76 resultados para Übergang Sekundarstufe I - Sekundarstufe II
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Considering the fact, in the real world, that information is transmitted with a time delay, we study an evolutionary spatial prisoner's dilemma game where agents update strategies according to certain information that they have learned. In our study, the game dynamics are classified by the modes of information learning as well as game interaction, and four different combinations, i.e. the mean-field case, case I, case II and local case, are studied comparatively. It is found that the time delay in case II smoothes the phase transition from the absorbing states of C (or D) to their mixing state, and promotes cooperation for most parameter values. Our work provides insights into the temporal behavior of information and the memory of the system, and may be helpful in understanding the cooperative behavior induced by the time delay in social and biological systems.
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Knowledge about cumulative effects of forest management alternatives on forest landscape is required to make forest management decision. In this paper,a spatially explicit landscape model,LANDIS,was applied to simulate forest landscape changes in 200 years under four management alternatives (no cutting,clearcutting,selective cutting I and II) in Youhao Forestry Bureau located in Small Khingan Mountains. APACK was used to calculate distribution area of the representative species and species age cohort for six species. The results showed:1) timber harvest decreased area percentage of representative conifer species,Pinus koraiensis,Picea koraiensis and Picea jezoensis,Larix gmelinii to some extent compared to no cutting. The most influencing cutting mode for the area percentage of Tilia amurensis and Quercus mongolica was selective cutting II,followed by selective cutting I and clearcutting. To the contrast,the change of area percentage of Betula phatyphylla was contrary to the management alternatives; 2) As to species age cohort composition,timber harvest significantly changed age structure,that is,it decreased over-matured age cohort of representative species,and increased seedling and middle-age cohort (B. phatyphylla was not included,because its area percentage of over-mature age cohort was the highest under clearcutting than other three scenarios).
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1.黑麂和费氏麂卫星DNA的克隆、序列分析和染色体定位 麂属动物在很短的时间内经历了快速的物种辐射,并且种间染色体数目存在巨大差异,是研究动物核型进化和物种起源的理想模型。近二十年来的分子细胞遗传学研究已基本上证实染色体串联融合(端粒-着丝粒融合)是麂属动物核型演化的主要染色体重排方式。尽管染色体串联融合的分子机制仍不清楚,但研究提示着丝粒区域的卫星DNA可能介导染色体的非同源重组。因此,着丝粒卫星DNA的克隆、分析序列以及染色体定位研究不仅有助于阐明麂属染色体核型演化规律,还可能揭示染色体串联融合的分子机制。迄今为止,上述研究工作已经在赤麂、小麂和小麂台湾亚种开展过。但是,尚无有关黑麂、费氏麂和贡山麂卫星 DNA 克隆、序列分析以及染色体定位研究的报道。 在本研究中,我成功地克隆了黑麂的卫星DNA I、II和IV,分别命名为BMC5、BM700和BM1.1k,并且从费氏麂中克隆了卫星DNA II,命名为FM700。对这些卫星DNA克隆进行序列分析,并将这些克隆探针分别与黑麂、费氏麂、贡山麂和小麂的染色体杂交。研究结果表明: 1)黑麂的卫星DNA I(BMC5)与小麂卫星DNA I(C5)序列高度相似,并且在小麂、黑麂、费氏麂和贡山麂染色体上的大部分串联融合位点处均有分布,因此卫星DNA I可能代表着染色体发生串联融合后保存下来,来源于麂属动物祖先染色体着丝粒的一种卫星DNA。卫星DNA I在这四种麂属动物染色体上的分布也表明黑麂、费氏麂和贡山麂与赤麂的核型演化过程相似,很可能从一个2n = 70的共同祖先通过一系列的串联易位进化而来。 2) 将卫星DNA II(BM700和FM700)克隆探针分别杂交到黑麂和费氏麂的染色体上,只检测到几对间隔分布的信号。这提示在核型进化过程中不同卫星DNA间可能发生了广泛的重组,从而导致卫星DNA II大量丢失。大部分重组断裂位点可能位于卫星DNA I 与卫星DNA II之间,或者在卫星DNA II 区域内。 2.六带犰狳重复序列家族的克隆、序列分析和染色体定位 六带犰狳属于犰狳科、贫齿目,是六带犰狳属中唯一的一个代表物种。系统发育研究认为贫齿目与非洲兽总目是有胎盘哺乳动物中最原始的两个类群。C显带结果揭示六带犰狳30%的基因组是由组成性异染色质构成的,并且C带分布的位置也较复杂,提示在六带犰狳基因组中存在多种重复序列元件。 为了研究六带犰狳异染色质的组成,我从六带犰狳的基因组中克隆了七种位点特异性的重复序列。根据测序结果以及它们在染色体上的分布,将这些重复序列分为五个重复序列家族。其中AMD-EcoRI 837与AMD-BglII 811的序列相似,都是由大小约116 bp的单位组成,分布在大多数染色体的着丝粒区域,同时在一些染色体臂也有分布。AMD-EcoRI 832,AMD-EcoRI 836和AMD-EcoRI 934是特定染色体的重复序列,并且都分布于着丝粒区域。另外,AMD-BglII 634,AMD-EcoRI 731两个克隆都属于长散在分布重复序列(L1),倾向于分布在G带阳性、富含AT碱基的区域,并且这两种重复序列在染色体上的定位与C带阳性的非着丝粒的异染色质区域很相似。本研究提供了六带犰狳异染色质区域的部分基因组信息,并且这些重复序列家族也可以用于研究六带犰狳及其近缘物种的系统发育关系。
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氨酰-tRNA合成酶(Aminoacyl-tRNA synthetases, aaRS)是一类在蛋白质生物合成中具有重要作用的酶,它可以活化氨基酸,并与相应的tRNA相识别,使得基因序列能够被精确的翻译成蛋白质序列,保证了生命体的严谨性和多样性。通常,每一类aaRS都包含有一个催化核心结构域(Catalytic central domain, CCD)和一个结合反密码子的结构域(Anticodon-binding domain, ABD)。大量研究显示,细菌与真核生物中的许多aaRS在一些细菌与真核生物中的基因进化机制与模式、氨酰化途径、结构与功能的进化模式等方面往往有着明显的差异。通过对这些差异的深入研究,对于理解蛋白质的结构、功能的进化将是非常有帮助的。虽然,造成这些差异的本质,目前仍不清楚,但是,所有的这些差异似乎提示,在细菌与真核生物的一些基本生命活动过程中的某些方面,可能还存在着目前尚未被人们所认识到的较大差异。 甘氨酰-tRNA合成酶(Glycyl-tRNA synthetase,GlyRS)在基因组中存在着两种寡聚体形式,即α2β2四聚体和α2二聚体。本研究的结果显示,四聚体和二聚体GlyRS的ABD并不同源,而它们的CCD却具有共同的起源。在进化过程中,由于基因的融合,二聚体GlyRS的ABD融合到α亚基上CCD后的C-末端,而四聚体GlyRS的ABD则加在了β亚基的C-末端。通常,同一物种中只存在一种寡聚体形式的GlyRS,但是在Magnetospirillum magnetotacticum基因组中同时存在GlyRS的两种寡聚体形式,并有多个同源的结构域,而这些同源的结构域很可能来源于不同的基因组。二聚体GlyRS存在于细菌、古细菌和真核生物中,而四聚体GlyRS仅在大多数细菌中发现。在从细菌到真核生物的进化过程中,GlyRS可能经历了一个复杂的进化历程。频繁的基因丢失和获得事件导致了GlyRS分布的差异。水平基因转移是四聚体GlyRS进化的一个主要因素。大量的细菌基因水平转移导致四聚体GlyRS基因可在植物中表达,而在动物中形成假基因。 通常,由于aaRS-I和aaRS-II具有不同的结构和催化机制,它们被认为在进化上没有联系。虽然,苯丙氨酰-tRNA合成酶(phenylalanyl-tRNA synthetase, PheRS)属于aaRS-II,但它的催化机制却类似于aaRS-I。结构域的进化分析表明,细菌、古细菌和真核生物的PheRS具有明显不同的结构,因而导致从细菌到真核生物的进化过程中,PheRS和 tRNAPhe间的识别机制发生了变化。序列分析表明,PheRS的结构域(包括CCD、ABD及其它结构域)与aaRS-I的某些结构域同源,因此,在进化上,PheRS是aaRS-II与aaRS-I之间联系的纽带。这些结果表明,在进化的过程中,aaRS-I和aaRS-II可能是由同一个共同的祖先CCD经过可变剪接和插入演化而来的,结构域间的不同组合导致aaRS-I和aaRS-II在结构和催化机制上的显著差异。
Resumo:
The elastic and electronic properties of hypothetical CoN3 and RhN3 with cubic skutterudite structure were studied by first principles calculations based on density functional theory. By choosing different initial geometries, two local minima or modifications were located on the potential energy surface, termed as modifications I and II. Both compounds are mechanically stable. For each compound, modification I is lower in energy than II. Thermodynamically stable phases can be achieved by applying pressures. Modification II is lower in energy than I at above 50 GPa for both compounds.
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Two novel bis(amine anhydride)s, NN-bis(3,4-dicarboxyphenyl)aniline dianhydride (I) and N,N-bis(3,4-dicarboxyphenyl)-p-tert-butylaniline (II), were synthesized from the palladium-catalyzed amination reaction of N-methyl-protected 4-chlorophthalic anhydride with arylamines, followed by alkaline hydrolysis of the intermediate bis(amine-phthalimide)s and subsequent dehydration of the resulting tetraacids. The X-ray structures of anhydride I and II were determined. The obtained dianhydride monomers were reacted with various aromatic diamines to produce a series of novel polyimides. Because of the incorporation of bulky, propeller-shaped triphenylamine units along the polymer backbone, all polyimides exhibited good solubility in many aprotic solvents while maintaining their high thermal properties. These polymers had glass transition temperatures in the range of 298-408 degrees C. Thermogravimetric analysis showed that all polymers were stable, with 10% weight loss recorded above 525 degrees C in nitrogen.The tough polymer films, obtained by casting from solution, had tensile strength, elongation at break, and tensile modulus values in the range of 95-164 MPa, 8.8-15.7%, and 1.3-2.2 GPa, respectively.
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The homoepitaxial crystallization in the films of a thermotropic liquid crystalline chloro-ply(aryl ether ketone) is studied by transmission electron microscopy (TEM) and electron diffraction (ED). The homoepitaxy takes place in the temperature range 330-320 degreesC, in which a highly-ordered smectic crystalline phase of the copolymer with a single-crystal-like banded structure is formed during the cooling process from the isotropic melt. The homoepitaxial crystallizations with angles of 32 degrees and 122 degrees between the two b axes are the major populations observed, and possess epitaxial contact planes of (100)(I)-(210)(II) and (010)(I)-(210)(II); respectively.
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Poly(aryl ether ketone ketone)s (PEKK) was a high-performance engineering plastics, By means of Wide Angle X-ray Diffraction (WAXD) and Differential Scanning Calorimetry (DSC) methods, PEKK samples crystallized in solvent induction, from glass state and from melting state were studied, Crystal forms I and II for PEKK were found, The formation of crystal form II was dependent on thermal history and solvent induction, and this form II had melting point 10 degrees C or so lower than that of form I crystallized from glass state, All PEKK samples had low melting peaks which were relevant to the polarization of PEKK molecular chain, while they had nothing to do with thermal history, The heat of fusion for PEKK low melting peaks accounted for,percentage of 2 to 10 or so of the whole heat of fusion, And PEKK has its equilibrium melting point of 409 degrees C.
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[(Bu(t)Cp)(2)LnCH(3)](2) (Ln = Nd, Gd) react with PhC=CH to form the dimeric alkynide-bridged complexes [(Bu(t)Cp)(2)LnC=CPh](2) [Ln = Nd (I), Gd (II)]. Both compounds crystallized from toluene in the monoclinic space group C2/c. The two complexes are homologous, composed of asymmetric metal-alkynide bridges with Nd-C, Gd-C (alkynide) bond lengths of 2.602(4), 2.641(5) (I) and 2.532(6), 2.601(7) Angstrom (II), respectively. The average Nd-C (ring) and Gd-C (ring) distances are 2.746(13) and 2.703(19)Angstrom.
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The redox potential, surface composition and oxygen species of a series of complex oxides LaMn1-xFexO3 (x=0-1) having perovskite structure (ABO(3)) have been investigated by means of XI'S. The variation of binding energies referring to Mn2p and Fe 2p under different treatment offerred an obvious evidence of redox between Mn and Fe, which could be expressed as Mn4+ + Fe(3-delta)+ Mn(4-delta)+ Fe3+ Feat Through computer fit three kinds of adsorbed oxygen species (O-I, O-II, O-III) have been evaluated based on the XPS spectra of O1s. From the variation of contents of different oxygen species, it could be concluded that. the redox occuring in the surface might be related with the adsorbed oxygen species O-I and O-II, furthermore the possibility of transfer of electron between adsorption site and oxygen was also discussed.
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PS I, PS II and light-harvesting complexes (LHC) in oxygen evolving photosynthetic organisms were reviewed. These organisms include cyanobacteria, red algae, brown algae, diatoms, chrysophytes, dinophytes, xanthophytes, crypophytes, green algae and green plants. The diversity of pigment-protein complexes that fuel the conversion of radiant energy to chemical bond energy was highlighted, and the evolutionary relationships among the LHC structural polypeptides and the characteristics of the fluorescence emission of PS I at 77 K was discussed.
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Gracilaria lemaneiformis Bory is an economically important alga that is primarily used for agar production. Although tetraspores are ideal seeds for the cultivation of G. lemaneiformis, the most popular culture method is currently based on vegetative fragments, which is labor-intensive and time-consuming. In this study, we optimized the conditions for tetraspore release and evaluated the photosynthetic activities of different colonies formed from the branches of G. lemaneiformis using a PAM (pulse-amplitude-modulated) measuring system. The results showed that variations in temperature and salinityhad significant effects on tetraspore yield. However, variations in the photon flux density (from 15 mu mol m(-2) s(-1) to 480 mu mol m(-2) s(-1)) had no apparent effect on tetraspore yield. Moreover, the PAM-parameters Y(I), Y(II), ETR(I), ETR(II) and F (v)/F (m) of colonies formed from different branches showed the same trend: parameter values of first generation branches > second generation branches > third generation branches. These results suggest that the photosynthetic activities of different colonies of branches changed with the same trend. Furthermore, photosynthesis in G. lemaneiformis was found to be involved in vegetative reproduction and tetraspore formation. Finally, the first generation branches grew slowly, but accumulated organic compounds to form large numbers of tetraspores. Taken together, these results showed that the first generation branches are ideal materials for the release of tetraspores.
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The ovary of triploid shrimp Fenneropenaeus chinensis was apparently impaired compared to that of the diploid shrimp at the same age. Therefore triploid shrimp ovary is possible to be taken as a model to understand the mechanism of ovary development of shrimp compared to that of the ovary of diploid shrimp at the same age. In the present study, a suppression subtractive hybridization (SSH) technique was applied to identify differentially expressed genes in the ovary between diploid and triploid shrimp. For the forward library (RNA from the ovary of triploid shrimp as the tester), 54 genes were identified. For the reverse library (RNA from the ovary of diploid shrimp as the tester), 16 genes were identified. The identified genes encoded proteins with multiple functions, including extracellular matrix components, cytoskeleton, cell growth and death, metabolism, genetic information processing, signal transduction/transport or immunity related proteins. Eleven differentially expressed genes were selected to be confirmed in the ovaries of triploid and diploid shrimp by semi-quantitative RT-PCR. Genes encoding spermatogonial stem-cell renewal factor, cytochrome c oxidase subunits I and II, clottable protein, antimicrobial peptide and transposase showed up-regulated expressions in the ovary of triploid shrimp. Genes encoding tubulin, cellular apoptosis susceptibility protein, farnesoic acid O-methyltransferase, thrombospondin and heat shock protein 90 genes showed higher expressions in the ovary of diploid shrimp. The differential expressions of the above genes are suggested to be related to the ovary development of shrimp. It will provide a new clue to uncover the molecular mechanisms underlying the ovarian development in penaeid shrimp. (C) 2010 Elsevier Inc. All rights reserved.
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The exploration and study in recent years shows that the upper Paleozoic in the east of Ordos Basin possesses major exploration potential, so it is necessary to have a comprehensive and synthetic research in this area. Following the guideline of T.A. Cross’s high resolution sequences stratigraphy and combined with sedimentology, the strata and sequence in the research area are divided and correlated. This paper emphasizes on the reservoir in this area and its major fruits are: Firstly, form the framework of the high sequence stratigraphy through mainly studying on the data of core, well drilling and field section combining. Then, think that the best reservoir formation mainly appears in the middle or lower part of long arising semi-cycle, and focus on A type and C1 middle sequence cycle that contributes to the development of formation. Next, think the sedimentary source mainly comes from the epimetamorphic crystalline basement in the north of the Ordoes Basin through analyzing depositional background, researching on sandstone petrography, distribution characteristics of the sedimentary system as well as researching on heavy mineral combination characteristics. Fourthly, give priority to Zizhou-Qingjian area for the first time and gain seven lithofacies paleography maps in the No.2 member of Shanxi and the No.8 member of Shihezi through using the method of isochronal lithofacies paleogeography mapping, then bring forth that Sh2 is mainly developed a type I sequence under the margin of ramp lake-basin background. Fifthly, through researching on the characteristics of reservoir petrography and diagenesis, think that all researched areas experienced compaction and cementation, and there is different types of rocks, only little of the primary pores that are made up of litharenite and lithoclastic quartz sandstone is left, while in lithoclastic quartz sandstone, there are still many primary pores Sixthly, through studying on pore types, microstructure, as well as physical property on the key formation, think that the researched area mostly appears typical low pore, low porosity and permeability, which mainly result from sedimentary and diagenesis. Lastly, through researching on classified evaluation in the key formation, productivity analysis, and combing with reservoir distribution, the researched area is divided into three parts, and think that exploration should be emphasized on formation I and II. The characteristics of sandstones distribution in Sh23 member, gas formation distribution and open flow capacity of exploitation well are all consistent properly with the results of reservoir comprehensive evaluation in this thesis proved by the gas production development in 2006.
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The Gangxi oil field has reached a stage of high water production. The reservoir parameters, such as reservoir physical characteristics, pore structure, fluid, have obviously changed. This thesis therefore carries out a study of these parameters that control reservoir characteristics, physical and chemical actions that have taken place within the reservoirs due to fluid injection, subsequent variations of reservoir macroscopic physical features, microscopic pore structures, seepages, and formation fluid properties. This study rebuilds a geologic model for this oil field, establishes a log-interpreting model, proposes a methodology for dealing with large pore channels and remnant oil distribution, and offers a basis for effective excavation of potential oil, recovery planning, and improvement of water-injection techniques. To resolve some concurrent key problems in the process of exploration of the Gangxi area, this thesis carries out a multidisciplinary research into reservoir geology, physical geography, reservoir engineering, and oil-water well testing. Taking sandstone and flow unit as objects, this study establishes a fine geologic model by a quantificational or semi-quantificational approach in order to understand the remnant oil distribution and the reservoir potential, and accordingly proposes a plan for further exploration. By rebuilding a geological model and applying reservoir-engineering methods, such as numerical simulation, this thesis studies the oil-water movement patterns and remnant-oil distribution, and further advances a deployment plan for the necessary adjustments and increase of recoverable reserves. Main achievements of this study are as follows: 1. The Minghazhen Formation in the Gangxi area is featured by medium-sinuosity river deposits, manifesting themselves as a transitional type between typical meandering and braided rivers. The main microfacies are products of main and branch channels, levee, inter-channel overflows and crevasse-splay floodplains. The Guantao Group is dominantly braided river deposit, and microfacies are mainly formed in channel bar, braided channel and overbank. Main lithofacies include conglomerate, sandstone, siltstone and shale, with sandstone facies being the principal type of the reservoir. 2. The reservoir flow unit of the Gangxi area can be divided into three types: Type I is a high-quality heterogeneous seepage unit, mainly distributed in main channel; Type II is a moderate-quality semi-heterogeneous seepage unit, mainly distributed in both main and branch channels, and partly seen within inter-channel overflow microfacies; Type III is a low-quality, relatively strong heterogeneous seepage unit, mainly distributed in inter-channel overflow microfacies and channel flanks. 3. Flow units and sedimentary microfacies have exerted relatively strong controls on the flowing of underground oil-water: (1) injection-production is often effective in the float units of Type I and II, whilst in the same group of injection-production wells, impellent velocity depends on flow unit types and injection-production spacing; (2) The injection-production of Type III flow unit between the injection-production wells of Type I and II flow units, however, are little effective; (3) there can form a seepage shield in composite channels between channels, leading to inefficient injection and production. 4. Mainly types of large-scale remnant-oil distribution are as follows: (1) remnant oil reservoir of Type III flow unit; (2) injection-production well group of remnant oil area of Type III flow unit; (3) remnant oil reservoirs that cannot be controlled by well network, including reservoir featured by injection without production, reservoir characterized by production without injection, and oil reservoir at which no well can arrive; (4) remnant oil area where injection-production system is not complete. 5. Utilizing different methods to deal with different sedimentary types, sub-dividing the columns of up to 900 wells into 76 chronostratigraphic units. Four transitional sandstone types are recognized, and contrast modes of different sandstone facies are summarized Analyzing in details the reservoirs of different quality by deciphering densely spaced well patterns, dividing microscopic facies and flow units, analyzing remnant oil distribution and its effect on injection-production pattern, and the heterogeneity. Theory foundation is therefore provided for further excavation of remnant oil. Re-evaluating well-log data. The understanding of water-flood layers and conductive formations in the Gangxi area have been considerably improved, and the original interpretations of 233 wells have changed by means of double checking. Variations of the reservoirs and the fluid and formation pressures after water injection are analyzed and summarized Studies are carried out of close elements of the reservoirs, fine reservoir types, oil-water distribution patterns, as well as factors controlling oil-gas enrichment. A static geological model and a prediction model of important tracts are established. Remaining recoverable reserves are calculated of all the oil wells and oil-sandstones. It is proposed that injection-production patterns of 348 oil-sandstones should be adjusted according to the analysis of adaptability of all kinds of sandstones in the injection-production wells.