Cultivation of the brown alga Hizikia fusiformis (Harvey) Okamura: controlled fertilization and early development of seedlings in raceway tanks in ambient light and temperature

Commercial cultivation of the dioecious brown macroalga Hizikia fusiformis (Harvey) Okamura in East Asia depends on the supply of young seedlings from regenerated holdfasts or from wild population. Recent development of synchronized release of male and female gametes in tumble culture provides a possibility of mass production of young seedlings via sexual reproduction. In this paper, we demonstrate that controlled fertilization can be efficiently realized in ambient light and temperature in a specially designed raceway tank in which the sperm-containing water has been recirculated. The effective fertilization time of eggs by sperm was found to be within six hours. Fast growth and development of the young seedlings relied on the presence of water currents. Velocity tests demonstrated that young seedlings of 2-3 mm in length could withstand a water current of 190 cm s(-1) stop without detachment. Culture experiments at 24 h postfertilization showed that elongation of both the seedlings and their rhizoids were not hampered by high irradiance up to 600 mu mol photons m(-2) stop s(-1) stop. However, growth was slightly retarded if cultured at a temperature of 16 degrees C compared to other culture temperatures of 22, 25 and 29 degrees C. No seedling detachment was observed after transfer of the young seedlings to raft cultivation in the sea after one and 1.5 months post-fertilization, indicating the feasibility of obtaining large quantity of seedlings in such a system.

Effective response of nonlinear composite under external AC and DC electric field

A perturbation method is used to study effective response of nonlinear Kerr composites, which are subject to the constitutive relation of electric displacement and electric field, D-alpha = epsilon(alpha)E + chi(alpha)vertical bar E vertical bar(2)E. Under the external AC and DC electric field E-app = E-a (1 + sinwt), the effective nonlinear responses and local potentials are induced by the cubic nonlinearity of Kerr materials at all harmonics. As an example in three dimensions, we have investigated this kind of nonlinear composites with spherical inclusions embedded in a host. At all harmonic frequencies, the potentials in inclusion and host regions are derived. Furthermore, the formulae of the effective linear and nonlinear responses are given in the dilute limit.

高山植物条纹狭蕊龙胆的分子亲缘地理学研究

草本植物由于较短的生活周期以及对环境变化的敏感性,可能会更好地揭示第四纪冰期以来植物居群变化的历史过程。分子亲缘地理学研究是揭示动植物居群历史的有力工具,但到目前为止对青藏高原草本植物的分子亲缘地理学研究几乎是空白。因此,本文选择在青藏高原及邻近地区生长的一年生高山草本植物条纹狭蕊龙胆为研究对象,进行了13个居群155个个体的叶绿体基因组（cpDNA）非编码片段trnH（GUG）-psbA基因间区序列变异检测,共发现7种单倍型,其中单倍型Hap A是分布最广的,而单倍型Hap E、Hap F和Hap G是拥有的居群所特有的。青藏高原东北部、东部及邻近地区的每个居群拥有的单倍型非常单一,而高原东南部横断山区的单倍型分布很集中,遗传多样性也相对较高。分子变异分析（AMOVA）结果表明整个分布区条纹狭蕊龙胆的遗传变异主要存在于居群间（73.05%）,且居群间的遗传分化很高（G_(ST)=0.805,F_(ST)=0.731,N_(ST)=0.859）,有着显著的亲缘地理学结构（N_(ST)〉G_(ST),P〈0.05）和较低的居群间的平均基因流（N_m=0.184）。结合巢式支系法分析（NCA）,根据本文的研究结果推测青藏高原东南部横断山区是该植物第四纪冰期时可能的避难所,而且在间冰期或冰期后,伴随着异域片段化和过去片段化从避难所发生范围扩张而形成当前单倍型及居群的分布格局。

植物药降压作用及其机制研究进展

植物药与传统的高血压治疗药物相比不但具有明显的降压作用，而且其副作用轻微，因而具有重要的临床应用价值。着重介绍一些植物药的降压作用，并且从药物对心脏、血管、血流动力学及血液指标等方面的影响对其可能的机制进行阐述。

甘、青两省春小麦遗传多样性演变

对甘、青两省自20世纪40年代以来生产上曾磊面积应用的200多个春小麦地方品种和育成品种资料进行了分析。结果表明，19个形态性状、5个农艺性状和2个品质性状都存在着广泛的遗传多样.蟾能成品种农艺性状和品质性状的遗传多样性总体上大于地方品种，但是从20世纪60年代开展春小麦杂交育种工作之后，育成品种形态性状、农艺性状和品质性状遗传多样性呈下降趋势。评价育种对小麦遗传多样性的影响，不能只将地方品种和育成品种的遗传多样性作一简单比较就得出结论，而是应该在遗传多样性演变的动态过程中去研究。

以超声为传感器的移动式机器人环境建模

本文提出了一种用超声测距传感器建立移动式机器人室内环境模型的新方法，并设计组装了一个多方位超声测距仪，通过并行I／O接口电路与子系统控制处理主机联接，做为环境建模的支持硬件。文中详细分析了超声传感器的测距特性，并推导出一种有效的识别真伪测距读数的方法－相关辨识法。在此基础上，提出了一种用真测距读数确定环境中约束体和自由空间分布的新方法，用网格模型图中各元素的特征值来表示对应环境子域的属性。为了实现环境信息的快速提取。匹配与刷新，文中定义了三种模型结构，并设计出“逐次扩展”快速建模算法。本文还讨论了测点选择方式。此外，还构设了几组平滑算子对所建模型图进行必要的平滑处理。最后，在一个真实环境和两个模拟环境下进行了建模实验。结果表明，以超声为传感器所建模型之精度可达厘米级，且基本可以满足建模实时性的要求。

东天山红山高硫型浅成低温铜-金矿床氧化带的形成机理和硫酸盐矿物的系列发现及意义

Located in the Paleozoic uplift along the southern margin of Tu-Ha basin in eastern Xinjiang, the newly discovered Hongshan Cu-Au deposit occurs in the superimposed Mesozoic volcanic basin upon the north section of later Paleozoic Dananhu-Tousuquan accretionary arc. Kalatage Cu-Au orebelt is controlled by NWW-trend faults, and includes Hongshan and Meiling Cu-Au deposits. The host rocks of Hongshan ore district are mainly rhyolitic-dacitic ignimbrites, whereas Cu-Au mineralization is closely related to quartz porphyry, rhyolitic porphyry and granitic porphyry. Mineralization styles are dominantly veinlet-disseminated and veinlet, occasionally stockwork. The mineral association is chalcopyrite, pyrite, bornite, chalcocite and sphalerite. The hydrothermal alteration consists of silicfication, sericitization, alunitization, pyrophylitization, illitization, hydromuscovitization, and chloritization. Hongshan Cu-Au deposit, on the edge of the desert, is one of the driest areas in eastrn Tianshan. Moreover， the highest temperature has been up to 60℃, and the average rainfall receives only 34.1mm/y. The light rainfall and rapid evaporation in the vicinity of this deposit have allowed the formation of a great variety of water-soluble sulfates. Oxidization zone of this deposit lies on the upper part of primary sulfide orebodies appearing with a depth of 50-60m, which is dominant in sulfate minerals. 1. Based on the field observation, the volcanic and sub-volcanic rock composition, hydrothermal alteration, ore structure and mineralization characteristics, this paper proposed that the Hongshan Cu-Au deposit belongs to a transitional type from high-sulfide epithermal to porphyry Cu-Au deposit, which corresponds with the typical HS-epithermal deposit such as Zijinshan Au-Cu deposit in Fujian Province, SE-China. 2. The Hongshan copper-gold deposit was controlled by the tectonic, stratum, magma activity and volcanic apparatus, whereas Au mineralization is closely related to quartz porphyry, rhyolitic porphyry and fine grained pyritization in hydrothermal activity, and Cu mineralization is closely related to quartz porphyry and hydrothermal explosive breccia. 3. Oxidation zone of Hongshan Cu-Au deposit lies on the upper part of primary sulfide orebodies deposit. 23 sulfate minerals were identified in this work. The results of samples XRD and chemical analysis were furthermore confirmed through thermal, infrared spectrum and mössbauer spectrum analysis. Among those, nine minerals as Ferricopiapite, Cuprocopiapite, Rhomboclase, Parabutlerite, Krausite, Yavapaiite, Metasideronatrite Kroehnkite and Paracoquimbite were founded in China for the first time. And Paracoquimbite was secondly reported in the world (first case reported at 1938 in Chile). 4. EPMA analysis shows that Al impurity in crystal lattice is important to polytype formation of paracoquimbite and coquimbite besides stack fault. 5. Compared with Meiling Cu-Au deposit in the same Kalatage ore belt from the characteristics of δ34S of barite, lithofacies, hydrothermal alteration and homogeneous temperature, Hongshan Cu-Au deposit belongs to the same metallogenic system of HS-epithermal type as Meiling Cu-Au deposit. But Hongshan Cu-Au deposit has less extensive alteration and shallower denudation. 6. Sulfur isotope analyses show that δ34S values of pyrites vary in the range of +1.86‰~+5.69‰, with an average of 3.70‰, mostly in the range of +1.86‰~+3.20‰, and δ34Scp<δ34Spy. Therefore ore-forming fluid of porphyry comes from mantle and was contaminated by the earth’s crust. Sulfur isotope has reached balance in ore-forming process. 7. Sulfur isotope analyses show that δ34S values of sulfates vary in the range of +2.15‰~+6.73‰, with an average of +3.74‰, mostly equals as δ34S values of primary sulfides in Hongshan Cu-Au deposit. So supergene sulfates inherit sulfur of primary sulfide. δ34S values are mostly same in different sulfates. As well as pyrite and chalcopyrite, volcanic hot spring and associated native sulfur underground also provide water medium and sulfur during the formation process of sulfate. 8. According to the EPMA of sample chalcopyrite and pyrite in Hongshan Cu-Au, the value of Cu/Ni is 0.98-34.72, mostly close to the value of 5, which shows that Hongshan deposit is a typical volcanogenic magmaic hypothermal deposit. Au and Ag, Zn, Te and Bi are positive correlation, Cu and Hg, Se, Sb are positive correlation, indicates Au and Cu don’t locate in the factor of mineralization of same mineralization groups. The reasons of gold concentration in the oxidation zone are: 1). Change of redox potential (Eh) makes gold to deposit from the liquid of mineralization zone; 2). PH is one of the most factors of gold’s deposition; 3). Soluble complex and colloid of gold can be adsorbed easily. 9. The biotite and hornblende K-Ar isotopic ages from the wall rock－quartz diorite, biotite granite and monzonite granite are 231.99±3.45Ma, 237.97±2.36Ma and 296.53±6.69Ma respectively. The ore-bearing rhyolitic breccia lava contains breccia of the biotite granite which indicates the volcanism and related Cu-Au mineralization occurred later than the granite, possibly in Mesozoic. K-Ar ages of granitoids in Sanya, Baishiquan and Hongliugou area and Molybdenite Re-Os age of Baishan Mo deposit all are in Triassic. Besides late Paleozoic magmatism, igneous magmatic event of Mesozoic was widespread in eastern Tianshan. 10. The K-Ar age dating indicates that the K-Ar age of Voltaite occurred below surface 1m is 56.02±3.98Ma, K-Ar age of Ferricopiapite occurred below surface 1.5m is 8.62±1.12Ma, K-Ar age of Yavapaiite occurred below surface 14 m is 4.07±0.39Ma, and K-Ar age of Voltaite occurred below surface 10 m is 14.73±1.73Ma. So the age interval of oxidation zone of Hongshan copper-golden bed is between 60 -3.38Ma. Oxidization occurred at Caenozoic era (from 65Ma), which can be identified through comparing with different deposits oxidation zone in other countries. The coupling between global tectonic event and climatic change event which occur from Caenozoic era has some effect on epigeosphere system, which can act on the surface of bed oxidation zone similarly. It induces that the age mentioned above coincide with collision of India-Asia and multistage uplifting of Qinhai-Tibet Plateau happened subsequently. Bed oxidation zone is the effect and record of collision and uplifting of Tibet Plateau. The strong chemical weathering of surface accumulation to which was leaded by PETM event occurred Paleocene and Eocene is the reason of Voltaite sharply rises. On the contrary, Ferricopiapite formed due to the global cold weather. The predecessor did much research through biota, isotopes, susceptibility, but this paper try to use different sulfate mineral instead of climatic change. So the research of sulfate minerals not only indicates a great deal of oxidized zone feature, but also the intergrowth of sulfate minerals may be used to trace paleoenviroment and paleoclimate of oxidation zone. 11. Analysis of the information of alteration and mineralization features of four bore cores, induced activity polarization well logging and Eh-4 geophysical section, deep mineralization anomaly objects of Hongshan ore districts shows low resistance, middle and high polarization, measurements of Eh-4 consecutive conductance section show the existing of concealed porphyry ore body deeper than 450m, on the top of and around rock body there are low resistance body ranged from 100-300Ω•m, this area may be the ore-bearing part. In a word, Hongshan Cu-Au deposit deposit is a combine of upper HS-style epithermal Au deposit and deeper porphyry mineralization system. It has great potential to find large HS-style epithermal-porphyry Au-Cu deposits. This paper consists of seven chapters and twenty seven sections. The geological character of deposit is basic condition in this work. Constitute of oxidation zone, research of sulfate mineral, relation between oxidation and primary zone, K-Ar ages of potassic sulfate are key parts of thesis. Genesis of ore deposit is the further expansion of this research. Analysis of ore-controlling factors is the penetration above basic. Analysis of potential is application of exploration.

白云鄂博碳酸岩脉的显微共聚焦激光拉曼光谱分析

白云鄂博矿区发育的脉状稀土碳酸岩，由于其结晶迅速，矿物颗粒细微，其中的微小矿物的鉴定一直是 一个难题。应用显微共聚焦激光拉曼光谱仪则能较好地解决这一问题。研究表明，白云鄂博地区存在富稀土 白云质岩浆碳酸岩脉，早期阶段形成碱性长石和铁白云石，无稀土矿化；铁白云石常常出溶铁质而自身则形成 方解石。霓石和方解石形成略晚，常常与氟碳铈矿等稀土矿物共生，出现强烈的稀土矿化；而无解理的方解石 则形成于更晚的岩浆期后热液阶段，发育大量的流体包裹体，并出现强烈的铌、稀土矿化。铌铁矿分布在氟碳 铈矿中和赤铁矿边缘，为热液交代作用的产物。早期结晶的矿物如碱性长石、铁白云石稀土矿化弱，岩浆晚期 分异出大量的流体相，稀土元素和sr等进入岩浆热液中，并在热液结晶矿物中富集，甚至在非平衡结晶的石英 中产生强烈的稀土矿化。结合岩相学显微观察， 微拉曼探针很好的揭示了这⋯地质过程。同时为白云鄂博 矿床铌、稀土矿化的热液交代成因提供了依据。