55 resultados para Mandeville, Bernard, 1670-1733.


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This paper presents an introduction to the application of ion traps and storage devices for cluster physics. Some experiments involving cluster ions in trapping devices such as Penning traps, Paul traps, quadrupole or multipole linear traps are briefly discussed. Electrostatic ion storage rings and traps which allow for the storage of fast ion beams without mass limitation are presented as well. We also report on the recently developed mini-ring, a compact electrostatic ion storage ring for cluster, molecular and biomolecular ion studies.

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In collisions between slow F2+ ions (30 keV) and molecular targets, adenine, scattered particle production yields have been measured directly by simultaneous detection of neutrals, positive and negative ions. The relative cross-section for a negative ion formation channel was measured to be 1%. Despite a slight decrease compared to a larger target, the fullerene C-60, the measured negative ion formation cross section is still at least one order of magnitude larger than the yield in ion-atom interactions.

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The differential cross sections of F-17 and O-17 elastic scattering products on Pb-208 have been measured at the Radioactive Ion Beam Line at Lanzhou (RIBLL). Two angular dispersion plots of ln(d sigma/d theta) versus theta 2 are obtained from the angular distribution of the elastic scattering differential cross sections. The angular dispersion plot exhibits a clear turning point for F-17 in the range of small scattering angles 6 degrees-20 degrees due to its exotic structure, but for O-17, the turning point is not observed in the same angular range. The experimental results have been compared with previous data of other groups. Systematical analysis on the available data supports the above conclusion that there is an exotic behaviour of the angular dispersion plot of weakly bound nuclei with halo or skin structure as compared with that of the ordinary nuclei near stable line. Therefore the turning point of the angular dispersion plot appears at small angle for weakly bound nuclei with halo or skin structure, and can be used as a new probe to investigate the halo and skin phenomena of weakly bound nuclei.

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We have studied the excitation and dissociation processes of the molecule W(CO)(6) in collisions with low kinetic energy (3 keV) protons, monocharged fluorine, and chlorine ions using double charge transfer spectroscopy. By analyzing the kinetic energy loss of the projectile anions, we measured the excitation energy distribution of the produced transient dications W(CO)(6)(2+). By coincidence measurements between the anions and the stable or fragments of W(CO)(6)(2+), we determined the energy distribution for each dissociation channel. Based on the experimental data, the emission of the first CO was tentatively attributed to a nonstatistical direct dissociation process and the emission of the second or more CO ligands was attributed to the statistical dissociation processes. The dissociation energies for the successive breaking of the W-CO bond were estimated using a cascade model. The ratio between charge separation and evaporation (by the loss of CO+ and CO, respectively) channels was estimated to be 6% in the case of Cl+ impact. (C) 2011 American Institute of Physics. [doi: 10.1063/1.3523347]

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Microscopic three-nucleon force consistent with the Bonn B two-nucleon potential is constructed, which includes Delta(1232), Roper, and nucleon-antinucleon excitation contributions. Recent results for the choice of the meson parameters are discussed. The forces are used in Brueckner calculations and the saturation properties of nuclear matter are determined. At the high densities,the nuclear equation of state and the symmetry energy are calculated. The corresponding neutron star mass-radius relations are presented.

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Due to a low mineral content, the sapropelic sediments depositing in Mangrove Lake, Bermuda, provide an excellent opportunity to explore for possible additions of sulfur to organic matter during the early stages of diagenesis. We evaluated early diagenetic organic sulfur transformations by monitoring the concentrations and stable isotopic compositions of a number of inorganic and organic sulfur pools, thereby accounting for all of the sulfur in the sediments. We have identified and quantified the following sulfur pools: porewater sulfate, porewater sulfide, elemental sulfur, pyrite sulfur, hydrolyzable organic sulfur (HYOS), chromium-reducible organic sulfur (CROS), and nonchromium-reducible organic sulfur (Non-CROS). Of the organic sulfur pools, the Non-CROS pool is by far the largest, followed by CROS, and finally HYOS. By 60 cm depth these pools contribute, respectively, to 85, 7.9, and 3.6% of the total solid phase sulfur. The HYOS pool is probably of biological origin and shows no interaction with the sulfur compounds produced during diagenesis. By contrast, CROS is produced, most likely, from the diagenetic addition of polysulfides to functionalized lipids in the upper, H2S-poor, elemental sulfur-rich, region of the sediment. A portion of this sulfur pool is unstable and decomposes on contact with the H2S-rich porewaters. The portion of CROS that remains in the sulfidic waters appears to readily exchange sulfur isotopes with H2S. While some of the Non-CROS pool is of biological origin, some is also formed by the diagenetic addition of sulfur to organic compounds in the upper H2S-poor region of the sediment. By contrast with CROS, Non-CROS is not diagenetically active in the H2S-rich porewaters. Overall, somewhere between 27 and 53 % of the organic sulfur buried in Mangrove Lake sediments is of diagenetic origin, with the remaining organic sulfur derived from biosynthesis. We extrapolate our Mangrove Lake results and calculate that in typical coastal marine sediments between 11 and 29 μmol g−1 of organic sulfur will form during early diagenesis, of which 2–5 μmol g−1 will be chromium reducible.

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A method for measuring the long- and medium-term turnover of soil organic matter is described. Its principle is based on the variations of 13C natural isotope abundance induced by the repeated cultivations of a plant with a high 13C/12C ratio (C4 photosynthetic pathway) on a soil which has never carried any such plant. The 13C/12C ratio in soil organic matter being about equal to the 13C/12C ratio of plant materials from which it is derived, changing the 13C content of the organic inputs to the soil (by altering vegetation from C3 type into C4 type) is equivalent to a true labelling in situ of the organic matter. Two cases of continuous corn cultivation (Zea mays: δ13C = −12%.) on soils whose initial organic matter average δ13C is −26%. were studied. The quantity of organic carbon originating from corn (that is the quantity which had turned-over since the beginning of continuous cultivation) was estimated using the 13C natural abundance data. After 13 yr, 22% of total organic carbon had turned-over, in the system studied. Particle size fractions coarser than 50μm on the one hand, and finer than 2μm on the other. contained the youngest organic matters. The turnover rate of silt-sized fractions was slower

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全球气候模型HADCM2SUL和CGCM1分别预测100a后全球年均温增加3.7℃和5.2℃,年降水增加30.7%和25.1%。为了研究东北森林对这两种预测方案的反应,使用logistic回归模型分析了东北森林8个建群种与11种环境因子之间的相关关系。结果表明,除了山杨和蒙古栎之外,年均温是决定其它树种存在与否的重要因子。采用模型结果预测现行气候条件下8个树种的分布并与其现实分布比较,发现针叶树种的总正确率、敏感度、指定度和错误肯定率均比阔叶树种的要高,而错误否定率比后者低,说明模型对针叶树种的拟合程度要优于对阔叶树种的拟合程度。在此基础上,预测了8个树种在两种气候变化方案下100a后的分布图。结果表明,在HADCM2SUL方案下,兴安落叶松、白桦、冷杉和云杉的覆盖率分别下降91.2%、67.4%、11.9%、10%;长白落叶松、红松和蒙古栎的覆盖率分别增长87.8%5、4.6%、31.3%;在CGCM1方案下,兴安落叶松、白桦、云杉、冷杉和红松的覆盖率分别下降99.2%8、9.9%、85.9%、83.2%、4.9%;长白落叶松、蒙古栎的覆盖率分别增长93.3%、27.5%;山杨在这两种方案下数量不变。

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大庆油田油泥样品经富集培养,平板分离,获得52株菌。排油性实验和表面张力测定表明,菌株B22、B24、B25产生的表面活性剂表面活性稳定,表面张力较低。温度、pH和NaCl浓度实验证实,细菌B22产生的生物表面活性剂可耐受120℃高温,另2种生物表面活性剂可耐受80℃;3种细菌生物表面活性剂对pH有广泛适应性,B22pH适应范围为4·0~13·0,B24、B25的pH适应范围为2·0~13·0;Na-Cl浓度对表面活性剂的生物活性影响不大。将3株菌的生物表面活性剂用于室内油泥处理实验,72h石油去除率达70%以上。

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A new compound, [Ni(en)(3)](2)[Ni(en)(2)(H2O)(2)][As6V15O42] . 4H(2)O, was first prepared by hydrothermal synthesis and characterized by elemental analysis, IR, TGA-DSC, ESR and single crystal X-ray diffraction. Crystal data: monoclinic, space group C-c, a = 1. 523 6(3) nm, b = 2. 051 8(4) nm, c = 2.395 9(5) nm, beta = 97. 41(3)degrees, V = 7.427(3) nm(3), Z = 4, R = 0. 057 0, wR(2) = 0.135 7. The polyanion consists of six AsO3 pyramids and fifteen VO5 pyramids. Counterions are complex ions with octahedral structure, which consist of NH2CH2CH2NH2 and Ni2+.

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Nonisothermal crystallization and melting behavior of poly(3-hydroxybutyrate) (PHB) and maleated PHB were investigated by differential scanning calorimetry using various cooling rates. The results show that the crystallization behavior of maleated PHB from the melt greatly depends on cooling rates and its degree of grafting. With the increase in cooling rate, the crystallization process for PHB and maleated PHB begins at lower temperature. For maleated PHB, the introduction of maleic anhydride group hinders its crystallization, causing crystallization and nucleation rates to decrease, and crystallite size distribution becomes wider. The Avrami analysis, modified by Jeziorny, was used to describe the nonisothermal crystallization of PHB and maleated PHB. Double melting peaks for maleated PHB were observed, which was caused by recrystallization during the heating process.

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多金属氧酸盐因其在医药临床、工业催化、功能材料等方面的广泛应用而引起人们的关注 [1~ 6 ] ,其中 ,有关钒化学的研究一直很活跃 ,钒具有与钼、钨明显不同的结构特性 ,钒可以采取 VO4 ,VO5和VO6 方式配位 ,同时 ,钒的价态可以是 + 3,+ 4和 + 5价 .由于钒可采取多种配位方式及多种价态 ,与钼酸盐和钨酸盐相比 ,钒酸盐更具有结构柔顺性 ,同时易形成低价或混合价态物种 .在以往的文献中 ,有关 P- V- O体系多金属氧酸盐的水热合成的研究已有大量的报道 [7] ,在常规溶液合成中 ,人们已对As- V- O体系进行了相对深入的研究 ,而有关水热合成的研究报道却很少 ,已见报道的砷钒化合物有K6 [As6 V15O4 2 ( H2 O) ]· 6H2 O[8,9] ,[As8V14 O4 2 ( H2 O) 1/2 ]4 - [10 ] ,[As8V14 O4 2 ( X) ]6 - [11] ( X=SO2 - 3,SO2 - 4,H2 O) .为了探究水热条件下 As- V- O体系的反应特性 ,我们开展了这方面的研究工作 ,并取得了突破性进展 .本文采用中温水热技术合成了含有机基团...