Simultaneous synthesis of polyaniline nanotubules and gold nanoplates

This paper describes a facile route for simultaneous synthesis of polyaniline (PANI) nanotubules and gold nanoplates. The inner diameter of PANI nanotubules was less than 10 nm and the length was several micrometers. At the same time, uniform single-crystal gold nanoplates with thicknesses of tens of nanometers were obtained.

Syntheses and crystalline structures of clusters Co-3(CO)(7)(mu(3)-S)(mu, eta(2)-SCNR2)

Through the reaction of Co-2(CO)(8) with four thiuram [R2NC(S)S](2), four new sulfur-capped trinuclear cobalt carbonyl clusters Co-3 (CO)(7) (mu(3)-S) (mu, eta(2)-S* C* NR2) ( I : R = Me; I : R = Et; II : R = i-Pr; IV : NR= -N [GRAPHICS] were prepared and characterized by elementary analysis, IR,H-1 NMR and MS spectroscopy. The crystal structure of the cluster Co-3(CO)(7)(mu(3)-S)[mu, eta(2)-S*C*N (i-Pr)(2)]( III) was determined by X-ray single crystal diffraction method. The crystal of m is monoclinic, belonging to space group P2(1)/n, and the cell parameters are as follows: a = 1, 145 2(2) nm, b = 1. 502 8(3) nm, c = 1, 214 4(2) nmj alpha = 90 degrees, beta = 92, 15(3)degrees, gamma = 90 degrees; V = 2. 088 5(7) nm(3) , Z = 4, F (000) = 1 096, D-c = 1. 747 mg . m(-3), mu = 2. 588 mm(-1), R=0. 040 7, R-w=0. 062 4, The structural analysis shows that cluster II has a pyrimidal Co3S framework and contains a heterocylic bridging bidentate ligand [mu, eta(2)-S* C* N (i-Pr)(2)] linked to the Co2 and Co3 atoms of the cluster by a cobalt-carbon and a cobalt-sulfur bond respectively.

Co_3(CO)_7(μ_3-S)(μ,η~2-SCNR_2)的合成和晶体结构

Co2 (CO) 8 与 4个二硫代双 (烷基硫代甲酰胺 )类前配体 [R2 NC(S) S]2 反应 ,得 4个含烷基硫代甲酰胺基的三核钴羰基硫簇合物 .通过元素分析、IR、 1H NMR和 MS等方法表征了它们的结构 ,用 X射线衍射法测定了其中一个簇合物 Co3 (CO) 7(μ3 - S) [μ,η2 - SCN(i- Pr) 2 ]( )的晶体结构 .晶体属单斜晶系 ,P2 1/n空间群 ,晶胞参数 a=1.1452 (2 ) nm,b=1.50 2 8(3) nm,c=1.2 144 (2 ) nm,α=90°,β =92 .15(3)°,γ =90°,V =2 .0 885(7) nm3 ,Z=4 ,F (0 0 0 ) =10 96 ,Dc=1.74 7mg· m-3 ,GOF(F2 ) =0 .835,μ=2 .588nm-1.最终因子 R[I>2 σ(I) ]=0 . 0 4 0 7,Rw=0 .0 6 2 4

Cross-Ocean distribution of Rhodobacterales bacteria as primary surface colonizers in temperate coastal marine waters

Bacterial surface colonization is a universal adaptation strategy in aquatic environments. However, neither the identities of early colonizers nor the temporal changes in surface assemblages are well understood. To determine the identities of the most common bacterial primary colonizers and to assess the succession process, if any, of the bacterial assemblages during early stages of surface colonization in coastal water of the West Pacific Ocean, nonnutritive inert materials (glass, Plexiglas, and polyvinyl chloride) were employed as test surfaces and incubated in seawater off the Qingdao coast in the spring of 2005 for 24 and 72 h. Phylogenetic analysis of the 16S rRNA gene sequences amplified from the recovered surface-colonizing microbiota indicated that diverse bacteria colonized the submerged surfaces. Multivariate statistical cluster analyses indicated that the succession of early surface-colonizing bacterial assemblages followed sequential steps on all types of test surfaces. The Rhodobacterales, especially the marine Roseobacter clade members, formed the most common and dominant primary surface-colonizing bacterial group. Our current data, along with previous studies of the Atlantic coast, indicate that the Rhodobacterales bacteria are the dominant and ubiquitous primary surface colonizers in temperate coastal waters of the world and that microbial surface colonization follows a succession sequence. A conceptual model is proposed based on these findings, which may have important implications for understanding the structure, dynamics, and function of marine biofilms and for developing strategies to harness or control surface-associated microbial communities.

Controlling electric field distribution by graded spherical core-shell metamaterials

This paper investigates analytically the electric field distribution of graded spherical core-shell metamaterials, whose permittivity is given by the graded Drude model. Under the illumination of a uniform incident optical field, the obtained results show that the electrical field distribution in the shell region is controllable and the electric field peak's position inside the spherical shell can be confined in a desired position by varying the frequency of the optical field as well as the parameters of the graded dielectric profiles. It has also offered an intuitive explanation for controlling the local electric field by graded metamaterials.

中国对虾育种方法研究与遗传连锁图谱的构建

本研究以中国对虾为材料，以杂交育种和选择育种为目标，进行了系统的中国对虾杂交育种试验、生长性状遗传参数试验及其分子遗传连锁图谱的构建工作。结果表明以不同地理群体杂交作为基础群体，然后采用系统的选择育种方法可以获得较好的选择效果。构建的遗传连锁图谱为中国对虾分子辅助育种提供一定的基础。这些试验结果为中国对虾合理系统的育种工作提供了理论基础和数据支持。其具体结果如下： 1. 试验对中国对虾黄渤海水域乳山湾群体（WYP）和朝鲜半岛南海群体（WKN）的2个群体及其杂交后代不同月龄生长情况和存活率进行了研究，测量体长（TL）、头胸甲长（CL）、头胸甲宽（CW）、第2、3腹节高（HST）、第2、3腹节宽（WST）、体重（BW）和存活率共7个性状，计算各项指标的杂种优势率，并对各性状进行了方差分析和多重比较。其3月龄生长情况和存活率研究结果表明，存活率在乳山湾群体（WYP♀）× 朝鲜半岛南海群体（WKN♂）杂交后代出现杂种劣势外，其他指标都表现出不同程度的杂种优势(4.37%～23.96% )。除了存活率外，杂交后代生长性状均显著高于亲本，乳山湾群体（WYP♀）×朝鲜半岛南海群体（WKN♂）杂交后代高于朝鲜半岛南海群体（WKN♀）× 乳山湾群体（WYP♂）杂交后代，黄渤海水域乳山湾群体高于朝鲜半岛南海群体后代。为确定测量性状与中国对虾体重的相关程度，建立了用体长(X1)，头胸甲宽(X2)，第2、3腹节宽(X3)，头胸甲长(X4)，第2、3腹节高(X5)估计体重的多元回归方程：Y = －2.056 + 0.03X1 + 0.076X2 + 0.078X3 + 0.033X4 + 0.043X5。 2. 中国对虾黄渤海水域乳山湾群体（WYP）和朝鲜半岛南海群体（WKN）2个群体及其杂交后代在4月龄时期的6个生长指标和存活率的杂种优势范围在0.514%到14.95%之间，WYP♀×WKN♂杂交后代在这7个指标中都高于WKN♀×WYP♂杂交后代。5月龄杂交后代也表现出一定程度的杂种优势，其范围在-9.000%～19.090%之间，但头胸甲长、第2、3腹节处高和存活率3个指标出现杂种劣势。不同杂交组合各个阶段生长发育情况和存活率在杂种优势表现出一定的规律。随着月龄的增加，WKN♀×WYP♂杂交后代杂种优势率有所增加，而WYP♀×WKN♂杂交后代的却有所降低。ANOVA分析结果表明，杂交后代在存活率方面与双亲差异不显著。4月龄的分析结果发现杂交后代在WST和BW这2个指标上存在显著差异。LSD多重比较结果显示，WYP♀×WKN♂杂交后代在BW指标上与亲本存在显著差异，在WST指标方面与其他3个组合的后代差异显著。5月龄的数据分析结果发现，杂交后代除体重存在显著差异外，其他各项指标差异均不显著。LSD多重比较结果发现，WKN♀×WYP♂杂交后代体重与其亲本WKN存在显著差异。 3. 对2个野生群体——朝鲜半岛南海岸群体（WKN）和黄渤海群体（WYP）和3个养殖群体——朝鲜半岛群体的养殖一代（FKN），黄海1号（HH1）和即抗98（JK98）进行杂交试验的研究，结果表明JK98 (♀)  WKN (♂)组合在存活率方面最高，其余的依次为WYP (♀) WKN (♂)，WKN (♀) WYP (♂)，FKN (♀)HH1 (♂) 和 WYP (♀) FKN (♂)。而在体重方面FKN(♀)  HH1(♂)组合最高，其余的依次为WKN (♀) WYP (♂)，WYP (♀) WKN (♂)，WYP (♀)FKN (♂) 和 JK98 (♀)WKN (♂)。在所有生长性状方面，JK98 (♀)  WKN (♂)在5个组合中是最低的。方差检测结果表明，TL、CL、HST、LL和BW这5个指标在不同组合间存在差异，而其他指标不存在差异。多重比较结果发现JK98 (♀)WKN (♂)组合的TL与其他组合间差异极显著，HST指标与WKN (♀) WYP (♂)，FKN(♀)  HH1(♂)和 WYP (♀)  WKN (♂)这3个组合差异显著，BW指标与WKN (♀) WYP (♂) 和 FKN(♀)  HH1(♂)差异显著。 4. 通过人工授精的方法建立了中国对虾21个半同胞家系，测量了中国对虾21个半同胞（46个全同胞）家系的TL、CL、CW、HST、WST、第1腹节长（FL）、第6腹节长（LL）。利用MTDFREML软件得到生长性状遗传力在0.15~0.35之间，属于中度遗传力范围。TL的遗传力为0.34±0.071，CL的为0.30±0.070，CW为0.35±0.077，WST为0.33±0.073，HST为0.33±0.073，FL的最低为0.15±0.044，LL的为0.24±0.059。各个性状间表现出高的正相关，其中CW和TL以及HST的遗传相关最大，FL和WST的遗传相关最小。 通过以上杂交育种和选择育种的研究，认为单纯的依靠杂交育种来改善中国对虾的育种工作可能具有一定的局限性。所以在实际的育种过程中，以中国对虾不同群体的杂交后代作为基础群体，并以此为基础进行系统的选择育种应该具有更大的潜力。 5. 本试验利用中国对虾F2群体和AFLP分子标记技术进行了遗传连锁图谱的构建。利用55对AFLP引物组合对F2家系的110个个体进行了研究，结果检测到532个符合作图策略的AFLP标记。利用卡方检验检测分离位点是否符合孟德尔分离定律。对于符合3：1比例的分离位点利用F2自交模型构建性别平均连锁图谱，对于符合1：1比例的分离位点利用拟测交理论分别构建中国对虾的雌性和雄性遗传连锁图谱。雌性、雄性和性别平均遗传图谱分别有28、35和44个连锁群，图谱实际长度分别为1090、1617和1772.1 cM。中国对虾遗传连锁图谱估计基因组长度为2420 cM，符合与人类基因组相比的对虾类基因组长度。中国对虾雄性遗传连锁图谱比雌性遗传连锁图谱长32.6%，这可能说明中国对虾不同性别存在不同的重组率。通过皮尔逊相关系数检测认为AFLP标记在中国对虾图谱上分布均匀。本文利用AFLP标记构建的中国对虾遗传连锁图谱为中国对虾基因组研究和遗传改良提供一定的基础，同时也应该开发微卫星等共显性标记，为遗传连锁图谱的整合提供条件。

关于我院发展技术科学的探讨

技术科学是与国计民生联系很密切的科学,在整个科学技术体系中占有很重要的位置。但是,对技术科学,特别是在我院如何发展等方面的问题上,长期以来意见不一,影响了这门学科的更好发展。周光召院长最近数次指出,今年我们重点要抓好技术科学方向的讨论,研究清楚我院技术科学如何发展的问题。为促进百家争鸣,并供领导部门决策时参考,本期特刊登沈阳自动化研究所所长蒋新松和力学研究所所长薛明伦就这方面问题发表自己见解的文章,期望能引起大家的讨论,欢迎大家踊跃投稿。

松辽徐家围子断陷层序地层充填模式及含油气性特征

Based on the principle and method of sequence, the author describes the sequence-filling model of the rifting basin of Xujiaweizi and its gas exploration potential. The object of this paper belongs to the area around Shengping-Wangjiatun anticline. Its srtatigraphy includes Huoshiling Formation (neutral and basic volcanic rocks), Shahezi Formation (coal bedding and mud and some sandstone) and Yingcheng Formation from bottom to top. These stratigraphy units are defined by author as mesosequences respectively. The author emphasizes that the main control factors of sequence change with the types of basin and stage of basin. So the sequence is researched according to the types of basin. This viewpoint is very new, and it is consistent with the principle of sequence. Volcanic action is very frequent and acute, topography difference is obvious. Between the volcanic events, Shahezi Formation is formed, which mainly consists-of sedimentary rocks. Based on the datum from seismic section and drilling core and well-logging, the author analyzes the single unit and unit set and system tract and sedimentary fancies, then, according to the accommodation space change and marking of sequence boundary, Shahezi Formation is divided into two Third-scale sequences. The sedimentary fancies and depth distribution are described. The author also pointed out that the volcanic rocks consume the accommodation space, so volcanic rocks can influence the development of sequence. Based on the concept of accommodation space, the author put volcanic rocks into sequence frame, which normally consists of sedimentary rocks. The topography of volcanic is controlled by lithology of volcanic rocks, the pattern of volcanic eruption and the topography before volcanic eruption. The topography of volcanic can influence sedimentation and the filling pattern of sedimentary rocks. The author describes the composition and lithology fancies and depth distribution of volcanic rocks. The volcanic rocks and Volcanic building, volcanic structure is recognized on seismic section. The author paid a special attention to the relationship between sedimentation and volcanism. Finally, the author analyses the combination of source-reservoir-cover unit in sequence frame. The mudstone of Shahezi Formation has a great depth, the Kerogene in it belongs to type II and III, which tends to produce gas. The Yingcheng Formation lies between Shahezi Formation and Denglouku Formation, belonging to good reservoir. The volcanic rocks of Huoshiling Formation often formed high building, which can capture the gas produced from Shahezi Formation. The stratigraphy of rifting basin of Xujiaweizi has the great potential of gas exploration. This paper claims the following creative points: 1. The author applied the principle and method of sequence to rifting basin, greatly extending its research area and topic issues. 2. The author pointed out that basin of different type and of different stage has a different type of sequence. This is caused by the different main control factors of sequence. 3. Put volcanic rocks into the sequence frame, discussing the probability of regarding the volcanic rocks as the component of sequence, dealing with the relationship between sedimentation and volcanism and its influence to the source-reservoir-cover system. 4. The author pointed out that the filling pattern of rifting basin are determined by the filling pattern of megasequence, whose filling pattern is determined by the filling pattern of system tract and the change of accommodation space.

低级变质岩在热液蚀变过程中的微量元素地球化学行为——以赣东北银山地区双桥山群为例

对江西银山地区双桥山群绢云母千枚岩及其原岩的稀土及微量元素的研究表明，热液蚀变过程中它们的地球化学行为十分复杂：热液蚀变作用并不使REE淋滤降低，反而导致ΣREE较其原岩普遍升高，但岩体接触带附近蚀变围岩的ΣREE则低于原岩。蚀变岩出现Eu亏损，ΣLREE／ΣHREE值降低。定量计算显示，ΣREE总升幅中有29～45％是由围岩质量迁移引起的表观浓缩效应，而另外的55～91％则是流体带入了REE；在绢云母千枚岩中绢云母可能是REE的主要寄主矿物相，REE主要以吸附作用的形式