红树林植物海榄雌化学成分研究

本论文对红树林植物海榄雌的化学成分进行了研究，对其中分离得到的部分化合物进行了初步的生物活性筛选。 海榄雌采自海南东寨港，样品干燥后用氯仿甲醇（1：1）浸泡提取，合并提取物，先后用石油醚、乙酸乙酯和正丁醇萃取。得到石油醚相、乙酸乙酯相、正丁醇相和水相。 各部分采用常规的硅胶柱层析、制备薄层层析、凝胶Sephadex LH-20柱层析、反相硅胶柱层析、半制备HPLC以及重结晶等手段分离得到28个化合物。利用各种现代波谱技术(IR、UV、ESI-MS、FAB-MS、HR-FAB-MS、1D-NMR、2D-NMR等)，确定了其中20个化合物的结构，其中包括2个新化合物：化合物A1 2′-O-(5-phenyl-2E, 4E-pentadienoyl)mussaenosidic acid和化合物A2 2′-O-(p-methoxycinnamoyl)mussaenosidic acid，以及13个首次从海榄雌中报道的化合物。 对得到的20个化合物A1－A20进行了DPPH自由基清除活性筛选，化合物A4、A5、A6和A16表现出较好的活性，其IC50分别为9.61 μg/mL、8.55 μg/mL、11.72 μg/mL和7.73 μg/mL；化合物A13和A15表现出中等强度的DPPH自由基清除活性，其IC50分别为34.80 μg/mL和44.90 μg/mL；其他化合物只表现出微弱活性，其IC50均大于100 μg/mL；阳性对照BHT的IC50为18.00 μg/mL。 对分离得到的部分样品进行了抑菌活性测试，各样品在测试浓度下对测试菌均未表现出明显的抑菌活性。

中国明对虾病原检测新方法及酚氧化酶通路相关基因的研究

对虾病害在世界范围内肆虐，给水产养殖和沿海农村经济造成了重大损失。在水产养殖的实践中快速检测水产动物的病害并及时采取隔离等措施对于控制病害尤为重要，其中关键的环节就是快速检测出病害，并在对虾免疫机制上寻找对虾疾病防治的有效方法。研究表明当对虾等甲壳动物受到外界病原刺激时，极微量的微生物多糖就可以激活proPO系统。激活过程中涉及和产生一系列活性物质，如黑色素、酚氧化酶原激活因子（PPA）、模式识别蛋白（BGBP、PGBP、LGBP、LBP）及其膜上受体和A2巨球蛋白等，它们可通过多种方式参与防御反应，包括提供调理素，促进血细胞吞噬作用，形成结节或包囊以及介导凝集和凝固，产生杀菌物质并且黑色素化。黑色素常常在节肢动物的体表形成黑色斑点，形成的色素沉着对机体起到保护作用。所以，酚氧化酶原激活的级联反应是节肢动物免疫的关键因素。本论文研究开发了以环等温介导技术（LAMP）为基础的检测对虾白斑病毒（WSSV）和鳗弧菌（V. anguillarum）的快速检测方法。并从对虾对病害的免疫机制为切入点，从中国明对虾体内克隆了酚氧化酶原（PrpPO）和丝氨酸蛋白酶FcSP3这两个免疫系统中重要的基因，分析了它们的分子结构特征，组织分布及应答鳗弧菌病原刺激的表达变化模式。 建立的对虾常见病害对虾白班病毒（WSSV）和鳗弧菌（V. anguillarum）的LAMP检测方法，经过实验比对和Blast检索，发现本研究中使用的引物，比已经报导的LAMP方法或者PCR方法具有更宽的检测范围（更低的假阴性）。检测WSSV的LAMP方法使用病毒的VP28基因设计引物，而鳗弧菌的检测方法使用empA基因设计引物。在方法中，首次提出加入UNG酶和dUTP的措施来预防污染，在实际检测中非常有效。LAMP方法与PCR检测方法的灵敏性比较也进行了研究，二者灵敏性相当。 依据中国明对虾血液cDNA文库提供的部分片段信息，结合SMART-RACE技术，克隆了酚氧化酶原（PrpPO）基因，通过序列比对分析发现，PrpPO基因cDNA全长为3040 bp，其中开放阅读框2061 bp，编码686个氨基酸，其中推测的信号肽为12个氨基酸。推测的序列与斑节对虾（P. monodon）同源性为93%,与短钩对虾（P. semisulcatus.）同源性为92%。real time RT-PCR实验结果表明， ProPO在血细胞中的相对表达量最高，肝胰脏中表达量最低。弧菌刺激实验中注射弧菌，刺激了血细胞和淋巴器官中的ProPO mRNA显著增加，说明在血细胞和淋巴器官中存在快速反应的ProPO通路。而ProPO mRNA量在淋巴器官中在时间上早于血液中升至最高，说明该动物在在病原刚开始入侵的时候先有淋巴器官发挥主要的免疫作用，随着时间推移血细胞便变成主要的免疫器官。 根据中国明对虾肝胰脏cDNA文库提供EST信息，经过SMART-RACE克隆了一个丝氨酸蛋白酶FcSP3基因，通过序列比对分析发现，该丝氨酸蛋白酶基因cDNA全长为1622 bp，其中开放阅读框1431 bp，编码477个氨基酸，其中推测的信号肽为22个氨基酸。推测的序列与疟蚊的丝氨酸蛋白酶（A. gambiae）同源性为33%,与丽蝇蛹集金小蜂的酚氧化酶原激活因子（N. vitripennis）同源性为32%，与东北大黑鳃金龟的酚氧化酶原激活因子（H. diomphalia）同源性为34%。淋巴器官中PPAⅡ表达量约为血液中表达量的47560倍，肝胰脏中的FCSP3表达量为血细胞表达量的6226倍。鳗弧菌注射对虾后，淋巴器官中刺激组和对照组FcSP3的mRNA量在刺激后6小时显著降低，但是刺激组的表达量明显高于对照组。刺激组的血细胞与肝胰脏中FcSP3 mRNA的相对表达量增高。而病原刺激后的血液与肝胰脏中的FcSP3 mRNA的增长趋势也在时间上先与ProPO mRNA。这说明FcSP3对ProPO有正调控的作用，但这个调控有一个时间差，并且在不同组织中有不同的调控效率。

Experimental evaluation of heterobeltiosis and heterosis between two populations of Pacific abalone Haliotis discus hannai Ino

A2 x 2 factorial cross between two populations of Pacific abalone Haliotis discus hannai Ino, collected separately from Dalian (D) in China and Miyagi (M) in Japan, was conducted to compare performances in fertilization rate, hatching rate, metamorphosis rate and growth at days 20, 43, 160 and 330 between purebreds (DD and MM) and crossbreds (DM and MD) and investigate the magnitude of heterobeltiosis (better parent) and heterosis (mid-parent). Heterobeltiosis and heterosis for all the traits analyzed were evidently different between crossbreds DM and MD. Heterobeltiosis in the crossbred DM varied among traits, with values of 2.5% for the fertilization rate, 2.2% for the hatching rate, -1.9% for the metamorphosis rate and 7.4% for the growth at the (lay 330. The crossbred DM displayed positive heterotic values for fertilization rate (5.4%), hatching rate (7.4%), metamorphosis rate (7.6%) and growth (12.0%) at the day 330. However, both heterobeltiosis and heterosis for all the traits in the crossbred MD were negative except those for the growth at days 20 and 43. The results indicate the importance of selecting superior hybrid varieties if the exploitation of hybrid vigor is considered in the Pacific abalone breeding program.

污水生化处理过程仿真及在A~2/O工艺改进中的应用

基于国际水协会IWA发布的国际评价基准Benchmark,建立了与污水处理厂实际特性相近的标准仿真平台。对污水处理传统A2/O工艺做了合理改进,在不影响出水水质的情况下,取消内回流。应用该平台分别对晴天、雨天与暴雨三种天气的工艺过程模拟,验证了工艺改进的合理性。仿真结果表明,与传统A2/O工艺相比,出水指标差别不大,但污泥泵能耗降低约50%。

A/O工艺城市污水生化处理过程建模与优化控制研究

可持续发展的要求增强了人类有效利用资源和环境保护的意识，而城市污水处理过程是水环境保护的一项重要内容。本文针对我国城市污水处理系统能耗高、出水水质不稳定以及工业毒水经常入侵的现状，以A/O工艺城市污水生化处理过程为研究对象，研究通过建模、控制和优化手段提高污水处理系统运行性能和降低运行降耗的理论和方法。论文工作是在国际水协会发布的典型工艺与污水处理厂实际运行环境相结合的基础上完成，内容主要涉及活性污泥模型简化、基于简化模型的工艺改进与过程模拟、仿真平台的建立、关键控制回路设计、工业毒水诊断与应对系统开发以及优化控制方法与应用研究。具体内容包括： (1) 基于国际评价基准benchmark实现了污水生化处理过程的稳态模拟和动态模拟，对A2/O工艺的改进进行了仿真研究和分析，结果表明在保证出水水质稳定达标的前提下，改进工艺由于取消了内回流，大大节约了回流泵的能耗。 (2) 在国际水协会活性污泥模型ASM1模型的基础上，结合我国污水处理过程特点，并充分考虑我国污水处理厂现场测量信息严重不足的现状，对ASM1模型的组分和反应过程进行简化，建立了简化的活性污泥模型，研究了难以测量的模型组分浓度与易测的常规水质指标的转换方法，针对温度对反应速率的影响，研究了模型参数的校正方法。在此基础上，开发了A/O工艺污水生化处理过程模拟与仿真平台，并对辽宁某污水处理厂的实际运行过程进行了模拟，取得了较好的模拟结果。 (3) 建立了完整的城市污水处理过程控制系统设计框架，引入入水有机负荷和比耗氧速率分别表征微生物（活性污泥）的“食物”（有机物）数量和微生物活性，进行了系统动态特性分析，在此基础上完成了入水流量串级控制、污泥浓度前馈－反馈控制、溶解氧前馈－串级控制三个控制回路的设计。针对溶解氧控制过程采用了仿人智能控制方法，在实际应用中取得了较好的控制效果。 (4) 针对城市污水处理厂经常遇到的工业毒水侵入的问题，开发了基于专家经验的工业毒水诊断与应对系统，编写了较为完备的专家规则，系统能够在毒水侵入时及时发出警报，并采取相应的应对措施，最大程度的降低污水处理厂的损失，该系统在辽宁某污水处理厂取得了较好的应用效果。 (5) 在优化控制方面，针对污水处理过程能耗过高的问题，设计了A/O工艺城市污水处理过程的优化控制策略。建立了只考虑底物与微生物两种组分的简化活性污泥模型，以溶解氧浓度和污泥排放量为决策变量，以污水处理厂日运行费用为性能指标，以物料平衡、水质排放标准等限制为约束条件，建立了完整的优化控制模型，实现了污水处理过程的最优控制，采用基于最优步长参数动态搜索的改进型梯度法进行最佳运行工况寻优。通过对辽宁某城市污水处理厂的优化，获得了当前溶解氧浓度设定值和污泥排放量的最优值，在保证出水水质稳定达标的前提下，污水处理厂日运行费用显著降低，为污水处理厂的实际操作提供了指导。

一种新型四自由度并联机器人

提出一种用铅垂导轨上 4个滑块作为原动件的新型四自由度并联机器人 .该并联机器人的动平台能够实现两个方向的移动以及绕两个方向轴线的转动 .研究了该并联机器人的运动学建模方法 ,给出了运动学正、逆解 ,用 Grassmann几何法分析了该并联机器人在其工作空间内不会出现奇异形位 .基于该四自由度并联机器人可以非常方便地开发具有大工作空间的五轴联动数控机床

四滑块平台机构及其运动学建模

提出一种用水平导轨上 4个滑块作为原动件的混合型 4自由度并联平台机构 ,该机构的动平台能够实现 2个方向的移动以及绕 2个方向轴线的转动。研究了该机构的运动学建模方法 ,给出了运动学正逆解 ,并阐述了其应用前景

并联机床平面约束机构误差分析与建模

针对五轴数控机床平面约束机构进行了误差分析 ,指出了并联机床平面约束机构误差主要影响因素为机构的制造误差和安装误差·前者与由其引起的约束机构顶边中点沿x方向的位移成非线性关系 ,而后者则成线性关系·提出了一种依据测量数据反演非线性误差模型的建模方法 ,给出了五轴并联机床约束机构实测信息与模型输出间的多项式误差模型·比较仿真结果与测量结果可知 ,基于上述方法建立的误差模型精确 ,进而利用该模型对机床进行实时精度补偿 ,可使机床x方向定位精度大为提高

基于测量数据反演并联机床非线性位姿误差模型

利用最小二乘技术识别模型参数 ,将非线性问题作线性化处理 ,提出了一种基于测量数据反演非线性误差模型的建模方法。结合算例 ,指出了此类模型设计应注意的问题。五轴并联机床约束机构误差模型仿真结果表明 ,由此得到的误差模型精度高。利用所得模型对机床位姿进行补偿 ,即可提高机床沿该位姿方向的定位精度

一种四自由度并联机构及其运动学建模

提出一种新型四自由度并联平台机构 ,该机构的动平台能够实现两个方向的移动 ,以及绕两个方向轴线的转动。研究了该机构的运动学建模方法 ,给出了运动学正、逆解。阐述其应用前景

一种四滑块驱动的并联机构及其运动学建模

提出了一种用水平导轨上 4个滑块作为原动件的 4自由度并联平台机构 ,该机构的动平台能够实现两个方向的移动以及绕两个方向轴线的转动 ,同时研究了该机构的运动学建模方法 ,给出了运动学正、逆解 ,并阐述了其应用前景。

基于四自由度并联机构的数控机床研究

介绍一种基于混合型四自由度并联平台机构开发的五坐标并联机床 .由于其独特的机构设计 ,与基于 Stewart平台的并联机床相比 ,X方向的进给运动与运动平台分离 ,改由工作台单独进给 ,因而其工作空间成倍增大 .采用龙门框架结构和滚珠丝杠支承方案使机床获得更高的刚度 .给出了该机床运动学逆解 ,控制系统采用基于 PC的数控系统进行五轴联动控制

四坐标位姿测量仪设计研究与误差分析

四坐标位姿测量仪是针对某轻型汽车底盘前悬置横梁上四孔位姿测量而设计的新型仪器·该测量仪以六自由度并联机构作为执行机构 ,能够迅速准确地到达被测孔的实际位置 ,测量头具有对非测量参数误差的自适应和自调整能力·采用比较法实现参数测量·该机构结构新颖 ,测量效率高·系统分析研究了各因素造成的测量误差 ,指出了减小测量误差的措施 ,从而为精确设计测量仪提供了可靠依据·

混凝土泵车布料机构自动浇筑及过程仿真

机器人化是提高工程机械施工控制自动化的关键问题·通过将泵车布料机构的浇筑区域离散为浇筑点集 ,对两浇筑点内轨迹利用冗余度机器人学的最小关节范数法的轨迹规划 ,并将两相临浇筑段自动连接和自动协调 ,从而实现了混凝土泵车布料机构浇筑过程自动轨迹规划·

黄东海及朝鲜海峡冰后期陆架沉积物的环境磁学研究

There are four chapters in this dissertation. The first chapter briefly synthesizes the basic theories, methods and present-day applying situation of environmental magnetism. The second chapter probes into the magnetic mineral diagenesis in the post-glacial muddy sediments from the southeastern South Yellow Sea and its response to marine environmental changes, using the muddy sediment of Core YSDP103 formed in the shelf since about 13 ka BP. The third chapter illustrates the high-resolution early diagenetic processes by investigating the rapidly deposited muddy sediments during the last 6 ka in Cores SSDP-102 and SSDP-103 from the near-shore shelf of Korea Strait. The fourth chapter presents the results of detailed rock magnetic investigation of the surface sediments from the fine-grained depositional area on the outer shelf of the East China Sea in an attempt to provide environmental magnetic evidence for the provenance of the fine-grained deposit. Core YSDP103 was retrieved in the muddy deposit under the cold eddy of the southeastern South Yellow Sea, and the uppermost 29.79 m core represents the muddy sediments formed in the shelf since about 13 ka BP. The lower part from 29.79 to 13.35 m, called Unit A2, was deposited during the period from the post-glacial transgression to the middle Holocene (at about 6 ~(14)C ka BP) when the rising sea level reached its maximum, while the upper part above 13.35 m (called Unit Al) was deposited in a cold eddy associated with the formation of the Yellow Sea Warm Current just after the peak of post-glacial sea level rise. For the the uppermost 29.79 m core, detailed investigation of rock-magnetic properties and analyses of grain sizes and geochemistry were made. The experimental results indicate that the magnetic mineralogy of the core is dominated by magnetite, maghemite and hematite and that, except for the uppermost 2.35 m, the magnetic minerals were subject to reductive diagenesis leading to significant decline of magnetic mineral content and the proportion of low-coercivity component. More importantly, ferrimagnetic iron sulphide (greigite) is found in Unit A2 but absent in Unit Al, suggesting the control of marine environmental conditions on the magnetic mineral diagenesis. Magnetic parameters show abrupt changes across the boundary between the Unit Al and A2, which reflects a co-effect of environmental conditions and primary magnetic components of the sediments on the diagenesis. Alternating zones of high and low magnetic parameters are observed in Unit A2 of Core YSDP103, which is presumably due to periodic changes of the concentration and/or grain size of magnetic minerals carried into the study area. Cores SSDP-102 and SSDP-103, two studied sediment cores from the Korea Strait contain mud sequences (14 m and 32.62 m in thickness) that were deposited during the last 6,000 years. Analyses of grain sizes and geochemistry of the cores have demonstrated that the sediments have uniform lithology and geochemical properties, however, marked down-core changes in magnetic properties suggest that diagenesis has significantly impacted the magnetic properties. An expanded view of early diagenetic reactions that affect magnetic mineral assemblages is evident in these rapidly deposited continental shelf sediments compared to deep-sea sediments. The studied sediments can be divided into four descending intervals, based on magnetic property variations. Interval 1 is least affected by diagenesis and has the highest concentrations of detrital magnetite and hematite, and the lowest solid-phase sulfur contents. Interval 2 is characterized by the presence of paramagnetic pyrite and sharply decreasing magnetite and hematite concentrations, which suggest active reductive dissolution of detrital magnetic minerals, the absolute minimum abundance of magnetite is reached at the end of this interval. Interval 3 is marked by a progressive loss of hematite with depth, and at the base of this interval, 82% to 88% of the hematite component was depleted and the bulk magnetic mineral concentration was reduced to the lowest value in the entire studied mud section. Interval 4 has an increasing down-core enhancement of authigenic greigite, which is interpreted to have formed due to arrested pyritization resulting from consumption of pore water sulfate with depth. This is the first clear demonstration from an active depositional environment for a delay of thousands of years for acquisition of a magnetization carried by greigite. This detailed view of diagenetic processes in continental shelf sediments suggests that studies of geomagnetic field behavior from such sediments should be conducted with care. Paleoceanographic and paleoclimatic studies based on the magnetic properties of shelf sediments with high sedimentation rates like those in the Korea Strait are also unlikely to provide a meaningful signature associated with syn-depositional environmental processes. The rock magnetic properties of the surface sediments from the fine-grained depositional area on the outer shelf of the East China Sea, an area surrounded by sands, are investigated with a view to providing information on the sediment provenance. Multiple magnetic parameters such as magnetic susceptibility (%), anhysteretic remanent magnetization (ARM), saturation rernanent magnetization (SIRM), coercivities of SIRM (Her), and S ratios (relative abundance of low-coercivity magnetic minerals) are measured for all 179 surface samples, and partial representative samples are examined for their magnetic hysteresis parameters, temperature-dependence of magnetic susceptibility and x-ray diffraction spectra. Our research indicates that the magnetic mineralogy is dominated by magnetite with a small amount of hematite and is primarily of pseudo-single domain (PSD) to multidomain (MD) nature with a detrital origin. In the surface sediments, the granulometry of magnetic fractions is basically independent of grain sizes of the sediment containing the magnetic grains, and the composition of magnetic minerals remains almost homogeneous, that is, with a relatively constant ratio of low to high coercivity fraction throughout the area. The magnetic concentration in the study area generally decreases to the east or southeast accompanied by magnetic-particle fining to the east or to the northeast. The geographic pattern of magnetic properties is most reasonably explained by a major source of sediment jointly from the erosion of the old Huanghe River deposit and the discharge of the Changjiang River. The rock magnetic data facilitate understanding of the transport mechanism of fine-grained sediments in the outer shelf of the East China Sea.