Bm-TFF2, a trefoil factor protein with platelet activation activity from frog Bombina maxima skin secretions

In mammals, trefoil factor family (TFF) proteins are involved in mucosal maintenance and repair, and they are also implicated in tumor suppression and cancer progression. A novel two domain TFF protein from frog Bombina maxima skin secretions (Bm-TFF2) has been purified and cloned. It activated human platelets in a dose-dependent manner and activation of integrin a(11b)beta(3) was involved. Aspirin and apyrase did not largely reduce platelet response to Bm-TFF2 (a 30% inhibition), indicating that the aggregation is not substantially dependent on ADP and thromboxane A2 autocrine feedback. Elimination of external Ca2+ with EGTA did not influence the platelet aggregation induced by Bm-TFF2, meanwhile a strong calcium signal (cytoplasmic Ca2+ release) was detected, suggesting that activation of phospholipase C (PLC) is involved. Subsequent immunoblotting revealed that, unlike in platelets activated by stejnulxin (a glycoprotein VI agonist), PLC gamma 2 was not phosphorylated in platelets activated by Bm-TFF2. FITC-labeled Bm-TFF2 bound to platelet membranes. Bm-TFF2 is the first TFF protein reported to possess human platelet activation activity. (c) 2005 Elsevier Inc. All rights reserved.

Enhanced expression of antifreeze protein genes drives the development of freeze tolerance in an Antarctica isolate of Chlorella vulgaris

In adaptation to new environments, organisms may accumulate mutations within encoding sequences to modify protein characteristics or acquire mutations within regulatory sequences to alter gene expression levels. With the development of antifreeze capability as the example, this study presents the evidence that change in gene expression level is probably the most important mechanism for adaptive evolution in a green alga Chlorella vulgaris. C. vulgaris NJ-7, an isolate from Antarctica, possesses an 18S rRNA sequence identical to that of a temperate isolate, SAG211-11b/UTEX259, but shows much higher freeze tolerance than the later isolate. The chromosomal DNA/cDNA of four antifreeze genes, namely hiC6, hiC12, rpl10a and hsp70, from the two isolates of C. vulgaris were cloned and sequenced, and very few variations of deduced amino acid sequences were found. In contrast, the transcription of hiC6, hiC12 and rpl10a was greatly intensified in NJ-7 compared to that in UTEX259, which is correlated to the significantly enhanced freeze tolerance of the Antarctica isolate. (C) 2009 National Natural Science Foundation of China and Chinese Academy of Sciences. Published by Elsevier Limited and Science in China Press. All rights reserved.

Effects of microcystin-RR on the antioxidant system of Bacillus subtilis

Microcystins are a kind of cyclic hepatotoxins produced by many cyanobacterial species. Many works have been done concerning, the toxic effects of microcystins on animals and plants. However, the reports about their effects on microbial cells are very limited. In the present paper, Bacillus subtilis (B. subtilis) was used to determine the dose- and time-effect of microcystin-RR, and the results showed that the activity of antioxidant enzymes including superoxide dismutase (SOD) and catalase (CAT) was significantly increased to that of control, when exposed to 5 or 10 mu g/ml microcystin-RR for 1 h. The contents of thiobarbituric acid-reactive sub-stances (TBARS) and glutathione (GSH) as well as glu-tathione reductase (GR) activity were obviously increased only when exposed to 10 mu g/ml microcystin-RR. For the time-effect of microcystin-RR on B. subtilis, the activities of antioxidant enzymes including SOD and CAT as well as GR activity and TBARS, GSH contents in B. subtilis were at first significantly increased, and then subsequently de-creased. These results suggested that microcystin-RR could induce the oxidative stress of B. subtilis for a short period. The antioxidant system protects B. subtilis from oxidative damage.

Differentiate performance of eight filter media in vertical flow constructed wetland: Removal of organic matter, nitrogen and phosphorus

A comparative study was conducted to reveal the differentiate effects of eight different filter media including gravel, zeolites, anthracite, shale, vermiculite, ceramic filter media, blast furnace steel slag and round ceramsite. The study mainly related to the eight different filter media's removal performances of organic matter, nitrogen and phosphorus in the vertical flow constructed wetland simulated system, which treating wastewater at hydraulic loading rate of 1000-2500 mm/d. The results indicated that the removal effects were closely related to the physical and chemical properties of medium materials. Anthracite-filled system had the highest removal rate for the total organic carbon (TOC), up to 70%, and the removal rates of other systems ranged from 20% to 30%. As for the five-day biochemical oxygen demand (BOD5), anthracite-filled and steel slag-filled systems had the highest removal rates, also up to 70%, as well as other systems all exceeded 50%. At the same time, for the total nitrogen (TN) and NH4(+)-N, the zeolites-filled and ceramic-filled systems had the best performances with the removal rates of more than 70%, the other way round, the removal rates of other systems were only about 20%. The distinguishable effects were also observed in removal performances of total phosphorus (TP) and total dissoluble phosphorus (TDP). The removal rates of TP and TDP in steel slag-filled systems were more than 90%, a much higher value, followed by that of the anthracite-filled system, more than 60%, but those of other systems being the less. Our study provided a potential mechanism to optimize the filter media design for the vertical flow constructed wetlands.

Taxonomic revision of water-bloom-forming species of oscillatorioid cyanobacteria

A polyphasic approach was used to clarify the taxonomy of the water-bloom-forming oscillatorioid cyanobacteria. Seventy-five strains of oscillatorioid cyanobacteria were characterized by 16S rDNA sequence analysis, DNA base composition, DNA-DNA hybridization, fatty acid composition, phycobilin pigment composition, complementary chromatic adaptation, morphological characters, growth temperature and salinity tolerance. Phylogenetic analysis based on 165 rDNA sequences divided the strains into six groups, all of which were clearly separated from the type species of the genus Oscillatoria, Oscillatoria princeps Gomont NIVA CYA 150. Therefore, these strains should be classified into genera other than Oscillatoria. Groups I-III were closely related to one another and groups IV-VI were distinct from one another and from groups I to III. Group I was further divided into two subgroups, group I-pc, which includes strains containing only phycocyanin (PC), and group I-pe, which includes strains containing large amounts of phycoerythrin (PE) in addition to PC. This phenotypic distinction was supported by DNA-DNA hybridization studies. Based on the properties examined herein and data from traditional, botanical taxonomic studies, the groups and subgroups were classified into single species and we propose either emended or new taxonomic descriptions for Planktothrix agardhii (type strain NIES 204(T)), Planktothrix rubescens (type strain CCAP 1459/22(T)) Planktothrix pseudagardhii sp. nov. (type strain T1-8-4(T)), Planktothrix mougeotii (type strain TR1-5(T)), Planktothricoides raciborskii gen. nov., comb. nov. (type strain NIES 207(T)), Tychonema bourrellyi (type strain CCAP 1459/11B(T)) and Limnothrix redekei (type strain NIVA CYA 277/1(T)).

中子晕核结构在引起核碎裂中的特殊作用

基于同位旋相关量子分子动力学模型,研究和对比分析了中子晕核11Li和相等质量稳定核11B在相同入射道条件下引起核碎裂反应中的特征.由于中子晕核松散的晕中子结构和小的分离能与相等质量稳定核相比具有容易碎裂的特征,因此在较低能区这种松散的晕结构有利于碎裂过程的发生,随入射能量升高,这种晕结构效应逐渐消失.而且这种在碎裂中的中子晕结构作用随靶核质量和碰撞参数的增加而减弱.

~(126)I高自旋态的识别

利用重离子融合蒸发反应12 2 Sn(11B ,5n2p)布居了双奇核12 6 I的激发态 ,首次建立了具有集体带结构特征的能级纲图 ,其中包括 2 0条新γ跃迁 .所建能级纲图的核素归属指定得到了核反应12 4 Sn(7Li,5n)的交叉支持 .简单讨论了所建带结构的可能组态 .

低能质子注入金属靶实验中的核现象研究

在低能 ( 60～ 360keV)质子注入氘化钛 (Ti2 Hx)、钛 (Ti)、钼底衬钛箔及钼 (Mo)和不锈钢 (SS)等金属样品的实验中 ,观测到了能量分别约为 3 9、5 6和 8 4MeV的带电粒子产物。用符合望远镜和吸收片法进行粒子鉴别的结果表明 :这些带电粒子均具有α粒子特性。 3种α粒子来自质子与不同靶核发生的垒下核反应。其中 ,能量为 3 9MeV的α粒子具有很高的产额 ,其对应核反应的准激发函数曲线在 150～ 330keV能区内 ,随入射质子能量增大呈指数增长趋势。上述反应产物可能源于11N( p ,α) 12 C ,11B( p ,α) 8Be和7Li( p ,α) 4 He等核反应。但相关靶核的来源仍有待解释。利用扫描电子显微镜观测到有微球状的奇异形貌

工业无线网络化控制系统结构及调度问题研究

无线通信技术在工业网络化控制系统中的应用已成为当今工业领域中的研究热点。然而无线通信技术在恶劣的工业环境中通信质量严重下降，使得现有无线通信技术在工业网络化控制系统中的应用受阻。为此在不断提高和改进无线信号传输性能的同时，更要在控制系统级层面上充分考虑无线通信技术的特点，进行相关系统结构和实时调度机制等方面的改进，以达到使系统产生的通信任务在应用层上得到可靠、实时调度的目的。同时也要从无线网络技术层面上入手，解决上层下达的通信任务在数据链路层中的实时调度问题。要设计适合工业无线网络化控制系统应用特点的MAC协议来有效调度网络所有节点的信息收发，减少高层下达的通信任务在网络中的平均时延，提高吞吐量，进而保证工业无线网络化控制系统的实时性。 因此，本文从工业无线网络化控制系统中的通信任务在数据链路层和应用层上的调度角度出发，以解决、改善工业无线网络化控制系统的实时性和可靠性等性能指标为目的。对工业无线网络化控制系统的结构、应用层调度策略和优化以及数据链路层中的MAC协议进行了系统的研究。主要工作和贡献有以下几点： （1）对工业网络化控制系统的基本问题和引入无线通信技术后产生的问题进行了探讨。在定性分析了工业环境对无线通信的影响及要求的同时，又推导出了无线通信的链路预算模型，并利用Matlab对该预算模型进行了建模，计算出了在工业级噪声指数和工业要求的误码率下，IEEE802.11b和IEEE802.15.4两大主流无线通信技术的链路预算情况及具体的量化数据。 （2）提出了工业无线网络化控制系统的双频二级拓扑结构和多路径传输机制。利用了无线信道特点和路径冗余优势，在系统级上改进了目前无线通信技术在工业网络化控制系统中的应用模式，部分缓解了无线通信技术在工业恶劣环境中的实时性和可靠性问题。为工业无线网络化控制系统结构的设计做了有益的尝试。同时，首次将DS-UWB技术应用于工业网络化控制系统中，设计出了基于该结构的UWB和FF及PROFIBUS的集成方案，为该结构的快速应用提供了有效的途径。 （3）提出了极大容忍无线通信时延的调度算法(GTD)。有效解决了工业无线网络化控制系统中周期性通信任务的实时性问题,部分弥补了因无线网络时延而导致周期性通信任务超时的缺陷。并针对GTD调度算法产生的通信窗口碎片问题进行了优化处理，又提出了面向非周期信息吞吐量最大化的优化调度算法，该算法提高了非周期性通信任务的吞吐量。同时，给出了基于这两种调度算法的非线性规划模型的调度时间表求解方法。 （4）提出了根据通信任务调度时间表进行分配无竞争期的混合CAP和CFP的MAC协议（HAF-MAC）。解决了工业无线网络化控制系统上层下达的周期性通信任务和非周期性通信任务在数据链路层中的实时调度问题，并有效解决了本文提出的应用层调度算法生成的预留时间可能存在浪费的问题。同时，在理论分析了HAF-MAC协议时隙利用率的基础上，提出了基于时隙的HAF-MAC（TSHAF-MAC）协议。TSHAF-MAC协议比HAF-MAC协议提高了时隙利用率，使吞吐量和平均延时得到了进一步改善，进而提高了非周期性通信任务的实时性。最后，对这两个协议进行了仿真建模与验证，进而较系统地解决了工业无线网络化控制系统中的通信任务的实时调度问题。 （5）分别将论文中的第三章和第四章的部分研究成果,在本人博士研究阶段研发的无线智能照明控制系统这一物理实验平台上进行了一定的验证。

大洋有孔虫微量元素研究

The most novel aspect of this thesis is the combination analysis of the boron isotopes and trace elements. What’s more, it also provides a reliable analytical technique, which is suitable for both boron isotopes and trace elements. Al/Ca values can be used to monitor the clay removal during the sample preparation. It is found that when Al/Ca>100 mol/mol, the measured boron isotopic compositions are always several permil lower than those properly cleaned. B/Ca ratios can be used to calculate the exact boron loaded for each sample. Otherwise, too much loading will lead to too long time for the whole analytical sequence, and too less loading might incur serious blank problem. One other benefit besides those discussed above is that the combination analysis of boron isotopes and trace elements on the same sample allows reconstruction of the marine carbonate system and atmospheric pCO2 without assumption of the other parameter. In the marine carbonate system, with the seawater pH from the foraminiferal 11B, one has to make an assumption on the other variable to obtain the rest four variables. A series studies found that U/Ca and B/Ca are potential proxies for seawater [CO32-]and [HCO3-], respectively. Since they are measured on the same sample with boron isotopes, hence, there is no spatial or temporal ambiguity in the incorporation of the two controlling parameters. With 11B and U/Ca, the reconstructed atmospheric pCO2 variations match the atmospheric pCO2 record from the Vostok ice core within ±20 ppm. The incorporations of U and B into foraminiferal carbonates are controlled by the overall growth rate of individual foraminifers and other possible factors. The reliable application of these proxies still require further calibrations. In a similar fashion, the combination analysis of boron isotopes and Mg/Ca also has great advantages. Mg/Ca has been proved to be a reliable proxy for the surface seawater temperature. With the combination analysis, one can determine the phase between changes in atmospheric pCO2 and surface seawater temperature, thus explore the cause and mechanism of the changes in atmospheric pCO2. .

利用MC-ICP-MS测定硼同位素及其在西藏地热和盐湖中的初步应用

Based on previous studies, boron can be separated from aqueous samples with Amberlite IRA-743 resin. Experiments on the elute temperature, elute volume and the dynamic resin exchange capacity have been performed in this study. Results show that the dynamic exchange capacity of the resin is 4.2mg B/g and at room temperature, boron fixed on the resin within this capacity level can be extracted quantitatively by using 5ml 2%HNO3. A new procedure has been developed for the measurement of boron isotope ratios in water samples using a Neptune MC-ICP-MS, after resolving the memory effect, which is a key problem, and investigating the impacts of mass bias and Si matrix effect. Using this method, it usually takes 20 min to perform one measurement on 0.1ppm boron solution with a precision of 0.23‰ (SD). If the relative deviation between a sample and the standard is large, the washout time needs to be doubled to achieve a higher precision. δ11B values of water samples from Yangbajing geothermal field vary from -10.53 to -9.13‰. Owing to the large difference B concentration and the small B isotope difference between deep geothermal water and surface water, B isotope ratios of the shallow geothermal fluids are dominated by the deep end member rather than the shallower one in the mixing process. As a consequence, δ11B-B relation is indicative basically of a dilution process. Vapor-liquid separation and calcite scaling also greatly influence B isotope fractionation. δ11B values of water samples from Dagejia geothermal field are from -15.98‰ to -11.67‰. Boron in Changma River near the field has two sources, freshwater lakes (Dajiamang Lake and Canke Lake) and geothermal waters. Finally, a preliminary discussion is included on boron geochemical characteristics of the salt lakes in Shuanghu area and other geothermal fields, to provide information for future studies on boron isotope geochemistry of geothermal systems and salt lakes in Tibet.

黄土风化过程的硼同位素地球化学研究

采用低硼高杂质离子样品硼同位素分析方法测定了黄土、古土壤样品中酸溶相硼含量及硼同位素组成。洛川黄土S0-S2剖面酸溶相硼含量变化范围为（0.8-2.7）×10-6，其δ11B值在-1.8~+18.6‰之间变化，多集中在0~+10‰之间。古土壤层的硼含量及δ11B值高于黄土层，尤以S1层表现最显著。引起剖面上酸溶相硼含量及δ11B值变化的主要原因是化学风化作用和粘土吸附作用强度的变化，气候条件变化所引起的风化作用强度的变化可能是酸溶相硼含量及δ11B值发生变化的原因。

海洋生物碳酸盐硼同位素技术研究及其应用

近些年来，利用海洋生物碳酸盐硼同位素重建古海水pH，计算当时大气CO2含量，进而推测古气候的变化已成为国际同位素地球化学界研究的热点问题，被称为δ11B-pH技术。古海水的δ11Bsw是否恒定、B(OH)4−和B(OH)3间理论的硼同位素分馏系数4/3是多少以及碳酸盐的δ11Bcarb是否等于海水B(OH)4−的δ11B4值是该技术成功的三个关键。但到目前为止以上三项问题还没得到完全证实。 为确定方解石的硼同位素组成与海水pH的依赖关系，已进行过大量实验研究。他们的结果与预期的假设一致，支持了B(OH)4-是掺入方解石结构主要形式的假设。但近期 Pagani(2005)指出B(OH)4-也许不是掺入方解石结构的主要形式，B(OH)3也可能同时掺入进碳酸盐。肖应凯等(2006)的无机碳酸盐沉积实验发现碳酸盐沉积和母液间的硼同位素分馏系数大于1的异常现象，认为碳酸钙中镁或其它微量元素的存在是重要原因，推断这是在高pH生成Mg(OH)2沉积后11B优先掺入的缘故，推断有B(OH)3掺入碳酸盐的可能。 以前进行的沉积实验，只考虑到碳酸钙本身，确实证明了硼只以或主要以B(OH)4-参与进生物碳酸钙。但天然的海洋生物碳酸盐含有镁、锶、铁等微量元素，这些微量元素的存在可能会改变硼的参与行为，从而对硼同位素分馏产生影响。现代珊瑚礁中水镁石普遍存在，这是否会影响珊瑚的硼同位素组成而导致δ11B-pH技术的误差还值得研究。 针对以上问题，主要对硼掺入进Mg(OH)2的形式及分馏机理，现代珊瑚中镁、锶等微量元素与硼浓度及硼同位素的关系进行研究，并用生物碳酸盐的硼同位素对陆相产出有孔虫的沉积环境进行判别。 通过研究，得到以下几点认识： 1. 在Mg(OH)2从pH9.5～13的含硼合成海水中沉积时，Mg(OH)2沉积11B的变化范围为-1.20‰～28.26‰，高于合成海水的11B (-7.00±0.07‰)，沉积和海水间的硼同位素分馏系数固/液变化范围为1.0177～1.0569，平均值为1.0329，这是H3BO3优先掺入的结果，造成11B在Mg(OH)2沉积中富集。 2. Mg(OH)2沉积的硼浓度和硼在Mg(OH)2沉积与滤液间的分配系数Kd的变化范围分别为228.61 g/g～937.79 g/g和9.31～494.20。高pH值时硼掺入Mg(OH)2的过程中吸附作用占有重要位置。 3. Mg(OH)2吸附实验表明，硼掺入Mg(OH)2非常迅速，4 h能达到平衡。平衡后Mg(OH)2中硼浓度[B]固和固相与溶液相间的分配系数Kd随pH设定的升高和固液比的降低而降低。而且最高的[B]固和Kd均远高于硼被金属氧化物或粘土矿物吸附时的对应值，表硼具有很强的掺入Mg(OH)2的能力。 4. 吸附平衡时溶液相的11B液f (-19.2‰～-17.8‰)均低于原始溶液的11B液i (-7.00±0.07‰)，计算的Mg(OH)2与平衡溶液间的硼同位素分馏系数固-液变化范围为1.0186～1.0220，平均值为1.0203。这充分表明，硼掺入Mg(OH)2时11B优先进入固相，这是B(OH)3优先掺入的结果。 5. 硼以B(OH)3和B(OH)4-两种形式同时掺入Mg(OH)2，并以B(OH)3优先掺入为主，pH设定越低掺入的B(OH)3比例越高。 6. 硼将通过吸附和与Mg(OH)2的沉淀反应而掺入Mg(OH)2，两者共同决定了Mg(OH)2中硼同位素分馏特征。 7. Ca、Sr、B和Na在珊瑚中均得到富集，而Mg在珊瑚中却是贫化的。珊瑚的B浓度主要不是由这几种元素决定的。 8. 珊瑚δ11Bcarb的变化范围为22.8‰～27.9‰，平均为25.2‰。除与B浓度相关性明显外，珊瑚δ11Bcarb与其它四种元素的相关性不强。北海涠洲岛、灯楼角和三亚三地珊瑚与海水间的分馏系数carb-sw分别为0.9839、0.9847和0.9850。珊瑚与海水B(OH)3间的分馏系数carb-3的变化范围为0.9772～0.9800，平均值为0.9788，随pH升高carb-3减小。珊瑚的平均δ11Bcarb基本位于采用=0.9772时理论计算的δ11B4曲线之上，而且都低于原始合成海水的δ11Bcarb，表明硼是以B(OH)3和B(OH)4-两种形式同时掺入进珊瑚中的，并以B(OH)4-优先掺入为主。 9. 由于B(OH)4- 和B(OH)3同时进入到珊瑚中，d11Bcarb=d11B4的假设不能成立，由所测定生物碳酸盐的δ11Bcarb值计算的海水pH值会产生误差，使δ11B-pH技术变得更为复杂。 10. 实验模拟与自然的真实情况是有差距的，不能完全用实验模拟来代替自然的真实情况。 11.杨户庄剖面的第四纪早期有孔虫的生存环境是非海相环境，不是“海侵”或“海泛”的结果；同时也表明有孔虫并非是特有的海洋生物，它完全可以在陆相环境中存在。