208 resultados para AQUEOUS TWO-PHASE SYSTEM
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The dependence of the structure of the hosts on the M ion radius in MMgAl10O17 (M = Be, Mg, Ca, Sr, Ba, Pb, Eu, Mn, Fe, Co, Ni, Zn, Cd, Sn) system was studied and the luminescence of Eu2+ the mixed phase system was discussed. When M ion radius is less than 0.10 nm, the system MMgAl10O17 constructs by the mixed phases consisting of manegtoplumbite and spinel, alpha-alumina or spinel and alpha-alumina. In the mixed phase of manegtoplumbite and spinel and alpha-alumina, Eu2+ ion preferentially occupies lattice site of the cations in manegtoplumbite well matched with the radius and charge of Eu2+. There exists only d-->f transition emission of Eu2+ and no characteristic emission of Eu3+ occurs in those hosts. In the mixed phase of spinel and alpha-alumina, Eu2+ can enter the lattice site of Mg2+ ion or Al3+ ion and the d-->f and f-->f transition of Eu2+ can been observed respectively. Meanwhile, since the radius and charge of matrix lattice ions substituted by Eu2+ do not match with those of Eu2+, the valence state of Eu2+ is unstable. Eu2+ is partly changed into Eu3+ and the emission of Eu3+ is obviously observed even under the condition of reduction atmosphere. If reaction temperature is more than 1 150 degrees C, Al2O3 forms alpha-Al2O3 structure, the f-->f transition of Eu2+ appears. If reaction temperature is less than 1 150 degrees C, a mixed phase of alpha-Al2O3 and gamma-Al2O3 is formed, the f-->f transition of Eu2+ disappears and a new band emission from d-->f transition of Eu2+ occurs.
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A blend of polyethersulfone (PES) and polycarbonate (PC) with a ratio of 40/60 was studied by scanning electron microscopy (SEM), dynamic mechanical analysis, and transmission electron microscopy (TEM). It was found that the PES-PC blend is a partially miscible, two-phase system, and an interfacial layer exists between the phases of PES and PC. Specific interaction resulting from the n-complex between PES and PC provides the driving force for formation of the interfacial layer. In addition, phase inversion behavior was also observed for the 40/60 composition.
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Interfacial waves propagating along the interface between a three-dimensional two-fluid system with a rigid upper boundary and an uneven bottom are considered. There is a light fluid layer overlying a heavier one in the system, and a small density difference exists between the two layers. A set of higher-order Boussinesq-type equations in terms of the depth-averaged velocities accounting for stronger nonlinearity are derived. When the small parameter measuring frequency dispersion keeping up to lower-order and full nonlinearity are considered, the equations include the Choi and Camassa's results (1999). The enhanced equations in terms of the depth-averaged velocities are obtained by applying the enhancement technique introduced by Madsen et al. (1991) and Schaffer and Madsen (1995a). It is noted that the equations derived from the present study include, as special cases, those obtained by Madsen and Schaffer (1998). By comparison with the dispersion relation of the linear Stokes waves, we found that the dispersion relation is more improved than Choi and Camassa's (1999) results, and the applicable scope of water depth is deeper.
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This paper considers interfacial waves propagating along the interface between a two-dimensional two-fluid with a flat bottom and a rigid upper boundary. There is a light fluid layer overlying a heavier one in the system, and a small density difference exists between the two layers. It just focuses on the weakly non-linear small amplitude waves by introducing two small independent parameters: the nonlinearity ratio epsilon, represented by the ratio of amplitude to depth, and the dispersion ratio mu, represented by the square of the ratio of depth to wave length, which quantify the relative importance of nonlinearity and dispersion. It derives an extended KdV equation of the interfacial waves using the method adopted by Dullin et al in the study of the surface waves when considering the order up to O(mu(2)). As expected, the equation derived from the present work includes, as special cases, those obtained by Dullin et al for surface waves when the surface tension is neglected. The equation derived using an alternative method here is the same as the equation presented by Choi and Camassa. Also it solves the equation by borrowing the method presented by Marchant used for surface waves, and obtains its asymptotic solitary wave solutions when the weakly nonlinear and weakly dispersive terms are balanced in the extended KdV equation.
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本论文内容主要分为4个部分:“有机锗化合物抑制Maillard反应的研究”、“Ge-132对体外培养幼鼠胰岛细胞的作用研究”、“PEG/磷酸盐双水相体系中生物大分子分配的研究”和“HPCPC(High Performance Centrifugal Partition Chromatography,高效离心分配色谱)双水相体系对生物大分子分离的研究”。前两部分主要从有机锗化合物防治糖尿病及其并发症的代谢机理和细胞学角度进行研究,本文引入HPCPC和双水相体系分离生物大分子的技术,为进一步阐明有机锗化合物在Maillard反应过程中的作用机理:对双水相体系中生物大分子的分配及HPCPC在双水相体系中分离生物大分子也做了大量的基础性研究,为开发HPCPC的应用作出了有价值的探索工作。本论文的主要创新点归纳如下:一、有机锗化合物对Maillard反应的抑制作用:针对国际上有机锗发展的前沿课题,在国内首先开展了有机锗化合物对Maillard反应抑制作用的研究,取得了有价值的研究结果。1、在模拟体内的生理条件下,研究了不同浓度Ge-132对精氨酸、组氨酸、甘氨酸和缬氨酸对Maillard反应荧光峰强度的影响:不同类型的氨基酸Maillard反应产物结构上的差异和不同浓度有机锗对组氨酸糖化反应420nm处特征吸光度的影响。2、苯丙氨酸是侧链带有苯环的芳香族氨基酸,是一种具有弱的天然荧光的生物小分子,其荧光最大发射位置在281.6nm。由于aillard反应是葡萄糖和氨基酸的-NHR基发生的反应,其反应产物的特征荧光在440nm附近。这两类荧光的发射位置相差较远,相互之间没有影响,因此利用荧光法观察Phe在反应过程中自身的荧光变化和Ge-132对Phe的Maillard反应荧光产物的抑制情况。3、血清白蛋白是哺乳动物体内的重要蛋白质,可作为多种内源性、外源性物质的存储和转运蛋白,其Maillard反应已经被广泛重视,但较复杂的实验条件限制了它的研究。通过观测蛋白质Maillard反应产物特征荧光的变化是一有效的研究方法。BSA的内源性荧光是由肽链色氨酸和酪氨酸残基贡献的,其最大发射位置340nm左右。其Maillard反应产物的特征荧光在440nm附近,这两类荧光发射位置相差较远,基本上没有影响,因此能够通过荧光光谱研究BSA的Maillard反应荧光产物的情况。本文观测了Ge-132对BSA的Maillard反应荧光产物的抑制作用,同时还通过荧光法确定了一个文献中没有的新的反应位点。4、本文研究了具有更高水溶性的一类双有机锗化合物(HO)_2Ge(CHR_1CHR_2COOH)_2.2H_20抑制Maillard反应的特性,结果证明它比Ge-132具有更高的抑制作用,我们通过化合物的构效关系解释了上述作用的机制。5、本文研究了Tb(Ge-132)_3和Eu(Ge-132)_3两种含稀土的配合物对氨基酸、蛋白质Maillard反应的影响,观察了稀土离子对Maillard反应体系的影响,对实验现象作出了合理的解释。二、Ge-132对体外培养幼鼠胰岛细胞的作用为进一步考察有机锗对糖尿病的防治作用,我们与白求恩医大合作,首次观察了Ge-132对体外培养的幼鼠胰岛细胞结构和功能的影响,研究了不同剂量的含锗化合物对幼鼠胰岛细胞分泌胰岛素的作用,认为低浓度的Ge-132对胰岛细胞分泌胰岛素具有明显的促进作用。该部分内容为首次报导。三、PEG/磷酸盐双水相体系中生物大分子分配的研究双水相萃取TPE(Aqueous Two-Phase Extraction)具有下述优点:生物相容性好、界面张力低、能量低、易于工业规模的放大、可以进行连续操作等。本论文系统地研究了各种蛋白质在PEG/磷酸盐体系中的分离情况,如在各种pH条件下,从6.8到9.2,各种分子量的PEG,包括PEGl000,2000,5000,6000,10000,和20000和磷酸盐双水相体系的物化性质,以及对lysozyme(溶菌酶),BSA(牛血清白蛋白),HSA(人血清白蛋白),Hemoglobin(血红蛋白)在各种体系中的分配系数,探讨了各种因素对生物大分子分配的影响。四、HPCPC在双水相体系对生物大分子分离的研究由于荧光光谱法证实了Ge-132对牛血清白蛋白Maillard反应的抑制作用。但对于如何能够分离出糖化产物,达到进行定量表征的目的是我们研究的一个重要内容。九十年代初,由日本研制出一种色谱中新技术HPCPC。HPCPC与传统的液相色谱(LC)和高效液相色谱(HPLC)不同,不需要固体作为支持体。流动相和固定相分别为两种不相混溶的液体,通过离心力的作用使其中一相作为固定相保持在类似多级萃取器的微小分配槽中,另一相作为流动相流经固定相。HPCPC在双水相体系的应用是一种利用多级连续萃取从双水相中分离生物物质的方法它具有运行时间快、高效高选择性,流动相与固定相之间比例可以任意改变,并在任何pH值均可进行正向和反向操作并且实验室规模可一步直接放大到生产规模。它不仅可以作为一种分离的工具,而且也是一种研究生物萃取反应动力学机理,反映热力学与动力学之间相关性的重要方法。本论文中研究了常用的两种双水相体系,利用PEG6000/Dex20000/H_20对BSA和Maillard反应产生的糖化BSA进行了初步分离,取得了一些阶段性结论。另外,通过对各种条件的筛选,选择了具有代表性的lysozyme和BSA,BSA和血红蛋白(Hb)进行HPCPC色谱仪上的分离,研究了色谱分离条件如:转数、流速、pH等对分离效率及理论塔板数的影响,取得了一系列重要的结论。为工业上大规模的生物样品分离提供了重要的参数。
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The interface thickness in two-component interpenetrating polymer networks (IPN) system based on polyacrylate and epoxy were determined using small-angle X-ray scattering (SAXS) in terms of the theory proposed by Ruland. The thickness was found to be nonexistent for the samples at various compositions and synthesized at variable conditions-temperature and initiator concentration. By viewing the system as a two-phase system with a sharp boundary, the roughness of the interface was described by fractal dimension, D, which slightly varies with composition and synthesis condition. Length scales in which surface fractals are proved to be correct exist for each sample and range from 0.02 to 0.4 Angstrom(-1). The interface in the present IPN system was treated as fractal, which reasonably explained the differences between Pored's law and experimental data, and gained an insight into the interaction between different segments on the interface. (C) 1997 Elsevier Science Ltd.
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To attempt to control the quantum state of a physical system with a femtosecond two-colour laser field, a model for the two-level system is analysed as a first step. We investigate the coherent control of the two-colour laser pulses propagating in a two-level medium. Based on calculating the influence of the laser field with various laser parameters on the electron dynamics, it is found the electronic state can be changed up and down by choosing the appropriate laser pulses and the coherent control of the two-colour laser pulses can substantially modify the behaviour of the electronic dynamics: a quicker change of two states can be produced even for small pulse duration. Moreover, the oscillatory structures around the resonant frequency and the propagation features of the laser pulses depend sensitively on the relative phase of the two-colour laser pulses. Finally, the influence of a finite lifetime of the upper level is discussed in brief.
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The present paper reports a study of the extraction of HNO3 with Cyancx923 (C923)-n-heptane. A third phase appears at different aqueous HNO3 concentrations for various initial C923 concentrations. Data analysis indicates that almost all of HNO3 and H2O are extracted into the middle phase. More HNO3 and water at a fixed ratio are solubilized in the reverse micelles or microemulsion in the third phase, which leads to a sharp increase of their concentration. The effect of temperature on the phase behavior of the three-phase system has also been investigated.
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Presented is an experimental study on the performance of an oil-gas multiphase transportation system, especially on the multiphase flow patterns, multiphase pumping and multiphase metering of the system. A dynamic simulation analysis is conducted to deduce simulation parameters of the system and similarity criteria under simplified conditions are obtained. The reliability and feasibility of two-phase flow experiment with oil and natural gas simulated by water and air are discussed by using the similarity criteria.
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In the present paper, we endeavor to accomplish a diagram, which demarcates the validity ranges for interfacial wave theories in a two-layer system, to meet the needs of design in ocean engineering. On the basis of the available solutions of periodic and solitary waves, we propose a guideline as principle to identify the validity regions of the interfacial wave theories in terms of wave period T, wave height H, upper layer thickness d(1), and lower layer thickness d(2), instead of only one parameter-water depth d as in the water surface wave circumstance. The diagram proposed here happens to be Le Mehautes plot for free surface waves if water depth ratio r = d(1)/d(2) approaches to infinity and the upper layer water density rho(1) to zero. On the contrary, the diagram for water surface waves can be used for two-layer interfacial waves if gravity acceleration g in it is replaced by the reduced gravity defined in this study under the condition of sigma = (rho(2) - rho(1))/rho(2) -> 1.0 and r > 1.0. In the end, several figures of the validity ranges for various interfacial wave theories in the two-layer fluid are given and compared with the results for surface waves.
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On the basis of a brief review of the continuum theory for macroscopic descriptions and the kinetic theory for microscopic descriptions in solid/liquid two-phase flows, some suggestions are presented, i.e. the solid phase may be described by the Boltzmann equation and the liquid phase still be described by conservation laws in the continuum theory. Among them the action force on the particles by the liquid fluid is a coupling factor which connects the phases. For dilute steady solid/liquid two-phase flows, the particle velocity distribution function can be derived by analogy with the procedures in the kinetic theory of gas molecules for the equilibrium state instead of being assumed, as previous investigators did. This done, more detailed information, such as the velocity probability density distribution, mean velocity distribution and fluctuating intensity etc. can be obtained directly from the particle velocity distribution function or from its integration. Experiments have been performed for dilute solid/liquid two-phase flow in a 4 x 6 cm2 sized circulating square pipe system by means of laser Doppler anemometry so that the theories can be examined. The comparisons show that the theories agree very well with all the measured data.
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The generation of attosecond pulses in a two-level system with permanent dipole moment is investigated. It is shown due to the presence of permanent dipole moments, that the plateau of the high-order harmonic generation spectrum can be extended to X-ray range. Moreover, attosecond pulses with higher intensity can be synthesized by using both even and odd harmonics because of their quantum interference. (c) 2006 Elsevier B.V. All rights reserved.
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A study of potassium ion transfer across a water \ 1,2-dichloroethane (W \ DCE) interface facilitated by dibenzo-18-crown-6 (DB18C6) with various phase volume ratio systems is presented. The key point was that a droplet of aqueous solution containing a redox couple, Fe(CN)(6)(3-)/Fe(CN)(6)(4-), with equal molar ratio, was first attached to a platinum electrode surface, and the resulting droplet electrode was then immersed into the organic solution containing a hydrophobic electrolyte to construct a platinum electrode/aqueous phase/organic phase system. The interfacial potential of the W \ DCE within the series could be externally controlled because the specific compositions in the aqueous droplet make the Pt electrode function like a reference electrode as long as the concentration ratio of Fe(CN)(6)(3-)/Fe(CN)(6)(4-) remains constant. In this way, a conventional three-electrode potentiostat can be used to study the ion transfer process at a liquid \ liquid (L \ L) interface facilitated by an ionophore with variable phase volume ratio (r = V-o/V-w). The effect of r on ion transfer and facilitated ion transfer was studied in detail experimentally. We also demonstrated that as low as 5 x 10(-8) M DB18C6 could be determined using this method due to the effect of the high phase volume ratio.
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Bayan Obo REE-Nb-Fe ore deposit is the largest REE deposit in the world. Owing to its unique type and tremendous economic value, this deposit has widely attracted interests from geological researchers and vast amount of scientific data have been accumulated. However, its genesis, especially ore-forming age and REE sources, have been under dispute for a long time. On the basis of previous research works, this paper mainly conducts studies on the Early Paleozoic ore-forming event in the Bayan Obo deposit. The following results and conclusions can be suggested: Sm-Nd isotopic analytical results of bastnaesite, beloeilite, albite and fluorite samples from a coarse-crystalline ore lode present an isochron age of 436±35Ma. Besides, Rb-Sr isotope dating of the coarse-crystalline biotite lode that intruded into banded ores gives an isochron age of 459±39Ma. The two ages verify the exist of Early Paleozoic ore-forming event at Bayan Obo, which characterized by extensive netted mineralization of REE fluorocarbonates, aeschynite and monazite, accompanied by widely fluorite-riebeckite-aegirine-apatite alteration. Sr-Nd isotope composition of vein minerals is located between EMI and ancient lower crust component in the ISr(t)-εNd(t) correlation diagram, indicating that there is a crustal contamination during veined mineralization. A large area late Paleozoic granitoids are distributed in the southeast region of east open pit of the mine. The granitoids intruded directly into the ore-bearing dolomite, and produced intense skarnization. Moreover, at 650-660m of the drill core on 22 line and 1598m level flat in the south of East Open Pit, we firstly found skarnization rocks. Single grain and low background Rb-Sr isochrone dating on phlogopite in skarn gives 309±12Ma. Considering the intruded contacting relationship, the late Paleozoic granitoids, already extended to the under part of REE ore bodies, must be posterior to the latest intense REE mineralization, and is only a destructive tectonic and magmatic activity. Fluid inclusion types of fluorite in the Bayan Obo deposit consist of multiphase daughter mineral-bearing inclusion, two or three phase CO2-bearing inclusion and two phase aqueous inclusion. Petrography, laser Raman analysis and microthermometry study indicate that the fluids involving in REE-Nb-Fe mineralization at Bayan Obo might be mainly of H2O-CO2-NaCl-(F-REE) system. The presence of REE-carbonate as a daughter mineral in fluid inclusions shows that the original ore-forming fluids are rich in REE elements.