Douteur testiculaire, un défi diagnostique [Testicular pain, a diagnostic challenge?].

Scrotal pain is frequently encountered in practice, as it affects 4 men in 1000, with a peak of incidence between the ages of 45 and 50. After excluding an urological or gastrointestinal cause, referred pain of musculoskeletal origin should be considered, even in the absence of back pain. Described by Dr. Robert Maigne, this referred pain originates from a minor intervertebral dysfunction of the thoracolumbar junction. Imaging of the spine is not helpful. Rather, the diagnosis is made by seeking pain triggered by the mobilization of the lumbar vertebrae; the pinch and roll skin manoeuvre will highlight this referred pain. Treatment is symptomatic, though manual therapies by spine specialists are also recommended.

Post-Plutonic Magmatism: from the Source to the Emplacement of an Upper Crustal Dyke Swarm, Adamello Massif, Italy

Magmas of the arc-tholeiitic and calc-alkaline differentiation suites contribute substantially to the formation of continental crust in subduction zones. Different geochemical-petrological models have been put forward to achieve evolved magmas forming large volumes of tonalitic to granitic plutons, building an important part of the continental crust. Primary magmas produced in the mantle wedge overlying the subducted slab migrate through the mantle and the crust. During the transfer, magma can accumulate in intermediate reservoirs at different levels where crystallization leads to differentiation and the heat transfer from the magma, together with gained heat from solidification, lead to partial melting of the crust. Partial melts can be assimilated and mix with more primitive magma. Moreover, already formed crystal cumulates or crystal mushes can be recycled and reactivated to transfer to higher crustal levels. Magma transport in the crust involves fow through fractures within a brittle elastic rock. The solidified magma filled crack, a dyke, can crosscut previously formed geological structures and thus serves as a relative or absolute time marker. The study area is situated in the Adamello massif. The Adamello massif is a composite of plutons that were emplaced between 42 and 29 million years. A later dyke swarm intruded into the southern part of the Adamello Batholith. A fractionation model covering dyke compositions from picrobasalts to dacites results in the cummulative crystallization of 17% olivine, 2% Cr-rich spinel, 18% clinopyroxene, 41% amphibole, 4% plagioclase and 0.1% magnetite to achieve an andesitic composition out of a hydrous primitive picrobasalt. These rocks show a similar geochemical evolution as experimental data simulating fractional crystallization and associated magma differentiation at lower crustal depth (7-10 kbar). The peraluminous, corundum normative composition is one characteristic of more evolved dacitic magmas, which has been explained in a long lasting debate with two di_erent models. Melting of mafic crust or politic material provides one model, whereas an alternative is fractionation from primary mantle derived melts. Amphibole occurring in basaltic-andesitic and andesitic dyke rocks as fractionating cumulate phase extracted from lower crustal depth (6-7.5 kbar) is driving the magmas to peraluminous, corundum normative compositions, which are represented by tonalites forming most of the Adamello Batholith. Most primitive picrobasaltic dykes have a slightly steepened chondrite normalized rare earth elements (REE) pattern and the increased enrichment of light-REE (LREE) for andesites and dacites can be explained by the fractional crystallization model originating from a picrobasalt, taking the changing fractionating phase assemblage and temperature into account. The injection of hot basaltic magma (~1050°C) in a closely spaced dyke swarm increases the surface of the contact to the mainly tonalitic wallrock. Such a setting induces partial melting of the wall rock and selective assimilation. Partial melting of the tonalite host is further expressed through intrusion breccias from basaltic dykes. Heat conduction models with instantaneous magma injection for such a dyke swarm geometry can explain features of partial melting observed in the field. Geochemical data of minerals and bulk rock further underline the selective or bulk assimilation of the tonalite host rock at upper crustal levels (~2-3 kbar), in particular with regard to light ion lithophile elements (LILE) such as Sr, Ba and Rb. Primitive picrobasalts carry an immiscible felsic assimilant as enclaves that bring along refractory rutile and zircon with textures typically found in oceanic plagiogranites or high pressure/low-temperature metamorphic rocks in general. U-Pb data implies a lower Cretaceous age for zircon not yet described as assimilant in Eocene to Oligocene magmatic rocks of the Central Southern Alps. The distribution of post-plutonic dykes in large batholiths such as the Adamello is one of the key features for understanding the regional stress field during the post-batholith emplacement cooling history. The emplacement of the regional dyke swarm covering the southern part of the Adamello massif was associated with consistent left lateral strike-slip movement along magma dilatation planes, leading to en echelon segmentation of dykes. Through the dilation by magma of pre-existing weaknesses and cracks in an otherwise uniform host rock, the dyke propagation and according orientation in the horizontal plane adjusted continuously perpendicular to least compressive remote stress σ3, resulting in an inferred rotation of the remote principal stress field. Les magmas issus des zones de subduction contribuent substantiellement à la formation de la croûte continentale. Les plutons tonalitiques et granitiques représentent, en effet, une partie importante de la croûte continentale. Des magmas primaires produits dans le 'mantle wedge ', partie du manteau se trouvant au-dessus de la plaque plongeante dans des zones de subduction, migrent à travers le manteau puis la croûte. Pendant ce transfert, le magma peut s'accumuler dans des réservoirs intermédiaires à différentes profondeurs. Le stockage de magma dans ces réservoirs engendre, d'une part, la différentiation des magmas par cristallisation fractionnée et, d'autre part, une fusion partielle la croûte continentale préexistante associée au transfert de la chaleur des magmas vers l'encaissant. Ces liquides magmatiques issus de la croûte peuvent, ensuite, se mélanger avec des magmas primaires. Le transport du magma dans la croûte implique notamment un flux de magma à travers différentes fractures recoupant les roches encaissantes élastiques. Au cours de ce processus de migration, des cumulats de cristaux ou des agrégats de cristaux encore non-solidifiés, peuvent être recyclés et réactivés pour être transportés à des niveaux supérieures de la croûte. Le terrain d'étude est situé dans le massif d'Adamello. Celui-ci est composé de plusieurs plutons mis en place entre 42 et 29 millions d'années. Dans une phase tardive de l'activité magmatique liée à ce batholite, une série de filons de composition variable allant de picrobasalte à des compositions dacitiques s'est mise en place la partie sud du massif. Deux modèles sont proposés dans la littérature, pour expliquer la formation des magmas dacitiques caractérisés par des compositions peralumineux (i.e. à corindon normatif). Le premier modèle propose que ces magmas soient issus de la fusion de matériel mafique et pélitique présent dans la partie inférieur de la croûte, alors que le deuxième modèle suggère une évolution par cristallisation fractionnée à partir de liquides primaires issus du manteau. Un modèle de cristallisation fractionnée a pu être développé pour expliquer l'évolution des filons de l'Adamello. Ce modèle explique la formation des filons dacitiques par la cristallisation fractionnée de 17% olivine, 2% spinelle riche en Cr, 18% clinopyroxène, 41% amphibole, 4% plagioclase et 0.1% magnetite à partir de liquide de compositions picrobasaltiques. Ce modèle prend en considération les contraintes pétrologiques déduites de l'observation des différents filons ainsi que du champ de stabilité des différentes phases en fonction de la température. Ces roches montrent une évolution géochimique similaire aux données expérimentales simulant la cristallisation fractionnée de magmas évoluant à des niveaux inférieurs de la croûte (7-10 kbar). Le modèle montre, en particulier, le rôle prépondérant de l'amphibole, une phase qui contrôle en particulier le caractère peralumineux des magmas différentiés ainsi que leurs compositions en éléments en traces. Des phénomènes de fusion partielle de l'encaissant tonalitique lors de la mise en place de _lons mafiques sont observée sur le terrain. L'injection du magma basaltique chaud (~1050°C) sous forme de filons rapprochés augmente la surface du contact avec l'encaissante tonalitique. Une telle situation produit la fusion partielle des roches encaissantes nécessaire à l'incorporation d'enclaves mafiques observés au sein des tonalites. Pour comprendre les conditions nécessaires pour la fusion partielle des roches encaissantes, des modèles de conduction thermique pour une injection simultanée d'une série de filons ont été développées. Des données géochimiques sur les minéraux et sur les roches totales soulignent qu'au niveau supérieur de la croûte, l'assimilation sélective ou totale de l'encaissante tonalitique modifie la composition du liquide primaire pour les éléments lithophiles tel que le Sr, Ba et Rb. Un autre aspect important concernant la pétrologie des filons de l'Adamello est la présence d'enclaves felsiques dans les filons les plus primitifs. Ces enclaves montrent, en particulier, des textures proches de celles rencontrées dans des plagiogranites océaniques ou dans des roches métamorphiques de haute pression/basse température. Ces enclaves contiennent du zircon et du rutile. La datations de ces zircons à l'aide du géochronomètre U-Pb indique un âge Crétacé inférieur. Cet âge est important, car aucune roche de cet âge n'a été considérée comme un assimilant potentiel pour des roches magmatiques d'âge Eocène à Oligocène dans les Alpes Sud Centrales. La réparation spatiale des filons post-plutoniques dans des grands batholites tel que l'Adamello, est une caractéristique clé pour la compréhension des champs de contraintes lors du refroidissement du batholite. L'orientation des filons va, en particulier, indiqué la contrainte minimal au sein des roches encaissante. La mise en place de la série de filon recoupant la partie Sud du massif de l'Adamello est associée à un décrochement senestre, un décrochement que l'on peut lié aux contraintes tectoniques régionales auxquelles s'ajoutent l'effet de la dilatation produite par la mise en place du batholite lui-même. Ce décrochement senestre produit une segmentation en échelon des filons.

Isozymic variability in a Brazilian collection of annatto (Bixa orellana L.)

The objectives of this work were to optimize the isozyme electrophoresis technique for Bixa orellana, and use isozyme markers for a preliminary survey on the genetic variability in Brazilian annatto germplasm accessions. Collection consisted of seed samples from sixty open pollinated trees, representing two Northern and four Southern geographic provenances. The extraction, electrophoresis, and interpretation of annatto isozymes are described. Three out of the twenty-one identified isozyme loci were polymorphic in the collection. The percentage of polymorphic loci (P = 21.05) and the expected heterozygosity in annatto (H T = 0.064) were low, compared to other tropical woody species. A UPGMA phenogram, constructed with Nei's genetic distances, clearly separated the germplasm provenant from North and Central Brazil. Variability was significantly higher among the accessions from Maranhão. A sharp genetic differentiation was detected between accessions from Maranhão and Pará States, despite their geographical proximity. The distinctive isozyme polymorphism, observed in the accessions from Maranhão, together with reports on local morphological heterogeneity in annatto fruit shape, color, and pubescence, calls for more detailed genetic and taxonomic investigation.

Mineralogical alteration of artificial meteorites during atmospheric entry. The STONE-5 experiment

The generic concept of the artificial meteorite experiment STONE is to fix rock samples bearing microorganisms on the heat shield of a recoverable space capsule and to study their modifications during atmospheric re-entry. The STONE-5 experiment was performed mainly to answer astrobiological questions. The rock samples mounted on the heat shield were used (i) as a carrier for microorganisms and (ii) as internal control to verify whether physical conditions during atmospheric re-entry were comparable to those experienced by "real" meteorites. Samples of dolerite (an igneous rock), sandstone (a sedimentary rock), and gneiss impactite from Haughton Crater carrying endolithic cyanobacteria were fixed to the heat shield of the unmanned recoverable capsule FOTON-M2. Holes drilled on the back side of each rock sample were loaded with bacterial and fungal spores and with dried vegetative cryptoendoliths. The front of the gneissic sample was also soaked with cryptoendoliths. <p>The mineralogical differences between pre- and post-flight samples are detailed. Despite intense ablation resulting in deeply eroded samples, all rocks in part survived atmospheric re-entry. Temperatures attained during re-entry were high enough to melt dolerite, silica, and the gneiss impactite sample. The formation of fusion crusts in STONE-5 was a real novelty and strengthens the link with real meteorites. The exposed part of the dolerite is covered by a fusion crust consisting of silicate glass formed from the rock sample with an admixture of holder material (silica). Compositionally, the fusion crust varies from silica-rich areas (undissolved silica fibres of the holder material) to areas whose composition is "basaltic". Likewise, the fusion crust on the exposed gneiss surface was formed from gneiss with an admixture of holder material. The corresponding composition of the fusion crust varies from silica-rich areas to areas with "gneiss" composition (main component potassium-rich feldspar). The sandstone sample was retrieved intact and did not develop a fusion crust. Thermal decomposition of the calcite matrix followed by disintegration and liberation of the silicate grains prevented the formation of a melt.</p> <p>Furthermore, the non-exposed surface of all samples experienced strong thermal alterations. Hot gases released during ablation pervaded the empty space between sample and sample holder leading to intense local heating. The intense heating below the protective sample holder led to surface melting of the dolerite rock and to the formation of calcium-silicate rims on quartz grains in the sandstone sample. (c) 2008 Elsevier Ltd. All rights reserved.</p>

Oxidation of methane at the CH4/H2O-(CO2) transition zone in the external part of the Central Alps, Switzerland: Evidence from stable isotope investigations

With the aim of understanding the mechanisms that control the metamorphic transition from the CH4- to the H2O-(CO2)-dominated fluid zone in the Helvetic domain of the Central Alps of Switzerland, fluid inclusions in quartz, illite ``crystallinity'' index, vitrinite reflectance, and the stable isotope compositions of vein and whole rock minerals and fluids trapped in quartz were investigated along four cross-sections. Increasing temperature during prograde metamorphism led to the formation of dry gas by hydrocarbon cracking in the CH4-zone. Fluid immiscibility in the H2O-CH4-(CO2)-NaCl system resulted in cogenetic, CH4- and H2O-dominated fluid inclusions. In the CH4-zone, fluids were trapped at temperatures <= 270 +/- 5 degrees C. The end of the CH4-zone is markedby a sudden increase of CO2 content in the gas phase of fluid inclusions. At temperatures > 270 +/- 5 degrees C, in the H2O-zone, the total amount of volatiles within the fluid decreased below 1 mol% with no immiscibility. This resulted m total homogenization temperatures of H2O-(CO2-CH4)-NaCl inclusions below 180 degrees C. Hydrogen isotope compositions of methane in fluid inclusion have delta D values of less than -100 parts per thousand in the CH4-zone, typical for an origin through cracking of higher hydrocarbons, but where the methane has not equilibrated with the pore water. delta D values of fluid inclusion water are around -40 parts per thousand., in isotopic equilibrium with phyllosilicates of the whole rocks. Within the CH4 to H2O(CO2) transition zone, delta D(H2O) values in fluid inclusions decrease to -130 parts per thousand interpreted to reflect the contribution of deuterium depleted water from methane oxidation. In the H2O-zone, delta D(H2O) values increase again towards an average of -30 parts per thousand which is again consistent with isotopic equilibrium with host-rock phyllosilicates. delta C-13 values of methane in fluid inclusions from the CH4-zone are around -27 parts per thousand in isotopic equilibrium with calcite in veins and whole rocks. The delta C-13(CH4) values decrease to less than -35 parts per thousand at the transition to the H2O-zone and are no longer in equilibrium with the carbonates in the whole rocks. delta C-13 values of CO, are variable but too low to be in equilibrium with the wall rock fluids, compatible with a contribution of CO2 from closed system oxidation of methane. Differences in isotopic composition between host-rock and Alpine fissure carbonate are generally small, suggesting that the amount of CO2 produced by oxidation of methane was small compared to the C-budget in the rocks and local pore fluids were buffered by the wall rocks during precipitation of calcite within the fissures. (c) 2006 Elsevier B.V. All rights reserved.

Pinnan ominaisuuksien karakterisointi kiiltomittalaitteella ja kiiltomittalaitteen soveltuvuus tuotannon laadunvarmistuksessa

Alahuulten, kärkilistojen, turboputkien ja telapinnoitteiden pinnankarheutta mitataan Rautpohjan tehtaalla nykyään pääosin koskettavalla pinnankarheusprofilometrilla. Profilometrin käyttö on hankalaa ja epäluotettavaa tai käytössä on muita ongelmia. Paperin kuituorientaation mittaamiseen käytetään nykyisin mm. TSO-menetelmää tai repäisymenetelmää. Tämän diplomityön tarkoituksena oli kartoittaa diffraktiiviseen optiseen elementtiin perustuvan kiiltomittalaiteprototyypin mahdollisuuksia karakteroida pinnan ominaisuuksia ja tutkia kiiltomittalaitteen soveltuvuutta tuotannon laadunvarmistuksessa. Alahuuli-, kärkilista-, turboputki-, telapinnoite- ja paperinäytteistä valmistettiinnäytesarjoja, jotka mitattiin nykymenetelmin ja kiiltomittalaitteella. Tulostenkorreloituvuutta tutkittiin ja taloudellista merkitystä arvioitiin investointilaskelmin. Paperin kuituorientaation, paperin pinnan kuituorientaation ja telapinnoitteiden mittaaminen kiiltomittalaitteella osoittautui taloudellisesti erittäin merkittäväksi. Ennen mahdollista kiiltomittalaitteen käyttöönottoa prototyyppiä on kehitettävä, kiillon korreloituvuutta tulee tutkia edelleen ja aiheesta on tehtävä lisätutkimuksia.

Cenomanian-Turonian transition in a shallow water sequence of the Sinai, Egypt

Environmental and depositional changes across the Late Cenomanian oceanic anoxic event (OAE2) in the Sinai, Egypt, are examined based on biostratigraphy, mineralogy, delta(13)C values and phosphorus analyses. Comparison with the Pueblo, Colorado, stratotype section reveals the Whadi El Ghaib section as stratigraphically complete across the late Cenomanian-early Turonian. Foraminifera are dominated by high-stress planktic and benthic assemblages characterized by low diversity, low-oxygen and low-salinity tolerant species, which mark shallow-water oceanic dysoxic conditions during OAE2. Oyster biostromes suggest deposition occurred in less than 50 m depths in low-oxygen, brackish, and nutrient-rich waters. Their demise prior to the peak delta(13)C excursion is likely due to a rising sea-level. Characteristic OAE2 anoxic conditions reached this coastal region only at the end of the delta(13)C plateau in deeper waters near the end of the Cenomanian. Increased phosphorus accumulations before and after the delta(13)C excursion suggest higher oxic conditions and increased detrital input. Bulk-rock and clay mineralogy indicate humid climate conditions, increased continental runoff and a rising sea up to the first delta(13)C peak. Above this interval, a dryer and seasonally well-contrasted climate with intermittently dry conditions prevailed. These results reveal the globally synchronous delta(13)C shift, but delayed effects of OAE2 dependent on water depth.

CO2-laserin soveltaminen WFU-paperin reunan leikkaamiseen

Tämän diplomityön tarkoitus oli selvittää CO2-laserin soveltuvuutta paperin reunan leikkaamiseen ennen liimapuristinta nopealle modernilleWFU-paperikoneelle. Merkittävimmät leikkauskokeet tehtiin leikkaamalla paperirataa todenmukaisissa olosuhteissa koekoneella. Koeleikkauksissa tutkittiin myös päällystettyjen paperilajien CO2-laserleikkausta. Paperin reunan koeleikkauksia suoritettiin leikkauspöytää vasten sekä telaa vasten. Leikkauspöytänä käytettiin korkeapainevesileikkaimelle suunniteltua leikkauspöytää, jota paranneltiin tämän työn yhteydessä paremmin laserleikkaukselle sopivaksi. Telaa vasten suoritetuilla leikkauksilla lasertehon tarve oli suurempi verrattuna pöytää vasten leikkaukseen samalla leikkausnopeudella ja samalla paperilajilla. Laserlaitteiston mitoittaminen oikein pelkkien arkkileikkauskokeiden perusteella ei ollut mahdollista. Myös rullilla tapahtuvia leikkauskokeita tarvittiin. Pöytää vasten tapahtuvaan leikkaamiseen tarvitaan 1000 W laserlaite paperin molemmille reunoille. Tämän tehoiset laserlaitteet riittävät kaikille Changshun PK 1:n paperilajeille niiden lajikohtaiseen maksimiajonopeuteen. Testatuista kolmesta polttovälistä antoi 5" polttoväli parhaat leikkaustulokset. Polttopisteen paikka voi vaihdella ± 0.75 mm paperin pinnasta vaikuttamatta silti merkittävästi lasertehon tarpeeseen. Laserleikatun paperin reuna oli hyvälaatuinen, eikä laserleikkaus aiheuttanut paperille epätoivottuja asioita kuten mustumista.

SC-paperirullien vanaisuuden syntymekanismien selvittäminen

Myllykoski Paper Oy:n PK6:n kapeiden asiakasrullien vanoittuminen on aiheuttanut tuotannonmenetyksiä. Tämän työn tavoitteena oli pyrkiä selvittämään SC-paperirullissa esiintyvän vanaisuuden syntymekanismeja ja sitä, kuinka pituusleikkurilla voitaisiin vähentää vanan muodostumista asiakasrulliin. Työn kirjallisuusosassa selvitettiin rullaustapahtumaa pituusleikkurilla, paperin rullautuvuuteen vaikuttavia tekijöitä ja SC-paperille soveltuvia pituusleikkurityyppejä. Tässäyhteydessä syvennyttiin vanan syntymekanismeihin ja vanan syntymisen mahdollisiin ehkäisymenetelmiin. Vanan muodostumiseen vaikuttavat rainassa olevat jyrkät muutokset mm. neliömassa- ja paksuuspoikkiprofiileissa sekä pituusleikkurin rullausasemien linjauksen virheellisyys. Työn kokeellinen osa jakautui kahteen osaan.Esikokeissa tilastoitiin vanarullien muodostuminen eri pituusleikkurin rullausasemien, rullausposition ja käytetyn superkalanterin mukaan. Vanarullien paperista tutkittiin poikkisuuntaisia profiileja vanan syntysyiden löytämiseksi. Vanarullat olivat pääasiassa rainan reunoista leikattuja ja esikokeiden aikana suurin osan vanarullista muodostui superkalanteri II:n tambuureista. Koeajossa tutkittiin pituusleikkurin ajoparametrien ja rullausposition vaikutusta vanan muodostumiseen kapeassa rainan reunaosasta leikattavassa rullassa. Paperissa olevan profiilivian aiheuttamaa vanaa ei pystytty poistamaan ajoparametrimuutoksilla poistamaan koeajossa. Pituusleikkurin rullausasemien ja telojen linjaus sekä liikkuvien osien välysten poistaminen vähensi vanan muodostumista. Paperin neliömassa- ja paksuusprofiileissa kapealla alueella tapahtuvat jyrkät muutokset lisäsivät merkittävästi vanan muodostumista. Paperin profiilien hallinnalla ja pituusleikkurin kuluvien osien ennakoivalla huollolla voidaan vähentää vanan muodostumista asiakasrulliin.

Raakafosfaatin liuotus ja ammonointi

Apatiittien käyttöä raaka-aineena lannoitteiden valmistusprosessissa on usein hankaloittanut lannoitelietteen viskositeetin kasvu, kun hapanta lannoitelietettä on neutraloitu ammoniakilla. Työn tarkoituksena oli tutkia lannoitelietteen viskositeettiin vaikuttavia tekijöitä ja tekijöiden vaikutusta lannoitteen ominaisuuksiin. Työn kirjallisen osan alkupuoliskolla käsiteltiin raakafosfaatteja ja fosfaattilannoitteita. Tämän jälkeen keskityttiin lannoitteiden valmistukseen sekä viskositeetin merkitykseen lannoiteprosesseissa. Työn kokeellisessa osassa tutkittiin raakafosfaatin, liuotushapon, liuotushappomäärän, ammonointiajan sekä apatiitti/fosforihappo-suhteen vaikutusta lannoitteen ominaisuuksiin. Kokeet aloitettiin raakafosfaatin liuotuksella happoon. Tämän jälkeen liete neutraloitiin ammoniakilla ja suoritettiin muiden ravinteiden lisäys. Lannoitelietteen viskositeettiin voimakkaimmin vaikuttavat tekijät olivat kokeissa käytetty liuotushappo, ammonointiaika sekä raakafosfaatti. Raakafosfaatilla, liuotushapolla sekä apatiitti/fosforihappo-suhteella havaittiin olevan suurin merkitys lannoitteen fosforin vesiliukoisuudelle.

Drogues, química i amor

Hi ha un eslògan que diu: "Sexe,droga i rock'n'roll". Aquests darrers dies s'ha fet públic el decomís a Colòmbia de sis tones de cocaïna amb destí a Espanya,i que l'any 2007 a Catalunya se'n van interceptar 81 d'haixix i es van confiscar 83 milions d'euros procedents del narcotràfic [...].

Reciclagem do lixo de informática: uma oportunidade para a química

Recycling and sustainable development are increasing in importance around the world. In Brazil, the new National Policy on Solid Wastes has prompted discussion on the future of electronic waste (e-waste). Brazil generates the greatest amount of e-waste among Latin American countries. Nevertheless complete recycling, including end processing of e-waste, does not occur in Brazil. This paper discusses the physical and chemical technologies currently used worldwide and in Brazil for printed circuit board recycling, with emphasis on metal recovery and plastic processing. The goal is to put in evidence the important role that chemistry can play in developing cheaper processes to recycle e-waste.

Risk factors associated with buffalo mastitis in the Brazilian Northeast

Risk factors for subclinical mastitis were studied in 474 buffaloes cows proceeding from four dairy farms located in the states of Pernambuco, Alagoas, Bahia and Ceará, Brazil. Milk samples (n=1896) of lactating buffaloes cows were examined for somatic cells count (SCC) and microbiologic exam, and a questionnaire composed by objective questions was applied in order to obtain animals and herd management data. Risk factors analysis was performed in two stages: univariate and mutivariate analysis. Two analysis were performed, one considering the animal classification for SCC as the dependent variable (<400,000 - negative; >400,000 - positive) and another, considering the microbiologic exam result (positive and negative). In the multivariate analysis considering SCC as dependent variable, the lack of teat washing was the only variable identified as a risk factor, so that farms without this procedure before the milking presented risk of infection of 2.68 (I.C. 1.49-4.83). In the multivariate analysis considering the microbiologic exam as dependent variable, it was observed that properties that performed the cleaning of the milking equipment manually presented risk of 1.85 (I.CI. 1.32-3.64), which was higher than those properties that performed the cleaning mechanically (p=0.019). Risk factors for the occurrence of subclinical mastitis in dairy buffaloes in Brazilian Northeast farms were related to the characteristics of improper milking management. Risk factors identified in this study must be carefully corrected in order to reduce the frequency of mastitis cases, and therefore, contribute for disease control and prevention in the herds.

A Test Bed Applied Mobile Robot Navigation

It is presented a test bed applied to studies on dynamics, control, and navigation of mobile robots. A cargo ship scale model was chosen, which can be radio-controlled or operated autonomously through an embedded control system. A control program, which manages on board mission execution, is implemented on a microcontroller. Navigation is based on an electronic compass, which includes automatic compensation for pitch and roll motions. Heading control loop is based on this sensor, and on a rudder positioning system. A propulsion control system is also implemented. Typical manoeuvres as the turning test and "zig-zag", were implemented and tested. They are included on a manoeuvre library, and can be accessed independently or in combined modes. The embedded system is also in charge of signal acquisition and storing during the missions. It is possible to analyse experiments on identification of ship dynamics, control, and navigation, through the data transferred to a PC by serial communication. Navigation is going to be improved by including inertial sensors on board, and a DGPS. Preliminary tests are aimed to ship identification, and manoeuvrability, using free model tests. Future steps include extending this system for developing other mobile robots as, ROVs, AUVs, and aerial vehicles.