双环戊二烯的催化氢脂基化制备三环单,双酯

双环戊二烯(DCPD)通过均相催化与一氧化碳及乙醇或甲醇反应生成四种三环单酯或三种三环双酯,其反应式如下:     

高效液相色谱法测定镇咳药中左旋羟基苯哌嗪含量

建立了高效液相色谱法(HPLC)测定镇咳药中左旋羟基苯哌嗪含量的方法,运用二极管阵列检测器(PAD),C18反相柱,以甲醇∶水(冰醋酸HAc调节pH值为6.5)∶三乙胺(TEA)(30∶70∶0.5,V/V/V),为流动相测定了3批镇咳药(利咳净糖浆)中左旋羟基苯哌嗪的含量分别为5772.65、809.25、833.2μg/mL,变异系数小于2%,回收率为99.1%~100.2%.该方法快速,精密度及准确度在允许范围内,可作为镇咳药中左旋羟基苯哌嗪的测定方法.     

液相色谱法测定地质样品中的芳香化合物

发展了用液相色谱法检测地质样品中芳香化合物的方法。对观察到的色谱峰进行了定性分析，了该法对油气地球化学勘探的意义。     

4,4’-二苯甲酰基联苯构象的分子力学研究

4,4’—二苯甲酰基联苯有两个三岔点,属于二元三岔共轭体系。从结构式上看,卽可把它作为二苯甲酮骨架的取代产物,又可看作是在联苯骨架上的取代。作为系统研究三岔共轭体系结构效应的部分工作,我们用QCFF/PI+MCA(Quantum Mechanical Extension of the Consistent Force Field to PI Electron System+Molecular Crystal Analysis)程序研究了其晶态和孤立态(气态)构象。研究结果表明,在孤立态中,联苯基的二个苯环的最小二乘     

紫外光度法间接测定脱脂乳中的芽孢数量

为了有效控制乳制品生产过程、保证质量,克服芽孢杆菌传统计数方法周期长的缺点,本实验通过分光光度法检测芽孢中特异性物质2,6-吡啶二羧酸(DPA)。根据DPA浓度与芽孢数量的关系,建立了快速检测脱脂乳中芽孢数量的方法。本研究对脱脂乳及其芽孢处理、DPA释放及采用紫外分光光度法检测做了研究。通过准确度和加标回收率检验,建立DPA含量与芽孢数的线性关系,回归方程为y=0.2084x-0.9363,r=0.6998,经验证可有效估测脱脂乳中芽孢数量(P<0.05)。     

超声波辐射下的固—液相转移催化法合成苯乙酰基芳基硫脲化合物

合成酸基硫减类化合物常用的方法是固一液相转移催化法“‘．因超声波辐射可以加快有机合成反应，提高产率，本文采用了超声波辐射与相转移催化相结合的方法，以聚乙二醇一400（PEG－400）为催化剂，二氯甲烷为溶剂，在常温下合成了10种N一苯乙酸基一N‘一芳基硫腺新化合物，产率大部分比相应的相转移催化法合成高．本法条件温和、操作简便、产率较高．仪器为CQ－250型超声波清洗器，频率33土2kHZ；PE1730FT－IR红外光谱仪，溪化钾压片；BRUKERAC七0核磁共振仪，CDCI。为溶剂，TMS为内标；PE－2400CHN元素分析仪．化合物（皿…     

Iron speciation related to color of Jurassic sedimentary rocks in Turpan Basin, northwest China

Mesozoic-Cenozoic reddish and green beds are widely distributed in northwest China. Mössbauer spectroscopy revealed that the composition of iron species varies with color in the middle-upper Jurassic sedimentary rocks from the Turpan Basin. Three main kinds of iron species were identified: (1) ferric iron of hematite (hem-Fe³⁺), (2) paramagnetic ferric iron (para-Fe³⁺), and (3) paramagnetic ferrous iron (para-Fe²⁺). Pyrite iron (pyr-Fe²⁺) was revealed only in a few samples. In general, there is a direct correlation between rock color, iron species and total iron content, however, in detail, this relationship is more complicated. The reddish rocks contain higher contents of total iron and hem-Fe³⁺, whereas the gray rocks contain much more para-Fe²⁺. However, relatively low hematite content cannot give red color to rocks, probably due to suppression by other pigments such as organic matter in black or chlorite in green. The dark or green rocks normally contain either only paramagnetic Fe²⁺ and paramagnetic Fe³⁺ species or these two species associated with hematite Fe³⁺, but the relative content of hematite species is lower. The variations of different iron species control lithological properties such as color and also may reflect the sedimentary conditions. Moreover, iron speciation in these rocks is one of the main factors, which result the color features of rocks in remote sensing imagery.This revised version was published online in November 2005 with corrections to the Cover Date.