13 resultados para Arrow in-flight characteristics
em Chinese Academy of Sciences Institutional Repositories Grid Portal
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in experiment, characteristics of silicon microring/racetrack resonators in submicron rib waveguides have been systematically investigated. It is demonstrated that only a transverse-electric mode is guided for a ratio of slab height to rib height h/H = 0.5. Thus, these microring/racetrack resonators can only function for quasi-transverse-electric mode, while they get rid of transverse-magnetic polarization. Electron beam lithography and inductively coupled plasma etching were employed and improved to reduce side-wall roughness for low propagation loss and high performance resonators. Then, the effects of waveguide dimensions, coupling region design, waveguide roughness, and oxide cladding for the resonators have been considered and analyzed. (C) 2008 Elsevier B.V. All rights reserved.
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Ti45--xZr35--xNi17+2rCU3 (x=0, 2, 4, 6 and 8) icosahedral quasicrystalline phase (I-phase) alloy powders are synthesized by mechanical alloying and subsequent annealing techniques, and the crystallographic and electrochemical characteristics are investigated. The alloy powders are I-phase, and the quasi-lattice constant decreases with increasing x value. The maximum discharge capacity of the I-phase alloy electrodes first increases and then decreases with increasing x value, and the Ti39Zr26Ni29Cu3 I-phase electrode exhibits the highest discharge capacity of 274 mAh g(--1). The high-rate dischargeability at the discharge current density of 240mA g(--1) increases from 55.31 % (x= 0) to 74.24% (x= 8). Cycling stability also increases with increasing x value. The improvement in electrochemical characteristics may be ascribed to the added nickel, which not only improves the electrochemical activity, but also makes the alloy more resistant to oxidation.
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毛壳菌属很多种类具有重要生防价值,其生防机理包括对植物病原真菌的重寄生作用、诱导植物产生抗病性、产生抗真菌活性的次生代谢产物等。迄今,学界对毛壳菌的研究主要集中在毛壳菌的生防机理,毛壳菌活性次生代谢产物的分离等方面。本研究致力于产抗生素的毛壳菌的种间原生质体融合,从产抗生素毛壳菌菌株的筛选开始,进而对产抗生素的角毛壳菌进行诱变选育,最终用产不同抗生素的角毛壳菌与球毛壳菌进行种间原生质体融合。主要有以下五方面研究结果。 1、毛壳菌抗真菌活性物质产生菌株的筛选:不同毛壳菌菌株发酵液采用琼脂扩散法对植物病原真菌进行抑菌活性试验,结果显示,菌株CH08和CH23的发酵液对芒果炭疽、苹果炭疽和马铃薯晚疫菌具有抑制作用。菌株CH16和CH17的发酵液对芒果炭疽菌、苹果炭疽菌有抑制作用。菌株CH21发酵液对辣椒炭疽菌和西瓜枯萎菌有抑制作用。经形态学研究,菌株CH08、CH16、CH17和CH23鉴定为球毛壳菌,菌株CH21鉴定为角毛壳菌。对角毛壳菌与球毛壳菌菌株发酵液抑菌谱比较,发现角毛壳菌与球毛壳菌发酵液具有明显不同的抑菌谱,表明角毛壳菌与球毛壳菌产生不同的抗真菌活性物质。 2、角毛壳菌(CH21)和球毛壳菌(CH08)原生质体制备和再生条件研究:考察了菌龄、酶浓度、稳渗剂及其浓度、酶解温度、酶解时间及再生培养基对原生质体制备和再生的影响。用菌龄为生长54 h的角毛壳菌菌丝,以0.06 M磷酸缓冲液(pH6.0)配制成含蜗牛酶15 mg/ml、溶壁酶10 mg/ml、蔗糖0.6 mol/L的酶解液,30℃酶解1.5 h,原生质体释放量2.02×107个/g;以PDA为再生培养基,0.7 mol/L的蔗糖再生稳渗剂,再生率可达51.45%。用菌龄为生长48 h的球毛壳菌菌丝,以0.06 M磷酸缓冲液(pH6.0)配制成含蜗牛酶15 mg/ml、溶壁酶10 mg/ml、蔗糖0.6 mol/L的酶解液,30℃酶解1 h,原生质体释放量达1.57×108个/g;以PDA为再生培养基,0.7 mol/L的蔗糖为再生稳渗剂,再生率可达41.48%。 3、角毛壳菌(CH21)原生质体紫外诱变选育:以CH21为出发菌株,制备原生质体进行紫外诱变,诱变条件为:15 w紫外灯,距离30 cm,照射90 s,致死率80%~85%。建立了诱变菌株初筛的双层平板筛选模型。经平板初筛和摇瓶复筛,获得一株突变菌株CH21-I-402,其发酵液抑菌活性较出发菌株提高18.3%。 4、抗性标记菌株的获得:菌株CH21-I-402和CH08抗生素药敏试验表明, CH21-I-402菌株对潮霉素有抗性、对G418(Geneticin)敏感,菌株CH08对潮霉素和G418都敏感。根癌农杆菌EHA105介导的新霉素磷酸转移酶基因转化球毛壳菌,经PCR检测,新霉素磷酸转移酶基因成功转化进菌株CH08-GR70,CH08-GR120。转化子对G418抗性提高3~4倍,对潮霉素仍然比较敏感。 5、以G418和潮霉素抗性为筛选标记的原生质体融合与融合菌株AFLP分析:制备角毛壳菌CH21-I-402和球毛壳菌CH08-GR70原生质体,以35%的PEG6000为助融剂进行原生质体融合,以65 μg/ml的潮霉素和60 μg/ml G418为抗性筛选标记,获得46个再生菌株。再生菌株连续传代5代后,再生菌株表现出多种形态类型。利用AFLP技术对再生菌株及亲本菌株基因组DNA分析表明,再生菌株PF1、PF26为融合菌株。抑菌活性测试表明,融合菌株PF26发酵液对芒果炭疽菌和苹果轮纹菌有强的抑制作用,且抑菌活性比亲本球毛壳菌明显提高。 Chaetomium spp. have great potentials as biocontrol agents against a range of plant pathogens on the basis of its mycoparasitism, induced plant disease resistance, production of antifungal metabolites, and so on. Previous researches on C. spp. mostly focused on the mechanisms of its biocontrol and the isolation of secondary metabolites. In this study, screening antifungal C. spp., mutation breeding of C. cupreum and interspecies protoplast fusion between C. cupreum and C. globosum were carried out, respectively. The corresponding results are as follows: Firstly, among more than 40 C. spp., the strains produced anti-fungal antibiotics were screened by agar diffusion experiments. Results showed that both CH08 and CH23 had inhibition against Colletotrichum gloeosporioides, Cladosporium fulvum, and Phytophthora infestans. Both CH16 and CH17 had inhibition against Colletotrichum gloeosporioides and Cladosporium fulvum. In addition, CH21 exhibited anti-fungal activity against Fusarium oxysporum f. sp niveum and Colletotrichum capsici. Furthermore, CH08, CH16, CH17 and CH23 were identified as C. globosum, CH21 was proved to be C. cupreum based on morphology. The comparison of the anti-fungal spectrum between C. cupreum and C. globosum, showed they could produce different antibiotics. Secondly, specified protocols for preparing and regenerating protoplasts from mycelia of C. cupreum CH21 and C. globosum CH08 were studied. The effects of the age mycelia, the concentration of enzyme, digestion temperature and time, kinds of osmotic stabilizer and regeneration medium on protoplasts preparation and regeneration were all optimized, respectively. In one protocol, with 15 mg/mL snailase, 10 mg/mL lywallzyme, 0.6 M sucrose, in 0.06 M phosphate buffer (pH6.0), and digested for 1.5 h at 30 ºC, 2.02×107 protoplasts from each gram mycelia were obtained from cultures of C. cupreum CH21 grown in potato dextrose broth (PDB) medium for 54 h. And when 0.7 M sucrose was used as osmotic stabilizer in the regeneration medium OPDA (potato dextrose agar with osmotic stabilize), the regeneration efficiency of protoplasts was 51.45%. In another protocol, with 15 mg/mL snailase, 10 mg/mL lywallzyme, 0.6 M sucrose, in 0.06 M phosphate buffer (pH6.0), and digested for 1 h at 30 ºC, 1.57×108 protoplasts from each gram mycelia were obtained from cultures of C. globosum CH08 grown in PDB for 48 h. And when 0.7 M sucrose was used as osmotic stabilizer in the regeneration medium OPDA, the regeneration efficiency of protoplasts was 41.48%. Thirdly, the mutagenesis conditions and secondary screening model of C. cupreum CH21 were explored. An 80% to 85% death rate could be achieved when the protoplasts of C. cupreum CH21 were irradiated by 15 w UV lamp from 30 cm distance for 90 s. In addition, the doublelayer plate’s method for the primary screening of high-producing antibiotics strains was established. A high yielding antibiotic mutant CH21-I-402 was obtained through the primary screening on plate and the secondary selection in Erlenmeyer flask, compared to the original CH21 strain, the antifungal activity of the mutant CH21-I-402 was increased by 18.3%. Fourth, the sensitivity to antibiotics of both C. cupreum CH21-I-402 and C. globusm CH08 was detected. Results showed C. cupreum CH21-I-402 was sensitive to G418 (Geneticin) (Gs) and resistant to Hygromycin B(Hr), and C. globusm CH08 was sensitive to both G418 (Geneticin) (Gs) and Hygromycin B(Hs). At the same time, neomycin phosphotransferase II (npt II) gene was transformed into C. globusm CH08(Gs, Hs) mediated by Agrobacterium tumefaciens EHA105, and the npt II gene was verified by polymerase chain reaction in resistance to G418 strains CH08-GR70 and CH08-GR120. The transformants still showed sensitive to Hygromycin B(Hs). Finally, a selection system for hybrids was set up by interspecies protoplast fusion between C. cupreum and C. globusm using dominant selective drug resistance markers. At first, protoplasts of C. cupreum CH21-I-402 (Hr, Gs) and C. globusm CH08-GR70 (Hs, Gr) were prepared, then the protoplasts were fused in the presence of 35% polyethylene glycol 6000 and regenerated on OPDA medium with 65 μg/ml Hygromycin B and 60μg/ml G418, at last 46 colonies with Hr and Gr were obtained. Even after 5 generations’ subculture, most of the colonies displayed significant difference in taxonomic characteristics with their parental strains. Regenerated strains PF1 and PF26 were confirmed as fusants by amplified fragment length polymorphisms analysis with the genomic DNA as the model. PF26 showed higher inhibitory activity against Colletotrichum gloeosporioides and Macrophoma kuwatsukai than that of the parental strain C. globusm.
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本文工作分为两个部分:第一部分是设计德国重离子研究中心(GSI)的一段新的次级束流线;第二部分计算了在建的R工已LLZ对裂变反应碎片的传输分离,同时为提高分离本领对RIBLLZ进行了优化计算和设计。FRS是德国重离子研究中心(GSI)的次级束流线。其分支FRS-CAVEB的终端是川JAD工N的实验终端,这条线的束流品质不理想(传输率只有0.1%),因此GSI拟将AI'AD州设备(原在CAVEB)移到CAVEC中,形成FRS一CAVEC束流线,又称FRS-R3Bcave。本文对FRS-CoveC进行了束流光学设计和计算,同时模拟了FRS-CAVEC对弹核碎裂反应的传输分离。新束线按计算结果安装了一个二极磁铁和3个四极磁铁,并通过了实验测试,测试结果表明:(1)系统具有良好的消色散特性,即系统在FRS出口和实验终端处达到了消色差。(2)系统的传输率基本符合理论计算值,相对CAVEB分支传输率提高了一个量级以上。当不放任何阻止物质在束流线上时,Ar主束传输率可以达到100%;当放置3mm厚的Sdntillator探测器在S2,S8,CaveC处时,主束传输率基本和理论计算值相近(640k-计算值,610k-实验值)。对比FRS-C八VEB的实验传输率(0.1%),可知通过改进,FRS-C八VEC的传输率将得到极大的改善。RIBLLZ是连接CSR两环之间的次级束流线。现有的RIBLLZ束流线设计的比较紧凑,立体角接收度大,使得所有粒子都可通过系统,可以作为零度质谱仪,尤其是可以将裂变产生的奇异核素注入到实验环进行质量测量。本文模拟了弹核碎片和裂变反应产生的次级束在现有的RIBLLZ上的传输情况。计算表明,现有的RIBLLZ对通过u裂变产生的大量较重奇异核素,具有很高的传输率。另一方面,现有的RIB七LZ在散焦面只有两个四极磁铁,为达到系统的消色差及较大的分辨率会使得Y方向的束流控制困难。基于此,对现有的R咸喝锻蓄尔\一些改进计算。还理论计算比较了两个系统对裂变反应的传输分离情况。玺认算试知飞(1)优化后的RIBLLZ系统对束流在Y方向的控制将更灵活。(2)对裂变反应产物的传输,除了作为零度质谱仪外还可以作为单一核素的分离器。(3浑税盯确集磁系统的传输率对降能器厚度敏感度降低,对于u裂变反应产生的132sn的传输率,当降能器厚度从19/cmZ变化到39/clnu时,传输率下降20%,而未优化的RIBLLZ系统的传输率将下降90%。
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In this work, we report the findings of a study on scanning electrochemical microscopy (SECM) to investigate the interfacial electron-transfer (ET) reaction between the 7,7,8,8-tetracyanoquinodimethane radical anion (TCNQ(.-)) in 1,2-dichloroethane and ferricyanide in an ice-like matrix (a mixture of insulting ice and conductive liquid) under low temperatures. Experimental results indicate that the formed liquid/ice-like matrix interface is superficially similar in electrochemical characteristics to a liquid/liquid interface at temperatures above -20 degreesC. Furthermore, imaging data show that the surface of the ice-like matrix is microscopically flat and physically stable and can be applied as either a conductive or an insulting substrate for SECM studies. Perchlorate ion was selected as the common ion in both phases, the concentrations of which controlled the interfacial potential difference. The effect of perchlorate concentration in the DCE phase on interfacial reactions has been studied in detail. The apparent heterogeneous rate constants for TCNQ(.-) oxidation by Fe(CN)(6)(3-) in another phase under different temperatures have been calculated by a best-fit analysis, where the experimental approach curves are compared with the theoretically derived relationships. Reaction rate data obey Butler-Volmer formulation before and after the freezing point, which is similar to most other known cases of ET reactions at liquid/liquid interfaces. However, there is a sharp change observed for heterogeneous rate constants around the freezing point of the aqueous phase, which reflects the phase transition. At temperatures below -20 degreesC, surface-confined voltammograms for the reduction of ferricyanide were obtained, and the ice-like matrix became an insulating one, which indicates that the aqueous phase is really a frozen phase.
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本文采用冲绳海槽北部柱状岩芯DOC024,通过对其微体古生物分析和地球化学分析,结合浮游有孔虫氧、碳同位素数据、AMS14C 测年结果和已有的研究资料,对7500年以来该区域古生产力演化、古上升流演化及黑潮对该区域的影响进行了分析探讨。 冲绳海槽北部,九州西南海区,全新世晚期7.5ka BP以来,该区的钙质和硅质生物生产力存在着显著的差异,钙质生物的生产量高值出现在7.0ka BP 左右,但在7.0-6.4ka BP 之后明显下降而且十分稳定;而3.0ka BP 左右是硅质生物生产量的高值期,3.0ka BP 之前硅质生物生产力逐渐增加,之后呈下降趋势;表层海水初级生产力亦在7.0ka BP 左右出现短暂的高值,之后呈下降趋势,波动较频繁,0.9kaBP前后也出现了较明显的高值。古生产力的这一变化过程可能主要反映了黑潮与陆架水混合过程,以及与其相关的上升流强度的变动。 冲绳海槽北部、九州西南海区,全新世7.5-7.0ka BP陆源物质影响明显, 7.0kaBP前后黑潮侵入并与陆架水强烈混合,7.0-6.0ka BP 期间黑潮影响逐渐控制了该区,上升流开始发生,温跃层开始变浅;约在6.0-2.0ka BP 之间上升流持续稳定发育,温跃层深度逐渐下降:6.0-5.0ka BP上升流影响作用于温跃层但对表层影响较小,5.0-4.0ka BP海水表层温度受上升流冷水影响降低;而约2.0-1.2ka BP,上升流减弱,海水表层温度回升;近1200 年来上升流加强、温跃层深度减小的趋势更加显著。上升流的发育明显地控制着温跃层深度的变化,上升流强度与黑潮强度密切相关,且在一定范围内有线性关系,冲绳海槽北部冷涡区域附近海洋环境的变化也存在着明显的区域性特征。 由于受冲绳海槽北部复杂的海洋环境、DOC024 柱状样中7.5ka BP 左右火山活动的扰动作用,使我们难以准确而详细地探讨全新世黑潮在冲绳海槽北部的变动;但根据对数据的分析讨论,并结合已有研究成果可以得出以下认识:在冲绳海槽北部,7.5aBP前后黑潮强度减弱,以至于几乎完全失去了对该海区的影响;7.0-2.0kaBP上升流的稳定发育说明了黑潮较稳定,仅有小幅波动;2.0-1.2kaBP上升流减弱,黑潮减弱;1.2kaBP伴随着气候的变暖,黑潮增强且幅度较大;0.3kaBP 随着气候变冷,黑潮有所减弱;总体上自7.0aBP前后黑潮入侵以来黑潮对该区的影响一直存在,而6.6kaBP以来黑潮底层水团对该区的影响比较稳定。
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In this paper, the detailed morphology of Prorocentrum donghaiense Lu from both field samples and cultures was examined, and a taxonomic comparison was made between P donghaiense and some related Prorocentrum spp. using morphological and molecular data and other published information. There were distinct differences among these species in morphological characteristics that historically have been presented as conservative features. The discrepancies extended beyond that of individual variations within the same species due to environmental factors. Therefore, these morphological features may not be conservative but, rather, polymorphic depending on environmental conditions. Based on this analysis, we suggest that the high-biomass bloom-forming species in the East China Sea, previously reported as Prorocentrum dentatum Stein, is P donghaiense Lu. The species reported from the East China Sea and Japanese and Korean waters appear to be the same species. Molecular data also suggest that P. dentatum (CCMP1517) and P. donghaiense are genetically identical. Therefore, the geographic distribution of P. donghaiense may be much wider than expected. (C) 2004 Elsevier B.V. All rights reserved.
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高级控制算法对于无人直升机实现高机动性非常重要,但是在实现上也经常受制于鲁棒性和实时性的要求。同时这些控制方法在飞行测试时也会带来高风险。本文介绍了一种自制的安装在机械臂上的直升机作为实验平台去验证控制方法的有效性和可行性,这个平台还能够保证飞行测试的安全性。实验结果显示,能够实现转速跟踪控制以及航向动力学的辨识,并证明平台的有效性。
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The past two decades have witnessed an unprecedented growth of interest in the palaeoenvironmental significance of the Pleistocene loess deposits in northern China. However, it is only several years ago that the Tertiary red clay sequence underlying Pleistocene loess attracted much attention. One of the major advances in recent studies of eolian deposits on the Loess Plateau is the verification of the eolian origin for the Tertiary red clay sediments. The evidence of the eolian origin for the red clay is mainly from geochemical and sedimentological studies. However, sedimentological studies of the red clay deposits are still few compared with those of the overlying loess sediments. To date, the red clay sections located near Xifeng, Baoji, Lantian, Jiaxian, and Lingtai have been studied, with an emphasis on magnetostratigraphy. These sections have a basal age ranging from ~4.3 Ma to ~7.0 Ma. The thickness of the sections varies significantly, depending perhaps on the development of local geomorphological conditions and the drainage system. Although the stratigraphy of the red clay sections has been recorded in some detail, correlation of the red clay sequences has not yet been undertaken. Geological records (Sun J. et al., 1998) have shown that during glacial periods of the Quaternary the deserts in northem China were greatly expanded compared with modern desert distribution. During interglacial periods, desert areas contracted and retreated mostly to northwestern China because of the increase in inland penetration of monsoonal precipitation. According to pedogenic characteristics of the red clay deposits, the climatic conditions of the Loess Plateau is warmer and wetter generally in the Neogene than in the late Pleistocene. Panicle analyses show that grain size distribution of the red clay sequence is similar to that of the paleosols in the Pleistocene loess record, thus implying a relatively remote provenance of the red clay materials. However, the quantitative or semiquantitative estimates of the distance from the source region to the Loess Plateau during the red clay development remains to be investigated. In this study, magnetostratigraphic and sedimentological studies are conducted at two thick red clay sequences-Jingchuan and Lingtai section. The objectives of these studies are focused on further sedimentological evidence for the eolian origin of the red clay, correlation of red clay sequences, provenance of the red clay, and the palaeoclimate reconstruction in the Neogene. Paleomagnetic studies show that the Jingchuan red clay has a basal age of 8.0 Ma, which is 1 million years older than the previously studied Lingtai section. The Lingtai red clay sequence was divided into five units on the basis of pedogenica characteristics (Ding et al., 1999a). The Jingchuan red clay sequence, however, can be lithologically divided into six units according to field observations. The upper five units of the Jingchuan red clay can generally correlate well with the five units of the Lingtai red clay. Comparison of magnetic susceptibility and color reflectance records of four red clay sections suggests that the Lingtai red clay sequence can be the type-section of the Neogene red clay deposits in northern China. Pleistocene loess and modem dust deposits have a unimodal grain-size distribution. The red clay sediments at Jingchuan and Lingtai also have a unimodal grain-size distribution especially similar to the paleosols in the Pleistocene loess record. Sedimentological studies of a north-south transect of loess deposits above S2 on the Loess Plateau show that loess deposits had distinct temporal and spatial sedimentary differentiation. The characteristics of such sedimentary differentiation can be well presented in a triangular diagram of normalized median grain size, normalized skewness, and normalized kurtosis. The triangular diagrams of the red clay-loess sequence at Lingtai and Jingchuan indicate that loess-paleosol-red clay may be transported and sorted by the same agent wind, thus extending the eolian record in the Loess Plateau from 2.6 Ma back to about 8.0 Ma. It has been recognized that during the last glacial maximum (LGM) the deserts in northern China had a distribution similar to the present, whereas during the Holocene Optimum the deserts retreated to the area west of the Helan Mountains. Advance-retreat cycles of the deserts will lead to changes in the distance of the Loess Plateau to the dust source regions, thereby controlling changes in grain size of the loess deposited in a specific site. To observe spatial changes in sedimentological characteristics of loess during the last glacial-interglacial cycle, the texture of loess was measured along the north-south transect of the Loess Plateau. Since the southern margin of the Mu Us desert during the LGM is already known, several models of grain size parameters versus the minimum distance from the source region to depositional areas were developed. According to these semiquantitative models, the minimum distance from the source region to Lingtai and Jingchuan areas is about 600 km during the Neogene. Therefore the estimated provenance of the Tertiary red clay deposits is the areas now occupied by the Badain Jaran desert and arid regions west of it. The ratio of the free iron to total iron concentration attests to being a good proxy indicator for the summer monsoon evolution. The Lingtai Fe_20_3 ratio record shows high values over three time intervals: 4.8-4.1 Ma, 3.4-2.6 Ma, and during the interglacial periods of the past 0.5 Ma. The increase in summer monsoon intensity over the three intervals also coincides with the well-developed soil characteristics. It is therefore concluded that the East-Asia summer monsoon has experienced a non-linear evolution since the late Miocene. In general, the East Asia summer monsoon was stronger in Neogene than in Quaternary and the strongest East Asia summer monsoon may occur between 4.1 and 4.8 Ma. The relatively small ice volume and high global temperature may be responsible for the strong summer monsoon during the early Pliocene.
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A strain of microalgae (Anabaena siamensis) had been cultured in a miniaturized bioreactor during a retrievable satellite flight for 15 days. By means of remote sensing equipment installed in the satellite, we gained the growth curve of microalgae population in space every day in real time. The curve indicated that the growth of microalgae in space was slower than the control on ground. Inoculation of the retrieved microalgae culture showed that the growth rate was distinctively higher than ground control. But after several generations, both cultures indicated similar growth rates. Those data showed that algae, can adapt to space environment easily which may be valuable for designing more complex bioreactor and controlled ecological life support system in future experiment. (C) 2006 Elsevier Ltd. All rights reserved.
Resumo:
本文研究了圆柱受限空间内的喷雾火焰嫩烧压力振荡的特性。为了更清楚地了解火焰的构造, 首先测量了火焰的温度场,在较大的一次风和二次风变化范围内, 测量了压力的振荡特性。结果表明,火焰的稳定是由回流区完成的, 在较小的一次风燃料当量比和中等的二次风量时, 振荡最强, 达到100Pa左右的量级,其频率为200-230Hz左右,分析表明燃烧室中的振荡是轴向驻波振荡。