994 resultados para 7038-401


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应用一氯二乙基铝和苄基氯催化剂体系进行了丁苯橡胶的阳离子环化反应。研究了反应温度、苄基氯/ 一氯二乙基铝比例、溶剂、原胶浓度对环化的影响。发现通过控制苄基氯/ 一氯二乙基铝比,可在高温(120℃) 、高原胶浓度(2~4%w/v)下进行丁苯橡胶的环化,制得特性粘度较原胶有大幅度降低,可溶性无凝胶的环化丁苯胶。通过对红外光谱、1H-NMR谱的初步解析,证实了环化反应的发生。

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Linear and nonlinear optical (NLO) properties of KNbO3 in various phases are calculated from their crystal structures. Nonlinear optical tensor coefficients are found to be very sensitive to the atomic geometry, changing as much as 85% between the ferroelectric tetragonal and rhombohedral phases. The predicted principal refractive indices are also found to be sensitive to their structural changes. In the tetragonal phase KNbO3 has the largest NLO responses, in the orthorhombic phase KNbO3 has the relative larger NLO coefficients, and in the rhombohedral structure KNbO3 has the large and homogeneous NLO properties. (C) 1998 Elsevier Science B.V. All rights reserved.

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A series of new macrocyclic aromatic esters have been efficiently synthesized from o-phthaloyl dichloride and various bisphenols, and unambiguously characterized by a combination of GPC, MS(FAB), FTIR and NMR. These macrocyclic oligomers undergo facile ring-opening polymerization in the presence of anionic initiators to give high molecular weight polyarylates.

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高纯氧化钇(Y2O3)作为YA系列激光晶体的重要原材料具有广泛的应用前景。限定有害杂质并使其低于极限含量的超高纯Y2O3的研究是提高YAG、YAP、YVO4等激光晶体质量、发展其他微电子、光电子材料的迫切需求,也是当前国内外十分关注的研究课题。研制在超净的工作环境下,采用改进的离子交换技术,并设法克服由于使用超细树脂而产生的阻力大、流速低,周期长的缺点。通过改变设备的长径比例和体积比例,实现大体积低浓度条件下的除杂工艺,并与络合、沉淀等多种方法联用的综合化学法,逐步去除Y2O3中的稀土和非稀土杂质,使其达

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Melt mixing of nylon 8 with neodymium oxide particles was carried out with a single-screw extruder. The crystal behaviors of plain nylon 6 and the neodymium oxide filled nylon 6 mixture were studied by means of isothermal crystallization kinetic analysis. Isothermal crystallization thermograms obtained by differential scanning calorimetry (DSC) were analyzed based on the Avrami equation. The neodymium oxide particles acted as a nucleating agent in the mixture. The overall rate of di-isothermal crystallization of the neodymium oxide filled nylon 6 mixture is higher than that of plain nylon 6. The mechanism and modes of plain nylon 6 were the same as those of neodymium oxide filled PA6 mixture.

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报道四元杂多化合物K10H3[Nd(SiMo7W4O39)2]·xH2O(简写为Nd(SiMo7W4)213-)聚吡咯(PPy)膜修饰电极的制备及其电化学性能.该电极保持了四元杂多化合物的电化学活性和电催化性能,并具有很好的稳定性,在酸性水溶液中对NO-2具有明显的催化作用.

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采用化学还原法制得直接甲醇燃料电池中甲醇阳极氧化的Pt/C和PtRu/C催化剂.结果表明后者比前者具有更高的催化活性.通过XRD和XPS的分析,阐明了Ru对提高甲醇电催化氧化活性的作用.

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本文合成了标题配合物,对其红外光谱进行了研究.测定了配合物的晶体结构,结果表明,晶体属三斜晶系,P1空间群,单胞参数:α=11.549(2)(?),b=14.122(3)(?),c=15.654(?),α=97.01(2)°,β=102.70(2)°,γ=105.43(2)°,V=2355.94(0.87)(?)~3,Z=2.晶体结构是采用Patterson法和差值Fourier合成解出.经全矩阵最小二乘法修正,最后偏差因子R=0.0337,R_w=0.0364.晶体中甘氨酸与Sm原子的结合方式有三种:第一种甘氨酸的羧基离子以螯合桥式与Sm原子配位;第二种甘氨酸以羧基桥式与同一单元的两个Sm原子配位;第三种甘氨酸以酸基桥式连结两个相邻单元中的相邻Sm原子而形成一维无限长链结构.此外,每个Sm原子还与两个水分子成键,其配位数为9.

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本文采用TG-DTA-DTG等技术研究了铽羧酸配合物的热分解过程,通过对中间产物进行红外光谱、元素分析、确定了热分解机理。采用三种方法尝试求得了希土羧酸配合物热分解过程的活化能和焓变,发现并总结了其相变过程。

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P wave velocity of the pumice sample from the middle Okinawa Trough and andesite sample from vicinity Yingdao volcanic island, Kyushu Japan were measured at temperature (from room temperature to 1500 C) and pressure (from room pressure to 2.4GPa) using a multi-anvil pressure apparatus called the YJ-3000 press. The measured data shows that at low temperature and low pressure (<1GPa, <800degreesC), the P wave velocity of pumice is lower than that of andesite, while at high temperature and high pressure (>1GPa, >800degreesC) the P wave velocity of pumice and andesite. becomes consistent (5.9km/s). The paper points out that 1GPa/800degreesC is the point of thermodynamic phase transformation Okinawa Trough pumice and vicinity andesite, and the point is deeper than 18km.

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This is a report of the study of the authigenic sulfide minerals and their sulfur isotopes in a sediment core (NH-1) collected on the northern continental slope of the South China Sea, where other geophysical and geochemical evidence seems to suggest gas hydrate formation in the sediments. The study has led to the findings: (1) the pyrite content in sediments was relatively high and its grain size relatively large compared with that in normal pelagic or hemipelagic sediments; (2) the shallowest depth of the acid volatile sulfide (AVS) content maximum was at 437.5 cm (> 2 mu mol/g), which was deeper than that of the authigenic pyrite content maximum (at 141.5-380.5 cm); (3) delta S-34 of authigenic pyrite was positive (maximum: +15 parts per thousand) at depth interval of 250-380 cm; (4) the positive delta S-34 coincided with pyrite enrichment. Compared with the results obtained from the Black Sea sediments by Jorgensen and coworkers, these observations indicated that at the NH-1 site, the depth of the sulfate-methane interface (SMI) would be or once was at about 437.5-547.5 cm and the relatively shallow SMI depth suggested high upward methane fluxes. This was in good agreement with the results obtained from pore water sulfate gradients and core head-space methane concentrations in sediment cores collected in the area. All available evidence suggested that methane gas hydrate formation may exist or may have existed in the underlying sediments.

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Based on the ray theory and Longuet-Higgins's linear,model of sea waves, the joint distribution of wave envelope and apparent wave number vector is established. From the joint distribution, we define a new concept, namely the outer wave number spectrum, to describe the outer characteristics of ocean waves. The analytical form of the outer wave number spectrum, the probability distributions of the apparent wave number vector and its components are then derived. The outer wave number spectrum is compared with the inner wave number spectrum for the average status of wind-wave development corresponding to a peakness factor P = 3. Discussions on the similarity and difference between the outer wave number spectrum and inner one are also presented in the paper. (C) 2002 Elsevier Science Ltd. All rights reserved.

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The effective thermal conductivity of graded composites with contact resistance on the inclusion surface is investigated. As an example, we have considered the graded composite media with a spherical particle embedded in a homogeneous matrix, where the thermal conductivity of spherical inclusion is an exponential function k(i) = c exp(betar) (where r is the inside distance of a point in particle from the center of the spherical particle in a spherical coordinate). For both heat contact resistance and perfect contact cases, we have given a reasonable effective medium approximation to calculate the effective conductivity. (C) 2003 Elsevier B.V. All rights reserved.

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Based on the Navier-Stokes equation, an equation describing the Langmuir circulation is derived by a perturbation method when the influences of Coriolis force and buoyancy force are both considered. The approach used in the analysis is similar to the works carried out by Craik and Leibovich [J. Fluid Mech. 73 (1976) 401], Leibovich [J. Fluid Mech. 79 (1977) 715] and Huang [J. Fluid Mech. 91 (1979) 191]. Potential applications of the equation proposed are discussed in the area of Antarctic circumpolar current.

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本文从赤潮发生前的现场模拟实验、赤潮发生时的现场培养实验和赤潮发生过程中的现场调查等方面,较为系统地研究了东海大规模赤潮对微型浮游动物群落结构的影响。 2005年长江口及邻近海区赤潮发生前,赤潮973MC2005-03航次在本海区进行了综合调查,期间分别于4月27日、5月4日和5月8日,在zzf1、zc18a和ra5三个站位利用现场船基培养的方法,研究了添加到赤潮密度106 cells L-1的东海原甲藻(Prorocentrum donghaiense)对微型浮游动物群落结构的影响。结果发现,赤潮密度的东海原甲藻对小型无壳纤毛虫的种群数量影响较大,而对中大型砂壳纤毛虫的影响较小,从而使得微型浮游动物群落有向中大型砂壳纤毛虫演替的趋势。在zzf1站位,小型无壳纤毛虫占绝对优势,添加东海原甲藻72 h后,优势种由管游虫(Cyrtostrombidium sp.)演替为另一种小型无壳纤毛虫急游虫4(Strombidium sp.4);在以中型砂壳纤毛虫百乐拟铃虫(Tintinnospsis beroidea)为优势种的zc18a站位,仍然是以此为优势种,但其在群落中的优势度更加明显;ra5站位也是以小型无壳纤毛虫为主,添加东海原甲藻72 h后,其群落结构由急游虫2(Strombidium sp.2)向中大型砂壳纤毛虫纤毛虫百乐拟铃虫和亚速岛网纹虫(Favella azorica)演替。不同站位微型浮游动物群落结构变化的差异与其本身的群落结构组成有一定关系,也与浮游植物的群落组成有关。zzf1和ra5站位实验组中微型浮游动物的总丰度和总生物量都低于对照组,而zc18a站位变化不明显,这是由于前两个站位实验组中的优势种管游虫(zzf1站位)和急游虫2(ra5站位)的丰度和生物量迅速下降,而zc18a站位实验组的优势种百乐拟铃虫的丰度和生物量比较稳定造成的。 2005年长江口及邻近海区赤潮发生时,赤潮973 MC2005-04航次在本海区进行了综合调查,期间分别于5月26日、5月28日、5月28日和5月29日,在xzm1、srb、sra1和hb8a四个站位利用现场培养的方法,研究了东海大规模赤潮对微型浮游动物群落结构的影响。结果发现,东海大规模赤潮对微型浮游动物群落结构的影响与赤潮藻的密度密切相关:xzm1、srb和sra1站位是赤潮区,两种赤潮藻的总密度分别为,1.3×106 cells L-1、1.8×106 cells L-1和5.6×106 cells L-1,而hb8a站位位于非赤潮区,两种赤潮藻的总密度仅为5×105 cells L-1;实验进行72 h后,在以大型砂壳纤毛虫网纹虫和筒壳虫(Tintinnidium sp.)为主的xzm1、srb和sra1站位,仍然是以这些大型砂壳纤毛虫为主,且其在群落中的百分比显著增大,尤其在赤潮藻密度最高的的sra1站位,这种演替趋势表现的最明显;而在以小型无壳纤毛虫急游虫2为主的hb8a站位,微型浮游动物群落向中型砂壳纤毛虫真丁丁虫(Eutintinnus sp.)演替。培养过程中微型浮游动物总丰度的变化以及总生物量的变化都与赤潮藻的密度密切相关:赤潮藻密度较低的xzm1站位和srb站位变化不大;赤潮藻密度较高的sra1站位则快速下降;而非赤潮区的hb8a站位呈快速上升的趋势。以上结果进一步表明东海大规模赤潮能使微型浮游动物群落向中大型砂壳纤毛虫演替。 在2006年4月18日-5月30日,赤潮973项目MC2006航次在长江口及其邻近海区围绕东海原甲藻和米氏凯伦藻赤潮进行了综合调查。为了研究该过程中微型浮游动物群落结构的变化,我们在南北5个断面共计21个站位进行了取样,样品涉及赤潮发生前期、发生期和消退期。本次调查共发现纤毛虫66种,其中砂壳纤毛虫有8属37种,寡毛类无壳纤毛虫25种,另外还有前口类3属4种。在赤潮发生前之前,小型无壳纤毛虫的丰度普遍较高,平均值为1574 ind L-1,而中大型砂壳纤毛虫的丰度普遍偏低,平均值仅为14 ind L-1;赤潮发生以后,在大多数站位小型无壳纤毛虫的丰度出现不同程度的下降,平均值降为171 ind L-1,而中大型砂壳纤毛虫的丰度出现一定程度的上升,平均值增至216 ind L-1。赤潮消退时,小型无壳纤毛虫丰度的平均值降为109 ind L-1,而中大型砂壳纤毛虫的丰度继续增长,变为401 ind L-1。不同微型浮游动物百分比的统计结果也表明:微型浮游动物群落由小型无壳纤毛虫向中大型砂壳纤毛虫演替的趋势:小型无壳纤毛虫在群落中百分比的平均值由赤潮发生前的62 %变为赤潮发生时的32 %,至赤潮消退时又降为15 %;而中大型砂壳纤毛虫百分比的平均值从赤潮发生前的10 %变为赤潮发生时的24 %,至赤潮消退时增至50 %。典型站位za3、za5、zb7和zb9的结果再次表明了赤潮发生过程中微型浮游动物群落由小型无壳纤毛虫向中大型砂壳纤毛虫演替的趋势。 由以上赤潮发生前的现场模拟实验、赤潮发生时的现场培养实验和赤潮发生过程中的现场调查的结果均可见,东海大规模赤潮可以改变微型浮游动物的群落结构,呈现由小型无壳纤毛虫向中大型砂壳纤毛虫演替的趋势,进而有可能影响中大型浮游动物等摄食者的种群数量和群落结构,最终可能会影响整个海洋生态系统的结构和功能。