稀土对Al—Mg—Si合金晶体结构参数的影响

在研究和探索稀土对铝合金作用机理的过程中,稀土的良好作用已为越来越多的研究所证实。目前,有关稀土对铝合金宏观组织和性能影响的研究报道较多,但有关稀土对铝合金晶体结构参数的影响报道很少。本文研究了稀土对Al-Mg-Si合金晶体结构参数的影响,可以说,稀土能够提高铝合金的机械性能,在宏观组织上表现为晶粒细化,在微观结构上表现为晶胞参数变小。

STUDY ON DEPOSITION POTENTIALS OF LITHIUM AND SODIUM-IONS AND DEPOLARIZATION IN BINARY CHLORIDE

Deposition potentials of Lithium and Sodium ions have been measured in binary chloride systems (LiCl-KCl, NaCl-KCl) by I-V curve method, to provide a theoretical base for preparing high purity Al-Li alloy by electrolysis in molten salt. The changes of free energy and enthalpy were calculated in terms of depolarization values on Al cathode. Thermodynamic meaning of depolarization was discussed in details and the empirical relation between binary alloy type and depolarization type was proposed. It is shown for the first time that the presence of a third element in Al-Li alloy can strengthen depolarization of Li ion at Al alloy cathode and give foundation for preparing high purity Al-Li-M ternary alloy. The effect of LiCl concentration on deposition potentials of Li ion at Al cathode in KCl-LiCl melt was studied and average active coefficient of LiCl was obtained.

STUDY OF THE CHLORINATION REACTION OF Li2CO3 WITH NH4Cl

The chlorination reaction of Li2CO3 with NH4Cl has been studied in detail by a series of thermal analysis methods. When NH4Cl/Li2CO3 mole ratio equals 4, Li2CO3 can be transformed into LiCl quantitatively in a stream of Ar gas flow. All residual NH4Cl is decomposed completely at 400 degrees C and carried away from the reaction cell by Ar gas.Analysis by X-Ray diffraction and Ion Chromatography show that there are almost no NH4Cl remained in The LiCl product. It is interested that the chlorination reaction can be applied to the determinations of phase diagram by thermal analysis method and the preparation of Al-Li alloy by electrolysis in molten salt.

STUDY ON MEASUREMENT OF DIFFUSION-COEFFICIENT OF LI ATOM IN LIQUID ALUMINUM

The tess potential-concentration curve was first applied to measure the concentration of an alloy. Attempt to use the V-c curve of Al-Li alloy in measuring the diffusion coeffictent of Li atom in liquid aluminium with anode chronopotentiometry at 720℃, was made and D_(Li/Al=4.94×10~(-5)cm~2·s~(-1) was obtained. The value is well consistent wish the theoretical value, D_(Li/Al)=4.85×10~(-5)cm~2·s~(-1) in terms of Stokes-Einstein equation.

Formation of Fe-oxyhydroxides from the East Pacific Rise near latitude 13 degrees N: Evidence from mineralogical and geochemical data

The mineralogical and geochemical characteristics of Fe-oxyhydroxide samples from one dredge station (long. 103 degrees 54.48'W, lat. 12 degrees 42.30'N, water depth 2655 m) on the East Pacific Rise near lat 13 degrees N were analyzed by XRD, ICP-AES, and ICP-MS. Most Fe-oxyhydroxides are amorphous, with a few sphalerite microlites. In comparison with Fe-oxyhydroxides from other fields, the variable ranges in the chemical composition of Fe-oxyhydroxide samples are very narrow; their Fe, Si, and Mn contents were 39.90%, 8.92%, and 1.59%, respectively; they have high Cu (0.88%-1.85%) and Co (65x10(-6)-704x10(-6)) contents, and contain Co+Cu+Zn+Ni > 1.01%. The trace-element (As, Co, Ni, Cu, Zn, Ba, Sr) and major-element (Fe, Ca, Al, Mg) contents of these samples are in the range of hydrothermal sulfide from the East Pacific Rise near 13 degrees N, reflecting that this type of Fe-oxyhydroxide constitutes a secondary oxidation product of hydrothermal sulfide. The Fe-oxyhydroxide samples from one dredge station on the East Pacific Rise near 13 degrees N are lower in Sigma REE (5.44x10(-6)-17.01x10(-6)), with a distinct negative Ce anomaly (0.12-0.28). The Fe-oxyhydroxide samples have similar chondrite-normalized rare-earth-element (REE) patterns to that of seawater, and they are very different from the REE composition characteristics of hydrothermal plume particles and hydrothermal fluids, showing that the REEs of Fe-oxyhydroxide are a major constituent of seawater and that the Fe-oxyhydroxides can become a sink of REE from seawater. The quick settling of hydrothermal plume particles resulted in the lower REE content and higher Mn content of these Fe-oxyhydroxides, which are captured in part of the V and P from seawater by adsorption. The Fe-oxyhydroxides from one dredge station on the East Pacific Rise near 13 degrees N were formed by secondary oxidation in a low temperature, oxygenated environment. In comparison with the elemental (Zn, Cd, Pb, Fe, Co, Cu) average content of hydrothermal sulfide samples from the East Pacific Rise near 13 degrees N, the Zn, Cd, and Pb contents of the Fe-oxyhydroxides are lower, and their Fe, Co, and Cu contents are higher.

华北北缘斜长角闪岩的部分熔融实验及其地质意义

基性岩类的（脱水）部分熔融实验是研究地球内部中酸性岩浆（熔体）形成的重要实验方法，自二十世纪70年代以来越来越受到地质学家的高度重视。华北北缘广泛分布的中生代埃达克质岩石的成因，十几年来引起国内外学者的激烈争论，至今仍没有定论。近年来的研究表明张家口地区同时出露的古老太古宙中基性下地壳岩石、中生代中酸性埃达克质岩浆岩以及汉诺坝基性麻粒岩包体等可能反映了源岩和熔融产物的综合信息，这为我们运用实验岩石学手段研究华北北缘埃达克质岩石成因提供了非常理想的条件。 本文在1.5-2.0GPa，800-1000℃条件下，对采自华北北缘的斜长角闪岩同时进行了块状与粉末状两种样品的部分熔融实验研究，利用电子探针对各实验产物进行了主量元素分析以及利用LA-ICP-MS对部分熔体进行了微量元素测试，进而比较了相同条件下块状和粉末状样品的熔融特征，并对比了实验获得的熔体与华北北缘中生代埃达克质岩石的地球化学特征，同时也将实验获得的残留体与汉诺坝基性麻粒岩包体进行了比较。获得以下主要认识： （1）相同的温度、压力和恒温时间条件下块状样品的熔融温度比粉末样品的更低。在1.5-2.0GPa，800℃时块状斜长角闪岩样品已经发生部分融融，而相同条件下粉末样品中没有观察到熔体，粉末样品的部分熔融发生在850℃左右。在850-1000℃温度范围内，相同条件下块状样品的熔体含量比粉末样品的熔体含量高出5-17vol.％，即相同条件下块状样品比粉末样品的熔融程度更高，说明块状样品更容易达到可以分凝形成岩浆的临界熔体分数（CMF），这可能暗示着自然界中的岩浆形成可能比以往通过粉末实验结果推测的更容易发生。此外，在较高的温度条件下（950-1000℃），块状样品与粉末样品的熔体在主量和微量元素上都具有大致相同的地球化学特征，可以认为二者在在岩石学应用上是等效的。 （2）1.5GPa下实验获得的熔体为花岗质－花岗闪长质熔体，850-1000℃熔体的主-微量元素的地球化学特征与华北北缘中生代埃达克质岩石的整体特征具有很好的相似性，并与实验原岩产地张家口地区的三个典型中酸性埃达克质岩体的地球化学特征类似。可以认为实验的斜长角闪岩在1.5GPa下部分熔融能够形成华北北缘中生代埃达克质岩石。2.0GPa下的实验熔体为花岗质－奥长花岗质成分，其主量和微量元素特征均与华北北缘埃达克质岩石存在较大的差别，说明该压力下不能够形成华北北缘埃达克质岩石。 （3）实验残留相主要组成为Hb+Cpx+Gt±Pl，相当于麻粒岩相或榴辉岩相的矿物组合。与汉诺坝基性麻粒岩包体的典型矿物组合Cpx+Opx+Pl存在较大差别，在化学成分上，残留相比麻粒岩包体也整体上富Fe、Al，而贫Mg、Ca。综合来看汉诺坝基性麻粒岩包体可能是多种源岩在相对低压的条件下经过多期部分熔融综合作用的结果，本次实验的原岩及条件难以完全解释其复杂的成因。 另外，针对实验熔体和华北北缘埃达克质岩石之间的一些差异，不排除可能同时存在其他与之类似的源岩，成分上具有相对富Mg、Ca而贫Fe、Al，以及不同程度的Th、U、Zr、Hf富集等特征，与斜长角闪岩一起部分熔融，共同形成中生代华北北缘的中酸性埃达克质岩石。

喀拉通克含矿岩体（Y2）的岩石学研究

从主元素化学来看，喀拉通克深成岩以低Ca、Al为特征，而火山岩（玄武岩类）以高Ca、Al为特征；在早期结晶矿物组合上，喀拉通克深成岩为橄榄石、斜方辉石和基性斜长石，而火山岩中斑晶以基性斜长石、背地里斜辉石为主，其次为橄榄石，没有见到斜方辉石斑晶，在Sr-Zr图和Nd-Zr图中二者具有较大差别。利用矿物温度计计算了橄榄石、辉石和斜长石的结晶温度。橄榄石是在稍高于1880℃下开始结晶的，二辉石共存时的温度为1100℃左右，基性斜长石的结晶温度也在1100℃左右，并定性讨论了二号岩体的水含量和氧逸度。比较详细地从定性和定量两方面探讨了岩体成岩压力范围，认为前人计算的7Kb过大。根据橄榄石和斜长石共存现象说明压力小于7Kb，单斜辉石中的铝含量进一步说明压力小于5Kb，最后半定量地利用角闪石地质压力计说明4Kb作为二号岩体的成岩压力是比较可信的。最后探讨了二号岩体所属系列和分异趋势。许多证据表明二号岩体属于钙碱系列岩体，比如结晶矿物类型和顺序等符合obsorn(1962)建立的造山带钙碱系列；在SiO2-K2O图和AFM图中皆落入钙碱系列；辉石的成分变化不具有富铁趋势；所有岩石都有一定量的角闪石；微量元素如Rb、K/Rb、Zr等以及稀土模式与岛弧钙碱岩浆相似。与世界著名钙碱系列岩体比较表明，它们共同的特征是产于造山带环境，岩石都有一定量的含水矿物存在，说明母岩浆富水对于钙碱系列的形成具有重要的作用。若将造岩矿物的成分变化范围投影到AFM图中，可以看出造成二号岩体如此钙碱系列演化线的原因在于岩石中橄榄石和辉石的富铁趋势很弱、岩石中含有较多的黑云母和角闪石以及随着分异进行结晶出越来越多的长石。二号岩体高Si、H2O，低Ca、Al的特征决定了二号岩体的矿物结晶顺序为橄榄石→斜方辉石→拉长石→单斜辉石→角闪石→黑云母，形成相应的岩相为橄榄苏长岩、苏长岩、辉长岩和闪长岩相。辉石的Mg~#值变化很窄，是由于二号岩体含水量较高，使辉石在高En值下停止结晶，而为含水矿物角闪石取代。以上通过对喀拉通克含矿岩体（Y2）的岩石学研究，可以得到如下结论：一、喀拉通克含矿岩体由橄榄苏长岩、苏长岩、辉长岩和闪长岩四个岩相组成。各个岩相是由同一母岩浆经分异形成的。岩体岩相的反环带结构说明岩体不可能是由均匀岩浆一次侵位就地分异形成，而是岩浆深部分异与构造活动结合的产物。二、喀拉通克含矿岩体的母岩浆是产于造山带的一种钙碱性岩浆，以高Si、H2O，低Ca、Al为特征，其母岩浆不z可能是科马提岩、洋中脊拉斑玄武岩、高铝玄武岩或碱性玄武岩浆中的任一种。三、喀拉通克含矿深成岩和该区火山岩在主元素、微量元素及矿物晶出顺序方面存在一定差异，这种差异不大可能是由结晶环境不同造成的，更可能的是两者起源于不同的母岩浆。四、从定性和定量两方面讨论了喀拉通克含矿岩体的成岩压力，从而将4Kb作为该岩体的成岩压力是比较可信的。五、从岩体分异趋势来看，喀拉通克含矿岩体属于钙碱系列岩体。造成钙碱系列分异趋势的主要原因在于岩石中橄榄石和辉石的富铁趋势很弱，岩石含有较多的黑云母和角闪石以及随着分异进行结晶出越来越多的长石。对于以上分异趋势的形成，岩浆富水起着较大的作用。富水一方面使辉石在高En值下停止结晶，以角闪石代替；另一方面使岩浆的氧逸度有所提高。

Étude critique de la densité électronique et des températures (excitation et ionisation) d'un plasma d'aluminium induit par laser

La caractérisation de matériaux par spectroscopie optique d’émission d’un plasma induit par laser (LIPS) suscite un intérêt qui ne va que s’amplifiant, et dont les applications se multiplient. L’objectif de ce mémoire est de vérifier l’influence du choix des raies spectrales sur certaines mesures du plasma, soit la densité électronique et la température d’excitation des atomes neutres et ionisés une fois, ainsi que la température d’ionisation. Nos mesures sont intégrées spatialement et résolues temporellement, ce qui est typique des conditions opératoires du LIPS, et nous avons utilisé pour nos travaux des cibles binaires d’aluminium contenant des éléments à l’état de trace (Al-Fe et Al-Mg). Premièrement, nous avons mesuré la densité électronique à l’aide de l’élargissement Stark de raies de plusieurs espèces (Al II, Fe II, Mg II, Fe I, Mg I, Halpha). Nous avons observé que les densités absolues avaient un comportement temporel différent en fonction de l’espèce. Les raies ioniques donnent des densités électroniques systématiquement plus élevées (jusqu’à 50 % à 200 ns après l’allumage du plasma), et décroissent plus rapidement que les densités issues des raies neutres. Par ailleurs, les densités obtenues par les éléments traces Fe et Mg sont moindres que les densités obtenues par l’observation de la raie communément utilisée Al II à 281,618 nm. Nous avons parallèlement étudié la densité électronique déterminée à l’aide de la raie de l’hydrogène Halpha, et la densité électronique ainsi obtenue a un comportement temporel similaire à celle obtenue par la raie Al II à 281,618 nm. Les deux espèces partagent probablement la même distribution spatiale à l’intérieur du plasma. Finalement, nous avons mesuré la température d’excitation du fer (neutre et ionisé, à l’état de trace dans nos cibles), ainsi que la température d’ionisation, à l’aide de diagrammes de Boltzmann et de Saha-Boltzmann, respectivement. À l’instar de travaux antérieurs (Barthélémy et al., 2005), il nous est apparu que les différentes températures convergeaient vers une température unique (considérant nos incertitudes) après 2-3 microsecondes. Les différentes températures mesurées de 0 à 2 microsecondes ne se recoupent pas, ce qui pourrait s’expliquer soit par un écart à l’équilibre thermodynamique local, soit en considérant un plasma inhomogène où la distribution des éléments dans la plume n’est pas similaire d’un élément à l’autre, les espèces énergétiques se retrouvant au cœur du plasma, plus chaud, alors que les espèces de moindre énergie se retrouvant principalement en périphérie.

Mecanismos de desgaste, história térmica e ciclo de vida de componentes de um motor de combustão interna de aeromodelo

We developed an assay methodology that considered the temperature variation and the scanning electron microscopy as a method to quantify and characterize respectively the consumption evolution in three 46 LA machines, with internal combustion and two-stroke engines, 7.64 cm3 cylinder capacity, 23.0 millimeters diameter and 18.4 millimeters course, RPM service from 2.000 to 16.000 rpm, 1.2 HP power, and 272 grams weight. The investigated engines components were: (1) head of the engine (Al-Si alloy), (2) piston (Al-Si alloy) and (3) piston pin (AISI 52100 steel). The assays were carried out on a desktop; engines 1 and 2 were assayed with no load, whereas in two assays of engine 3 we added a fan with wind speed that varied from 8.10 m/s to 11.92 m/s, in order to identify and compare the engine dynamic behavior as related to the engines assayed with no load. The temperatures of the engine s surface and surroundings were measured by two type K thermopairs connected to the assay device and registered in a microcomputer with data recording and parameters control and monitoring software, throughout the assays. The consumed surface of the components was analyzed by scanning electron microscopy (SEM) and microanalysis-EDS. The study was complemented with shape deformation and mass measurement assays. The temperature variation was associated with the oxides morphology and the consumption mechanisms were discussed based on the relation between the thermal mechanical effects and the responses of the materials characterization

Efeito no processo ECAP (EQUAL CHANNEL ANGULAR) na microestrutura e nas propriedades mecânicas de uma liga comercial de alumínio AA3104

Pós-graduação em Engenharia Mecânica - FEG

Interações de alguns ácidos orgânicos com minerais e um latossolo vermelho

Pós-graduação em Agronomia (Energia na Agricultura) - FCA

Verificação da qualidade da água e dos sedimentos no rio Tietê entre as barragens de Promissão e Ibitinga

Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES)

Novel estimation of the humification degree of soil organic matter by laser-induced breakdown spectroscopy

Soil organic matter (SOM) constitutes an important reservoir of terrestrial carbon and can be considered an alternative for atmospheric carbon storage, contributing to global warming mitigation. Soil management can favor atmospheric carbon incorporation into SUM or its release from SOM to atmosphere. Thus, the evaluation of the humification degree (HD), which is an indication of the recalcitrance of SOM, can provide an estimation of the capacity of carbon sequestration by soils under various managements. The HD of SOM can be estimated by using various analytical techniques including fluorescence spectroscopy. In the present work, the potential of laser-induced breakdown spectroscopy (LIBS) to estimate the HD of SUM was evaluated for the first time. Intensities of emission lines of Al, Mg and Ca from LIBS spectra showing correlation with fluorescence emissions determined by laser-induced fluorescence spectroscopy (LIFS) reference technique were used to obtain a multivaried calibration model based on the k-nearest neighbor (k-NN) method. The values predicted by the proposed model (A-LIBS) showed strong correlation with LIFS results with a Pearson's coefficient of 0.87. The HD of SUM obtained after normalizing A-LIBS by total carbon in the sample showed a strong correlation to that determined by LIFS (0.94), thus suggesting the great potential of LIBS for this novel application. (C) 2014 Elsevier B.V. All rights reserved.

Electrochemical studies of copper, copper-aluminium and copper-aluminium-silver alloys: Impedance results in 0.5M NaCl

The electrochemical behaviour of Cu, Cu-Al and Cu-Al-Ag alloys in aqueous solutions of NaCl (0.5 M, pH = 3.00) was studied by means of voltammetric methods and electrochemical impedance spectroscopy. The surfaces were examined by SEM and EDX analysis. Cu-Al-Ag alloy shows a potentiodynamic behaviour similar to that of the pure copper electrode while the Cu-Al alloy presents some minor differences. In the active dissolution region the electrodes suffer pitting corrosion and in the other potential regions there are the formation of a passivant film with composition depending on the potential. The impedance responses of the electrodes are discussed. An electrodissolution mechanism is proposed and the effect of the alloying elements upon the impedance response and polarisation curves is explained. The main effects are due to the production of copper and silver chlorides and aluminium oxides/ hydroxides at the corroding interface. The addition of Al or (Al + Ag) increases the corrosion resistance of pure copper. © 1995.

SOLUTE-DERIVED THERMAL STABILITY OF NANOCRYSTALLINE ALUMINUM AND PROCESSING FACTOR INFLUENCE ON THE FORMATION OF AL6MN QUASICRYSTALS IN MELT-SPINNING

Thermal stability of nanograined metals can be difficult to attain due to the large driving force for grain growth that arises from the significant boundary area constituted by the nanostructure. Kinetic approaches for stabilization of the nanostructure effective at low homologous temperatures often fail at higher homologous temperatures. Thermodynamic approaches for thermal stabilization may offer higher temperature stability. In this research, modest alloying of aluminum with solute (1 at.% Sc, Yb, or Sr) was examined as a means to thermodynamically stabilize a bulk nanostructure at elevated temperatures. After using melt-spinning and ball-milling to create an extended solid-solution and nanostructure with average grain size on the order of 30-45 nm, 1 h annealing treatments at 673 K (0.72 Tm) , 773 K (0.83 Tm) , and 873 K (0.94 Tm) were applied. The alloys remain nanocrystalline (<100 nm) as measured by Warren-Averbach Fourier analysis of x-ray diffraction peaks and direct observation of TEM dark field micrographs, with the efficacy of stabilization: Sr>Yb>Sc. Disappearance of intermetallic phases in the Sr and Yb alloys in the x-ray diffraction spectra are observed to occur coincident with the stabilization after annealing, suggesting that precipitates dissolve and the boundaries are enriched with solute. Melt-spinning has also been shown to be an effective process to produce a class of ordered, but non-periodic crystals called quasicrystals. However, many of the factors related to the creation of the quasicrystals through melt-spinning are not optimized for specific chemistries and alloy systems. In a related but separate aspect of this research, meltspinning was utilized to create metastable quasicrystalline Al6Mn in an α-Al matrix through rapid solidification of Al-8Mn (by mol) and Al-10Mn (by mol) alloys. Wheel speed of the melt-spinning wheel and orifice diameter of the tube reservoir were varied to determine their effect on the resulting volume proportions of the resultant phases using integrated areas of collected x-ray diffraction spectra. The data were then used to extrapolate parameters for the Al-10Mn alloy which consistently produced Al6Mn quasicrystal with almost complete suppression of the equilibrium Al6Mn orthorhombic phase.