69 resultados para 106-115 cm


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无水NdCl_3与甲基萘锂以1:2摩尔比在THF中反应分离得到一种黑色产物,该产物与环辛四烯反应,分离得到标题化合物,测定了这一新配合物的晶体结构。该晶体属单斜晶系,空间群P2/c,晶胞参数a=1.7858(7)nm,b=1.3243(4)nm,c=1.8085(6)nm,β=106.52(4)°,V=4.10nm~3,D_c=1.268 g/cm~3,Z=4,F(000)=1660,R=0.0774,R_w=0.0733。配合物分子由不相连的阴阳离子对组成,阴离子是由中心钛离子与二个对称的环辛四烯组成,阳离子是由一个锂离子和四个THF分子配位而成,另有二个THF分子作为填充分子存在于晶胞中。

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The crystal structure of [Mn(thiamine)Cl2(H2O)]2[thiamine]2Cl4.2H2O has been determined by X-ray diffraction methods. The compound contains a cyclic dimer of a complex cation with two thiamine ligands bridged by two Mn(II) ions across a crystallographic center of symmetry. Each Mn(II) is coordinated by two chloride atoms, a water molecule, a N(1') atom of the pyrimidine from a thiamine and an O(53) atom of the hydroxyethyl side chain from another thiamine. There are two free-base thiamine molecules related by a center of symmetry in the unit cell, which form a base-pair through the hydrogen bonds. Both the independent thiamine molecules in the asymmetric unit assume the common F conformation with phi-T = 10.0(9) and 3.6(10) and phi-P = 85.6(7) and 79.6(7), respectively. The compound provides a possible model for a metal-bridged enzyme-coenzyme complex in thiamine catalysis. Crystallographic data: triclinic, space group P1BAR, a = 12.441(4), b = 13.572(4), c = 11.267(3) angstrom, alpha = 103.15(2), beta 89.03(3), gamma = 115.64(2)-degrees, Z = 1, D(calc) = 1.524 g cm-3, and R = 0.050 for 3019 observed reflections with I > 3-sigma(I).

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本文研究了端羟基丁腈橡胶(HTBN)对环氧树脂的增韧作用。加入10—20phr的HTBN,环氧树脂性能可以大幅度提高,粘接碳钢剪切强度30MPa,冲击强度9×10~(-2)J/cm~2,浇注试样抗张强度61MPa,伸长10%,玻璃化温度115℃;不加HTBN的环氧树脂固化物,剪切强度24MPa,冲击强度34×10~(-2)J/cm~2,抗张强度30MPa,伸长5%,玻璃化温度124℃。 本文还通过DSC、SEM研究观察到增韧环氧树脂的两相结构。

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AMS(14)C dating and grain-size analysis for Core PC-6, located in the middle of a mud area on the inner shelf of the East China Sea (ECS), were used to rebuild the Holocene history of the East Asian winter monsoon (EAWM). The 7.5-m core recorded the history of environmental changes during the postglacial transgression. The core's mud section (the upper 450 cm) has been formed mainly by suspended sediment delivered from the Yangtze River mouth by the ECS Winter Coastal Current (ECSWCC) since 7.6 kyr BP. Using a mathematical method called "grain size vs. standard deviatioW', we can divide the Core PC-6's grain-size distribution into two populations at about 28 mu m. The fine population (< 28 mu m) is considered to be transported by the ECSWCC as suspended loads. Content of the fine population changes little and represents a stable sedimentary environment in accord with the present situation. Thus, variation of mean grain-size from the fine population would reflect the strength of ECSWCC, which is mainly controlled by the East Asian winter monsoon. Abrupt increasing mean grain size in the mud section is inferred to be transported by sudden strengthened ECSWCC, which was caused by the strengthened EAWM. Thus, the high resolution mean grain-size variation might serve as a proxy for reconstruction of the EAWM. A good correlation between sunspot change and the mean grain-size of suspended fine population suggests that one of the primary controls on centennial- to decadal-scale changes of the EAWM in the past 8 ka is the variations of sun irradiance, i.e., the EAWM will increase in intensity when the number of sunspots decreases. Spectral analyses of the mean grain-size time series of Core PC-6 show statistically significant periodicities centering on 2463, 1368, 128, 106, 100, 88-91, 7678, and 70-72 years. The EAWM and the East Asian summer monsoon (EASM) agree with each other well on these cycles, and the East Asian Monsoon (EAM) and the Indian Monsoon also share in concurrent cycles in Holocene, which are in accord with the changes of the sun irradiance. (c) 2005 Elsevier B.V. All rights reserved.

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高原115(原代号96-115号)是中国科学院西北高原生物研究所于1992年以(太谷核不育系*91-233)F_1为母本,{加拿大11号*[繁6*(R211*苦瓜)F_4]F_5}F_5紫黑色小麦为父本进行杂交,采用系谱法选育而成的春小麦品种。2001年12月通过青海省农作物品种审定委员会审定。

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云南会泽铅锌矿床位于扬子板块西缘川黔滇铅锌银多金属成矿域的中南部,严格受断裂带的控制。流体包裹体、铅同位素和锶同位素的证据表明,成矿流体为不同性质流体的混合物,具有多源性。大部分矿物流体包裹体均一温度变化于150~250℃之间,部分包裹体大于300℃;盐度变化范围5%~21%,ω(NaCl)平均为13.24%;密度0.546~1.129g/cm^3;均一瞬间压力145×10^5~754×10^5Pa;成矿深度2200~2450m。流体混合后,由于大幅度的降压作用,使得成矿流体发生沸腾,流体产生过饱和,并最终导致金属矿物的析出。因此,这明显有别于MVT矿床,是一个新型的铅锌矿床。

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Direct methanol fuel cells (DMFCs) consisting of multi-layer electrodes provide higher performance than those with the traditional electrode. The new electrode structure includes a hydrophilic thin film and a traditional catalyst layer. A decal transfer method was used to apply the thin film to the Nafion(R) membrane. Results show that the performance of a cell with the hydrophilic thin film is obviously enhanced. A cell with the optimal thin film electrode structure operating at I M CH3OH, 2 atm oxygen and 90degreesC yields a current density of 100 mA/cm(2) at 0.53 V cell voltage. The peak power density is 120 mW/cm(2). The performance stability of a cell in a short-term life operation was also increased when the hydrophilic thin film was employed. (C) 2002 Elsevier Science B.V. All rights reserved.

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A five-layer catalyst coated membrane (CCM) based upon Nation 115 membrane for direct methanol fuel cell (DMFC) was designed and fabricated by introducing a modified Nafion layer between the membrane and the catalyst layer. The properties of the CCM were determined by SEM, cyclic voltammetry, impedance spectroscopy, ruinous test and I-V curves. The characterizations show that the modified Nation layers provide increased interface contact area and enhanced interaction between the membrane and the catalyst layer. As a result, higher Pt utilization, lower contact resistance and superior durability of membrane electrode assembly was achieved. A 75% Pt utilization efficiency was obtained by using the novel CCM structure, whereas the conventional structure gave 60% efficiency. All these features greatly contribute to the increase in DMFC performance. The DMFC with new CCM structure presented a maximum power density of 260 MW cm(-2), but the DMFC with conventional structure gave only 200 mW cm(-2) under the same operation condition. (c) 2005 Elsevier B.V. All rights reserved.