433 resultados para Intermetallic precipitates
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Linear and nonlinear optical properties of silicon suboxide SiOx films deposited by plasma-enhanced chemical-vapor deposition have been studied for different Si excesses up to 24¿at.¿%. The layers have been fully characterized with respect to their atomic composition and the structure of the Si precipitates. Linear refractive index and extinction coefficient have been determined in the whole visible range, enabling to estimate the optical bandgap as a function of the Si nanocrystal size. Nonlinear optical properties have been evaluated by the z-scan technique for two different excitations: at 0.80¿eV in the nanosecond regime and at 1.50¿eV in the femtosecond regime. Under nanosecond excitation conditions, the nonlinear process is ruled by thermal effects, showing large values of both nonlinear refractive index (n2 ~ ¿10¿8¿cm2/W) and nonlinear absorption coefficient (ß ~ 10¿6¿cm/W). Under femtosecond excitation conditions, a smaller nonlinear refractive index is found (n2 ~ 10¿12¿cm2/W), typical of nonlinearities arising from electronic response. The contribution per nanocrystal to the electronic third-order nonlinear susceptibility increases as the size of the Si nanoparticles is reduced, due to the appearance of electronic transitions between discrete levels induced by quantum confinement.
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An analysis of silicon on insulator structures obtained by single and multiple implants by means of Raman scattering and photoluminescence spectroscopy is reported. The Raman spectra obtained with different excitation powers and wavelengths indicate the presence of a tensile strain in the top silicon layer of the structures. The comparison between the spectra measured in both kinds of samples points out the existence in the multiple implant material of a lower strain for a penetration depth about 300 nm and a higher strain for higher penetration depths. These results have been correlated with transmission electron microscopy observations, which have allowed to associate the higher strain to the presence of SiO2 precipitates in the top silicon layer, close to the buried oxide. The found lower strain is in agreement with the better quality expected for this material, which is corroborated by the photoluminescence data.
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The distribution of low molecular weight carboxylic acids (LMWCA) was investigated in pore water profiles from two porphyry copper tailings impoundments in Chile (Piuquenes at La Andina and Cauquenes at El Teniente mine). The objectives of this study were (1) to determine the distribution of LMWCA, which are interpreted to be the metabolic byproducts of the autotroph microbial community in this low organic carbon system, and (2) to infer the potential role of these acids in cycling of Fe and other elements in the tailings impoundments. The speciation and mobility of iron, and potential for the release of H+ via hydrolysis of the ferric iron, are key factors in the formation of acid mine drainage in sulfidic mine wastes. In the low-pH oxidation zone of the Piuquenes tailings, Fe(III) is the dominant iron species and shows high mobility. LMWCA, which occur mainly between the oxidation front down to 300 cm below the tailings surface at both locations (e.g., max concentrations of 0.12 mmol/L formate, 0.17 mmol/L acetate, and 0.01 mmol/L pyruvate at Piuquenes and 0.14 mmol/L formate, 0.14 mmol/L acetate, and 0.006 mmol/L pyruvate at Cauquenes), are observed at the same location as high Fe concentrations (up to 71.2 mmol/L Fe(II) and 16.1 mmol/L Fe(III), respectively). In this zone, secondary Fe(111) hydroxides are depleted. Our data suggest that LMWCA may influence the mobility of iron in two ways. First, complexation of Fe(III), through formation of bidentate Fe(III)-LMWCA complexes (e.g., pyruvate, oxalate), may enhance the dissolution of Fe(III) (oxy)hydroxides or may prevent precipitation of Fe(III) (oxy)hydroxides. Soluble Fe(III) chelate complexes which may be mobilized downward and convert to Fe(II) by Fe(III) reducing bacteria. Second, monodentate LMWCA (e.g., acetate and formate) can be used by iron-reducing bacteria as electron donors (e.g., Acidophilum spp.), with ferric iron as the electron acceptor. These processes may, in part, explain the low abundances of secondary Fe(III) hydroxide precipitates below the oxidation front and the high concentrations of Fe(II) observed in the pore waters of some low-sulfide systems. The reduction of Fe(III) and the subsequent increase of iron mobility and potential acidity transfer (Fe(II) oxidation can result in the release of H+ in an oxic environment) should be taken in account in mine waste management strategies.
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The stable carbon and oxygen isotope compositions of fossil ostracods are powerful tools to estimate past environmental and climatic conditions. The basis for such interpretations is that the calcite of the valves reflects the isotopic composition of water and its temperature of formation. However, calcite of ostracods is known not to form in isotopic equilibrium with water and different species may have different offsets from inorganic precipitates of calcite formed under the same conditions. To estimate the fractionation during ostracod valve calcification, the oxygen and carbon isotope compositions of 15 species living in Lake Geneva were related to their autoecology and the environmental parameters measured during their growth. The results indicate that: (1) Oxygen isotope fractionation is similar for all species of Candoninae with an enrichment in 18O of more than 30/00 relative to equilibrium values for inorganic calcite. Oxygen isotope fractionation for Cytheroidea is less discriminative relative to the heavy oxygen, with enrichments in 18O for these species of 1.7 to 2.30/00. Oxygen isotope fractionations for Cyprididae are in-between those of Candoninae and Cytheroidea. The difference in oxygen isotope fractionation between ostracods and inorganic calcite has been interpreted as resulting from a vital effect. (2) Comparison with previous work suggests that oxygen isotope fractionation may depend on the total and relative ion content of water. (3) Carbon isotope compositions of ostracod valves are generally in equilibrium with DIC. The specimens' δ13C values are mainly controlled by seasonal variations in δ13CDIC of bottom water or variation thereof in sediment pore water. (4) Incomplete valve calcification has an effect on carbon and oxygen isotope compositions of ostracod valves. Preferential incorporation of at the beginning of valve calcification may explain this effect. (5) Results presented here as well as results from synthetic carbonate growth indicate that different growth rates or low pH within the calcification site cannot be the cause of oxygen isotope 'vital effects' in ostracods. Two mechanisms that might enrich the 18O of ostracod valves are deprotonation of that may also contribute to valve calcification, and effects comparable to salt effects with high concentrations of Ca and/or Mg within the calcification site that may also cause a higher temperature dependency of oxygen isotope fractionation.
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New isotopic results on bulk carbonate and mollusc (gastropods and bivalves) samples from Lake Geneva (Switzerland), spanning the period from the Oldest Dryas to the present day, are compared with pre-existing stable isotope data. According to preliminary calibration of modern samples, Lake Geneva endogenic calcite precipitates at or near oxygen isotopic equilibrium with ambient water, confirming the potential of this large lake to record paleoenvironmental and paleoclimatic changes. The onset of endogenic calcite precipitation at the beginning of the Allerod biozone is clearly indicated by the oxygen isotopic signature of bulk carbonate. A large change in delta(13)C values occurs during the Preboreal. This carbon shift is likely to be due to a change in bioproductivity and/or to a `'catchment effect'', the contribution of biogenic CO2 from the catchment area to the dissolved inorganic carbon reservoir of the lake water becoming significant only during the Preboreal. Gastropods are confirmed as valuable for studies of changes in paleotemperature and in paleowater isotopic composition, despite the presence of a vital effect. Mineralogical evidence indicates an increased detrital influence upon sedimentation since the Subboreal time period. On the other hand, stable isotope measurements of Subatlantic carbonate sediments show values comparable to those of pure endogenic calcite and of gastropods (taking into account the vital effect). This apparent disagreement still remains difficult to explain.
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The compounds responsible for the colours and decorations in glass and glazed ceramics include: colouring agents (transition metal ions), pigments (micro-and nano-precipitates of compounds that either do not dissolve or recrystallize in the glassy matrix) and opacifiers (microcrystalline compounds with high light scattering capability). Their composition, structure and range of stability are highly dependent not only on the composition but also on the procedures followed to obtain them. Chemical composition of the colorants and crystallites may be obtained by means of SEM-EDX and WDX. Synchrotron Radiation micro-X-ray Diffraction has a small beam size adequate (10 to 50 microns footprint size) to obtain the structural information of crystalline compounds and high brilliance, optimal for determining the crystallites even when present in low amounts. In addition, in glass decorations the crystallites often appear forming thin layers (from 10 to 100 micrometers thick) and they show a depth dependent composition and crystal structure. Their nature and distribution across the glass/glazes decorations gives direct information on the technology of production and stability and may be related to the color and appearance. A selection of glass and glaze coloring agents and decorations are studied by means of SR-micro- XRD and SEM-EDX including: manganese brown, antimony yellow, red copper lusters and cobalt blue. The selection includes Medieval (Islamic, and Hispano Moresque) and renaissance tin glazed ceramics from the 10th to the 17th century AD.
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Työn ensimmäisenä tarkoituksena oli kartoittaa kiinteä-neste ja neste-neste uuttomenetelmillä pihkan ja valkopihkan määrä Stora Enso Kabelin tuotantolinja 4:llä. Työn kannalta oli myöstärkeää saada selvyys saostumien koostumuksesta. Lopullinen päämäärä oli automatisoida fiksatiivin annostelu uuden, jatkuvatoimisen märänpäänanalysaattorin avulla. Mäntyosuuden kasvattaminen hiokemassassa lisää hydrofobisten partikkeleiden lukumäärää, minkä uskotaan lisäävän saostumariskiä. Työtä varten kehitetty neste-neste uuttomenetelmä, jota ei ole liiemmin paperiteollisuudessa käytetty, voi olla hyvä menetelmä lipofiilisten komponenttien määrän arviointiin tietyssä määrässä massa- tai prosessivesinäytettä. Virtaussytometri-menetelmän avulla tutkittiin pihka- tai valkopihkapartikkeleiden määrää ja kokojakaumaa eri prosessinäytteissä. Virtaussytometri-menetelmällä mitattujen valkopihkapartikkeleiden lukumäärän ja päällystetyn hylyn saostimen suodoksen sameuden välille löytyiselvä korrelaatio. Fiksatiivimäärän vaikutusta päällystetyn hylyn saostimen suodoksen sameuteen tutkittiin koeajojaksolla, jossa fiksatiivin annostelua säädettiin käsin. Käytetyt annosmäärät eivät riittäneet sameuden pitämiseen tasaisena matalalla tasolla.
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Työssä esisuunniteltiin Kemira Pigments Oy:lle uusi titanyylisulfaatin elektrolyyttinen pelkistyslaitos. Suurin syy uuden laitoksen suunnitteluun oli nykyisen laitoksen aiheuttamat korkeat H2SO4-pitoisuudet pelkistyslaitoksen läheisyydessä. Työn kirjallisuusosassa käsitellään elektrolyysilaitteiston suunnitteluun liittyviä seikkoja ja esitellään titanyylisulfaatin elektrolyyttiseen pelkistykseen liittyvää tutkimustietoa. Ennen uuden laitoksen suunnittelua suoritettiin nykyisellä pelkistyslaitoksella koeajoja, joiden tarkoituksena oli antaa lähtötiedot uuden laitoksen suunnittelulle. Koeajot osoittivat mm., että pelkistys on edullisinta suorittaa alhaisella virrantiheydellä n. 300…400 A/m2 ja vesilaimennuksen avulla anolyytin H2SO4-pitoisuus saadaan säädettyä tasolle, jossa titaani ei saostu. Kärynpoistoyhteisiin asennettujen pesuvesisuuttimien avulla saatiin titaanin saostuminen kärynpoistokanaviin estettyä. Uudesta titanyylisulfaatin elektrolyyttisestä pelkistyslaitoksesta laadittiin mm. seuraavat dokumentit: prosessin virtauskaavio ja ainevirtakenttä, PI-kaavio, layout-kuvat laitoksesta ja sen sijoituksesta sekä rakennepiirros elektrolyysialtaasta. Hankkeelle tehtiin kustannusarvio tarkkuudella ±20 %, jonka loppusummaksi saatiin 1 489 000 €. Laitoksen vuotuisten käyttökustannuksien arvioitiin olevan n. 105 000 €. Investoinnista aiheutuvien vuotuisten annuiteettikustannusten arvioitiin olevan n. 237 000 € 16,3 % korolla.
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Työssä tutkittiin, mikä on kustannustehokkain tapa lisätä ilmastuskapasiteettia ja selvitettiin, saostaako vesilaitokselta flotaatioaltaasta poistettava ferrisulfaattisakka jäteveden fosforia esiselkeyttimessä. Työssä määritettiin teoreettinen hapentarve ilmastusaltaassa maksimikuormituksen aikana ja hapensiirtonopeus jäteveteen olemassa olevalla laitteistolla. Hapensiirtonopeuden funktion korjauskertoimet ja sekä kokonaishapensiirtokerroin määritettiin laboratorio-olosuhteissa. Lisäksi laskettiin kuinka paljon nykyisten ilmastimien kautta saadaan happea jäteveteen liukenemaan ja verrattiin tätä lukua teoreettiseen hapentarpeeseen. Jälkimmäistä menettelytapaa käyttäen arvioitiin lisähapen tarve. Tulokseksi saatiin, että maksimi BOD-kuormituksen aikana happea tarvitsee saada jäteveteen liuotettua 5200 m³/d lisää. Ilmastuskapasiteetin lisäyksen kustannuslaskelmassa verrattiin neljää vaihtoehtoa: puhdasta happea liuotettuna happimattojen kautta tai OKI-ilmastimen kautta, onsite-happilaitoksen puhdasta happea liuotettuna OKI-ilmastimen kautta tai ilman happea liuotettuna jäteveteen EDI-ilmastimien kautta. Laskelmat osoittivat uusien EDI-ilmastimien hankinnan olevan edullisin vaihtoehto pitkällä aikavälillä. Vaikka EDI-ilmastimien investointikustannukset ovat korkeat, tulevat ne käyttökustannuksiltaan kaikkein edullisimmaksi. Vesilaitokselta tulevan rautasuolasakan fosforia saostavaa vaikutusta tutkittiin laboratoriossa astiakokein. Näytteet otettiin vesilaitokselta jätevesilaitokselle menevästä rautasuolasakasta sekä esiselkeyttimen kirkasteesta. Näitä eri suhteissa keskenään sekoittamalla saatiin selville, että rautasuolasakka ja sakan mukana tuleva reagoimaton rautasuola saostavat liukoista ja kokonaisfosforia esiselkeytyksessä.
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In this article, we explore the possibility of modifying the silicon nanocrystal areal density in SiOx single layers, while keeping constant their size. For this purpose, a set of SiOx monolayers with controlled thickness between two thick SiO2 layers has been fabricated, for four different compositions (x=1, 1.25, 1.5, or 1.75). The structural properties of the SiO x single layers have been analyzed by transmission electron microscopy (TEM) in planar view geometry. Energy-filtered TEM images revealed an almost constant Si-cluster size and a slight increase in the cluster areal density as the silicon content increases in the layers, while high resolution TEM images show that the size of the Si crystalline precipitates largely decreases as the SiO x stoichiometry approaches that of SiO2. The crystalline fraction was evaluated by combining the results from both techniques, finding a crystallinity reduction from 75% to 40%, for x = 1 and 1.75, respectively. Complementary photoluminescence measurements corroborate the precipitation of Si-nanocrystals with excellent emission properties for layers with the largest amount of excess silicon. The integrated emission from the nanoaggregates perfectly scales with their crystalline state, with no detectable emission for crystalline fractions below 40%. The combination of the structural and luminescence observations suggests that small Si precipitates are submitted to a higher compressive local stress applied by the SiO2 matrix that could inhibit the phase separation and, in turn, promotes the creation of nonradiative paths.
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Työssä pyrittiin selvittämään syitä kipsin saostumiseen ammoniumsulfaattikiteyttämön putkilämmönvaihtimien pinnalle ja miten epätoivottua saostumista voitaisiin estää. Lämmönvaihtimissa virtaa ammoniumsulfaattia, jossa on epäpuhtautena kalsiumia, joka saostuu pinnoille kalsiumsulfaattina. Kirjallisuusosassa tarkasteltiin kiteytymisen mekanismia ja kipsin kiteytymiseen vaikuttavia tekijöitä. Saostumien estoaineita ja niiden vaikutusta kipsin kiteytymiseen sekä kipsin liukoisuutta ammoniumsulfaattiliuoksessa käsiteltiin myös kirjallisuusosassa. Kipsin kiteytymiseen vaikuttavia tekijöitä selvitettiin laboratoriokokeilla, joissa pyrittiin simuloimaan lämmönvaihdinta lämpövastuksella. Laboratoriokokeissa kokeiltiin erilaisia saostuman estoaineita ja pyrittiin löytämään prosessiin mahdollisimman tehokas kipsin kiteytymisen estoaine. Lämmönvaihtimien toiminnan tehokkuutta eli muodostuneen saostuman vaikutusta lämmönsiirtymiseen tutkittiin veden luovuttaman lämpövirran avulla. Lämmönvaihtimien tukkeutumista selvitettiin putkien vaihdon tarpeen perusteella. Kalsiumpitoisuuden vaihteluja prosessivirroissa selvitettiin kalsiumtaseen avulla. Saostumiseen vaikuttavien tekijöiden lisäksi selvitettiin mistä ja kuinka paljon kalsiumia kulkeutuu prosessiin ja poistuu sieltä. Työn tarkoituksena oli löytää ratkaisu, jolla epätoivottua saostumista lämmönvaihdin-ten pinnoille pystyttäisiin vähentämään joko kemiallisesti tai muuttamalla prosessi-muuttujia. Kalsiumia havaittiin olevan eniten pelkistämön sisäisissä ammoniumsul-faattiliuoskierroissa. Kalsiumtaseen perusteella kalsiumia poistuu pelkistämöltä eniten kipsinä ammoniumsulfaattituotteen mukana. Laboratoriokokeissa havaittiin polykar-boksylaattien estävän kipsin kasvua parhaiten, joskin estoaineen oikealla annostuksel-la havaittiin olevan suuri vaikutus. Lämmönvaihtimien saostuman havaittiin olevan kipsin ja glauberiitin seos. Vaippapuolen luovuttamien lämpövirran arvojen perusteel-la pystyttiin seuraamaan putkien tukkeutumista.
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A Cu/Fe granular film, formed from a multilayer film and composed of particles of Fe imbedded in Cu, has had several of its important properties investigated. Measurements include ferromagentic resonance, magnetoresistance, Mössbauer effect, magnetic viscosity, and magnetization. The two‐phase behavior of these immiscible alloy systems, and the effect of multilayering on the shape of the magnetic precipitates, can explain some of these properties. An explanation of the ferromagnetic resonance line shape is proffered. An extraordinary macroscopic quantum tunneling effect is found to govern the magnetic relaxation at the lowest temperatures.
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Brain damage caused by an acute injury depends on the initial severity of the injury and the time elapsed after the injury. To determine whether these two variables activate common mechanisms, we compared the response of the rat medial septum to insult with a graded series of concentrations of a-amino-3-hydroxy-5-methyl-4-isoxazole propionic acid (AMPA) with the time-course effects of a low dose of AMPA. For this purpose we conducted a dose-response study at concentrations of AMPA between 0.27 and 10.8 nmol to measure atrophy of the septal area, losses of cholinergic and GABAergic neurons, astroglial and microglial reactions, and calcification. Cholinergic neurons, whose loss paralleled the degree of septal atrophy produced by AMPA, are more sensitive than GABAergic neurons to the injury produced by AMPA. At doses of AMPA above 2.7 nmol, calcification and the degree of microglial reaction increased only in the GABAergic region of the septal area, whereas atrophy and neuronal loss reached a plateau. We chose the 2.7-nmol dose of AMPA to determine how these parameters were modified between 4 days and 6 months after injection. We found that atrophy and neuronal loss increased progressively through the 6-month study period, whereas astrogliosis ceased to be observed after 1 month, and calcium precipitates were never detected. We conclude that septal damage does not increase with the intensity of an excitotoxic insult. Rather, it progresses continuously after the insult. Because these two situations involve different mechanisms, short-term paradigms are inappropriate for interpreting the pathogenic mechanisms responsible for long-term neurodegenerative processes.
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High-dose carbon-ion-implanted Si samples have been analyzed by infrared spectroscopy, Raman scattering, and x-ray photoelectron spectroscopy (XPS) correlated with transmission electron microscopy. Samples were implanted at room temperature and 500°C with doses between 1017 and 1018 C+/cm2. Some of the samples were implanted at room temperature with the surface covered by a capping oxide layer. Implanting at room temperature leads to the formation of a surface carbon-rich amorphous layer, in addition to the buried implanted layer. The dependence of this layer on the capping oxide suggests this layer to be determined by carbon migration toward the surface, rather than surface contamination. Implanting at 500°C, no carbon-rich surface layer is observed and the SiC buried layer is formed by crystalline ßSiC precipitates aligned with the Si matrix. The concentration of SiC in this region as measured by XPS is higher than for the room-temperature implantation.
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The precise nature of the reaction between chromium chloride and potassium niobate at specific pH levels 12.0, 10.8 and 7.6 has been studied by means of electrometric techniques involving pH and conductometric titrations. The well defined breaks and inflections in the titration curves provide cogent evidence for the formation and precipitation of chromium ortho-Cr2O3.3Nb2 O5, hexa-4Cr2O3.9Nb2 O5 and meta-Cr2O3.3Nb2 O5 niobates in the vicinity of pH 7.5, 6.8 and 5.6, respectively. Analytical investigations of the precipitates have also been carried out which substantiate the results of the electrometric study.