and prehnite from evolved fluids.

A role of Toc33 in the protochlorophyllide-dependent plastid import pathway of NADPH:proto¬chlorophyllide oxidoreductase (POR) A

NADPH: protochlorophyllide oxido reductase (POR) A is a key enzyme of chlorophyll biosynthesis in angiosperms. It is nucleus-encoded, synthesized as a larger precursor in the cytosol and imported into the plastids in a substrate-dependent manner. Plastid envelope membrane proteins, called protochlorophyllide dependent translocon proteins, Ptcs, have been identified that interact with pPORA during import. Amongthem are a 16-kDa ortholog of the previously characterized outer envelope protein Oep16 (named Ptc16) and a33-kDa protein (Ptc33) related to the GTP-binding proteins Toc33 and Toc34 of Arabidopsis. In the present work, we studied the interactions and roles of Ptc16 and Ptc33 during pPORA import. Radio labeled Ptc16/Oep16 was synthesized from a corresponding cDNA and imported into isolated Arabidopsis plastids. Crosslinking experiments revealed that import of35S-Oep16/Ptc16 is stimulated by GTP.35S-Oep16/Ptc16forms larger complexes with Toc33 but not Toc34. Plastids of the ppi1 mutant of Arabidopsis lacking Toc33, were unable to import pPORA in darkness but imported the small subunit precursor of ribulose-1,5-bisphosphate carboxylase/oxygenase (pSSU), precursor ferredoxin (pFd) as well as pPORB which is a close relative of pPORA. In white light, partial suppressions of pSSU, pFd and pPORB import were observed. Our results unveil a hitherto unrecognized role of Toc33 in pPORA import and suggest photo oxidative membrane damage, induced by excess Pchlide accumulating in ppi1 chloroplasts because of the lack of pPORA import, to be the cause of the general drop of protein import.

Morteros fotocatalíticos: análisis de su autolimpieza en función del tipo de cemento y rugosidad superficial.

En este Trabajo fin de master se explicará el funcionamiento de la fotocatálisis que presentan los materiales con adición de óxido de titanio en tamaño de nanopartículas, el cual les confiere ciertas cualidades especiales. Una vez conocido el funcionamiento de la fotocatálisis se estudiará la influencia de ciertos factores, que no han sido tratados en profundidad hasta el momento en los materiales en base cemento, para mejorar las propiedades autolimpiantes, como son; el tipo de cemento o la rugosidad superficial, ya que sin duda, la composición que tenga el cemento y la rugosidad que se le confiera en los acabados, influirá en el comportamiento autolimpiante, por ello se hace necesario un estudio en el que se evaluarán que cementos proporcionan una mayor efectividad en función de sus composición y que rugosidad superficial funciona mejor en la autolimpieza, debido a esto se estudiarán morteros con acabados lisos y con distintas rugosidades hasta 1.5mm de irregularidad. Para poder realizar este estudio se elaborará una caracterización de los morteros, que se utilizarán en la evaluación de las cualidades autolimpiantes, comparándolos con otros de idéntica dosificación, pero sin adición de oxido de titanio. Posteriormente sabiendo cuantitativamente cuales son sus características y si la adición de oxido de titanio modifica alguna de sus propiedades, pasar a evaluar sus características autolimpiantes, esto se hará, añadiendo a las probetas perfectamente curadas por inmersión durante mas de 28 días, distintos colorantes en disoluciones acuosa, como son la Rodamina B y el Azul de metileno. Una vez coloreadas las probetas, se medirá la degradación del color mediante un aparato conocido como espectrofotómetro, el cual nos dirá la variación de color en escala CIELAB. Con estos datos se podrá cuantificar de una manera más o menos precisa cuales son los cementos que presentan unas cualidades autolimpiantes mejores y cuales son los acabados superficiales, que presentan mayor autolimpieza, datos importantes de conocer a la hora de fabricar elementos a los cuales se les quiera dotar de este tipo de cualidades.

Hábitos alimentarios y de actividad física en un grupo de adolescentes de la Comunidad de Madrid y su relación con el rendimiento académico

Objetivo Analizar y valorar la dieta de un grupo de alumnas de E.S.O de Madrid, y profundizar en la relación entre patrones de alimentación, rendimiento físico y rendimiento académico. Material y métodos Estudio descriptivo y transversal, de una muestra de 16 adolescentes de sexo femenino (15–18 años) del Instituto de Educación Secundaria de Sevilla la Nueva. Se realizó un análisis prospectivo de la dieta de 72 horas, medición antropométrica, un cuestionario de actividad física y otro general. Resultados Se observó un IMC medio de 20,9. El grupo presentó altos niveles de actividad física, con una media de 4 horas semanales (excluyendo las horas de Educación Física). El rendimiento académico se consideró como bueno, con una calificación media de 7. En promedio, la ingesta calórica total de las estudiantes fue de 2131±517 Kcal. El consumo energético se distribuye: 42% lípidos, 42% hidratos de carbono y 16% proteínas. Las grasas saturadas aportaron el 14% de la ingesta calórica, y el colesterol superó los valores recomendados. La ingesta de fibra, calcio, hierro, magnesio, vitamina D y vitamina E estaban por debajo de las recomendaciones. Conclusiones La dieta de las estudiantes de secundaria de Sevilla la Nueva es normocalórica, con un aporte excesivo de lípidos, en especial de grasas saturadas y colesterol, y un aporte deficitario de hidratos de carbono y ciertos micronutrientes como el Ca, Mg, Fe, la vitamina D y E. El hecho de realizar más horas semanales de EF no empeora el rendimiento académico y mejora la calificación en la materia de EF.