Electron transfer between Eu3+ and Ce3+ in SrM-F-4 matrix

Emissions of europium (II) and europium (III) have been observed in SrMgF4:Eu and SrMgF4:Eu,Ce phosphors which are synthesized in Ar flow, It is notable that the intensity of the ESR peaks corresponding to Eu2+ is increased when cerium ion is incorporated which can be explained by electron transfer mechanism.

Quantitative Determination of Microcystins in Rat Plasma by LC-ESI Tandem MS

A rapid and sensitive method was developed and validated for the determination of MCYST (microcystin)-RR, -LR, and [Dha(7)] MCYST-LR in rat plasma by liquid chromatography-tandem mass spectrometry. The analytes were extracted from rat plasma by protein precipitation, followed by solid-phase extraction. Liquid chromatography with electrospray ionization mass spectrometry, operating in selected reaction monitoring (SRM) mode, was used to quantify MCYST-RR, -LR, and [Dha(7)] MCYST-LR in rat plasma. The recoveries for each analyte in rat plasma ranged from 70.8 to 88.7%. The calibration curve was linear within the range from 0.005 to 1.25 mu g mL(-1). The limit of detection were 1.4, 1.0, 0.6 ng mL(-1) for MCYST-RR, -LR, and [Dha(7)] MCYST-LR. The overall precision was determined on three different days. The values for within- and between-day precision in rat plasma were within 15%. This method was applied to the identification and quantification of microcystins in rat plasma with acute exposure of microcystins via intravenous injection.

Simultaneous determination of microcystin-LR and its glutathione conjugate in fish tissues by liquid chromatography-tandem mass spectrometry

A sensitive and selective liquid chromatography-tandem mass spectrometry method was developed and validated for the simultaneous quantitative determination of microcystin-LR (MC-LR) and its glutathione conjugate (MC-LR-GSH) in fish tissues. The analytes were extracted from fish liver and kidney using 0.01 M EDTA-Na-2-5% acetic acid, followed by a solid-phase extraction (SPE) on Oasis HLB and silica cartridges. High-performance liquid chromatography (HPLC) with electrospray ionization mass spectrometry, operating in selected reaction monitoring (SRM) mode, was used to quantify MC-LR and its glutathione conjugate in fish liver and kidney. Recoveries of analytes were assessed at three concentrations (0.2, 1.0, and 5 mu g g(-1) dry weight [DW]) and ranged from 91 to 103% for MC-LR, and from 65.0 to 75.7% for MC-LR-GSH. The assay was linear within the range from 0.02 to 5.0 mu g g(-1) DW, with a limit of quantification (LOQ) of 0.02 mu g g(-1) DW. The limit of detection (LOD) of the method was 0.007 mu g g(-1) DW in both fish liver and kidney. The overall precision was determined on three different days. The values for within- and between-day precision in liver and kidney were within 15%. This method was applied to the identification and quantification of MC-LR and its glutathione conjugate in liver and kidney of fish with acute exposure of MC-LR. (c) 2007 Elsevier B.V. All rights reserved.

基于支持向量机的Internet流量分类研究

准确的网络流量分类是众多网络研究工作的基础,也一直是网络测量领域的研究热点.近年来,利用机器学习方法处理流量分类问题成为了该领域一个新兴的研究方向.在目前研究中应用较多的是朴素贝叶斯(nave Bayes,NB)及其改进算法.这些方法具有实现简单、分类高效的特点.但该方法过分依赖于样本空间的分布,具有内在的不稳定性.因此,提出一种基于支持向量机(support vector machine,SVM)的流量分类方法.该方法利用非线性变换和结构风险最小化(structural risk minimization,SRM)原则将流量分类问题转化为二次寻优问题,具有良好的分类准确率和稳定性.在理论分析的基础上,通过在实际网络流集合上与朴素贝叶斯算法的对比实验,可以看出使用支持向量机方法处理流量分类问题,具有以下3个优势:1)网络流属性不必满足条件独立假设,无须进行属性过滤;2)能够在先验知识相对不足的情况下,仍保持较高的分类准确率;3)不依赖于样本空间的分布,具有较好的分类稳定性.

Direct characterization of bitter acids in a crude hop extract by liquid chromatography-atmospheric pressure chemical ionization mass spectrometry

The applicability of on-line coupling of reversed-phase high-performance liquid chromatography to atmospheric pressure ionization tandem mass spectrometry for the separation and characterization of hop acids mixture from the crude extract of Humulus lupulus was investigated. The solvent system consisting of acetonitrile-aqueous formic acid was used to give proper separation of the six main hop bitter acids within 30 min. Further structural information about the components was acquired by collision-induced dissociation (CID). On the basis of analyses of the fragmentation patterns of the major alpha- and beta-bitter acids respectively, identification of the minor ones was performed using selected reaction monitoring (SRM) with a group of qualitatively relevant selected precursor-product ion transitions for each bitter acid in a single high performance liquid chromatography (HPLC) run. Using this technique, six minor hop acids, including "adprelupulone" observed for the first time in natural resources, were detected along with the six major acids. This hyphenated techniques provides potency for rapid qualitative determination of analogs and homologs in mixtures. (C) 2004 American Society for Mass Spectrometry.

Determination of mercury in biological samples using organic compounds as matrix modifiers by inductively coupled plasma mass spectrometry

A method was developed for the determination of total mercury in biological samples. The effects of aqueous ammonia, ethylenediamine and triethanolamine on Hg signal intensity by inductively coupled plasma mass spectrometry has been evaluated and the possible mechanisms discussed. It has been proved that the signal intensity of Hg significantly increases with adding, in the presence of small amounts of aqueous ammonia, ethylenediamine or triethanolamine. The normalized intensity (the signal intensity ratio with amine and without amine) of Hg increases as the concentration of aqueous ammonia, ethylenediamine or triethanolamine increases, but the degree of enhancement of aqueous ammonia was smaller than that of ethylenediamine and triethanolamine. The normalized intensity of Hg with aqueous ammonia, ethylenediamine and triethanolamine decreases as the nebulizer flow rate increases, but decreasing degree of aqueous ammonia was smaller than that of ethylenediamine and triethanolamine. The higher the RF powers the higher the normalized intensity of Hg at the same nebulizer flow rate. The addition of aqueous ammonia, ethylenediamine and triethanolamine into analytical solutions significantly improved the transport efficiency of Hg. The detection limit of Hg is improved about ten times by the addition of ethylenediamine or triethanolamine under the optimum experimental parameters. The method has been used to determine mercury in biological standard reference materials (SRM). The analytical results are very close to the certified values and the determined values for similar samples.

顺丁橡胶的长链支化与支化临界分子量

用拟合粘度曲线法研究了顺丁橡胶的支化参数,得到了支化临界分子量M,进而计算出支化度λ。其结果用标准参考物SRM 146的测定结果验证,表明方法是可靠的;而λ值与用Drott法的结果相比。后者平均偏高百分之几。

Determination of tetrodotoxin by liquid chromatography coupled with electrospray ion-trap mass spectrometry

Two methods for tetrodotoxin analysis using liquid chromatography coupled with electrospray iontrap mass spectrometry (LC-ESI-MS) have been established with C,, reversed phase column and hydrophilic interaction liquid chromatography (HILIC) column, respectively. Sensitivity and reproducibility of the methods were compared. The method using C-18 column in selected ion monitoring (SIM) mode had a detection limit (S/N = 3) of 120 pg, and a good linearity of the calibration curve was obtained for tetrodotoxin (r = 0. 9992). High reproducibility of the method was observed, with a relative standard deviation (RSD) below 10%. The method using HILIC column in SIM mode and selected reaction monitoring (SRM) mode had detection limits (S/N = 3) of 15 and 3.75 pg, respectively. Good linearity of the calibration curves was obtained for tetrodotoxin (r = 0. 9996 and 0. 9998 in SIM and SRM mode, respectively). T he reproducibility was high in SIM mode but relatively poor in SRM mode. Based on the results, the method using HILIC column in SIM mode was suggested for the analysis of tetrodotoxin with LC-MS system.

青藏高原两种草甸地表通量季节变化特征

2003年1月-2004年7月运用涡度相关法技术研究青藏高原金露梅(Potentilla fruticosa)灌丛草甸(SWM)和藏嵩草(Kobresia humilis)沼泽化草甸(SRM)的地表通量。结果表明：二者地表湍流通量都具有明显的季节变化和日变化，其中感热通量以4月最大，1月最小，而潜热通量则以5月最大；感热通量随着季节的变动而显著变化，在相同月份中沼泽化草甸白天最大值大于灌丛草甸，日变化振幅比灌丛草甸强；白天潜热通量达到最大值的时间和波动强度因季节不同而各异，在非生长季节白天最大值在13～15 h，日波动较弱，生长季节最大值在12 h，日波动较强；高寒草甸地表湍流通量与温度间存在着线性关系；不同季节感热通量：沼泽化草甸>灌丛革甸，而潜热通量与感热通量各异，在1月沼泽化革匈>灌丛草甸，在4和10月，沼泽化草甸<灌丛草甸，在7月二者基本一致。

土石混合体细观结构力学及其边坡稳定性研究

Soil-rock mixture (S-RM) refers to one extremely uneven loose rock and soil materials system with certain stone content. Its formation has started since Quaternary and it is composed of block stone, fine grained soil and pore with certain project scale and high strength. S-RM has extensive distribution in nature, especially in southwest China where the geotectonic background is complicated, the fracture activity is developed and the geomorphological characteristics of high mountain and steep gorge area are protuberant. This kind of complicated geologic body has developed wider in these areas. S-RM has obvious difference with the general soil or rock (rock mass) in physical and mechanical properties because its two components-“soil” and “rock-block” has extreme differences in physical and mechanical properties. The proposition of S-RM and its deep research are needed in the modern engineering construction. It is also the necessity in the modern development of rock and soil mechanics. The dissertation starts from the meso-structural characteristics of soil-rock and takes a systematic research on its meso-structural mechanics, deformation and failure mechanism and the stability of S-RM slope. In summary, it achieves the following innovative results and conclusions. There are various views on the conception of S-RM and its classification system. Based on the large number of field tests, the dissertation makes the conception and classification of S-RM more systematic. It systematically proposed the conception of meso-structural mechanics of S-RM. Thus the dissertation has laid a foundation for its deep study. With the fast development of the computer technology and digital image processing theory, digital image processing technology has been successfully applied in many fields and provided reliable technology support for the quantitative description of the structural characteristics of S-RM. Based on the digital image processing technology, the dissertation systematically proposes and developed the quantitative analysis method and quantitative index for the meso-structure of S-RM. The results indicate that the meso-structure such as its internal soil-rock granularity composition, the soil-rock shape and the orientability has obvious self-organization in the macro statistical level. The dissertation makes a systematic research on the physical mechanical properties, deformation and failure mechanism of S-RM based on large field test. It proposes the field test for the underwater S-RM and deduces the 3D data analysis method of in-situ horizontal push-shear test. The result indicates that S-RM has significant phenomenon of shear dilatancy in the shearing process, and its dilatancy will be more obvious with the increased proportion of rock or the decreased confining pressure. The proportion of rock has great effect on the strength of S-RM and rock-block, especially the spatial position of particles with comparatively big size has great effect on the shape and spatial position of the sample shear zone. The dissertation makes some improvements in the single ring infiltration test equipment and its application on the permeability of S-RM. The results indicate that the increasing of rock-block would make it more difficult for the soil to fill in the vacuity between the rock-block and the proportion would increase which would result in the increased permeability coefficient. The dissertation builds the real meso-structural model of S-RM based on the digital image processing technology. By using geometric reconstruction technology, it transfers the structural mode represented by Binary image into CAD format, which makes it possible to introduce the present finite element analysis software to take research on numerical experimental investigation. It systematically realizes leaping research from the image，geometric mode, to meso-structural mechanics numerical experiment. By using this method, the dissertation takes large scale numerical direct-shear test on the section of S-RM. From the mesoscopic perspective, it reveals three extended modes about the shear failure plane of S-RM. Based on the real meso-structural model and by using the numerical simulation test, the character and mechanics of seepage failure of S-RM are studied. At the same time, it builds the real structural mode of the slope based on the analysis about the slope crosssection of S-RM. By using the strength reduction method, it takes the research on the stability of S-RM and gets great achievements. The three dimensional geometric reconstruction technology of rock block is proposed, which provides technical support for the reconstruction of the 3D meso-structural model of S-RM. For the first time, the dissertation builds the stochastic structure model of two-dimensional and three-dimensional polygons or polyhedron based on the stochastic simulation technique of monte carlo method. It breaks the traditional research which restricted to the random generation method of regular polygon and develops the relevant software system (R-SRM2D/3D) which has great effect on meso-structural mechanics of S-RM. Based on the R-SRM software system which randomly generates the meso-structural mode of S-RM according to the different meso-structural characteristics, the dissertation takes a series of research on numerical test of dual axis and real three-axis, systematically analyses the meso destroy system, the effects of meso-structural characteristics such as on the stone content, size composition and block directionality on the macro mechanical behavior and macro-permeability. Then it proposes the expression of the upper and lower limit for the macro-permeability coefficient of the inhomogeneous geomaterials, such as S-RM. By using the strength reduction FEM, the dissertation takes the research on the stability of the slope structural mode of the randomly formed S-RM. The results indicate that generally, the stability coefficient of S-RM slope increases with the increasing of stone content; on the condition of the same stone content, the stability coefficient of slope will be different with different size composition and the space position of large block at the internal slop has great effect on the stability. It suggests that meso-structural characteristics, especially the space position of large block should be considered when analyzing the stability of this kind of slope and strengthening design. Taking Xiazanri S-RM slope as an example, the dissertation proposes the fine modeling of complicated geologic body based on reverse engineering and the generation method of FLAC3D mode. It resolves the bottleneck problem about building the fine structural mode of three-dimensional geological body. By using FLAC3D, the dissertation takes research on the seepage field and the displacement field of Xiazanri S-RM slope in the process of reservoir water level rising and decreasing. By using strength reduction method, it analyses the three-dimension stability in the process of reservoir water level rising and decreasing. The results indicate that the slope stability firstly show downward trend in the process of reservoir water level rising and then rebound to increase; the sudden drawdown of reservoir water level has great effect on the slope stability and this effect will increase with the sudden drawdown amplitude rising. Based on the result of the rock block size analysis of S-RM, and using R-SRM2D the stochastic structure model of Xiazanri S-RM slope is built. By using strength reduction method, the stability of the stochastic structure model is analysis, the results shows that the stability factor increases significantly after considering the block.

黄土—古土壤沉积物中酸溶相硼的分离及其同位素测定

用０．５ｍｏｌ／ＬＨＣｌ提取黄土、古土壤中的酸溶相成分，并用混合树脂法和硼特效树脂法两方法叠加以硼进行分离和纯化，Ｃｓ２ＢＯ２＾＋法测同位素比值。结果表明，虽然混合树脂法和硼特效脂法都是较成熟的方法，但用来处理杂质离子含量相对高而硼含量低的样品深液并不成功。两种方法叠加处理后达到理想的效果，重复处理黄土－古土壤样品的精度（２ＲＳＤ）在０．４‰～０．４‰之间，，这与标样(mST SRM 951)水平(0．3‰)接近，说明处理方法是可行的。用此方法首次测定了洛川黄土．古土壤沉积物中酸溶相的硼同位煮组成。

中国南方含硒建造中硒稳定同位素与化学形态的地质意义

氧化还原敏感元素硒的地球化学循环非常复杂, 它的循环主要受氧化还原势、酸碱度、温度、压力等条件的控制。长期以来，关于硒的主要研究集中在环境生物地球化学领域。对于硒的地质地球化学行为的研究，学者们认为硒不可能独立形成矿床,它主要以伴生元素的形式赋存于一些热液矿床（如，拉尔玛硒-金热液矿床等）。 二十世纪末, 我国学者开始关注硒的矿床地球化学行为, 发现了目前唯一的渔塘坝沉积型的独立硒矿床。另外，下寒武统底部黑色岩系（如，遵义牛蹄塘组）处于地球发展演化的关键时期且富集了众多的有用金属元素, 因此它引起了全世界广大地质学家的普遍关注和重视。这些黑色岩系的共同特点是含有大量的有机质和丰富的金属元素(PGE，Cu，Ni，Mo，Au，U，V，Mn，Fe，Co，Bi，Cr，Se等)。但遵义牛蹄塘组中Ni-Mo多金属层的成因一直争论不休。 本文以拉尔玛硒-金热液矿床、渔塘坝独立硒矿床、遵义黄家湾含Ni-Mo-Se多金属层剖面为研究对象，主要通过硒稳定同位素的测试和不同化学形态的分析结合其他的地球化学参数（如，C-S-Fe体系，氧化还原敏感元素），示踪富硒地层的沉积环境，研究不同地质体系中硒稳定同位素的组成，进而完善硒同位素的理论体系，探讨硒富集过程中的形态迁移途径，并为矿床的形成提供更完善的地球化学证据。通过一系列的研究工作，我们取得了以下几点认识： (1) 通过不同的消解方法准确测定了低硒,高硒样品的总硒含量,相对标准偏差小于10%，而且不同的消解方法测得同样的结果, 满足了地质样品中微量元素的测试要求。由于不同消解方式存在自身的优缺点,我们建议根据不同的样品类型,不同的研究目的选取合适的消解方法。 (2) 通过巯基棉吸附装置达到了纯化富集样品硒的目的, 硒的回收率一般大于90%, 满足同位素测试的需要。应用自制的氢化物发生器与Nu-MC-ICP-MS联用,实现了在线气体进样测试硒稳定同位素的目的。 采用标准样品匹配测试方法校正仪器测试过程中的质量分馏。 硒稳定同位素的测试精度为2δ=0.30‰, 标准NIST SRM 3149采用与样品同样的处理方法,没有发现前处理过程的同位素分馏。 (3) 传统地球化学参数对沉积环境的指示意义。通过氧化还原敏感微量元素及其与TOC的关系和C-S-Fe体系的分析，对渔塘坝独立硒矿床的多元素富集及沉积环境, 遵义黑色岩系沉积环境进行了详细的解释。TS-TFe的关系表明样品中有过量的硫存在，可能为有机硫或为其他亲硫元素提供有利的沉淀条件。C-S-Fe体系及微量元素指数V/(V + Ni) 说明渔塘坝矿区的硅质岩和页岩的沉积环境为缺氧到静海环境， Ni/Co、V/Cr几乎不能作为该区缺氧环境的指示参数, 后者可能由于Cr的外源输入（碎屑、热液等）所致。 C-S-Fe体系及微量元素指数V/(V + Ni)体系指示遵义黑色岩系的沉积环境为微含氧到缺氧的条件, 但对于Ni-Mo矿而言, V/(V + Ni)体系指示其为含氧条件沉积，这可能与Ni-Mo多金属层的成因有关。但铁的硫化度可以指示Ni-Mo多金属层极端的缺氧还原环境。 (4) 硒的形态对古氧化还原条件和矿物质来源的示踪意义。黑色岩系的硒形态分布不同于海洋沉积物，体现了成岩作用对硒形态分布的改变。黑色岩系中硒的主要形态为有机结合态和硫化物/硒化物结合态。硫化物/硒化物结合态比例与铁的硫化程度（DOS）之间明显的相关关系说明在海洋环境中硒主要通过氧化还原反应富集在富有机质的沉积物与沉积岩中。这种相关关系与岩石类型没有关系，这使得将硫化物、硒化物结合的Se（-II）比例作为一个氧化还原条件示踪剂更加可行。DOS与硫化物/硒化物结合态硒的关系，及Se（IV）与Se（-II）的关系均说明遵义牛蹄塘组的K-斑脱岩形成于碱性的氧化环境，Ni-Mo多金属层沉积于微酸性的极端还原环境，而渔塘坝矿床形成于微碱性的还原缺氧环境。生物的同化作用与异化作用之间本身存在互补关系，但这种互补关系却存在不同的转化趋势。不同的转化趋势可能主要受氧化还原反应和酸碱度的控制，其他的地质作用也可能起着重要作用（如，硅酸盐、Fe（II）的含量，硫化物、有机质含量，风化程度等）。同时我们发现相同的氧化还原条件下可能存在不同的富集途径。Ni-Mo多金属层中极少的有机结合态硒暗示海洋同生沉积主要被生物异化还原控制，而沉积物从海洋富集硒的途径主要为直接由Se（VI）和Se（IV）到Se（-II）的还原途径，从高价态到元素态的还原途径可能偶有发生但强度很小。 (5) 硒稳定同位素对矿床成因及物质来源的示踪意义。热液或表生环境中,硒的再次活化迁移对硒同位素的大范围分馏是很重要的。较少的硫化物结合态硒和较大范围的硒同位素组成说明渔塘坝矿床形成时经历了多次氧化还原过程。干酪根硒同位素组成与全岩相似, 而且样品富集轻同位素暗示该矿床硒来的富集主要通过海洋硒的生物吸收同化异化还原与多次无机氧化还原实现。对于拉尔玛金硒矿床而言，未蚀变岩体的硫化物结合态硒富集轻同位素，而后期低温流体的蚀变作用导致蚀变岩体中硫化物结合态硒富集重同位素。干酪根的硒同位素组成暗示热液输入的硒为该矿床硒的主要来源，硒从热液直接进入干酪根的机制是一致的。随着硫含量的增加岩石和矿体中的硒逐渐富集重同位素, 说明海水对矿床富集的贡献是很有限的。遵义黑色岩系中硒同位素组成与Se（-II）之间的关系, 单质硒的缺乏，硒的富集与同位素的关系说明，热液为主要的硒来源，而早寒武世海水中的硒主要通过Se（VI）和Se（IV）到Se（-II）的直接生物还原实现。三个区域的S/Se比值综合说明硫与硒的共同沉降过程中不存在硒的同位素分馏。不同化学形态的分布与不同形态中硒稳定同位素的结合可能会更好的解释硒的全球地球化学循环。 (6) 根据目前硒的同位素分馏体系及所测得的数据,我们初步建立了不同时代、不同成因黑色岩系中硒稳定同位素的分馏模式。