2-乙基己基磷酸单(2-乙基己基)酯萃淋树脂分离-火花源质谱法测定高纯氧化镱中痕量稀土杂质

本文采用萃取色谱法以2-乙基已基膦酸单(2-乙基已基)酯(P_507)萃淋树脂为固定相,以HCI-NH_4CI体系为淋洗液,研究了99.999%~99.9999%的高纯Yb_2O_3中稀土杂质和Yb基体的分离条件,将杂质淋洗液富集于复合螯合剂-活性碳上,经灼烧灰化后制成样品电极,进行质谱测定.测定下限达 0.01~0.05 μg/g,可用于高纯 Yb_2O_3中杂质的测定.回收率在80%以上.

Construction of bacterial artificial chromosome libraries for Zhikong Scallop Chlamys farreri

Two Large-insert genomic bacterial artificial chromosome (BAC) libraries of Zhikong scallop Chlamys farreri were constructed to promote our genetic and genomic research. High-quality megabase-sized DNA was isolated from the adductor muscle of the scallop and partially digested by BamH I and Mbo I, respectively. The BamH I library consisted of 53 760 clones while the Mbo I library consisted of 7 680clones. Approximately 96 % of the clones in BamH I library contained nuclear DNA inserts in average size of 100 kb, providing a coverage of 5.3 haploid genome equivalents. Similarly, the Mbo I library with an average insert of 145 kb and no insert-empty clones, thus providing a genome coverage of 1.1 haploid genome equivalents.

Assembly of the protoplasm of Codium fragile (Bryopsidales, Chlorophyta) into new protoplasts

The cell organelles of the coenocytic alga Codium fragile (Sur.) Hariot aggregated rapidly and protoplasts were formed when its protoplasm was extruded out in seawater. Continuous observation showed that there were long and gelatinous threads connecting the cell organelles. The threads contracted, and thus the cell organelles aggregated into protoplasmic masses. The enzyme digestion experiments and Coomassie Brilliant Blue and Anthrone stainings showed that the long and gelatinous threads involved in the formation of the protoplasts might include protein and saccharides as structure components. Nile Red staining indicated that the protoplast primary envelope was non-lipid at first, and then lipid materials integrated into its surface gradually. The fluorescent brightener staining indicated that the cell wall did not regenerate in the newly formed protoplasts and they all disintegrated within 72 h after formation. Transmission electron microscopy of the cell wall of wild C. fragile showed electron-dense material embedded in the whole cell wall at regular intervals. The experiments indicated that C. fragile would be a suitable model alga for studying the formation of protoplasts.

小型桡足类种群动力学研究

小型桡足类在生态系统中的重要作用近年来得到了广泛的关注，在近岸生态系统中，小型桡足类起着相当重要的作用。但关于小型桡足类种群动力学的研究在国内还处于起步阶段，因此我们选取了国内沿岸海域常见优势种小拟哲水蚤、双刺纺锤水蚤、太平洋纺锤水蚤及强额拟哲水蚤等四种小型桡足类为研究对象，探讨其种群动力学相关方面的变动机制。本文在2005年10月－2006年9月选取胶州湾为主要的研究海域，进行了一周年的小型桡足类的采样和培养实验研究。在胶州湾，小拟哲水蚤（Paracalanus parvus）全年出现，其种群数量变动呈现双峰型，在夏季（6月和8月）达数量高值，在冬季（1月）有一个小的高峰。种群数量在4月达全年最低值，在7月份数量也有一个明显的数量降低。从空间分布上来讲，该水蚤在冬季主要以CV期桡足幼体存在于湾南和湾外区域，湾北数量很少；从春末开始，各期幼体开始在各海区广泛分布。小拟哲水蚤在胶州湾几乎全年产卵（2月份除外），但较高的产卵率主要集中在春末到秋初，最大产卵率出现在5月，达27.9 eggs female-1d-1。总体来讲，在胶州湾小拟哲水蚤的产卵率与温度、叶绿素及体长均呈显著正相关，但与盐度呈负相关关系。从不同的区域来看，胶州湾湾北区域小拟哲水蚤产卵率较高，最高值出现在湾北6月份，产卵率达到了60.8 eggs female-1d-1。大于10 eggs female-1d-1的产卵率在湾北持续了6个月（4－9月），在湾口持续了5个月（4－8月），而在湾外只持续了3个月（5－7月）。小拟哲水蚤生物量在6月份达到最高值（6.15 mg C m-3），在4月达到全年最低值（0.028 mg C m-3）。次级生产的变动从4月到9月与生物量的变动趋势完全相似，但冬季生物量的高峰并没有伴随次级生产的高峰值，分析其原因是由于冬季低的生长率所致。小拟哲水蚤在整个胶州湾平均的年次级生产为158.41 mg C.m-3yr -1。强额拟哲水蚤（Paracalanus crassirostris）在胶州湾只在夏末到秋季出现，最大数量出现在8月份。从强额拟哲水蚤的分布区域来看，从湾内到湾外有递减趋势。在2006年9月份，只有湾北有部分种群，其他区域几乎没有该种出现。该种最大产卵率出现在8月，达11.2 eggs female-1d-1。强额拟哲水蚤生物量的变动与次级生产的变动趋势相似，最大值也都出现在8月份。该水蚤在胶州湾平均年次级生产仅为2.12 mg C m-3yr-1。双刺纺锤水蚤(Acartia bifilosa)在胶州湾是全年出现，其种群数量在5－6月份突发性增加达全年最高值（>8000 ind. m-3），之后又急剧下降。从该种的区域分布来看，5－6月份数量的高峰主要出现在湾北区域，7月份虽然各区域数量均下降，但大部分种群集中在湾外区域。双刺纺锤水蚤在胶州湾几乎全年产卵（1－2月除外），产卵率的最高值出现在4月，达16.5 eggs female-1d-1。4月份雌体高的产卵率为5月份种群数量的大量增加提供了补充。双刺纺锤水蚤生物量与次级生产的变动趋势一致，在5－6月份达到高值，在秋冬季次级生产较低。双刺纺锤水蚤在整个胶州湾平均的年次级生产为114.61 mg C m-3yr-1。太平洋纺锤水蚤（Acartia pacifica）在胶州湾季节性出现，在冬春季节消失，从夏季开始出现。该种在5月零星出现，种群数量在6月份开始增多，到7月份达到最高值2356 ind. m-3，之后在8月数量锐减至196 ind. m-3。从区域分布来看，该水蚤在胶州湾只出现在湾北和湾南区域，湾外区域几乎没有，而且呈现湾北到湾南递减的趋势。6月份数量大部分出现在湾北区域，到7月份才有一部份在湾南出现。太平洋纺锤水蚤在其出现季节均产卵，最大产卵率出现在6月份，达37.17 eggs female-1 d-1，部分补充了7月份太平洋纺锤水蚤种群数量的大量增加。太平洋纺锤水蚤生物量与次级生产的变动趋势相似，在7月份达到了最高值，在11月达到最低值。太平洋纺锤水蚤在胶州湾平均的年次级生产为45.63 mg C m-3yr-1。胶州湾四种小型桡足类总的年次级生产为~320 mg C m-3 yr-1。

Relevance of molecular weight of chitosan and its derivatives and their antioxidant activities in vitro

The antioxidant potency of different molecular weight (DMW) chitosan and sulfated chitosan derivatives was investigated employing various established in vitro systems, such as superoxide (O-2(.-))/hydroxyl ((OH)-O-.) radicals scavenging, reducing power, iron ion chelating. As expected, we obtained several satisfying results, as follows: Firstly, low molecular weight chitosan had stronger scavenging effect on O-2(.-) and (OH)-O-. than high molecular weight chitosan. For example the O-2(.-) scavenging activity of low molecular weight chitosan (9 kDa) and high molecular weight chitosan (760 kDa) were 85.86 % and 35.50 % at 1.6 mg/mL, respectively. Secondly, comparing with DMW chitosan, DMW sulfated chitosans had the stronger inhibition effect on 0(2)(.-). At 0.05 mg/mL, the scavenging activity on O-2(.-) reached 86.26 %, for low molecular weight chitosan sulfate (9 kDa), but that of low molecular weight chitosan (9 kDa) was 85.86 % at 1.6 mg/mL. As concerning chitosan and sulfated chitosan of the same molecular weight, scavenging activities of sulfated chitosan on superoxide and hydroxyl radicals were more pronounced than that of chitosan. Thirdly, low molecular weight chitosan sulfate had more effective scavenging activity on 02 and (OH)-O-. than that of high molecular weight chitosan sulfate. Fourthly, DMW chitosans and sulfated chitosans were efficient in the reducing power, especially LCTS. Their orders were found to be LCTS > CTS4 > HCTS > CTS3 > CTS2 > CTS1 > CTS. Fifthly, CTS4 showed more considerable ferrous ion-chelating potency than others. Finally, the scavenging rate and reducing power of DMW chitosan and sulfated derivatives increased with their increasing concentration. Moreover, change of DMW sulfated chitosans was the most pronounced within the experimental concentration. However, chelating effect of DMW chitosans were not concentration dependent except for CTS4 and CTS1. (C) 2004 Elsevier Ltd. All rights reserved.

巨穗小麦种质株高的基因定位

巨穗小麦新种质材料是一具有茎杆粗壮、叶片短宽直立、大穗、大粒、高结实率等特点的种质资源。本研究应用单体分析和双端体分析方法对241材料进行了遗传学研究。结果表明，小麦新种质材料241的1A，3A，5A和4B染色体上具有控制株高的隐性基因，6B染色体上具有控制株高的显性基因，其中3A，5A和6B染色体上的基因表现为强效，1A和4B染色体上的基因表现为弱效。通过双端体分析进一步将控制株高的基因定位到1AS，3AS，5AL和4BL上。

PUMA760切割作业力与位置混合控制

本文介绍在 PUMA760 上实现了的切割作业控制系统。我们在 PUMA760 控制系统中引进了力传感器信号,加入了力控制算法,通过调整机器人手部位置,控制机器人与环境物体间的相互作用力。在 VAL 系统中加入了根据传感器信号动作的指令,实现了一种机器人力与位置的混合控制。用扩充后的 VAL 系统编程,成功地使 PUMA760完成了多种材料的切割作业。

VAL系统的分析和部分改进

本文是对PUMA－760型机器人的主控制器软件，并进行向VAL－II系统改进。PUMA－760是属于程序控制系统类型的机器人，它包括时间控制装置，信息处理器和执行装置。PUMA－760 的系统控制方式是采用分级控制方式，由一台 PDP－11/23机和八台八位微机组成的二级控制系统，PDP-11/23 作为主控机，六台微机分另对六个轴进行伺服控制，一台微机用于示教盒控制，最后一台微机用于软盘管理。VAL-II 系统在 VAL 系统的基础上，加入了数值运算功能，网络管理和结构化程序设计语句，使得 VAL-II 语言更加清晰，它的向条结构化语句类似于 PASCAL语言中的结构语句（面向用户），网络管理上它采用DEC公司的网络设计标准，数值运算由于引进了浮点运算器，所以它比起 VAL 语言有更强的运算能力。目前汉字卡片的应用，使得终端汉字化成为可能，这里暂且进行了显示信息的改造。关于传感器指令，经分析VAL系统，我所的 PUMA－760 已具备力觉，视觉等指令。

Model 75图象处理系统止软件开发方法的研究

Model 75是一个先进的图象处理机，它大量采用了先进的硬件技术，从而使其具有一般通用机无法相比的强大处理能力。System 575是运行于Model 75上的图象处理软件系统。它有比较完善的图象处理能力，然而System 575却没有一种好的软件开发方法，致使我所购进Model 75以来没能充分利用它的强大能力。针对这种情况，本文探讨了一种能自由运用Model 75的软件开发方法。由于Model 75不同于一般的通用机，因而很好地使用Model 75必须建立在对它的结构有清楚的了解的基础上。本文在大量实验的基础上对Model 75的结构及功能特点做了分析。为验证本人对Model 75的理解和本文所述方法的正确性，本人做了两个较大的实验，一个是运动模糊图象的恢复，一个是道路寻找的可变此值方法。本文介绍了这两个实验。实验表明本文所述的开发方法是有效的，解决了在Model 75上开发软件的难题。

基于三重震相波形模拟研究亚洲东北部上地幔过渡带速度结构

Both the global and regional P wave tomographic studies have revealed significant deep structural heterogeneities in subduction zone regions. In particular, low-velocity anomalies have been observed beneath the descending high-velocity slabs in a number of subduction zones. The limited resolution at large depths and possible trade-off between the high and low velocities, however, make it difficult to substantiate this feature and evaluate the vertical extent of the low-velocity structure. From broadband waveform modeling of triplicated phases near the 660-km discontinuity for three deep events, we constrained both the P and SH wave velocity structures around the base of the upper mantle in northeast Asia. For the two events beneath the southern Kurile, the rays traveled through the lowermost transition zone and uppermost lower mantle under the descending Pacific slab. Our preferred models consistently suggest normal-to-lower P and significantly low SH velocities above and below the 660-km discontinuity extending to about 760-km depth compared with the global IASP91 model, corroborating previous observations for a slow structure underneath the slab. In contrast, both high P and SH velocity anomalies are shown in our preferred models for the Japan subduction zone region, likely reflecting the structural feature of a slab stagnant above the 660-km discontinuity. The velocity jumps across the 660-km discontinuity were found to be on average 4.5% and 7% for P and S waves under the south Kurile, and 3% and 6% under the Japan subduction zone. The respective velocity contrasts in the two regions are consistent with mineralogical models for colder slab interior and hotter under-slab areas. Based on mineral physics data, the depth-averaged ~1.5% P and ~2.5% SH velocity differences in the depth range of 560-760 km between the two regions could be primarily explained by a 350~450K temperature variation, although the presence of about 0.5wt%~1wt% water might also contribute to the subtle velocity variations near the base of the transition zone in the southern Kurile. From our modeling results, we speculate that the slow structure in the southern Kurile may be correlated to the low velocity zone observed previously around the 410-km discontinuity under Northern Honshu. Both are probably associated with a thermal anomaly rooted in the lower mantle beneath the subduction zone in northeast Asia.

五台山区义兴寨岩体、车厂－北台岩体地球化学和变质作用及其大地构造意义

There are many Archean TTG grey suites in the Wutaishan area, northern Shanxi Province, China. In the past one hundred years, many geologists have done excellent research work in the Wutaishan and its adjacent regions. However, the TTG suites were almost neglected. Located in the northern slope of Mt. Hengshan-namely the Archean Hengshan Island Arc, intruded the Zhujiafang supercrustal rocks at almost 2.5Ga, the Yixingzhai TTG Suite is originated from partial melting of the ancient lower crust upper mantle by REE and trace elements, and the emplacement occurred in an Archean island arc. The rocks are mainly of tonalitic, I type, and calc-alkaline trends are found in the magmatic evolution. At almost 1.8 Ga, the suite was transformed to be dome-like schists in an arc-arc collision event, and the rocks were metamorphosed to an extent of amphibolitic to granulitic facies. The peak metamorphic condition is of 710-760 ℃/0.68-0.72GPa, and the subsequent cooling history is recorded as 560-620 ℃/0.46-0.60GPa. In the center of the Mt. Wutaishan-known as the Archean Wutaishan Island Arc, intruded the Archean Chechang-Beitai TTG Suite, which is of 2.5Ga old and of trondhjemitic and tonalitic, with coexisting I- and S-types and a trondhjemitic magmatic evolution trend. Through REE and trace elements, the suite is believed to be from the partial melting of the ancient lower crust or upper mantle. The 1.8 Ga collision event also made the suite gneissic and the it was metamorphosed to be amphibolitic facies, whose peak condition is approximately of 680 (±50) ℃/0.7Gpa, and the subsequent cooling process is recorded as 680 (±50) ℃、550(±50) ℃、420(±10) ℃. Crustal growth is fulfilled through magmatic intrusion as well as eruption at about 2.5Ga, arc-arc collision at about 1.8 Ga in the Wutaishan area and its environs. Additionally, the biotite-muscovite and muscovite-plagioclase geothermometers are refined, and the biotite-hornblende geothermometer is developed in this dissertation.

华南地壳岩石弹性和变形性质的高温高压实验研究

The South continent of China lies to southeast of Eurasia block. It is an active area from the view of crust growth and continent spread and is a transition zone between continental crust and oceanic crust. The compressional wave velocities and anisotropies of typical crustal metamorphic rocks were determined at high temperature (up to 1000 ℃) and high pressure(up to 800MPa). The experimental results show that the velocities generally increase with pressure, and is unaffected by temperature up to around 550 ℃. But the velocities of all experimental samples start to drop above a temperature point. For an example, this greatly reduce the speed of wave propagation in amphibolite and serpentinite above 760 ℃ and above 550 ℃ respectively, which may be due to dehydrate of amphibole and serpentine. P-wave anisotropy coefficients of those rocks range from 2% to 10% at 800MPa and 500 ℃. The anisotropies decrease with increasing pressure at room temperature, but hardly change as function of temperature at constant 800MPa or 600MPa pressure. The average velocity of the six crustal rocks is 6.28km/s under the condition of 800MPa and 550 ℃, which is consistent with the result of deep seismic sounding data. Based on this experimental result, we deduce there may exist a lot of felsic granulites and amphibolites at the depth of 15-25km underground. With increasing temperature and pressure, the deformation behavior of the rocks undergoes from localized brittle fracture, semi-brittle deformation (cataclastic flow or semi-brittle faulting, semi-brittle flow) to homogeneous crystal-plastic flow. This transition is associated with mechanical behavior and micro-mechanism. It is very important to understanding earthquake source mechanics, the strength of the lithosphere and the style of deformation. The experiments were conducted at temperature of 600-1000 ℃, confining pressure of 500MPa, and stain rates of 10~(-4)-10~(-6) S~(-1). For fine-grained natural amphibolite, the results of experiments show that brittle faulting is major failure mode at temperature <600 ℃, but crystal-plastic deformation is dominate at temperature >800 ℃, and there is a transition with increasing temperature from sembrittle faulting to cataclastic flow and sembrittle flow at temperature of 670-750 ℃. For medium-grained natural Felsic granulite, the results of experiments show that brittle faulting is major failure mode at temperature <500 ℃, but crystal-plastic deformation is dominate at temperature >700 ℃, and there is a transition with increasing temperature from semibrittle faulting to cataclastic flow and sembrittle flow at temperature of 500-600 ℃.

富磷过铝质岩浆体系的实验研究

富磷过铝质岩浆是过铝质岩浆体系中的一个重要类型，它通常以富P，高ASI[铝饱和指数，Al2O3/(Na2O+K2O+CaO)摩尔比值]，贫Fe、Mg、Ca，强烈亏损REE、Th、Y，与稀有金属(W、Sn、Be、Nb、Ta)矿化具有成因联系为特征。富磷过铝质岩浆体系的性状及其演化的地球化学特征、岩浆液态分离、磷酸盐-硅酸盐矿物对平衡对熔体相中磷的制约以及富磷过铝质岩浆－热液体系中微量元素(包括REE)地球化学行为等科学问题尚未得到系统解决，目前更缺乏实验地球化学的直接证据。对上述科学问题的研究、探索，将有助于了解富磷过铝质岩浆体系形成和演化的地球化学特征，有助于揭示磷对微量元素(包括稀有、稀土元素)地球化学行为的影响，这对于理解过铝质岩浆体系成岩、成矿作用过程具有重要的理论和实际意义。 本文以天然钠长花岗岩为初始物，针对上述内容，开展了不同PTX条件下高温高压下实验研究，获得了如下重要认识： 1) 确定了100 MPa条件下磷对过铝质岩浆液相线温度的影响。随着体系中P2O5的含量增大，液相线温度由1.91 wt%P2O5的780 C降至4.83 wt%P2O5的760C、7.71 wt%P2O5的740 C，即体系中每增加1 wt%P2O5，液相线温度降低约7~10 C； 2) 不同PTX条件下的实验产物中均未见不混溶球粒结构、乳滴结构或流动构造，初步推断富磷过铝质岩浆体系中可能不存在单纯由磷引起的岩浆液态分离现象； 3) 锰铝榴石-磷灰石矿物平衡反应制约着形成过铝质初始岩浆中P2O5含量，熔体相中P2O5含量在750 C的0.47~0.80 wt%、830 C的0.35~2.26 wt%范围内。熔体相中的P2O5含量与ASI之间存在二次函数关系(P2O5 wt%=3.5×ASI2-11.3×ASI+9.5 )。锰铝榴石溶解，促使体系中Al2O3活度增大，含锰氟磷灰石的溶解及其端元磷灰石结晶之间的化学平衡，导致熔体相中P2O5的降低，很可能是熔体中P2O5随体系ASI增大而降低的机制。 4) 不同PTX条件下稀有金属元素(W、Sn、Be、Nb、Ta)在流体/熔体相间的分配系数(Dif/m)<<0.1，预示着W、Sn、Be、Nb、Ta强烈富集在富磷过铝质熔体相中。由此，可推测富P过铝质岩浆体系的演化晚期，不太可能分异出富含上述成矿元素的成矿流体。随着岩浆分异演化的进行，残余熔体相中最终导致绿柱石、锆石、锡石、铌钽矿物等矿物饱和结晶，形成有经济意义的花岗岩型或伟晶岩型稀有金属矿床。 5) 不同PTX条件下REE在流体/熔体间的分配系数(DREE)随REE的原子序数增大而逐渐降低，构成右倾的平滑曲线，不存在在Nd-Pm、Gd、Ho-Er处的拐点；Y与Ho在流体/熔体相间分配系数的比值(DY/DHo)约为1，不受体系温度、压力和P2O5含量变化的影响。上述实验结果揭示，富磷过铝质量岩浆演化至岩浆-热液过渡阶段，熔体-流体作用不会导致Y-Ho间的分异，不会引起REE间的分异，因此，富磷过铝质岩浆演化晚期的熔体-流体作用过程不可能是产生稀土“四分组”效应的根本机理。