PHOTOELASTIC ANALISYS IN THE LOWER REGION OF VERTEBRAL BODY L4

Objective: To analyze the shear forces on the vertebral body L4 when submitted to a compression force by means of transmission photoelasticity. Methods: Twelve photoelastic models were divided into three groups, with four models per group, according to the positioning of the sagittal section vertebrae L4-L5 (sections A, B and C). The simulation was performed using a 15N compression force, and the fringe orders were evaluated in the vertebral body L4 by the Tardy compensation method. Results: Photoelastic analysis showed, in general, a homogeneous distribution in the vertebral bodies. The shear forces were higher in section C than B, and higher in B than A. Conclusion: The posterior area of L4, mainly in section C, showed higher shear concentrations, corresponding to a more susceptible area for bone fracture and spondylolisthesis. Economic and Decision Analyses Development of an Economic or Decision Model. Level I

The Cysteine-Rich Protein Thimet Oligopeptidase as a Model of the Structural Requirements for S-glutathiolation and Oxidative Oligomerization

Thimet oligopeptidase (EP24.15) is a cysteine-rich metallopeptidase containing fifteen Cys residues and no intra-protein disulfide bonds. Previous work on this enzyme revealed that the oxidative oligomerization of EP24.15 is triggered by S-glutathiolation at physiological GSSG levels (10-50 mu M) via a mechanism based on thiol-disulfide exchange. In the present work, our aim was to identify EP24.15 Cys residues that are prone to S-glutathiolation and to determine which structural features in the cysteinyl bulk are responsible for the formation of mixed disulfides through the reaction with GSSG and, in this particular case, the Cys residues within EP24.15 that favor either S-glutathiolation or inter-protein thiol-disulfide exchange. These studies were conducted by in silico structural analyses and simulations as well as site-specific mutation. S-glutathiolation was determined by mass spectrometric analyses and western blotting with anti-glutathione antibody. The results indicated that the stabilization of a thiolate sulfhydryl and the solvent accessibility of the cysteines are necessary for S-thiolation. The Solvent Access Surface analysis of the Cys residues prone to glutathione modification showed that the S-glutathiolated Cys residues are located inside pockets where the sulfur atom comes into contact with the solvent and that the positively charged amino acids are directed toward these Cys residues. The simulation of a covalent glutathione docking onto the same Cys residues allowed for perfect glutathione posing. A mutation of the Arg residue 263 that forms a saline bridge to the Cys residue 175 significantly decreased the overall S-glutathiolation and oligomerization of EP24.15. The present results show for the first time the structural requirements for protein S-glutathiolation by GSSG and are consistent with our previous hypothesis that EP24.15 oligomerization is dependent on the electron transfer from specific protonated Cys residues of one molecule to previously S-glutathionylated Cys residues of another one.

The Carmaphycins: New Proteasome Inhibitors Exhibiting an alpha,beta-Epoxyketone Warhead from a Marine Cyanobacterium

Two new peptidic proteasome inhibitors were isolated as trace components from a Curacao collection of the marine cyanobacterium Symploca sp. Carmaphycin A (1) and carmaphycin B (2) feature a leucine-derived a,beta-epoxyketone warhead directly connected to either methionine sulfoxide or methionine sulfone. Their structures were elucidated on the basis of extensive NMR and MS analyses and confirmed by total synthesis, which in turn provided more material for further biological evaluations. Pure carmaphycins A and B were found to inhibit the beta 5 subunit (chymotrypsin-like activity) of the S. cerevisiae 20S proteasome in the low nanomolar range. Additionally, they exhibited strong cytotoxicity to lung and colon cancer cell lines, as well as exquisite antiproliferative effects in the NCI60 cell-line panel. These assay results as well as initial structural biology studies suggest a distinctive binding mode for these new inhibitors.

Exercise Training Restores Cardiac Protein Quality Control in Heart Failure

Exercise training is a well-known coadjuvant in heart failure treatment; however, the molecular mechanisms underlying its beneficial effects remain elusive. Despite the primary cause, heart failure is often preceded by two distinct phenomena: mitochondria dysfunction and cytosolic protein quality control disruption. The objective of the study was to determine the contribution of exercise training in regulating cardiac mitochondria metabolism and cytosolic protein quality control in a post-myocardial infarction-induced heart failure (MI-HF) animal model. Our data demonstrated that isolated cardiac mitochondria from MI-HF rats displayed decreased oxygen consumption, reduced maximum calcium uptake and elevated H2O2 release. These changes were accompanied by exacerbated cardiac oxidative stress and proteasomal insufficiency. Declined proteasomal activity contributes to cardiac protein quality control disruption in our MI-HF model. Using cultured neonatal cardiomyocytes, we showed that either antimycin A or H2O2 resulted in inactivation of proteasomal peptidase activity, accumulation of oxidized proteins and cell death, recapitulating our in vivo model. Of interest, eight weeks of exercise training improved cardiac function, peak oxygen uptake and exercise tolerance in MI-HF rats. Moreover, exercise training restored mitochondrial oxygen consumption, increased Ca2+-induced permeability transition and reduced H2O2 release in MI-HF rats. These changes were followed by reduced oxidative stress and better cardiac protein quality control. Taken together, our findings uncover the potential contribution of mitochondrial dysfunction and cytosolic protein quality control disruption to heart failure and highlight the positive effects of exercise training in re-establishing cardiac mitochondrial physiology and protein quality control, reinforcing the importance of this intervention as a nonpharmacological tool for heart failure therapy.

Ammonia losses estimated by an open collector from urea applied to sugarcane straw

The quantification of ammonia (NH3) losses from sugarcane straw fertilized with urea can be performed with collectors that recover the NH3 in acid-treated absorbers. Thus, the use of an open NH3 collector with a polytetrafluoroethylene (PTFE)-wrapped absorber is an interesting option since its cost is low, handling easy and microclimatic conditions irrelevant. The aim of this study was to evaluate the efficiency of an open collector for quantifying NH3-N volatilized from urea applied over the sugarcane straw. The experiment was carried out in a sugarcane field located near Piracicaba, São Paulo, Brazil. The NH3-N losses were estimated using a semi-open static collector calibrated with 15N (reference method) and an open collector with an absorber wrapped in PTFE film. Urea was applied to the soil surface in treatments corresponding to rates of 50, 100, 150 and 200 kg ha-1 N. Applying urea-N fertilizer on sugarcane straw resulted in losses NH3-N up to 24 % of the applied rate. The amount of volatile NH3-N measured in the open and the semi-open static collector did not differ. The effectiveness of the collection system varied non-linearly, with an average value of 58.4 % for the range of 100 to 200 kg ha-1 of urea-N. The open collector showed significant potential for use; however, further research is needed to verify the suitability of the proposed method.

Protein turnover, amino acid requirements and recommendations for athletes and active populations

Skeletal muscle is the major deposit of protein molecules. As for any cell or tissue, total muscle protein reflects a dynamic turnover between net protein synthesis and degradation. Noninvasive and invasive techniques have been applied to determine amino acid catabolism and muscle protein building at rest, during exercise and during the recovery period after a single experiment or training sessions. Stable isotopic tracers (13C-lysine, 15N-glycine, ²H5-phenylalanine) and arteriovenous differences have been used in studies of skeletal muscle and collagen tissues under resting and exercise conditions. There are different fractional synthesis rates in skeletal muscle and tendon tissues, but there is no major difference between collagen and myofibrillar protein synthesis. Strenuous exercise provokes increased proteolysis and decreased protein synthesis, the opposite occurring during the recovery period. Individuals who exercise respond differently when resistance and endurance types of contractions are compared. Endurance exercise induces a greater oxidative capacity (enzymes) compared to resistance exercise, which induces fiber hypertrophy (myofibrils). Nitrogen balance (difference between protein intake and protein degradation) for athletes is usually balanced when the intake of protein reaches 1.2 g·kg-1·day-1 compared to 0.8 g·kg-1·day-1 in resting individuals. Muscular activities promote a cascade of signals leading to the stimulation of eukaryotic initiation of myofibrillar protein synthesis. As suggested in several publications, a bolus of 15-20 g protein (from skimmed milk or whey proteins) and carbohydrate (± 30 g maltodextrine) drinks is needed immediately after stopping exercise to stimulate muscle protein and tendon collagen turnover within 1 h.

Variação espacial e temporal da trama trófica bentônica de um ambiente costeiro à plataforma continental adjacente no Atlântico Sudoeste: análise de isótopos estáveis

A análise das razões de isótopos estáveis de carbono (δ13C) e nitrogênio (δ15N) vem sendo utilizada para identificar as fontes primárias de carbono dos ecossistemas e traçar as interações tróficas entre seus componentes. Nesse contexto, a variabilidade espacial e temporal da trama trófica bentônica da Baía de Santos e da plataforma continental interna e média, ao largo da costa sul do estado de São Paulo, Brasil (23,9-24,5°S), foi investigada durante o inverno de 2005 e o verão de 2006. A matéria orgânica particulada em suspensão (MOPS), zooplâncton, macroalgas, vegetais terrestres (C3), sedimento e 21 categorias de consumidores bentônicos foram analisados. Segundo os valores de δ13C, a MOPS foi a principal fonte primária de matéria orgânica. A análise de regressão entre os valores médios de δ15N e δ13C indicou, no inverno, semelhanças nas assinaturas isotópicas dos consumidores bentônicos entre a plataforma interna e média e diferenças entre essas e as da baía. Por outro lado, no verão, foram observadas diferenças nessas assinaturas entre a baía, a plataforma interna e a média. Os valores de 13C dos consumidores decresceram do ambiente costeiro em direção à plataforma média, enquanto os de 15N aumentaram. Em relação ao δ13C, houve diferença da MOPS, possivelmente pela contribuição de produção primária nova (PPN) ou do microfitobentos no verão. Quanto ao δ15N, o enriquecimento da mesma categoria trófica no gradiente ambiental pode ser devido às diferenças na MOPS, resultante da PPN na plataforma interna no verão, decorrente da entrada da Água Central do Atlântico Sul (ACAS), que enriquece a água oligotrófica nessa área

Redox regulation of the proteasome via S-glutathionylation

The proteasome is a multimeric and multicatalytic intracellular protease responsible for the degradation of proteins involved in cell cycle control, various signaling processes, antigen presentation, and control of protein synthesis. The central catalytic complex of the proteasome is called the 20S core particle. The majority of these are flanked on one or both sides by regulatory units. Most common among these units is the 19S regulatory unit. When coupled to the 19S unit, the complex is termed the asymmetric or symmetric 26S proteasome depending on whether one or both sides are coupled to the 19S unit, respectively. The 26S proteasome recognizes poly-ubiquitinylated substrates targeted for proteolysis. Targeted proteins interact with the 19S unit where they are deubiquitinylated, unfolded, and translocated to the 20S catalytic chamber for degradation. The 26S proteasome is responsible for the degradation of major proteins involved in the regulation of the cellular cycle, antigen presentation and control of protein synthesis. Alternatively, the proteasome is also active when dissociated from regulatory units. This free pool of 20S proteasome is described in yeast to mammalian cells. The free 20S proteasome degrades proteins by a process independent of poly-ubiquitinylation and ATP consumption. Oxidatively modified proteins and other substrates are degraded in this manner. The 20S proteasome comprises two central heptamers (β-rings) where the catalytic sites are located and two external heptamers (α-rings) that are responsible for proteasomal gating. Because the 20S proteasome lacks regulatory units, it is unclear what mechanisms regulate the gating of α-rings between open and closed forms. In the present review, we discuss 20S proteasomal gating modulation through a redox mechanism, namely, S-glutathionylation of cysteine residues located in the α-rings, and the consequence of this post-translational modification on 20S proteasomal function.

Deposit-feeding in benthic macrofauna : Tracer studies from the Baltic Sea

A low content of organic matter, which is largely refractory in nature, is characteristic of most sediments, meaning that aquatic deposit-feeders live on a very poor food source. The food is derived mainly from sedimenting phytodetritus, and in temperate waters like the Baltic Sea, from seasonal phytoplankton blooms. Deposit-feeders are either bulk-feeders, or selective feeders, which preferentially ingest the more organic-rich particles in the sediment, including phytodetritus, microbes and meiofauna. The soft-bottom benthos of the Baltic Sea has low species biodiversity and is dominated by a few macrobenthic species, among which the most numerous are the two deposit-feeding amphipods Monoporeia affinis and Pontoporeia femorata, and the bivalve Macoma balthica. This thesis is based on laboratory experiments on the feeding of these three species, and on the priapulid Halicryptus spinulosus. Feeding by benthic animals is often difficult to observe, but can be effectively studied by the use of tracers. Here we used the radioactive isotope 14C to label food items and to trace the organic matter uptake in the animals, while the stable isotopes 13C and 15N were used to follow feeding on aged organic matter in the sediment. The abundance of M. balthica and the amphipods tends to be negatively correlated, i.e., fewer bivalves are found at sites with dense populations of amphipods, with the known explanation that newly settled M. balthica spat are killed by the amphipods. Whether the postlarvae are just accidentally killed, or also ingested after being killed was tested by labelling the postlarvae with 14C and Rhodamine B. Both tracer techniques gave similar evidence for predation on and ingestion of postlarval bivalves. We calculated that this predation was likely to supply less than one percent of the daily carbon requirement for M. affinis, but might nevertheless be an important factor limiting recruitment of M. balthica. The two amphipods M. affinis and P. femorata are partly vertically segregated in the sediment, but whether they also feed at different depths was unknown. By adding fresh 14C-labelled algae either on the sediment surface or mixed into the sediment, we were able to distinguish surface from subsurface feeding. We found M. affinis and P. femorata to be surface and subsurface deposit-feeders, respectively. Whether the amphipods also feed on old organic matter, was studied by adding fresh 14C-labelled algae on the sediment surface, and using aged, one-year-old 13C- and 15N-labelled sediment as deep sediment. Ingestion of old organic matter, traced by the stable isotopes, differed between the two species, with a higher uptake for P. femorata, suggesting that P. femorata utilises the older, deeper-buried organic matter to a greater extent. Feeding studies with juveniles of both M. affinis and P. femorata had not been done previously. In an experiment with the same procedure and treatments as for the adults, juveniles of both amphipod species were found to have similar feeding strategies. They fed on both fresh and old sediment, with no partitioning of food resources, making them likely to be competitors for the same food resource. Oxygen deficiency has become more wide-spread in the Baltic Sea proper in the last half-century, and upwards of 70 000km2 are now devoid of macrofauna, even though part of that area does not have oxygen concentrations low enough to directly kill the macrofauna. We made week-long experiments on the rate of feeding on 14C-labelled diatoms spread on the sediment surface in different oxygen concentrations for both the amphipod species, M. balthica and H. spinulosus. The amphipods were the most sensitive to oxygen deficiency and showed reduced feeding and lower survival at low oxygen concentrations. M. balthica showed reduced feeding at the lowest oxygen concentration, but no mortality increase. The survival of H. spinulosus was unaffected, but it did not feed, showing that it is not a surface deposit-feeder. We conclude that low oxygen concentrations that are not directly lethal, but reduce food intake, may lead to starvation and death in the longer term.

Ecología y estatus trófico del erizo de mar Diadema antillarum (Philippi, 1845) en los fondos rocosos de las Islas Canarias (Gran Canaria, España)

La explosión demográfica de erizo Diadema antillarum en los ecosistemas sumergidos rocosos del litoral canario está provocando una intensa desertización, generando los popularmente conocidos como fondos de “blanquizales” debido al color blanco que adquiere el recubrimiento calcáreo. Se analizaron los parámetros morfométricos, de densidad poblacional, ecología trófica e interacción específica de la especie de erizo D. antillarum (Philippi, 1845) durante los años 2005, 2006 y 2007 en los fondos rocosos de la isla de Gran Canaria, Islas Canarias, España. Se evaluaron cuatro blanquizales con diferente orientación geográfica y con características bióticas y abióticas distintas, lo que permitió analizar el papel trófico de D. antillarum bajo diferentes condiciones; además de la evaluación de la biomasa de las especies algales halladas en los fondos rocosos donde habita la especie. El estudio hace un especial énfasis en la evaluación de la distribución, discriminación y selección de las diversas fuentes algales consumidas por Diadema antillarum a través de un seguimiento de la asimilación de los productores primarios por los consumidores, mediante el uso de los isótopos estables 13C y 15N Los resultados no mostraron una variación estacional de la morfometría de D. antillarum. Sin embargo, si existe una variación respecto al tamaño del erizo con la profundidad. La especie mostró una disminución de su tamaño cuanto mayor era la profundidad. Asimismo los resultados exhibieron una correlación negativa entre la densidad poblacional de D. antillarum y el tamaño del erizo. Hay una clara tendencia a hallar las tallas pequeñas de erizos conforme aumenta la maduración o desarrollo de los blanquizales. Se encuentran tallas menores cuando la densidad de erizos supera los 5 erizos • m-2. La mayor densidad promedio encontrada en este estudio fue de 12, 83 erizos • m-2 y la talla menor fue de un diámetro de caparazón menor a 2 cm y un ancho de la linterna de Aristóteles de 0,8 cm; la categoría de diámetro de caparazón más abundante fue la comprendida en el rango de 3,5-5,4 cm. Las firmas isotópicas de la fuentes algales y del músculo de D. antillarum mediante el uso de modelos de mezcla permitieron concluir que en términos generales el género Laurencia resultó un constituyente principal en la dieta de D. antillarum en los diferentes blanquizales; los géneros Colpomenia, Padina, Sargassum, Hypnea, y Jania son constituyentes importantes en la dieta de D. antillarum cuando habita en sustratos de blanquizales desarrollados (maduros), de la misma forma que Dictyota, Zonaria, Liagora, Lobophora, y Stypocaulon constituyen fuentes importantes en los blanquizales menos desarrollados (inmaduros), mostrando un alto grado de solapamiento de fuentes. D. antillarum presentó una asimilación diferencial, independientemente de la disponibilidad del alimento. La dieta de D. antillarum refleja una composición algal específica dependiendo de la etapa de maduración del blanquizal El estudio proporciona una herramienta cuantitativa que permite separar ambientes diferentes - hábitats que experimentan diferentes grados de perturbación- a través de la evaluación de una asimilación diferencial de las algas por parte de D. antillarum.

Oxygen and Chlorophyll Distribution in the Eastern Atlantic Ocean from 0º to 35ºS.

Programa de doctorado en Oceanografía. Trabajo presentado para la obtención del Diploma de Estudios Avanzados.

Struktur- und Funktionsanalyse der zytokinbindenden Domäne des humanen Interleukin-6-Rezeptors

Die Familie der IL-6-Typ-Zytokine (IL-6, IL-11, CT-1, CNTF, LIF, OSM, BSF-3) ist durch eine vierhelikale Faltung gekennzeichnet. Alle Zytokine dieser Familie agieren über einen Rezeptorkomplex, der als gemeinsame Komponente mindestens ein Molekül gp130 enthält. IL-6 und IL-11 signalisieren über ein gp130-Homodimer, während CT-1, CNTF, LIF und OSM ein Heterodimer aus gp130 und dem strukturell verwandten LIFR oder, im Falle des OSM, auch OSMR verwenden. Die Rezeptoren der vierhelikalen Zytokine sind in ihrem extrazellulären Bereich modulartig aus Ig- und Fibronektin-Typ-III-ähnlichen Domänen aufgebaut. Sie besitzen als gemeinsame Struktureinheit ein zytokinbindendes Modul (CBM) aus zwei Fibronektin-Typ-III-ähnlichen Domänen, die durch vier konservierte Cysteine in der N-terminalen und ein konserviertes WSXWS-Motiv in der C-terminalen Domäne charakterisiert sind. Auf Zielzellen bindet IL-6 an den spezifischen IL-6 Rezeptor, worauf der Komplex aus IL-6/IL-6R mit dem Signaltransduktor gp130 assoziiert. Der IL-6R besteht in seinem extrazellulären Bereich aus drei Domänen. Die N-terminale Ig-ähnliche Domäne ist für die biologische Aktivität nicht notwendig. Die Domänen 2 und 3 bilden das CBM, welches auch in löslicher Form agonistisch wirkt. In der vorliegenden Arbeit wurden die strukturellen und funktionellen Eigenschaften der dritten extrazellulären Domäne des IL-6R untersucht. Das Protein läßt sich effizient in Bakterien exprimieren und in vitro renaturieren. Es konnte gezeigt werden, daß Domäne 3 für die Bindung an IL-6 ausreichend ist, der Komplex aus D3 und IL-6 jedoch nicht mehr mit dem gp130-Molekül assoziieren kann. Da der lösliche IL-6R (bestehend aus D2 und D3) in der Lage ist, an gp130 zu binden und ein biologisches Signal auszulösen, weisen diese Daten der C-terminalen CBM-Domäne (D3) eine ligandenbindende Funktion und der N-terminalen CBM-Domäne eine wichtige Rolle bei der Komplexbildung mit gp130 und Signalinduktion zu. Die gezeigte Expressions- und Renaturierungsstrategie für D3 wurde zur Markierung des Proteins mit 15N und 13C für die mehrdimensionale, heteronukleare NMR-Spektroskopie angewandt. Die hierdurch ermöglichte Strukturaufklärung von D3 als einer eindeutig in die Ligandenbindung involvierten Teilstruktur wird umfassendere strukturelle Informationen über den IL-6R-Komplex liefern, als es die bisherigen Mutations- bzw. Modellbaustudien konnten.

Stable isotope investigations of atmospheric nitrous oxide

ZusammenfassungDie Analyse von Isotopenverhältnissen ist von wachsender Bedeutung bei der Untersuchung von Quellen, Senken und chemischen Reaktionswegen atmosphärischer Spurengase. Distickstoffoxid (N2O) hat vier isotopisch einfach substituierte Spezies: 14N15N16O, 15N14N16O, 14N217O und 14N218O. In der vorliegenden Arbeit wurden massenspektrometrische Methoden entwickelt, die eine komplette Charakterisierung der Variationen im Vorkommen dieser Spezies ermöglichen. Es wird die bisher umfassendste Darstellung dieser Variationen in Troposphäre und Stratosphäre gegeben und mit Bezug auf eine Reihe von Laborexperimenten detailliert interpretiert.Die Laborexperimente machen einen großen Anteil dieser Doktorarbeit aus und konzentrieren sich auf die Isotopenfraktionierung in den stratosphärischen N2O-Senken, d. h. Photolyse und Reaktion mit elektronisch angeregten Sauerstoffatomen, O(1D). Diese Prozesse sind von dominantem Einfluß auf die Isotopenzusammensetzung von atmosphärischem N2O. Potentiell wichtige Parameter wie Temperatur- und Druckvariationen, aber auch Veränderungen der Wellenlänge im Fall der Photolyse wurden berücksichtigt. Photolyse bei stratosphärisch relevanten Wellenlängen > 190 nm zeigte immer Anreicherungen von 15N in beiden Stickstoffatomen des verbleibenden N2O wie auch in 17O und 18O. Die Anreicherungen waren am mittelständigen N-Atom signifikant höher als am endständigen N (mit mittleren Werten für 18O) und stiegen zu größeren Wellenlängen und niedrigeren Temperaturen hin an. Erstmalig wurden für 18O und 15N am endständigen N-Atom Isotopenabreicherungen bei 185 nm-Photolyse festgestellt. Im Gegensatz zur Photolyse waren die Isotopenanreicherungen bei der zweiten wichtigen N2O-Senke, Reaktion mit O(1D) vergleichsweise gering. Jedoch war das positionsabhängige Fraktionierungsmuster dem der Photolyse direkt entgegengesetzt und zeigte größere Anreicherungen am endständigen N-Atom. Demgemäß führen beiden Senkenprozesse zu charakteristischen Isotopensignaturen in stratosphärischem N2O. Weitere N2O-Photolyseexperimente zeigten, daß 15N216O in der Atmosphäre höchstwahrscheinlich mit der statistisch zu erwartenden Häufigkeit vorkommt.Kleine stratosphärische Proben erforderten die Anpassung der massenspektrometrischen Methoden an Permanentflußtechniken, die auch für Messungen an Firnluftproben von zwei antarktischen Stationen verwendet wurden. Das 'Firnluftarchiv' erlaubte es, den gegenwärtigen Trend und die präindustriellen Werte der troposphärischen N2O-Isotopensignatur zu bestimmen. Ein daraus konstruiertes globales N2O-Isotopenbudget ist im Einklang mit den besten Schätzungen der Gesamt-N2O-Emissionen aus Böden und Ozeanen.17O-Messungen bestätigten die Sauerstoffisotopenanomalie in atmosphärischem N2O, zeigten aber auch, daß N2O-Photolyse die Sauerstoffisotope gemäß einem massenabhängigen Fraktionierungsgesetz anreichert. Eine troposphärische Ursache für einen Teil des Exzeß-17O wurde vorgeschlagen, basierend auf der Reaktion von NH2 mit NO2, wodurch die Sauerstoffisotopenanomalie von O3 über NO2 an N2O übertragen wird.

Modernismi Litici 1922-1942. La pietra nell'Architettura Moderna

Leggere il progetto del Moderno e le sue culture costruttive in relazione alla storia e allo sviluppo della tecnologia, consente di esplorare alcuni aspetti dell’Architettura Moderna in Europa. Oltre alla più famosa, e maggiormente studiata, triade dei materiali ‘moderni’ – l’acciaio, il calcestruzzo e il vetro – la pietra ha svolto un importante ruolo nella definizione sia dello stile che della costruzione moderna. La costruzione in pietra è stata sempre associata alla tradizione e quindi deliberatamente dimenticata dal Movimento Moderno, durante la fase cruciale della modernizzazione della società e quindi dell’architettura e della costruzione. La pietra tuttavia testimonia la delicata transizione dalla tradizionale arte del costruire alle nuove tecnologie. La ricerca ha studiato l’evoluzione delle tecniche costruttive in pietra in Francia ed in Italia, durante gli anni ’20 e ’30, in relazione alle nuove tecniche industrializzate e i linguaggi delle avanguardie. La ricerca è partita dallo studio dei manuali, delle riviste e dei progetti presentati sulle loro pagine. In Italia e in Francia il rivestimento in pietra si afferma come un sistema costruttivo ‘razionale’, dove la costruzione moderna converge lentamente verso nuove soluzioni; questo sistema ha avuto negli anni ’20 e ’30 un ruolo centrale, nel quale è stato possibile un dialogo, senza contraddizioni, tra i materiali ‘moderni’ e la pietra. L’evoluzione dalle tradizionali tecniche costruttive verso i nuovi sistemi tecnologici, ha determinato una nuova costruzione in pietra che è alla base di una modernità che non rifiuta questo materiale tradizionale, ma lo trasforma secondo i nuoci principi estetici.

Soil application of Meliaceae derivatives: effect on carbon and nitrogen dynamics in the soil-plant system

The effect of soil incorporation of 7 Meliaceae derivatives (6 commercial neem cakes and leaves of Melia azedarach L.) on C and N dynamics and on nutrient availability to micropropagated GF677 rootstock was investigated. In a first laboratory incubation experiment the derivatives showed different N mineralization dynamics, generally well predicted by their C:N ratio and only partly by their initial N concentration. All derivatives increased microbial biomass C, thus representing a source of C for the soil microbial population. Soil addition of all neem cakes (8 g kg-1) and melia leaves (16 g kg-1) had a positive effect on plant growth and increased root N uptake and leaf green colour of micropropagated plants of GF677. In addition, the neem cakes characterized by higher nutrient concentration increased P and K concentration in shoot and leaves 68 days after the amendment. In another experiment, soil incorporation of 15N labeled melia leaves (16 g kg-1) had no effect on the total amount of plant N, however the percentage of melia derived-N of treated plants ranged between 0.8% and 34% during the experiment. At the end of the growing season, about 7% of N added as melia leaves was recovered in plant, while 70% of it was still present in soil. Real C mineralization and the priming effect induced by the addition of the derivatives were quantified by a natural 13C abundance method. The real C mineralization of the derivatives ranged between 22% and 40% of added-C. All the derivatives studied induced a positive priming effect and, 144 days after the amendment, the amount of C primed corresponded to 26% of added-C, for all the derivatives. Despite this substantial priming effect, the C balance of the soil, 144 days after the amendment, always resulted positive.