Impact of wide bandgap p-type nc-Si on the performance of a-Si solar cells

This paper reports the impact of a wide bandgap p-type hydrogenated nanocrystalline silicon (nc-Si:H) on the performances of hydrogenated amorphous silicon (a-Si:H) based solar cells. The player consists of nanometer-sized Si crystallites and has a wide effective bandgap determined mainly by the quantum size-confinement effect (QSE). By incorporation of this p-layer into the devices we have obtained high performances of a-Si:H top solar cells with V-infinity=1.045 V and FF=70.3 %, and much improved mid and bottom a-SiGe:H cells, deposited on stainless steel (SS) substrate. The effects of the band-edge mismatch at the p/i-interface on the I-V characteristics of the solar cells arc discussed on the bases of the density-functional approach and the AMPS model.

Orientation relationship between hexagonal inclusions and cubic GaN grown on GaAs(001) substrates

Cubic GaN/GaAs(0 0 1) epilayers and hexagonal inclusions are characterized by X-ray diffraction (XRD), Photoluminescence (PL), Raman spectroscopy, and transmission electron microscopy (TEM). The X-ray {0 0 0 2} and (1 0 (1) over bar 0) pole figures show that the orientation relationships between cubic GaN and hexagonal inclusions are (1 1 1)//(0 0 0 1), <1 1 2 >//<1 0 (1) over bar 0 >. The distribution of hexagonal inclusions mainly results from the interfacial bonding disorder in the grain boundaries parallel to hexagonal <0 0 0 1 > directions and the lattice mismatch in <0 0 0 1 > directions on {1 0 (1) over bar 0} planes. In order to reduce the energy increase in cubic epilayers, hexagonal lamellas with smaller sizes in <0 0 0 1 > directions often nucleate inside the buffer layer or near the interface between the buffer layer and the epitaxial layer, and penetrate through the whole epitaxial layer with this orientation relationship. (C) 2001 Elsevier Science B.V. All rights reserved.

Anisotropic strain in (100) ZnSe epilayers grown on lattice mismatched substrates

We show that part of the reflectance difference resonance near the E-0 energy of ZnSe is due to the anisotropic in-plane strain in the ZnSe thin films, as films grown on three distinctly different substrates, GaAs, GaP, and ZnS, all show the resonance at the same energy. Such anisotropic strain induced resonance is predicted and also observed near the E-1/E-1+Delta(1) energies in ZnSe grown on GaAs. The theory also predicts that there should be no resonance due to strain at, the E-0+Delta(0) energy, which is consistent with experiments. The strain anisotropy is rather independent of the ZnSe layer thickness, or whether the film is strain relaxed. For ZnSe films with large lattice mismatch with substrates, the resonance at the E-1/E-1+Delta(1) energies is absent, very likely due to the poor crystalline quality of the 20 nm or so surface layer. (C) 2000 American Vacuum Society. [S0734-211X(00)05604-3].

Strain relaxation of GeSi alloy with low dislocation density grown on low-temperature Si buffers

We have developed a low-temperature (LT) growth technique. Even with Ge fraction x upto 90%, the total thickness of fully relaxed GexSi1-x buffers can he reduced to 1.7 mu m with dislocation density lower than 5 x 10(6) cm(-2). The surface roughness is no more than 6 nm. The strain relaxation is quite inhomogeneous From the beginning. Stacking faults generate and form the mismatch dislocations in the interface of GeSi/LT-Si. (C) 1999 Elsevier Science B.V. All rights reserved.

Heteroepitaxy of cubic GaN: influence of interface structure

We report on the epitaxial growth and the microstructure of cubic GaN. The layers are deposited by plasma-assisted molecular beam epitaxy on GaAs and Si substrates. Despite the extreme lattice mismatch between these materials, GaN grows in the metastable cubic phase with a well-defined orientation-relationship to the GaAs substrate including a sharp heteroboundary. The preference of the metastable phase and its epitaxial orientation originates in the interface structure which is found to be governed by a coincidence site lattice.

Aluminum induced crystallization of strongly (111) oriented polycrystalline silicon thin film and nucleation analysis

A polycrystalline silicon thin film was fabricated on glass substrate by means of aluminum induced crystallization (AIC). Al and alpha-Si layers were deposited by magnetron sputtering respectively and annealed at 480A degrees C for 1 h to realize layer exchange. The polycrystalline silicon thin film was continuous and strongly (111) oriented. By analyzing the structure variation of the oxidation membrane and lattice mismatch between gamma-Al2O3 and Si, it was concluded that aluminum promoted the formation of (111) oriented silicon nucleus by controlling the orientation of gamma-Al2O3, which was formed at the early stage of annealing.

MutS蛋白识别DNA错配机制的研究

DNA生物合成过程中DNA聚合酶会错误的掺入一些碱基而导致错配，这些错配的碱基如果不能被及时地更正将会引起机体广泛的突变。DNA错配修复系统正是基于这样一种需要而产生的，它能够切除含有错配的DNA片段并重新合成出一段正确的DNA，因此对于维持基因组的稳定性具有重要的意义。 大肠杆菌DNA错配修复系统包含11种蛋白活性，并可分为起始、切割和修复三个阶段。起始阶段的第一个步骤是错配识别，这一功能是由一种叫作MutS的蛋白来完成的，它能够特异性的识别并且结合到错配上，然后引发下游一系列的修复反应。为了更深入的理解MutS蛋白识别镶嵌在随机DNA序列中的错配的机制，我们纯化了MutS及其突变体蛋白，构建了一个2279 bp的在1/4位置带有G/T错配的DNA片段和一个具有同样长度与序列的完全配对的DNA片段，然后在原子力显微镜下观察MutS及突变体蛋白与这两种DNA底物的作用方式。结果表明MutS蛋白不但能与错配的DNA结合也能与完全配对的DNA结合，而且MutS蛋白能够诱导这两种DNA底物形成一种形似a字母的环状结构，在这种结构中MutS蛋白位于两条DNA臂的交叉处。我们发现这些环状结构是在MutS蛋白寻找错配的过程中形成的，因为随着时间推移越来越多的错配位点会被MutS蛋白占据。这些结果表明MutS蛋白非特异性的结合到DNA上，然后诱导DNA形成a环状结构，并且凭借a环结构的形成对DNA的两条臂同时进行扫描以便寻找出错配的碱基对。根据以上结果我们推测a环模式是MutS蛋白寻找错配的一种机制。这些研究也为用单分子的手段研究蛋白与DNA的相互作用提供了一种可行的方法。

Cd、Cu污染胁迫对拟南芥幼苗错配修复相关基因表达的影响

土壤重金属污染问题已成为影响我国持续农业和生态环境质量的重要因素，引起了人们的广泛关注。由于传统污染诊断方法的缺点，急需建立土壤污染生态毒理学诊断方法，生物标记物技术则是其中的研究热点之一。本文采用营养液培养的方法，以模式植物拟南芥为试材，采用半定量反转录聚合酶链式反应（RT-PCR）技术，结合传统分析方法研究了Cd、Cu在不同胁迫水平下对拟南芥幼苗的形态、生理及分子水平的毒性效应，并在此基础上，比较和分析不同测试指标对Cd、Cu胁迫响应的敏感性，进而筛选对Cd、Cu胁迫响应敏感的生物标记物。主要结果如下： 1 不同浓度Cd和Cu污染胁迫下，拟南芥幼苗生长均受到不同程度的影响 幼苗初生根伸长均受到明显抑制，而地上部叶片数、地上部鲜重却没有显著的变化。重金属首先作用于植物的根系，根系的生长对胁迫响应的敏感性高于地上部。 2 幼苗地上部的可溶性蛋白含量受到不同程度干扰，而在不同浓度的Cd、 Cu处理下，叶绿素含量变化不明显，表明幼苗地上部可溶性蛋白质含量对胁迫的敏感性高于叶绿素含量的变化。 3 幼苗地上部错配修复（MMR）和增殖细胞核抗原（PCNA）基因都明显 地出现了表达诱导或表达抑制，表明MMR和PCNA基因表达的变化对Cd、Cu胁迫表现出较高的敏感性。 4 幼苗地上部的可溶性蛋白质含量及幼苗地上部MMR和PCNA基因表达 均对Cd和Cu污染胁迫具有较高的敏感性，两者均可用于指示Cd和Cu污染的敏感生物标记物。基因表达变化图谱虽然对污染胁迫响应比较敏感，是一种污染胁迫响应敏感的生物标记物，但其在生态毒理诊断中的应用还需进一步的实验对其予以证明。

镉胁迫对拟南芥幼苗错配修复相关基因表达及突变的影响

土壤重金属污染是影响农业可持续发展和生态环境的重要问题，而通过生物标记物方式对污染土壤进行早期诊断已成为环境科学领域的研究热点。本文以M&S营养液为培养介质，以拟南芥为供试材料，以错配修复基因MutS 2 homolog (atMSH2)，atMSH3，atMSH7，细胞增殖核抗原1 和2 (atPCNA1和atPCNA2)为检测目的基因，分别采用半定量反转录-聚合酶链式反应（RT-PCR）技术、克隆及测序技术研究了Cd在不同胁迫水平（0，0.125，0.25，1.0，3.0 mg•L-1 ）上对上述错配修复相关基因表达和atMSH2基因突变的影响，并与拟南芥幼苗形态、生理指标的毒性效应进行比较分析，筛选出对Cd污染胁迫敏感的生物标记物。主要结果如下： 1. 不同浓度（0，0.125，0.25，1.0，3.0 mg•L-1 ）Cd处理7天后，拟南芥幼苗叶片数、地上部鲜重变化与对照相比差异均不显著；而根长随Cd胁迫强度的增加明显降低； 2. 不同浓度（0，0.125，0.25，1.0，3.0 mg•L-1 ）Cd处理7天后，叶绿素含量变化与对照相比差异均不显著； 地上部可溶性蛋白含量随Cd浓度的增加变化明显，0.125 mg•L-1 Cd处理下，地上部可溶性蛋白含量显著增加，而在0.25，1.0和3.0 mg•L-1 Cd时降低，但仍高于对照； 3. 地上部atMSH2，atPCNA1，atPCNA2基因表达量的变化与Cd胁迫浓度呈明显的倒U字型关系，分别在0.125mg•L-1，0.25mg•L-1和0.125mg•L-1 Cd时达到最大值。地上部可溶性蛋白含量变化趋势与atMSH2，atPCNA1，atPCNA2基因表达量的变化相似，均可作为对Cd污染胁迫敏感的潜在生物标记物。 4. 对不同浓度（0，0.125，0.25，1.0，3.0 mg•L-1 ）Cd处理7天后，拟南芥atMSH2基因PCR后的扩增产物进行回收、纯化、克隆和测序。测序结果表明，0.25 mg•L-1 Cd处理拟南芥atMSH2基因在第8个和第9个外显子之间的内含子有一个碱基转换；在1.0 mg•L-1 Cd处理下，拟南芥在第10个外显子有一个碱基转换。

基于错配修复系统的基因突变检测生物芯片研究

许多人类疾病和微生物抗药性的产生都是由基因组中单个碱基的替换、插入或缺失等基因突变引起的。因此，迫切需要发展快速、高通量基因突变检测方法来实现对基因疾病和细菌抗药性的早期诊断。本研究针对匕述需求发展了纂于DN八错配修复系统的墓因突变检测生物芯片方法。根据DNA错配修复MtltS蛋白结构与功能上的高度保守性，通过PCR从E.coli K-12基因组中扩一增出DNA错配修复基因，甩石（2.56kb）。通过基因水平的分子操纵，构建了Trx-His6-MutS（THM）、Trx-His6-Linker peptide-Muts（THLM）、Trx-His6-GFP-Linker peptide-MutS（THGLM）和Trx-His6-Linker peptide-Strep-tagll-Linker peptide-MutS（THLSLM）的融合基因并在大肠杆菌中进行了IPTG诱导表达。SDS-PAGE分析表明均有一与预期分子量相应的诱导表达条带出现，其表达量占菌体蛋白的30％左右，且以可溶形式存在。融合蛋白中Trx和His6亲和肤能增加表达蛋白的可溶性及便于蛋白的纯化。连接肤的加入增大了融合蛋白各个成分之间的距离，减少空间位阻，使各个蛋白能够较大程度地保持其原有的生物活性。MLltS融合蛋白的生物活性鉴定结果表明：它们既能识别、结合含有错配碱基的DNA双链，又保留了其它融合成分的生物活性。利用融合蛋白THLSLM中的Strep-tagII与Streptavidin相互作用的天然特性，使融合蛋白THLSLM在StrePtavidin修饰过的芯片基质上自动布阵沉积，制作成蛋白质芯片来识别、结合样品中含有错配或未配刘碱基的DNA双链。THGLM、THLM-Cy3和THLSLM能够使MutS蛋白显示不同的标记信号，通过它们识别并结合固定在DNA芯片基质上的基因片段来发展基因突变检测DNA芯片方法。利用基于MutS的蛋白质芯片和DNA芯片方法对含有不同错配类型、不同长度的DNA片段和错配序列背景对错配结合的影响做了深入研究，证明了MutS介导的基因突变检测生物芯片方法的可行性。基于MutS蛋白的鳌因突变检测生物芯片方法借用了生物系统本身的DNA错配修复（Mismatch Repair，MMR）机制。DNA错配修复过程是许多修复蛋白之间的相互作用共同完成的，其中蛋白MutS、MutL和MutH在肠道细菌例如大肠杆菌的甲基定向错配修复中起决定作用。这些修复蛋白的相关研究也引起了越来越多学者的关注，但对于MutL蛋白的体外生物功能一直存在争议，从而限制了该蛋白的应用研究。本研究利用基因的体外拼接技术构建了融合蛋白Trx-Hi56-Linker peptide-MutL（THLL）、Trx-His6-GFP-Linker peptide-MutL（THGLL）和Trx-His6-Linker peptide-Strep-tagII-Linker peptide-MutL（THLSLL）。非变性凝胶电泳鉴定MutL融合蛋白体外生物功能结果表明：THLL、THGLL和THLsLL都能增加融合蛋白Trx-His6-Linker peptide-MutS（THLM）与含有错配碱基DNA双链的结合，但受ATP浓度变化的影响很大。通过融合蛋白THGLL中绿色荧光蛋白（Green Fluorescent Protein，GFP）的荧光信号或THLSLL中Strep-tagII的特性并利用酶学反应来指示该蛋白的存在，发展了体外研究DNA错配修复蛋白MtuS和MutL之间相互作用的简便方法。本研究以构建的MutS融合蛋白为分子识别元件发展了基因突变检测生物芯片并利用构建的MutL融合蛋白发展了体外研究DNA错配修复蛋白MLuS和MutL之间相互作用的简便方法。建立的融合分子系统方法也为研究其它的蛋白质或生物大分子之间的相互作用提供了一个技术平台。此外，本研究构建的融合蛋白THGLL及其 DNA错配修复蛋白与GFP的融合构想还可用来进行DNA错配修复基因产物的表达与基因突变频率和人类肿瘤恶性程度的相关性研究。

香港地区湍蛙遗传多样性研究

依据线粒体上ND2和CO1两个变异较大的基因序列分析了香港地区香港湍蛙7种群、华南湍蛙1种群，以及大陆其他地区华南湍蛙7种群，戴云湍蛙1种群，武夷湍蛙1种群的系统发育关系，进而探讨香港湍蛙的遗传多样性、香港湍蛙特有性、如何确定香港湍蛙最佳保护单元以及这四种湍蛙的物种分类地位。 1． 香港湍蛙保护遗传学研究 香港湍蛙核苷酸传多样性较低，从其遗传多样性信息、单倍型网络分析、中性检验值以及岐点分布结果一致显示香港湍蛙很可能经历了瓶颈后的扩张，种群正在由一个较小的有效种群大小迅速增长, 有足够的时间通过变异用于积累单倍型的多态性, 而对于提高核苷酸多样化而言, 时间尚短（Nei M et al，1975，Avise J C，2000；李明等，2003）。 分子变异分析结果显示香港湍蛙种群间存在较多的基因交流，且系统发育树上各种群间交叉在一起，没有形成与地理单元相关的分支，而从其单倍型网络看，他们源于共同的祖先，是一个单系群，与地理单元间没有形成显著的遗传分化。因此应作为一个进化显著单元（ESU）。结合其与其他湍蛙发育关系及遗传距离以及野外采集信息认为香港湍蛙只在香港地区有分布，属于香港特有种。该物种内遗传多样性较低，又属于世界自然保护联盟红皮书中的近危种，同时也是《野生动物保护条例》中的受保护野生动物，且由于香港城市建设等使得其栖息环境受到威胁，因此在香港特别行政区应该受到重点保护。 从单倍型分布和核苷酸多样性可以看出大榄涌种群和城门种群具有较高的单倍型多样性和核苷酸多样性，应该作为保护的重点区域。 2. 华南湍蛙东、南沿海种群间系统关系 华南湍蛙分布广，各种群存在着丰富的遗传多样性信息且中部种群广西龙胜和湖南张家界种群核苷酸多样性明显高于其他边缘种群华南湍蛙。种群间几乎没有基因交流，且各种群间无共享单倍型，可见已形成了显著的遗传分化。各种群间遗传距离都较远，其中广东南昆山种群以及福建三港种群与其他种群距离最远，因此可以推测其他种群（广东深圳、香港大屿山、广西龙胜和防城以及湖南张家界种群）可能为独立进化的种群。但是否是一新种或一隐存种，还需要结合形态学进行更深入的研究。 本研究中无论从系统关系看还是从遗传距离看，大屿山种群与深圳种群最近，支持陈坚峰等将其定为华南湍蛙，即华南湍蛙新增一个分布点：香港大屿山。 系统树上广西防城种群（支B）与龙胜和湖南种群（支A）形成姐妹群。香港大屿山种群与深圳种群先形成姐妹群（支C），但却没有与其距离很近的广东南岭及南昆山种群（支D）形成姐妹群，可能粤北和粤中的环境及气候较复杂因此与粤南其他种群形成了明显的隔离。同时可以看出华南湍蛙种群遗传分化与地理距离没有显著的相关性。 3. 四种湍蛙间的系统关系 根据线粒体CO1基因建立四种湍蛙间的系统关系及其遗传距离，很清楚地看到，香港湍蛙与戴云湍蛙关系很近，而华南湍蛙则与武夷湍蛙较近。然而，戴云湍蛙同一个种群内部共有两个单倍型DY1和DY2，且两个单倍型间遗传距离大于DY1与香港湍蛙间遗传距离，更远远大于香港湍蛙种群内部的距离，即戴云湍蛙内部两个单倍型间遗传距离达到了种级水平，同样在系统发育树上这两个单倍型与香港湍蛙形成并系。但是，戴云湍蛙种内在形态上差异不显著。因此，其是否属于萌芽物种分化形成（budding speciation）或已经完全分化为两个不同的种值得进一步研究？ 与戴云湍蛙香港湍蛙关系类似，从系统树上看华南湍蛙不形成单系，而是分成两个大支，与武夷湍蛙形成并系，且福建和南昆山的华南湍蛙与武夷湍蛙遗传距离远大于武夷湍蛙种内福建种群与浙江种群的遗传距离，达到了种级分化水平。由此，可以推断武夷湍蛙是有效种。系统树上广东深圳、香港大屿山、广西防城和龙胜以及湖南张家界种群与华南湍蛙福建及南昆山各种群间遗传距离已超出了种内各种群间的遗传距离，但是至于这一支是否应为另外一个种，有必要扩大采样，并结合核基因及形态信息进行进一步研究。 MtDNA of ND2 and CO1 gene were used to investigate genetic diversity of Amolops in Hongkong .We collected seven populations of A. hongkongensis,，one population of A.ricketti from Hong Kong and other seven populations of A.ricketti from East and South of Chinese mainland. As well as one population of A. daiyunensis and one population of A.wuyiensis Phylogenetic relationship were analyzed of four species. Discussed whether A.hongkongensis is an endemic species and how can we make the conservation and management decisions. 1. Conservation Genetics of A. hongkongensis A. hongkongensis has a low nucleotide diversity, the results of genetic diversity, haplotype network, neutrality test and the mismatch distributions indicate that A. hongkongensis experienced a recent expansion after a bottle neck. They had enough time to accumulated haplotype diversity, but it’s too short to have a high nucleotide diversity（Nei M et al，1975，Avise J C，2000；Li et al，2003）. The result of AMOVA reveals that it has much gene exchange among the populations of A. hongkongensis. The clades of the phylogenetic tree were mixed together, no significant genetic differentiation among 8 populations and they share the same ancestor from the network analysis, these indicate that they are monophyly and should be protected as one ESU. Combined with the information of relationships of interspecies, genetic distance and distribution investigate, We conclude that A. hongkongensis is an endemic species of Hong Kong. Considering on the status of low genetic diversity in A.hongkongensis, and this species was listed in the IUCN red list as near threatened, as well as listed in the . Furthermore, it’s habitat loss and degradation more rapidly as the human activity got higher and higher. So it’s urgent to protect them in Hong Kong. Our results suggest that Tai Lam Wu and TAI MO Shan -Shing Mun populations have the higher priority to be protected because their higher genetic diversity. 2．Phylogenetic relationships among populations of Amolops ricketti from the Southern and eastern China A. ricketti has the considerable genetic diversity of mitochondrial haplotypes within and among populations, and Mitochondrial DNA diversity was higher in populations at the central area of the present distribution range of the frog，i. e. the Longsheng population and Zhangjiajie population, than at the edges of their distribution range. They have no share haplotype among populations, and have a significant genetic differentiation. Genetic distance is high among the populations, especially the distance of Nankun and Sangang group with others, which suggested that they evolved independently. May be there is a cryptic species or a new species, a further study is needed. The results of gene tree and the genetic distance clearly demonstrate that the population from LanTau island is A. ricketti, so we agree with Chen et al(2005) . That means A.ricketti have a new distribution site: LanTau island, HongKong. Phylogenetic relationships were analyzed through NJ and Mrbayes methods and got a consistent topological structure, the structure indicated that the ingroup were comprised four groups. Populations Longsheng and Zhangjiajie were first clustered as clade A; Populations Fangcheng was clustered together (clade B) as a sister group to clade A；Populations Shenzhen and Lantau island were sister groups and clustered as clade C；Then the clade D included populations Nankunshan and Nanling in Guangdong province and Sangang in Fujian province. 3. Phylogenetic Relationships among these four specises Phylogenetic relationships based on 1503bp CO1 gene and the genetic distance show that A. hongkongensis close to A. daiyunensis whereas A.ricketti near to A.wuyiensis. Nevertheless, there are two haplotypes in A.daiyunensis and the genetic distance between them higher than the distance between DY1 with A. hongkongensis. A. hongkongensis is nested in the paraphyletic ancestral species A. daiyunensis. Without significant difference in the morphological characters, So, we considered both A.daiyunensis and A.hongkongensis are valid species, may be this represents a case of ‘budding speciation’ like Batrachuperus pinchonii(Fu and Zeng,2008) in the population of A. daiyunensis. Just like two species above A. wuyiensis and A. ricketti are not monophyly, instead, A.wuyiensis is nested in the paraphyletic ancestral species A.ricketti. We need do more research to make sure whether they are new species.

黄河上游青海沙蜥种组的系统地理学研究

沙蜥属（Phrynocephalus）的卵胎生类群主要分布在我国青藏高原，包括南疆沙蜥（P. forsythii）、西藏沙蜥（P. theobaldi）、红尾沙蜥（P. erythrurus）、贵德沙蜥（P. putjatia）和青海沙蜥（P. vlangalii）。其卵胎生生殖方式适应了高寒生境，与青藏高原隆升有关。纵观前人的研究，上述几种卵胎生沙蜥的分类、系统发育关系以及生物地理都还存在疑问。本文研究了分布在若尔盖湿地的青海沙蜥红原亚种（P. v hongyuanensis）以及分布在黄河上游其它地区青海沙蜥种组的地理分布格局，并探讨了其形成机制。 青海沙蜥在黄河上游主要分布于若尔盖湿地以及青海湖周边地区。若尔盖湿地青海沙蜥红原亚种的生境由于沼泽的形成被切割成不连续的斑块，通过遗传分析可以推测这种特殊生境对它们遗传结构的影响。其次，贵德沙蜥、青海沙蜥的青海湖周边各居群以及若尔盖湿地居群之间的系统地理格局还未见报道。因此本文以居群为单位，将它们作为一个复合体，通过系统地理研究，可以了解其种群遗传结构，据此分析相关的地质历史事件对其分布的影响。主要结果如下： 1. 若尔盖湿地青海沙蜥红原亚种的种群遗传结构： 共研究了三个地理单元（红原（HY）、辖曼（XM）、玛曲（MQ））的7个采集点的72个个体。所有ND4-tRNALeu序列比对得到785 bp的片断，定义了9种单倍型。结果显示总的核苷酸多样性较低，单倍型多样性较高。分子变异分析（AMOVA）显示3个单元间差异显著（P<0.01），遗传变异主要存在于地理单元间，占62.61%。除MQ单元，XM各居群与HY居群混杂在一起，单倍型网络图没有显示出单倍型和地理位置的对应关系。XM单元单倍型的不配对分布（Mismatch distribution）为明显左移的单峰，且Fu’s Fs test为负值，表明XM单元可能经历了近期种群扩张，有足够的时间积累单倍型的多态性，还不足以大幅提高核苷酸多样性，这是其单倍型多样性较高和核苷酸多样性较低的原因。MQ单元遗传多样性低而与其他单元显著分化，推测这与3万年前黄河在若尔盖玛曲之间贯通有关。近期沼泽的形成对XMb居群的隔离时间短，使得其遗传多样性低但还不足以形成大的遗传差异。无论黄河的贯通还是沼泽的形成其隔离形成的时间都不长，其作用改变了单倍型出现的频率，也出现了一些特有单倍型，但共享单倍型还广泛存在，还不足以使得不同居群之间形成较大的遗传距离。 2. 黄河上游青海沙蜥种组的分布格局与地史过程的关系： 黄河上游青海沙蜥种组包括贵德沙蜥、青海沙蜥指名亚种的青海湖周边各居群、青海沙蜥红原亚种若尔盖湿地居群、以及青海湖以西的部分居群（序列由Genbank下载获得），总计22个居群189个样品。所有ND4-tRNALeu序列比对得到703个位点，定义了39种单倍型。以南疆沙蜥为外群构建的贝叶斯树以及MP法构建的无根树，都分为A、B两大组。其中A包括若尔盖湿地居群以及玛多居群（A1）、青海湖以西的居群和兴海居群（A2）、西藏沙蜥；B包括青海湖以南的居群和天祝居群（B1）、青海湖以东北的居群（B2）。单倍型网络图分别对应了系统发育树上的各支。按照系统发育结果分组进行分子变异分析，得到组间变异占88.63％，各组间差异显著（P=0.000）。种群遗传结构分析得到，A1和B2可能经历了近期的种群扩张，前者扩张时间约为0.105－0.189 Ma B.P.（million years before present），后者为0.057－0.102 Ma B.P.，可能与末次间冰期的气候变暖有关。A2和B1对应的两个地理单元都具有较强的种群遗传结构，较为稳定。 青海沙蜥种组A、B两大支之间遗传距离大，分化明显，分化大约发生在4.29－2.38 Ma B.P.，推测青藏运动的A幕运动后复杂的地形变化可能是它们产生分化的原因。B1和B2分化大约发生在1.73－0.96 Ma B.P.，这与湟水流域构造运动发生的时间相符。在早、中更新世时期，B1支内部各居群可能有交流，中更新世末共和盆地出现的抬升以及河流溯源改道等事件可能是引起这支内部多个单倍型丢失的原因。A1、A2支的分化可能与倒数第三次冰期降临之后气候变冷、阿尼玛卿山的大冰帽有关。 The viviparous group of genus Phrynocephalus is mainly distributed in the Qinghai –Tibetan Plateau, including P. forsythii、P. theobaldi、P. erythrurus、P. putjatia and P. vlangalii. These species are adapted well to the cold clime there, and the origin of this group was the result of a vicariance event associated with the uplifting of the Qinghai -Tibetan Plateau. Although many works have been done, there are still several questions about classification、phylogenetic relationships and the biogeography of this group. The phylogeographic pattern of the P. vlangalii complex on the upper reaches of the Yellow River and the P. v. hongyuanensis in Zoige Wetland were studied in this thesis. On the upper reaches of the Yellow River, P. vlangalii complex are distributed in Zoige Wetland and the southeast and northeast region of Kuku-noor Lake. Because of the forming of the wetland in Zoige, the habitats for sand lizards are divided into many discontinuous ones, and it is necessary to analyze genetic structure in these unique habitats. The phylogeographic patter among P. putjatia、populations of P. vlangalii in the southeast region of Kuku-noor Lake and populations of P. vlangalii in Zoige Wetland hasn’t been studied yet, and the complicated geological events of the Plateau may play an important role in the populations’ diversity and species forming there. So these populations were gathered as a complex, and phylogeographic analysis were used to clarify these doubts. According to the two topics above, this thesis has two parts of results as follows: 1. Three geographic units of P. vlangalii hongyuanensis in Zoige Wetland were defined, and they were Xiaman （XM）、Hongyuan （HY） and Maqu （MQ）. 785bp fragments of the mtDNA ND4-tRNAleu were determined from 72 samples and nine haplotypes were identified. As a whole, the nucleotide diversity was low，but the haplotype diversity was high. Analysis of molecular variance （AMOVA） showed that the three units were distinctly different（P<0.01），and 62.61% of the total genetic diversity was attributable to variation among units. There were 3 haplotypes shared among XM and HY，and no geographic clustering was observed except MQ from the TCS network. The results from the mismatch distribution analysis and Fu’s Fs test implied that there might be a recent population expansion in the XM unit, and this may be the reason why XM had a high haplotype diversity but a low nucleotide diversity. We estimate that the MQ and XMb have lower diversities because of some very recent geographic events, such as the formation of the Yellow river’s upriver and the Zoige Wetland. Although they are distinctly different, not enough time has passed for them to have diverged a great genetic distance. 2. 189 samples in 22 populations of P. vlangalii complex were collected, including P. putjatia、populations of P. vlangalii in the southeast and northeast region of Kuku-noor Lake、 populations of P. vlangalii in Zoige Wetland and the data from Genbank. 703bp ND4-tRNALeu sequences identified 39 haplotypes. P. forsythii was selected as outgroup, and both the Bayesian tree and the MP unrooted tree were divided into two groups（A、B）. A included populations in Zoige Wetland and Xinghai（A1）、populations in the west of Kuku-noor Lake（A2）、P. theobaldi, and B included populations in the southeast of Kuku-noor Lake and Tianzhu（B1）、populations in the northeast of Kuku-noor Lake（B2）. The haplotype network agreed with these groups. AMOVA showed that these five groups were distinctly different（P<0.01）, and 88.63% of the total genetic diversity was attributable to variation among groups. There might be recent population expansion in A1 and A2, which corresponded to the dry climate of the last interglacial period. The expansion times were 0.189-0.105 Ma B.P. and 0.102-0.057 Ma B.P., respectively. A2 and B1 had strong genetic structure. The large genetic distance between A and B showed that they had been separated from each other for a long time（about 4.29-2.38 Ma B.P.）, and it corresponded to the A phase of Qingzang Movement. The diversity between B1 and B2 at 1.73-0.96 Ma B.P. may be caused by the geological event in Huangshui valley. In early Pleistocene, populations in B1 may have gene flow because of geographic linkage, and later the uplift of the Plateau and the change of river route there made a few haplotypes lost. A1 and A2 were divided into two parts by A’nyemaqen Mountains at 0.66-0.37 Ma B.P., which maybe corresponded to glaciations at about 0.7 Ma B.P.

Transition from the exhibition to the nonexhibition of negative differential thermal resistance in the two-segment Frenkel-Kontorova model

An extensive study of the one-dimensional two-segment Frenkel-Kontorova FK model reveals a transition from the counterintuitive existence to the ordinary nonexistence of a negative-differential-thermal-resistance NDTR regime, when the system size or the intersegment coupling constant increases to a critical value. A “phase” diagram which depicts the relevant conditions for the exhibition of NDTR was obtained. In the existence of a NDTR regime, the link at the segment interface is weak and therefore the corresponding exhibition of NDTR can be explained in terms of effective phonon-band shifts. In the case where such a regime does not exist, the theory of phonon-band mismatch is not applicable due to sufficiently strong coupling between the FK segments. The findings suggest that the behavior of a thermal transistor will depend critically on the properties of the interface and the system size.

Structural and PL properties of Cu-doped ZnO films

Cu-doped ZnO films with hexagonal wurtzite structure were deposited on silicon (1 1 1) substrates by radio frequency (RF) sputtering technique. An ultraviolet (UV) peak at similar to 380nm and a blue band centered at similar to 430nm were observed in the room temperature photoluminescent (PL) spectra. The UV emission peak was from the exciton transition. The blue emission band was assigned to the Zn interstitial (Zn-i) and Zn vacancy (V-Zn) level transition. A strong blue peak (similar to 435 nm) was observed in the PL spectra when the alpha(Cu) (the area ratio of Cu-chips to the Zn target) was 1.5% at 100 W, and ZnO films had c-axis preferred orientation and smaller lattice mismatch. The influence of alpha(Cu) and the sputtering power on the blue band was investigated.

黄土高原半干旱区集流灌草立体配置与水分调控

该区干旱与水土流失并存 ,降雨量时空分配不均 ,且水热并不同步 (在春夏 ,植物常因缺水而枯死 ) ,致使生态环境建设中恢复植被的难度大。为此 ,采用工程整地措施与灌草立体配置模式 ,发展集流灌草植被 ,调蓄土壤水分 ,促进灌草植被的快速恢复。结果表明 ,在水平阶营造柠条和披碱草 ,在生长初期 0～ 50 0 cm土层含水量可分为 3个明显的层次 ;在生长的第 4年随着灌草根系深扎 ,土壤水分过耗 ,出现明显的干土层 ,分布深度在 1 2 0～ 2 0 0 cm,厚度为 1 0 0 cm。在第 8年干土层扩大到 1 0 0～ 30 0 cm,厚度为 2 0 0 cm。第 1 4年土壤含水量有所回升 ,但幅度不大 ,同第 8年相比 ,仅提高 1 .5～ 2 .0个百分点。水平阶的柠条灌木林随着生长时间的延续 ,其水分贮量变化是否增加 ,仍有待继续研究。该区 0～ 50 0 cm多年土壤贮水量 ,在生长初期 ( 4月份 ) ,1 5年生柠条480 .1 5mm,1 2年生沙棘、山桃分别为 41 4.6mm和 385.4mm,在生长末期 ( 1 0月 ) ,柠条 498.31mm,沙棘 42 3.31 mm,山桃 ...