Direct support and general support maintenance repair parts and special tools list for receiver, radio frequency, Weinschel, model VM-4A, NSN 4931-01-041-1564 and tracking oscillator, Weinschel, model VM-4A/H0-2, NSN 6695-01-102-4342.

Includes index.

An analysis of holding cost impact on housing affordability in relation to midsized Greenfield residential property developments in South East Queensland

The position of housing demand and supply is not consistent. The Australian situation counters the experience demonstrated in many other parts of the world in the aftermath of the Global Financial Crisis, with residential housing prices proving particularly resilient. A seemingly inexorable housing demand remains a critical issue affecting the socio-economic landscape. Underpinned by high levels of population growth fuelled by immigration, and further buoyed by sustained historically low interest rates, increasing income levels, and increased government assistance for first home buyers, this strong housing demand level ensures problems related to housing affordability continue almost unabated. A significant, but less visible factor impacting housing affordability relates to holding costs. Although only one contributor in the housing affordability matrix, the nature and extent of holding cost impact requires elucidation: for example, the computation and methodology behind the calculation of holding costs varies widely - and in some instances completely ignored. In addition, ambiguity exists in terms of the inclusion of various elements that comprise holding costs, thereby affecting the assessment of their relative contribution. Such anomalies may be explained by considering that assessment is conducted over time in an ever-changing environment. A strong relationship with opportunity cost - in turn dependant inter alia upon prevailing inflation and / or interest rates - adds further complexity. By extending research in the general area of housing affordability, this thesis seeks to provide a detailed investigation of those elements related to holding costs specifically in the context of midsized (i.e. between 15-200 lots) greenfield residential property developments in South East Queensland. With the dimensions of holding costs and their influence over housing affordability determined, the null hypothesis H0 that holding costs are not passed on can be addressed. Arriving at these conclusions involves the development of robust economic and econometric models which seek to clarify the componentry impacts of holding cost elements. An explanatory sequential design research methodology has been adopted, whereby the compilation and analysis of quantitative data and the development of an economic model is informed by the subsequent collection and analysis of primarily qualitative data derived from surveying development related organisations. Ultimately, there are significant policy implications in relation to the framework used in Australian jurisdictions that promote, retain, or otherwise maximise, the opportunities for affordable housing.

Hysteresis in model spin systems

The authors study the hysteretic response of model spin systems to periodic time-varying fields H(t) as a function of the amplitude H0 and the frequency Omega . At fixed H0, they find conventional, squarish hysteresis loops at low Omega , and rounded, roughly elliptical loops at high Omega , in agreement with experiment. For the O(N to infinity ), d=3, ( Phi 2)2 model with Langevin dynamics, they find a novel scaling behaviour for the area A of the hysteresis loop, of the form (valid for low fields) A approximately=H0066 Omega 0.33.

Antarctic ice shelf melting and its impact on the global sea ice-ocean system

Earth s ice shelves are mainly located in Antarctica. They cover about 44% of the Antarctic coastline and are a salient feature of the continent. Antarctic ice shelf melting (AISM) removes heat from and inputs freshwater into the adjacent Southern Ocean. Although playing an important role in the global climate, AISM is one of the most important components currently absent in the IPCC climate model. In this study, AISM is introduced into a global sea ice-ocean climate model ORCA2-LIM, following the approach of Beckmann and Goosse (2003; BG03) for the thermodynamic interaction between the ice shelf and ocean. This forms the model ORCA2-LIM-ISP (ISP: ice shelf parameterization), in which not only all the major Antarctic ice shelves but also a number of minor ice shelves are included. Using these two models, ORCA2-LIM and ORCA2-LIM-ISP, the impact of addition of AISM and increasing AISM have been investigated. Using the ORCA2-LIM model, numerical experiments are performed to investigate the sensitivity of the polar sea ice cover and the Antarctic Circumpolar Current (ACC) transport through Drake Passage (DP) to the variations of three sea ice parameters, namely the thickness of newly formed ice in leads (h0), the compressive strength of ice (P*), and the turning angle in the oceanic boundary layer beneath sea ice (θ). It is found that the magnitudes of h0 and P* have little impact on the seasonal sea ice extent, but lead to large changes in the seasonal sea ice volume. The variation in turning angle has little impact on the sea ice extent and volume in the Arctic but tends to reduce them in the Antarctica when ignored. The magnitude of P* has the least impact on the DP transport, while the other two parameters have much larger influences. Numerical results from ORCA2-LIM and ORCA2-LIM-ISP are analyzed to investigate how the inclusion of AISM affects the representation of the Southern Ocean hydrography. Comparisons with data from the World Ocean Circulation Experiment (WOCE) show that the addition of AISM significantly improves the simulated hydrography. It not only warms and freshens the originally too cold and too saline bottom water (AABW), but also warms and enriches the salinity of the originally too cold and too fresh warm deep water (WDW). Addition of AISM also improves the simulated stratification. The close agreement between the simulation with AISM and the observations suggests that the applied parameterization is an adequate way to include the effect of AISM in a global sea ice-ocean climate model. We also investigate the models capability to represent the sea ice-ocean system in the North Atlantic Ocean and the Arctic regions. Our study shows both models (with and without AISM) can successfully reproduce the main features of the sea ice-ocean system. However, both tend to overestimate the ice flux through the Nares Strait, produce a lower temperature and salinity in the Hudson Bay, Baffin Bay and Davis Strait, and miss the deep convection in the Labrador Sea. These deficiencies are mainly attributed to the artificial enlargement of the Nares Strait in the model. In this study, the impact of increasing AISM on the global sea ice-ocean system is thoroughly investigated. This provides a first idea regarding changes induced by increasing AISM. It is shown that the impact of increasing AISM is global and most significant in the Southern Ocean. There, increasing AISM tends to freshen the surface water, to warm the intermediate and deep waters, and to freshen and warm the bottom water. In addition, increasing AISM also leads to changes in the mixed layer depths (MLD) in the deep convection sites in the Southern Ocean, deepening in the Antarctic continental shelf while shoaling in the ACC region. Furthermore, increasing AISM influences the current system in the Southern Ocean. It tends to weaken the ACC, and strengthen the Antarctic coastal current (ACoC) as well as the Weddell Gyre and the Ross Gyre. In addition to the ocean system, increasing AISM also has a notable impact on the Antarctic sea ice cover. Due to the cooling of seawater, sea ice concentration and thickness generally become higher. In austral winter, noticeable increases in sea ice concentration mainly take place near the ice edge. In regards with sea ice thickness, large increases are mainly found along the coast of the Weddell Sea, the Bellingshausen and Amundsen Seas, and the Ross Sea. The overall thickening of sea ice leads to a larger volume of sea ice in Antarctica. In the North Atlantic, increasing AISM leads to remarkable changes in temperature, salinity and density. The water generally becomes warmer, more saline and denser. The most significant warming occurs in the subsurface layer. In contrast, the maximum salinity increase is found at the surface. In addition, the MLD becomes larger along the Greenland-Scotland-Iceland ridge. Global teleconnections due to AISM are studied. The AISM signal is transported with the surface current: the additional freshwater from AISM tends to enhance the northward spreading of the surface water. As a result, more warm and saline water is transported from the tropical region to the North Atlantic Ocean, resulting in warming and salt enrichment there. It would take about 30 40 years to establish a systematic noticeable change in temperature, salinity and MLD in the North Atlantic Ocean according to this study. The changes in hydrography due to increasing AISM are compared with observations. Consistency suggests that increasing AISM is highly likely a major contributor to the recent observed changes in the Southern Ocean. In addition, the AISM might contribute to the salinity contrast between the North Atlantic and North Pacific, which is important for the global thermohaline circulation.

Hysteresis in model spin system

The aim of this paper is to construct a nonequilibrium statistical‐mechanics theory to study hysteresis in ferromagnetic systems. We study the hysteretic response of model spin systems to periodic magnetic fields H(t) as a function of the amplitude H0 and frequency Ω. At fixed H0, we find conventional, squarelike hysteresis loops at low Ω, and rounded, roughly elliptical loops at high Ω, in agreement with experiments. For the O(N→∞), d=3, (Φ2)2 model with Langevin dynamics, we find a novel scaling behavior for the area A of the hysteresis loop, of the form A∝H0.660Ω0.33. We carry out a Monte Carlo simulation of the hysteretic response of the two‐dimensional, nearest‐neighbor, ferromagnetic Ising model. These results agree qualitatively with the results obtained for the O(N) model.

Soft chemical synthesis of new layered and three-dimensional oxide hydrates, hxVxW1-xO3×yH2O, related to WO3×2 H2O and WO3. times.1/3 H2O

Two new vanadium-tungsten oxide hydrates of the formulas, H0.125V0.125W0.875O3.1.5H2O (I) and Ho.33V0.33W0.67O3.1/3H2O (II), have been synthesized by acid-leaching of LiVWO6 with aqueous HNO3/HCl. While phase I obtained by treatment of LiVWO6 with dilute HNO3/HCl possesses an orthorhombic structure (a = 7.77(3), b = 13.87(6), c = 7.44(3) angstrom) related to WO3.2H2O, phase II, prepared by refluxing LiVWO6 with concentrated HNO3, is isostructural with WO3.1/3H2O. Dehydration of II around 330-degrees-C yields a hexagonal phase (III, a = 7.25(4), c = 7.74(3) angstrom) isotypic with hexagonal WO3. Both land III exhibit redox and acid-base intercalation reactivity characteristic of layered and tunnel structures.

Influência de tratamentos térmicos nas propriedades mecânicas e metalúrgicas em liga odontológica à base de níquel-cromo.

É crescente a preocupação com o desenvolvimento de materiais adequados a trabalharem interagindo com o corpo humano. Diversas pesquisas têm sido realizadas no desenvolvimento de biomateriais aplicáveis na odontologia, este empenho é justificável pelo grande número de intervenções cirúrgicas para extração de dentes realizadas em todo o mundo. Durante o processo de fabricação de reconstruções dentárias, que utilizam sistemas metalocerâmicos, é utilizado um tratamento térmico que tem a função de promover a adesão da porcelana ao metal. Entretanto, sabe-se que tratamentos térmicos podem alterar a microestrutura do material metálico, modificando suas propriedades. Este trabalho avaliou as modificações causadas em propriedades mecânicas e microestruturais da liga à base de níquel (FIT CAST-SB) utilizada para fins odontológicos, quando a mesma é submetida ao tratamento térmico para adesão da porcelana (denominado de queima). A liga foi inicialmente fundida através da técnica de centrifugação e cera perdida. Posteriormente, um grupo de amostras (grupo TT) foi submetido ao tratamento térmico de queima para adesão da porcelana e o outro grupo (grupo F), permaneceu apenas submetido ao processo de fundição. Os grupos F e TT foram submetidos a ensaio de tração. Nos grupos F e TT, e no material como recebido pelo fabricante (grupo CR), foram realizados ensaios de microdureza e caracterização microestrutural, esta ultima através da técnica de microscopia eletrônica de varredura (MEV). Os grupos F e CR foram submetidos à análise química quantitativa (em um espectrômetro de emissão atômica) e semi-quantitativa por um sistema de Energy Dispersive Spectroscopy (EDS) acoplado ao MEV, sendo que esta ultima técnica também foi aplicada ao grupo TT. A técnica de tratamento digital de imagem foi aplicada às micrografias dos grupos F e TT, para a determinação de possíveis modificações quantitativas nas fases presentes, antes e após o tratamento térmico. Todos os resultados dos ensaios foram submetidos ao teste de hipótese nula (H0), para a distribuição t de Student. Concluiu-se que, para as amostras testadas, o limite de resistência foi superior ao fornecido pelo fabricante, respectivamente 559,39 e 545,55 MPa para os grupos F e TT, contra 306 MPa do fabricante. Enquanto o limite de escoamento foi ligeiramente inferior, 218,71 e 240,58 MPa para os grupos F e TT, respectivamente, contra 258 MPa do fabricante. Os resultados de microdureza ficaram entorno de 70HV, superior aos 21HV fornecido pelo fabricante. Pode-se afirmar, com 95% de confiabilidade, que não houve variação nas propriedades mecânicas e na microestrutura (quantidades de fases presentes e tamanho) antes e após a queima para adesão da porcelana, para os corpos de prova testados. A microestrutura da liga, quando observada em MEV no modo elétrons retroespalhados (modo BSE), é formada por uma matriz de estrutura dendrítica e coloração cinza, uma segunda fase interdendrítica de coloração branca e aspecto rendilhado, e precipitados de coloração preta, apresentando também porosidades.

中国三种野生稻的遗传变异与保护生物学研究

稻属(OryzaL．)隶属禾本科(Poaceae)之稻族(OryzeaeDUmort.)，广布于全球热带与亚热带地区。目前认为该属约含20个野生种和2个栽培种，中国产4个种。亚洲栽培稻(O. sativaL．)是世界上最重要的粮食作物之一，而在中国则为第一粮食作物。在稻种基因库中，发掘野生稻中丰富的遗传多样性是解决当今人口与粮食矛盾的必由之路。因此，保护野生稻的遗传多样性举世瞩目。针对热带与亚热带地区的环境恶化而导致野生稻居群的大量绝灭与急剧萎缩的状况，制订有效的策略，最大限度地保护野生稻的遗传多样性已迫在眉睫。然而，目前对野生稻种内遗传多样性的知识十分贫乏，缺乏制订保护策略的科学基础。这一问题在中国尤为突出。本文基于1994-1995年对中国三种野生稻濒危状况的调查结果，利用等位酶分析对普通野生稻26个居群，药用野生稻8个居群和疣粒野生稻l7个居群进行了遗传多样性的研究，并重点对目前育种价值最大而濒危程度最高的普通野生稻从五个方面作了进一步的探讨。最后根据遗传多样性的研究结果讨论了它们的濒危原因，并提出了初步的保护策略。主要结果如下： 一．普通野生稻D．rufipogon Griff. 在中国的三种野生稻中，普通野生稻的遗传多样性水平最高(A=1.33，P= 0.227，Ho=0.033和He=_0.068)，遗传分化水平较低(Fst=0,310)。广西与广东的居群较其它地区的居群具有较丰富的遗传变异。因此，华南可能是中国普通野生稻的遗传多样性中心;云南现存的所有三个居群的遗传多样性水平偏低(A=1.10.p=0.148，Ho=0.007和He=0.079)，与该地区栽培稻丰富的遗传多样性形成鲜明对照，普通野生稻居群间的遗传一致度与地理距离无明显相关。 1．通过14个中央居群与5个边缘居群的对比研究表明了边缘居群的遗传结构明显不同于中央居群：其遗传多样性水平与遗传分化均低予中央居群，杂合子比中央居群更为不足。而且，从中央居群到边缘居群，位点的多态性逐渐丧失，遗传多样性水平递减，一些多态位点的等位基因频率逐渐地发生变化。 2. 通过7个受栽培稻基因渗入的居群与5个隔离较好居群的对比研究表明，被渗入居群虽然在形态上表现出复杂的变异式样，但遗传多样性水平并无相应的增高。栽培稻基因流对野生居群遗传结构的影响可能主要是遗传同化，即阻止其居群内与居群间的遗传分化。 3. 通过对2个低纬度居群与2个北缘居群两个生活史阶段的遗传多样性研究表明繁育系统是影响普通野生稻居群遗传结构的因素之一。在低纬度居群中种子阶段的遗传变异高于植株阶段，在高纬度居群中则相反。 4．通过对北缘居群(江西东乡)1980年，1985年和1994年的居群遗传结构的研究，发现该居群的遗传结构逐渐在发生变化，表现为遗传多样性水平不断下降，居群越来越偏移哈迪一温伯格平衡和杂合子变得越来越缺乏。 5．通过对一个典型的普通野生稻居群（元江居群）的居群内遗传结构的研究，表明遗传变异在3个亚居群间分布不均衡，基因型里聚集分布，使得亚居群间有一定的遗传分化。导致其居群遗传结构的亚划分的主要原因可能是有限的基因流(Nm=0.964H0=0.044和He=0.056)。海南的居群具有较高的遗传多样性，故海南可能为中国药用野生稻的遗传多样性中心。该物种有较高水平的遗传分化(Pst=0788，I=0.775)，且剧烈的遗传分化主要发生在海南与大陆间，有多达12个等位基因固定在两个地区的居群中：遗传分化也发生予地区内的居群间。 三. 疣粒野生稻0.meyeriana Baill.subsp.granulata Nees et Arn.ex Watt. 疣粒野生稻的遗传多样性水平(A=1.Ot5，p—0.0633，Ho- 0.022和He=O.O16)在三种野生稻中最低，但居群遗传分化却很高(FsT=0.859)。海南的遗传多样性水平与云南差别不大。剧烈的遗传分化不仅发生在海南与云南之间，而且还发生在地区内，甚至在很小地区内的居群阍。对每个地区来说，居群间的遗传一致度与地理距离明显相关，符合“隔离一距离”模型。该物种是克隆植物，遗传变异贫乏但居群遗传分化剧烈是这类植物的特征。 四. 对保护中国野生稻遗传资源的启示 中国的三种野生稻是居群水平上而非物种水平上的的濒危。人类的剧烈干拢和生境遭受破塥是导致它们濒危的主要原因。对普通野生稻和药用野生稻来说，人为的干扰导致了它们现存的居群变小且相互隔离，居群间的基因流受阻，遗传漂变的作用在小群体中显得尤为突出，并与严重的近交相交织，导致遗传多样性大量丧失，居群的遗传结构也进一步改变，从而产生真正遗传学上的濒危，甚至灭绝。对于普通野生稻的大多数居群来说，栽培稻频繁的基因流带来的遗传同化，也会直接或间接地引起濒危甚至消亡。 鉴于普通野生稻有69.0%的遗传多样性存在于居群内，收集种质资源时应在遗传变异丰富的居群中，特别在其遗传多样性中心的居群中取较多数量的个体，还应在不同的地理区域选择2～3个遗传变异丰富、彼此遗传差异大的居群作为代表，捕获存在于居群间的遗传变异。原位保护点的设置应优先考虑以下类型的居群：a．与栽培稻基因流隔离好的居群;b．边缘居群;c．严重受威胁的居群;原位保护区应在其遗传多样性中心设立，选择有数个相邻的较大居群。 鉴于药用野生稻有21.2%的遗传多样性存在于居群内，在收集种质资源时原则上应选择较多的居群，而在每个居群中取较少的个体。海南与大陆居群间的遗传差异较大，故两地的居群都必须收集;药用野生稻的居群通常较小，建议设立原位保护点即可。海南与大陆均须设立保护点，而且在每个地区内应保护尽可能多的居群。对地区间或地区内的居群间进行人工移植，促进基因流，对增强各居群的适应能力会有裨益。 鉴于仅有14.1%的遗传变异存在予疣粒野生稻的居群内，取样的原则是在云南和海南均取尽可能多的居群，而对每个居群取少数个体即可;该种的居群有时较大，其居群内往往有一定的遗传分化，故收集遗传资源时应按亚居群取样;建议在云南与海南各设置2～3个原位保护区，其中可优先考虑我国分布面积最大的云南思茅地区的居群。

山东山旺中新世气候定量重建的综合研究

新生代以来，全球气候经历了一系列的冷暖交替，呈现总体变冷的趋势。对该时期不同区域气候变化过程的深入研究有助于我们更好地理解现今全球气候变化规律。中新世是新生代古气候与古环境演变的一个重要转折时期，定量重建山东山旺中新世气候是认识和理解中国东部与东亚新近纪气候演变的一个关键环节。 将化石植物作为气候代用指标，用于研究过去全球气候变化，已经广为国际科学界接纳。国际上，定量研究第三纪气候的植物学方法按照不同原理可以划分为两大类，其各自代表分别为基于化石的现存最近亲缘类群生态适应度推演古气候参数值的共存分析法（Coexistence Approch, CA ）和基于叶片形态特征与气候相关关系的叶缘分析（Leaf Margin Analysis, LMA ）与气候叶片多变量程序（Climate Leaf Analysis Multivariate Program, CLAMP）。两大主流方法各有优势，也各有局限性。前人运用两大主流方法对山旺中新世植物群相同地层，同套数据的分析结果表明：LMA 和CLAMP 所估测年均温数值要显著低于CA 所估测的数值。其差异的原因既可能是LMA 和CLAMP 由于埋藏因素的影响造成估测值偏低，也可能由于CA 数据库数据主要来自于欧洲和北美而缺乏东亚的资料所致。 本论文提出了一种新的方法——分布区叠加分析（Overlapping Distribution Analysis, ODA ）对山旺中新世古气候进行定量重建。ODA 采用最近亲缘类群在叠加区间的气候参数来重建化石植物所生活的当时当地的气候。其详细步骤如下：1. 鉴定化石植物和认定它们的最近亲缘类群（尽量到种级水平）。2. 调查这些最近亲缘类群的分布数据（包括经度、纬度和海拔数据）。某些类群可能会有不止一个最近亲缘类群，须将这些最近亲缘类群的分布数据合并。3. 对分布数据分析，得出包含最多类群的最大叠加区间。4. 调查在最大叠加区间中气象站点的气候数据。5. 按照公式（1）和（2）来转换年均温数据TU=T0 - (HU -H0)×Γ (1); TL=T0 - (HL -H0)×Γ (2) 其中HU (m) 是海拔叠加区间的上界; HL (m) 是海拔叠加区间的下界; H0 (m) 气象站的实测海拔; T0 (ºC) 气象站的实测年均温; TU (ºC) 在海拔叠加区间气温的下界; TL (ºC) 在海拔叠加区间气温的上界; 系数Γ 为大气垂直直减率，年均温为0.5ºC/100m，最冷月均温为 0.45ºC/100m，最热月均温为 0.6ºC/100m。同样的方法，在海拔叠加范围内最冷月均温与最热月均温范围也可以确定，而降水量则采用气象台站的原始数据。6. 在这些转换数据的基础上，得出年均温，最冷月均温，最热月均温，年较差和年平均降水量波动范围。 ODA 分析结果表明：山旺中新世时期年均温为10.9-14.5oC，年较差为21.1-22.7oC，最冷月均温为-0.5-3.3oC，最热月均温为21.9-25.0oC，年平均降水量为1107.3-1880.0mm 。同时本论文还定量恢复了山旺硅藻土矿各层的古气候参数，其所估测的古气候参数数值与CLAMP 和LMA 的结果一致，而与CA 不同。对山旺气候参数的恢复表明，虽然其中新世年均温与现在相似，但最冷月均温要高于现在。 本项研究的创新之处是选择同一个研究地点（山东山旺），依据同一套数据（化石植物的类群资料），采用国际上以不同原理为基础的主流方法，同时加入我们自己提出的新方法，进行的古气候重建，对所获得气候参数值进行对比和验证，并对其存在的差异进行分析和探讨。

鄱阳湖南矶山自然保护区鲤、鲫的随机扩增多态DNA分析

利用RAPD(随机扩增多态)标记分析湖内鲤、鲫群体遗传多样性,从40个随机引物中各筛选出8个引物适合鲤、鲫群体RAPD扩增。在鲤群体中,共检测出60条带,其中多态性带42条,多态位点比率为70.00%;而在鲫群体中,共检测出61条带,其中多态性带40条,多态位点比率为65.57%。用POPGENE软件分析实验数据,结果显示:湖内鲤群体的遗传多样性水平(He=0.230 1,H0=0.391 0)和鲫群体的遗传多样性水平(He=0.218 6,H0=0.375 8)都较高,都有较大的遗传变异。而在鲤、鲫群体

InGaAs/GaAs量子点阵列中的能级计算

根据八带k·p理论,在三维InGaAs/GaAs量子点阵列中求解kx=ky=kz=0 处的有效质量哈密顿H0的本征值,得到InGaAs量子点中导带中电子基态EC1,第一激发态EC2和重空穴态EHH1的能级.随着In组分从30%增加100%,InGaAs量子点中EC2到EC1的带内跃迁波长从18.50 μm 蓝移到11.87 μm,而EC1到EHH1的跃迁波长则从1.04 μm红移到1.73 μm;随着量子点高度从1.0 nm增加到 5.0 nm,In0.5Ga0.5As和InAs量子点中EC1到EC2的带内跃迁都从束缚态-连续态型转换到束缚态-束缚态型,对应于两种量子点的带内跃迁波长分别从8.12 μm (5.90 μm)红移到 53.47 μm(31.87 μm),两种量子点中EC1到EHH1的跃迁波长分别从1.13 μm(1.60 μm)红移到1.27 μm(2.01 μm).

农田防护林主带间距离的确定——基于林带结构与风速降低的关系(英文)

本文通过对9条分布均匀、相对较窄的不同疏透度(透光疏透度,下同)(0.13～0.33)的树木林带和不同疏透度(0.00～0.80)风障组合的野外风速观测,确定了树木林带和风障的最适疏透度分别为0.25和0.13。基于林带结构(疏透度)与风速降低的关系,确定了林带主带间距离的主要参数,即,林带结构系数(δ)和以主害风为代表的小气候参数(Lrp)。另外,通过对林带树木的野外调查,应用树木解析技术确定林带成林高(H0)。因此,树木林带的主带间距可以通过林带结构系数、希望降低风速的比例和树木生长模型来确定。本文以杨树林带为例,具体确定了杨树林带的主带间距。该研究结果不仅适于树木林带的设计,同时适于其它生物材料或人工风障的设计。图4表5参40。

中国东北西部地区沙质荒漠化过程与植被动态关系的生态学研究——群落多样性与沙质荒漠化过程

依据东北西部沙质荒漠化地区植被的分类与排序,分析了不同演替梯度上植被群落多样性指数与DCA排序坐标值的相关关系,利用其探讨群落多样性与沙质荒漠化过程的关系;科尔沁沙地、呼伦贝尔沙地,1)植物群落的生态优势度λ、Renyi的均匀度E1与群落分布的地下水位有显著的相关关系;2)植物群落Hill的多样性指数H0,H1、Hill的均匀度Eh、Hill指数的均匀度E′1与海拔、湿润系数、Thornthwaite指数、降水量、地下水位、放牧干扰等有显著的相关关系;3)植物群落Renyi的多样性指数N0,N1、Heip修正的均匀度Ep、Alatalo修正的均匀度E′h与经度、温暖指数、冷暖指数、Thornthwaite指数、土壤有机质、地下水位、放牧等干扰有显著的相关关系。4)呼伦贝尔沙地的完工-海拉尔沙带,樟子松林、贝加尔针茅羊草草甸草原;科尔沁沙地的油松林、羊草草甸草原、丛生禾草草原具有较高的多样性,各群落类型随着沙质荒漠化过程的逐渐加剧,物种丰富度逐渐降低,其递减趋势分为旱生沙化系列、湿生沙化系列、盐水至水生系列。按各群落类型的物种丰富度递减顺序可分为6个级别,6个级别所含的群落类型分别对应着稳定沙地(A、B),固定沙丘(C),半固定沙丘(D),半流动沙丘(E),流动沙丘(F)。

雨生红球藻诱变育种及突变株的筛选

虾青素是良好的着色剂，具有超强的抗氧化、捕获自由基、抗癌变，抗紫外线辐射、增强免疫等功能，在医疗、水产、食品和化妆品等生产领域有着广泛的市场。雨生红球藻（Haematococcus pluvialis）是一种单细胞的绿藻，在逆境条件下可积累高达4%干重的虾青素，是目前已知的天然虾青素含量最高的生物资源，规模化培养雨生红球藻是获取天然虾青素的最佳途径。 目前实验室研究和规模化培养使用的藻株多为出发株，存在一些缺陷：养殖过程中易被其它微藻、变形虫、原生动物、细菌等污染；只适合低温培养，28℃以上生长受抑制；生长相对较慢，培养周期长；尽管雨生红球藻是已知的天然虾青素含量最高的生物资源，但其含量仍然需要提高以适合规模化生产。因此筛选出温度适应范围广、生长速率快、虾青素含量高的雨生红球藻株一直是努力的方向。 本研究选用化学诱变剂甲基磺酸乙酯（EMS）和叠氮钠(NaN3)以及物理诱变剂紫外线（UV)分别处理雨生红球藻，测定各种诱变剂的致死率，及对红球藻生长和虾青素积累的影响，根据实验结果确定合适的诱变剂量和诱变时间，通过初筛、复筛、再次诱变等分离、筛选出生长速度快、虾青素含量高的单一藻株并进一步利用高压液相色谱等方法进行鉴定。 实验结果表明：浓度为0.2％-1.0％EMS处理4h，雨生红球藻H2的死亡率7%-35%；紫外线照射2min-10min，雨生红球藻H0的死亡率10%-98％；叠氮钠30mg/L－270 mg/L处理24h，雨生红球藻H0的死亡率为20％-100％。各种诱变剂诱变结束后立即观察发现死亡细胞的形态相似但存活细胞相态有所不同，死亡细胞呈浅绿色，轮廓模糊，形状不规则，质壁间隙消失，胞内有白色空泡；EMS处理后存活细胞，呈圆球状，部分失去鞭毛和前端突起，游动缓慢，处理后第二天，细胞即恢复游动和分裂，分裂方式与正常细胞相似。紫外线和叠氮钠处理后存活细胞壁加厚，呈深绿色，圆球状，部分失去鞭毛和突起，严重抑制细胞的游动和分裂，出现不动细胞，培养一段时间后才出现分裂细胞，游动的和不动的存活细胞主要是采用不对称无性繁殖，这与正常细胞的不对称无性繁殖有所不同，正常细胞中不对称无性繁殖的母细胞多为不动细胞。紫外线和叠氮钠处理后部分细胞还产生大量的小孢子（配子？），直径较小1-4m，在母细胞内不停摆动，四、五天后逐渐脱离母细胞。这和以前描述的有性繁殖很相似，但由于没观察到后期孢子配对过程和缺乏小孢子的DNA含量和倍性的有关数据，不能确定观察到的小孢子现象为雨生红球藻的有性繁殖。 各种诱变剂处理后，各组存活藻株的生长和虾青素积累情况同对照组相比发生了变化：EMS实验中0.4％EMS组生长速率提高24％，其它组的细胞生长速率有所降低。各组单细胞虾青素含量和积累速率均高于对照组，其中0.4％和0.8％处理组单细胞内虾青素含量分别提高了76％和90％，积累速率分别提高了69％和115％；紫外线实验中4min、6min和10min组生长速率分别提高20％、17％和35%，各组藻细胞虾青素积累速率有不同程度的提高，其中2min组和10min组虾青素积累速率提高幅度最大分别为32%和31%，单细胞内虾青素含量除10min处理组提高48%，其它各组均有不同幅度的降低；叠氮钠实验中60mg/L、120mg/L和180mg/L组细胞生长速率分别提高了13％、20％和9％，各组藻细胞内虾青素含量和虾青素积累速率得到明显的提高。其中60 mg/L和180 mg/L组单细胞内虾青素含量提高幅度最大，分别提高75%和140%。180mg/L和240mg/L组虾青素积累速率提高幅度最大，分别为280％和250％。 诱变后通过固体平板分离，得到一系列单一藻株，其中0.4%浓度EMS处理雨生红球藻H2 4h后分离到H2-419在生物量上比H2高出20％,但虾青素含量提高幅度不大。用UV对突变株H2-419再次诱变得到较稳定的藻株H2-419-4，培养五个月后与H2相比生物总量提高68%，单细胞内虾青素含量提高28％，经高压液相色谱分析证明H2-419-4类胡萝卜素提取物中主要成分仍然为虾青素，和出发株H2相比色素成分没有发生变化，只是各成分比例有所不同。 还分析研究了其它单一藻株，但或是稳定性较差，或虾青素含量高而生长慢。如雨生红球藻H2经0.02％EMS诱变十天，分离得到的E-L-22和出发株相比虾青素产量提高40％，但生物总量上降低了27％；5min紫外线照射雨生红球藻H0后，分离得到的UV-5-16和UV-5-14在生物总量分别提高7％和36％。叠氮钠200mg/L处理24h分离得到的藻株N-2-42生物总量提高43％，但藻株N-2-43生物总量比出发株降低8％。