9 resultados para Shatter Cones

em Chinese Academy of Sciences Institutional Repositories Grid Portal


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Planar graphite has been extensively studied by Raman scattering for years. A comparative Raman study of several different and less common non-planar graphitic materials is given here. New kinds of graphite whiskers and tubular graphite cones (synthetic and natural) have been introduced. Raman spectroscopy has been applied to the characterization of natural graphite crystal edge planes, an individual graphite whisker graphite polyhedral crystals and tubular graphite cones. Almost all of the observed Raman modes were assigned according to the selection rules and the double-resonance Raman mechanism. The polarization properties related to the structural features, the line shape of the first-order dispersive mode and its combination modes, the frequency variation of some modes in different carbon materials and other unique Raman spectral features are discussed here in detail.

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The performance of 23 kinds of waveriders, derived from different conical flowfields, is analyzed by the numerical computation under the conditions of fight speed of Mach 6, attack angle of 0° and flight altitude of 30 km. These results indicate that the performance is influenced by the shapes and the width to height ratios (W/H ) of generating cones. The geometrical parameter and the lift coefficient are proportional to W/H, while the drag coefficient and the lift to drag ratio (L/D ) have extreme values. Considering the base drag and the computation errors, the waverider with the highest L/D is cut from the elliptical cone’s flowfield (W/H = 1.5―1.618), and the configuration with the lowest drag can also be obtained at W/H = 1:1.5. Accordingly, good suggestions are proposed for practical design based on these computational results.

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A method based on the computational fluid dynamics (CFD) is presented for a flexible waverider's design. The generating bodies of this method could be any cones. In addition, either the leading edge or the profile of the scramjet's inlet is used as the waverider's definition curve, parameterized by the quadric function, the sigmoid function or the B-spline function. Furthermore, several numerical examples are carried out to validate the method and the relevant codes. The CFD results of the configurations show that all the designs are successful. Moreover, primary suggestions are proposed for practical design by comparing the geometrical and aerodynamic performances of the cone-derived waveriders at Mach 6.

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近几年,松果采摘对红松林的健康构成了极大的威胁。本文在野外调查研究的基础上,结合史料分析研究了松果采摘对红松地面种源贮藏量分布状况、红松林主要乔木树种组成和幼苗幼树更新等的影响,通过与20世纪70年代相应数据对比,结合红松更新过程与动物的关系,分析了松果采摘对红松林生态系统健康的影响。研究结果表明:(1)松果采摘后,红松林地面红松种子数量少,大部分是废种子,且主要呈单粒状分布,地面红松种子贮藏量1582-2640粒/hm2,仅为70年代的0.3-0.5%,废种子比值大于67.8%,单粒状占总簇数的46.8-77.1%。(2)“采摘掠青”对种子质量具有显著影响,9月15日与8月20日采摘的松果相比,种子千粒重增加了69%,种仁重增加了30.3%,出仁率增加了2.7%,球果鲜重减少了20.0%,种子重增加了21.3%,出种率增加了51.7%。(3)与红松林中其他主要更新树种相比,采摘使红松更新不良,红松幼苗数量大大减少,减少幅度达49.5-95.0%。(4)破坏了红松天然更新规律,2000年是结实年,但2002年并没有出现更新年。(5)林分中红松小径级植株占比值很小,而大径级比值大,呈生长下降性种群;而其它主要伴生树种与此相反,呈生长增长性种群。(6)以松籽为主要食物来源的动物食物链遭到破坏,红松林生物群落结构发生变化。在此分析基础上,提出了以松果采摘为例的长白山自然保护区健康管理策略,以期为保护区管理提供科学依据。

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岷江柏(Cupressus chenggiana S. Y. Hu)是我国川甘地区特有的珍稀濒危乔木,一般生长在干旱的河谷区,在涵养水源和保护水 土等方面起着重要的作用。本文选择4个岷江柏种群,采用了野外调查和室内实验相结合的研究方法,调查岷江柏种群结实状况, 分析种子和球果形态特征,阐明种子发芽的基本特征,研究岷江柏种子贮藏过程中几个生理指标的动态变化特点,目的是为岷江柏 种苗繁育、自然更新能力评估以及珍稀濒危机制分析提供理论依据。研究得出如下结论:1.岷江柏球果呈椭球形,长为1.5~ 2.2cm,宽为1.5~1.9cm,质量为1.7~4.2g,球果鳞片数量为8~11片,球果内种子数量一般在40~70粒。岷江柏种子为椭圆形,长 为3.58~4.02mm,宽为3.10~3.15mm,厚为0.96~1.11mm,千粒重为3.1~3.5g。岷江柏的结实率很低,并且有显著的地理差异和 大小年差异。2. 岷江柏种子发芽温度范围是5℃~30℃,其中种子的适宜发芽温度范围是10℃~25℃。种子最适发芽温度随着贮藏 时间的增加而变化。在适宜温度范围内,种子发芽周期为20d。温度对种子的发芽势和T50有显著影响,对种子发芽率没有显著影响 ;光照有利于种子发芽;岷江柏种子的发芽特征是岷江柏保护种子资源、防止物种濒危的一种环境适应,有助于岷江柏种子提高发 芽率和幼苗的存活率。岷江柏种子是一种耐贮藏的正常性种子,在短期贮藏过程中,贮藏温度和种子含水量对于种子生理指标和种 子发芽没有显著影响。3. 岷江柏种子在短期贮藏过程中,千粒重没有显著变化;含水量都经历了先下降,再稳定的过程;粗脂肪 含量和可溶性糖含量逐渐降低;可溶性蛋白含量和丙二醛含量逐渐增加;脯氨酸含量在贮藏1~7个月时变化差异不明显,但是贮藏 7~10个月后显著增加。岷江柏种子的各个生理指标之间的相关性差异不显著。4. 岷江柏球果和种子的形态特征存在显著的地理差 异。岷江柏种子的发芽能力的地理性差异不大,种群间差异不大。岷江柏种群的地理差异由种群特征、生境特征和气候特征共同决 定。5. 在岷江柏的人工繁育中,对于刚刚采集的种子,发芽温度在15℃~25℃比较适合,其中以25℃最佳;而对于短期贮藏(4~ 10个月)后的种子,发芽温度在10℃~25℃均可,以15℃~20℃为最佳。野外播种的最适时间为4~6月,6~9月的间歇性干旱和降 水波动可能是限制岷江柏自然更新的因素之一。在短期贮藏过程中,种子可以采用常规室温贮藏,可以节约成本。Cupressus chenggiana is a specific and endangered plant in Sichuan and Gansu provinces of China, and it usually grows in dry valley and plays an important role in water supply and soil and water conservation in the dry valley of alpine and canyon region of southwest China. The research selected four Cupressus chenggiana populations and used the methods of the field investigation and the lab experiments. The fruiting characters of Cupressus chenggiana populations, the morphological characters of seeds and cones, the germination characters of seeds and the store physiological dymatics of several factors of seeds have been studied in order to give some theoretical advices on the artificial propagation and the ability of natural regeneration and the endangered principle of Cupressus chenggiana in the paper. The main results may be clarified as follows: 1. The cones of Cupressus chenggiana are ellipsoidal, length ranged from 1.5 to 2.2cm, with ranged from 1.5 to 1.9 cm, weight ranged from 1.7 to 4.2g, the number of cone squama ranged from 8 to 11, and the seed number of per cone ranged from 40 to 70. The seeds of Cupressus chenggiana are elliptical, length ranged from 3.58 to 4.02 mm, width ranged from 3.10 to 3.15 mm, thickness ranged from 0.96 to 1.11 mm, and the weight of 1000 seeds ranged from 3.1 to 3.5g. The fruiting rate of Cupressus chenggiana is very low, and the fruiting period of Cupressus chenggiana has the geographical differences and the big or small year differences. 2. Seed germination temperature is between 5℃ and 30℃, while the suited temperature is between 10℃ and 25℃. The optimum temperature of seed germination will change as the store time of seeds changes logner. The cycle of seed germination can persist 20 days in the range of the suited temperature. The germination temperatures have significant influences on the germination potential and T50, but have no significant infuluences on the germination rate. The photoperiod is in favor of seed germination. The characters of Cupressus chenggiana seed germination represent a kind of environmental adaptability to protect the seed sources and endangered species, and it can give help to increase the germination rate of seeds and the livability of seedings. The seeds of Cupressus chenggiana are a kind of orthodox seeds that can endure the long time storage. In the short time storage, the store temperatures and the moisture contents of seeds have no significant infuluences on the physiological factors and the germination of seeds, but the store time has significant influences on the physiological factors of seeds. 3. In the short store course of Cupressus chenggianna seeds, the 1000 seed weight has no significant variation; The moisture content descends at the beginning of the storage, but has no significant variation later; The crude fat content and the soluble sugar content descend gradually; The soluble protein content and MDA content increase gradually; The praline content has no significant variation after 1~7 months storage, but increase significantly after 7~10 months storage. The correlations of different physiological factors are not significant. 4. The morphological characters of cones and seeds of four populations exist significant differences. The germination of Cupressus chenggiana seeds has no significant geographical variation. The geographical variation of Cupressus chenggiana populations can be ascribed to the population characters, climate and environment. 5. In the course of artificial propagation of Cupressus chenggiana, it is favored that the germination temperature of newly collected seeds is between 15℃ and 25℃, while the optimum temperature is 25℃. After the short storage ranged from 4 months to 10 months, it is favored that the germination temperature is between 10℃ and 25℃, while the optimum temperature is ranged from 15℃ to 20℃. The field sowing optimum time is between April and June, and the interval drought and fallrain fluctuation between July and September may be one of the reasons that restrict natural regeneration of Cupressus chenggiana. In the short storage, seeds can be stored in the condition of room temperature.

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This paper illustrated the relationships between P. koraiensis and animal,and discussed the effect of cones picking on quantity and structure of animal, P. koraiensis regeneration,biomass,services,structure and succession,and nutrient cycle of the ecosystem.It showed that cones picking has damaged the integrity and function of ecosystem health in term of the concepts and characteristics of ecosystem health.The paper was aiming at the strategies to resolve the relationships between cones picking and ecosystem health maintaining in order to give scientific foundations for protection and management of broad-leaved P.koraiensis forest in Changbai Mountain.

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Post-collisional, potassic igneous rocks are widely distributed in the Hoh Xil area of the northern Tibetan Plateau. Based on the field work, petrography, mineral chemistry, K-Ar geochronology, element and Sr-Nd-Pb isotope geochemistry, this thesis systematically studied the spatial and temporal distribution of the volcanic rocks, chemical characteristics, formation mechanism and partial melting mechanism of the magma source region, geodynamic setting of magmatism, as well as crustal assimilation and fractional crystallization (AFC). The results show that: 1. The Miocene (7.77-17.82 Ma) volcanic products dominantly are trachandesite and trachy, and subordinate rhyolites, associated with stike-slip faults and thrust faults, formed morphology of small lava platforms and cinder cones. 2. Phenocrysts in the lavas are augite, andesine, sanidine, calcic amphibole and subordinate orthopyroxene, biotite and Ti-Fe oxides, displaying typical quench texture. Equilibrium temperatures and pressures of clinopyroxene phenocrysts indicate the magma chamber is located in upper-middle crust. 3. Rhyolites are the products of crustal melting and fractionation of shoshonitic magmas. The source region of intermediate magmas is enriched continental lithospheric mantle, which contains residual minerals such as phlogopite, rutile and spinel, and enriched by subducted sediments during earlier multi-episodes of subduction. 4. Upwelling of asthenosphere provides heat for source region melting, and faults provide channels for magma eruption. 5. Northward underthrusting of Indian continental lithosphere and southward of backstop of Asian continental lithosphere resulted in upwelling of hot asthenosphere. Geochemical characteristics of the potassic magmatism in North Tibet are dominantly controlled by source region composition, partial melting, and crustal assimilation and fractional crystallization (AFC).