979 resultados para Amherst, Jeffery Amherst, 1st Baron, 1717-1797.


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The analytical expressions of quasi-first and second order homogeneous catalytic reactions with different diffusion coefficients at ultramicrodisk electrodes under steady state conditions are obtained by using the reaction layer concept. The method of treatment is simple and its physical meaning is clear. The relationship between the diffusion layer, reaction layer, the electrode dimension and the kinetic rate constant at an ultramicroelectrode is discussed and the factor effect on the reaction order is described. The order of a catalytic reaction at an ultramicroelectrode under steady state conditions is related not only to C(Z)*/C(O)* but also to the kinetic rate constant and the dimension of the ultramicroelectrode; thus the order of reaction can be controlled by the dimension of the ultramicroelectrode. The steady state voltammetry of the ultramicroelectrode is one of the most simple methods available to study the kinetics of fast catalytic reactions.

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The conditions for quasi-first and second order homogeneous catalytic reactions and their variation with each other at an ultramicrodisk electrode in the steady state are discussed in this paper. The order of reaction can be controlled by changing the dimension of the ultramicroelectrode: the second order reaction can be changed to quasi-first by decreasing the dimension of the ultramicroelectrode. An example of this is given. The main factor effect on the reaction order is the dimension of the ultramicroelectrode. The K4Fe(CN)6-aminopyrine system is selected to confirm the theory, the experiments showing that the system is a second order reaction at a 432 mum microelectrode, and a quasi-first order reaction at a 19 mum ultramicroelectrode. The kinetic constant of the system can be determined by applying the previous theory of homogeneous catalytic reaction.

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The reaction of EuCl3, AlCl3 and C6Me6 in toluene gives the Eu(II) complex [Eu(eta-6-C6Me6)(AlCl4)2]4; X-ray crystal determination shows the molecule to be a cyclotetramer, in which the four Eu(C6Me6)AlCl4 units are connected via four groups of eta-2-AlCl4.

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自然界水体(如地下水、湖泊、河流及海洋)中的天然有机质(NOM)因具有显著的生态及环境功能而受到人们的广泛关注。NOM作为全球碳循环的主要组成部分,是水体中异养型微生物生长所需碳及能量的重要来源。此外,NOM对湖泊生态系统中的多种物理、化学过程具有不同程度的影响:NOM中的有机酸对淡水体系的酸度具有控制作用而且对酸沉降有一定的缓冲作用;NOM通过减弱可见光及紫外线照射从而影响淡水系统的光化学环境,这一方面降低了水体中自养生物的繁衍速度,同时保护水生生物免受有害的紫外线辐射。更为重要的是,NOM能够影响环境中污染物的命运,比如重金属离子和疏水性有机污染物与天然有机质结合后,其迁移途径、溶解度、生物可利用性及毒性受到明显的控制,这样其对环境中生物的危害性减弱。多环芳烃(PAHs)是一类对环境危害极大的疏水性有机污染物,多数PAHs对有机体具有毒性和致癌性而被美国环保署(EPA)列为优先处理的污染物。因此,确定NOM-PAHs反应的强弱,即PAHs在NOM中的分配系数(Kdoc)以及NOM的物化特性对Kdoc的影响对于预测PAHs毒性和生物可利用性大小、了解NOM-PAHs相互作用的机理及确立污染预测模型具有十分重大的意义。前人的研究结果表明,多环芳烃与天然有机质相互作用的分配系数Kdoc的与PAHs的疏水度(即Kow大小)、NOM的物化特性(如芳香度、脂肪碳含量、分子量及极性等)和水化学参数(pH、离子强度等)有很大的相关性。然而,许多学者在NOM的物化特性对分配系数的影响方面存有较大分歧。前人在研究天然有机质与多环芳烃之间的相互作用时所用的NOM多为腐殖质,即水体NOM中的疏水性组分,而其中的亲水性组分与PAHs的结合作用文献中却鲜见提及,因此人们对其结合作用的特性如反应机理和结合作用强弱等的了解十分有限。 本论文利用XAD树脂分离技术把红枫湖水体中天然有机质分成了疏水性酸、碱、中性物质和亲水性酸、碱、中性物质等六种有机组分。同时运用元素分析、有机碳分析仪、紫外-可见分光光度,高效液相体积排阻色谱、三维荧光光谱和荧光偏振技术等现代分析方法,对各有机组分的物理、化学特性进行了表征。荧光光谱技术被用于研究水化学参数对腐殖质荧光特性和分子构型的影响以及测定Amherst腐殖酸(Amherst HA)、垃圾渗滤液富里酸(LF FA)和红枫湖NOM有机组分与多环芳烃苝、菲和蒽的结合系数(分配系数、条件稳定常数)并探讨了影响分配系数的各种因素和NOM与多环芳烃相互作用的机理。本论文的获得的主要结果如下: 1. 在水化学参数对腐殖质荧光特性及分子构型的影响方面: 在NOM与PAHs相互作用过程中,腐殖质的分子构型起着关键性的作用,而其分子构型又受到其本身的浓度、溶液的pH和离子强度等水化学参数的影响。本论文运用三维荧光光谱和荧光偏振技术研究了水化学参数对腐殖质荧光特性的影响,并由此推断其分子构型变化情况。实验结果表明随着腐殖质浓度、溶液的pH和离子强度的改变,腐殖质荧光特性(如荧光强度、荧光峰位和荧光偏振值等)出现不同程度的变化,揭示了腐殖质分子构型的改变。因此,本实验结果有利于深入了解腐殖质的分子构型及其对吸附PAHs的重要影响,对理解NOM的环境行为具有一定的理论价值。 2. 运用荧光猝灭滴定法研究Amherst HA和红枫湖NOM有机组分对多环芳烃苝、菲和蒽的吸附作用,结果表明NOM对多环芳烃的吸附能力与其中芳香结构单元有很强的相关性,logKdoc值与NOM在280 nm处的摩尔吸收(ε280)和分子量有线性度较高的正比关系,而C/H原子比值对不饱和碳含量(芳香度)并没有很好的指示作用。同时,脂肪碳(0-50 ppm)中的聚亚甲基碳对吸附PAHs也有很大的贡献,而有机组分的极性与分配系数有明显的负相关性。不同种类的多环芳烃与NOM有机组分的结合能力有很大的差异,这取决于不同PAHs的疏水度大小。本研究结果有利于弥合前人在NOM物化特性对PAHs吸附能力的影响方面的分歧,揭示了NOM的组成和结构在与PAHs等疏水性有机污染物相互作用方面的重要影响。 3. 在结合机理方面,苝与NOM有机组分结合的Stern-Volmer图具有较高的线性度,这表明其结合机理以疏水反应(或分配)为主,而菲和蒽与有机组分相互作用的吸附等温线显示较多的非线性特征表明极性反应为主要反应机理,结合过程以吸附为主。在红枫湖NOM有机组分中,疏水性组分显示对PAHs较高的结合能力,同时疏水性组分与PAHs相互作用的吸附等温线具有较高的线性度。这一结果揭示了不同种类的PAHs和各NOM有机组分之间结合机理的差异,加深了人们对NOM与PAHs相互作用机理的认识。 4. 前人在研究pH、离子强度等水化学参数对分配系数的影响方面得到的结果多有矛盾之处,同时,对实验结果的解释也不尽相同。本实验结果表明分配系数随pH增加而下降;离子强度对分配系数的影响比较复杂,就总体趋势而言,增加离子强度有利于对PAHs吸附能力的提高,这一结果初步揭示了水化学参数对PAHs分配系数的影响,丰富了人们对其影响机理的认识。 5. 运用荧光偏振技术测定了蒽与Amherst HA、LF FA和红枫湖NOM有机组分的条件稳定常数,结果如下:随着NOM浓度增加,蒽的荧光偏振值不断下降,这表明蒽的分子构型由平面线性向圆柱状转变。在所有NOM样品中,土壤源的Amherst HA与蒽结合的条件稳定常数最大(pH 4时logK=5.6,pH 6时 logK=5.4);就NOM有机组分而言,疏水性组分的logK变化范围在pH 6时为(4.4-5.2),而亲水性组分为(4.3-4.8),这表明疏水性组分具有相对较高的蒽吸附能力。实验结果有利于了解PAHs与NOM相互作用前后的分子构型变化情况,揭示了不同的NOM有机组分在吸附PAHs过程中的差异。

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The water sorption and desorption behaviour of three commercial polyacid-modified composite resins used in clinical dentistry have been studied in detail. Cured specimens of each material were subjected to two successive water uptake cycles in an atmosphere of 93% relative humidity, with one intervening desorption cycle in a desiccating atmosphere over concentrated sulfuric acid. Specimens were found to absorb and desorb water according Fick's law until Mt/M(infinity) values of approximately 0.5. Diffusion rates for uptake varied between cycles, ranging from 2.37-4.53 x 10(-9 )cm(2) s(-1) for 1st cycle to 0.85-2.72 x 10(-8 )cm(2 )s(-1) for 2nd cycle. Desorption rates were similar to those for 2nd cycle sorption, and ranged from 0.86 to 5.47 x 10(-8 )cm(2 )s(-1). Equilibration times for 1st cycle water uptake were greater than for 2nd cycle sorption and for desorption and overall the behaviour of polyacid-modified composites in a high humidity atmosphere was similar to that of conventional composites in water. It is concluded that the hydrophilic components of the former do not bring about an enhanced rate of water transport.

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this paper is about EU “soft policies” on immigrant integration. It analyzes the “Common Basic Principles” (CBPs) and the “European Integration Fund” (EIF), two devices that have been recently established within this framework. It adopts the theoretical perspective of the “anthropology of policy” and “governmentality studies”. It shows the context of birth of the aforementioned devices, as well as their functioning and the assessment done by the actors implied in the elaboration/implementation/evaluation of the related policies. It is based both on documentary research as well as direct observation and interviews done to the actors implied. It concludes that the PBC and the EIF should be considered as a “technology of government”, that strives to align the conduct of the actors with the governmental aims, as well as it produces specific practices and knowledge. It also underlines an intrinsic feature of many policies: their “congenital failure”, since they are (often) disputed and resignified by situated actors, who are embedded in asymmetrical power relations.

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Modern scientific world-view has undermined traditional myths, the functional survival of which seems to depend today in the West on a positivist justification. This would place them in the field of real History, through their study and revitalization by pseudoscientific disciplines such as the Atlantis and the ancient astronaut hypotheses. These have inspired new epic poems in (regular) verse that combine classic and/or biblical myths with a (pseudo)scientific modern world-view. For example, the critical rewriting of Noah’s myth by using the ancient astronaut hypothesis as a fictional device to produce a contemporary kind of plausibility allowed Abel Montagut to renew epic poetry, updating it also by adopting science fiction chronotopes in order to structure his fictional construction and to generate a high ethical sense for our time. Thus, his Poemo de Utnoa (1993) / La gesta d’Utnoa (1996), which has become a major classic of the literature in Esperanto thanks to its original version in this language, is a landmark of both science fiction and neo-biblical epics. This poem is written from a secular and purely literary perspective.

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Past measurements of the radiocarbon interhemispheric offset have been restricted to relatively young samples because of a lack of older dendrochronologically secure Southern Hemisphere tree-ring chronologies. The Southern Hemisphere calibration data set SHCal04 earlier than AD 950 utilizes a variable interhemispheric offset derived from measured 2nd millennium AD Southern Hemisphere/Northern Hemisphere sample pairs with the assumption of stable Holocene ocean/ atmosphere interactions. This study extends the range of measured interhemispheric offset values with 20 decadal New Zealand kauri and Irish oak sample pairs from 3 selected time intervals in the 1st millennium AD and is part of a larger program to obtain high-precision Southern Hemisphere 14C data continuously back to 200 BC. We found an average interhemispheric offset of 35 ± 6 yr, which although consistent with previously published 2nd millennium AD measurements, is lower than the offset of 55–58 yr utilized in SHCal04. We concur with McCormac et al. (2008) that the IntCal04 measurement for AD 775 may indeed be slightly too old but also suggest the McCormac results appear excessively young for the interval AD 755–785. In addition, we raise the issue of laboratory bias and calibration errors, and encourage all laboratories to check their consistency with appropriate calibration curves and invest more effort into improving the accuracy of those curves.

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