56 resultados para kinematics and dynamics


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It has been a difficult problem faced by seismologists for long time that how exactly to reconstruct the earth's geometric structure and distribution of physical attributes according to seismic wave's kinematical and dynamic characteristics, obtained in seismological observation. The jointing imaging of seismic reflector and anisotropy attributes in the earth interior is becoming the research hot spot. The limitation of shoot and observation system makes that the obtained seismic data are too scarce to exactly reconstruct the geological objects. It is popular that utilizing only seismic reflection traveltimes or polarizations information make inversion of the earth's velocity distribution by fixing seismic reflector configuration (vice versa), these will lead to the serious non-uniqueness reconstruction due to short of effective data, the non-uniqueness problem of reconstructing anisotropy attributes will be more serious than in isotropy media. Obviously it is not enough to restrict the media structure only by information of seismic reflection traveltimes or polarizations, which even sometimes will lead to distorted images and misinterpretation of subsurface structure. So we try to rebuild seismic reflection structure (geometry) and media anisotropic structure (physics) in the earth interior by jointing data of seismic wave kinematics and dynamics characteristics, we carry out the new experiment step by step, and the research mainly comprises of two parts: one is the reconstruction of P-wave vertical velocity and anisotropic structure(Thomsen parameter s and 8) in the transversely isotropic media with vertical symmetrical axis(VTI) by fixing geometrical structure, and the other is the simultaneous inversion of the reflector surface conformation and seismic anisotropic structure by jointing seismic reflection traveltimes and polarizations data. Simulated annealing method is used to the first research part, linear inversion based on BG theory and Simulated annealing are applied to the second one. All the research methods are checked by model experiments, then applied to the real data of the wide-angle seismic profile from Tunxi, Anhui Province, to Wenzhou, Zhejiang Province. The results are as following The inversion results based on jointing seismic PP-wave or PSV-wavereflection traveltimes and polarizations data are more close to real model than themodels based simply on one of the two data respectively. It is shown that the methodwe present here can effectively reconstruct the anisotropy attributes in the earth'sinterior when seismic reflector structure is fixed.The layer thickness, P-wave vertical velocity and Thomsen anisotropicparameters {s and 8) could be resolved simultaneously by jointing inversion ofseismic reflection traveltimes and polarizations with the linear inversion methodbased on BG theory.The image of the reflector structure, P-wave vertical velocity and theanisotropy parameters in the crust could be obtained from the wide-angle seismicprofile from Tunxi (in Anhui Province), to Wenzhou (in Zhejiang Province). Theresults reveal the difference of the reflector geometrical structure and physicalattributes in the crust between Yangtze block and Cathaysia block, and attempt tounderstand the characteristics of the crustal stress field in the areas.

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Phenolic marine natural product is a kind of new potential aldose reductase inhibitors (ARIs). In order to investigate the binding mode and inhibition mechanism, molecular docking and dynamics studies were performed to explore the interactions of six phenolic inhibitors with human aldose reductase (hALR2). Considering physiological environment, all the neutral and other two ionized states of each phenolic inhibitor were adopted in the simulation. The calculations indicate that all the inhibitors are able to form stable hydrogen bonds with the hALR2 active pocket which is mainly constructed by residues TYR48, HIS110 and TRP111, and they impose the inhibition effect by occupying the active space. In all inhibitors, only La and its two ionized derivatives La_ion1 and La_ion2, in which neither of the ortho-hydrogens of 3-hydroxyl is substituted by Br, bind with hALR2 active residues using the terminal 3-hydroxyl. While, all the other inhibitors, at least one of whose ortho-sites of 3- and 6-hydroxyls are substituted by Br substituent which take much electron-withdrawing effect and steric hindrance, bind with hALR2 through the lactone group. This means that the Br substituent can effectively regulate the binding modes of phenolic inhibitors. Although the lactone bound inhibitors have relatively high RMSD values, our dynamics study shows that both binding modes are of high stability. For each inhibitor molecule, the ionization does not change its original binding mode, but it does gradually increase the binding free energy, which reveals that besides hydrogen bonds, the electrostatic effect is also important to the inhibitor–hALR2 interaction.

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Detritus, as a nutrients reservoir, affects the trophic structure and dynamics of communities and supports a greater diversity of species and longer food chains. Detritivorous fish is an important organism to regenerate the nutrients from sediments. Despite the numerous studies on the nutrients cycle in fish, only a few attempts have been made to quantify the regenerating ability. In the present study, we chose the common detritivorous fish redeye mullet as the research object. Redeye mullet is also a common poly-culture fish in China. Diet, including a commercial diet mostly used in aquaculture and a home-made diet with contents close to detritus, was used and considered as a fixed factor. Temperature was also considered as a fixed factor as much research has shown that temperature has significant effects on fish metabolism. Moreover, body size was regarded as a covariate under analysis of covariance. Three key nutrients, namely carbon, nitrogen and phosphorus, were used to measure the nutrient-regenerating ability of redeye mullet under laboratory conditions. The results showed that the nutrient regeneration in percent of the consumption decreased with increasing temperature. Carbon and nitrogen regeneration of redeye mullet fed on commercial diet was lower than those of the home-made diet group, while the opposite was found for phosphorus. In each group, the amount of regenerated nutrients increased linearly with body size. Fed on the home-made diet, 5-g fish at 25 degrees C can regenerate 210.822 mg C, 37.533 mg N and 0.727 mg P per day.

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利用虚拟现实技术虚拟出月球机器人在月面上的作业环境和作业过程,是提高机器人作业的安全系数和工作效率的一条有效途径。在3D重建得到的虚拟月面环境中,如果采用通常的单纯基于运动学(或者动力学)模型的仿真方法,对机器人的作业和运动进行虚拟,那么机器人与地形交互的过程中容易产生接触偏差。而且,随着仿真时间的推进,这种接触偏差会逐渐积累并不断增大,进而严重影响仿真测试的精度和效果。为了消除月球机器人仿真中的轮地交互误差,在分析误差来源的基础上,提出了基于运动学优化的解决方法。最后利用实际的虚拟现实仿真系统,验证了所提出方法的有效性。

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海洋环境通常是不确定、非结构化和未知的 ,而远程AUV(LAUV)的避障声纳对环境感知有一定的局限 ,因此很难建立起精确、完整和统一的三维环境模型 .LAUV实时避障是一个实时性很强的动态过程 ,它不但与环境有关 ,而且还与LAUV的运动学约束、动力学特性和操纵性有关 .针对上述问题本文提出了一种基于复合控制的三维实时模糊避障方法

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Subgrid nonlinear interaction and energy transfer are analyzed using direct numerical simulations of isotropic turbulence. Influences of cutoff wave number at different ranges of scale on the energetics and dynamics have been investigated. It is observed that subgrid-subgrid interaction dominates the turbulent dynamics when cut-off wave number locates in the energy-containing range while resolved-subgrid interaction dominates if it is in the dissipation range; By decomposing the subgrid energy transfer and nonlinear interaction into 'forward' and 'backward' groups according to the sign of triadic interaction, we find that individually each group has very large contribution, but the net of them is much smaller, implying that tremendous cancellation happens between these two groups.

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Evaporative convection and instability give rise to both scientific and technological interests. Practically, a number of the industrial applications such as thin-film evaporators, boiling technologies and heat pipes concern with the evaporation process of which through the vapor-liquid interface the heat and mass transfer occur. From a physical viewpoint, one of interesting questions is the mechanisms of convection instability in thin-liquid layers induced by the coupling of evaporation phenomenon and Marangoni effect at the mass exchanged interface. Classical theories, including Rayleigh’s and Pearson’s, have only successfully explained convection in a liquid layer heated from below without evaporation. However these theories are unable to explain the convection in an evaporating thin layer, especially liquid layer is cooled from below. In present paper, a new two-sided model is put forward rather than the one-sided model in previous works. In previous works, the vapor is treated as passive gas and dynamics of vapor has been ignored. In this case, the vapor liquid system can be described by one-sided model. In our two-sided model, the dynamics of vapor should be considered. Linear instability analysis of the Marangoni-Bénard convection in the two-layer system with an evaporation interface is performed. We define a new evaporating Biot number which is different from the Biot number in one-sided model and obtain the curves of critical Marangoni number versus wave number. In our theoretical results, the Biot number and the evaporating velocity play a major role in the stability of the vapor-liquid system.

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理论上分析了静动结合的化学腐蚀法制备探针的具体机理及过程。在静态腐蚀的过程中, 利用流体力学Young-Laplace方程的一级近似解获得了光纤插入到HF酸中形成的新月形高度。在动态腐蚀过程中, 详细分析了当静态腐蚀时间和动态腐蚀时间分别取不同值时, 光纤移动速度对光纤探针结构的影响。利用此法可制备出尖端锐利、大锥角或多锥体等各种结构的光纤探针。这为实验上制备出性能优良的探针, 为拓宽扫描近场光学显微镜的应用范围奠定基础。将上述理论分析的结果与本文实验中所得初步结果进行了比较, 所得结果一致。

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旱冬瓜(Alnus nepalensis)和潺槁木姜子(Litsea glutinosa)是云南省无量山黑长臂猿(Nomascus concolor)栖息地中的两种常见乔木.利用最近邻体法和Heygi单木竞争指数模型,对两个种群的分布格局 和竞争情况进行分析.结果表明,旱冬瓜在不同生长阶段均呈现随机分布,而伴生的潺槁木姜子种群则呈 现随机分布一聚集分布一均匀分布的变化趋势.种问竞争和物种自身生物学特性对两个种群的分布格局具 有显著影响.旱冬瓜种群的龄级结构为衰退型,潺槁木姜子种群则为成长型.

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The concentrations of alkylphenols (APs) were investigated in water, sediments and submersed macrophytes from the Moon Lake, Wuhan city, China. The water samples contained APs, ranging up to 26.4 mu g l(-1) for nonylphenol (NP) and 0.68 mu g l(-1) for octylphenol (OP). APs were found in the sediment samples with concentrations ranging from 4.08 to 14.8 for NP and from 0.22 to 1.25 mu g l(-1) dry weight for OP. The samples from the site near former sewage inlet showed the highest concentrations of APs in both water and sediments. The results of distribution pattern and dynamics of NP and OP in submersed macrophytes of the Moon Lake showed that the two pollutants were all found in Myriophyllum verticillatum, Elodea nuttallii, Ceratophyllum oryzetorum, and Potamageton crispus collected from the Moon Lake. For NP, M. verticillatum had the highest capacity of accumulation, followed by E. nuttallii, C. oryzetorum and P. crispus. However the distribution pattern of OP differed from that of NP, and the highest amount of accumulation was observed in E. nuttallii, followed by M. verticillatum, P. crispus, and C. oryzetorum. The temporal pattern of APs was also observed in submersed macrophytes from March to May, and the highest accumulation period was in May. (c) 2008 Elsevier Ltd. All rights reserved.

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Time resolved magneto-optic Kerr rotation measurements of optically induced spin quantum beats are performed on heavily doped bulk (Ga,Mn)As diluted magnetic semiconductors (DMS). An effective g-factor of about 0.2-0.3 over a wide range of temperature for both as-grown and annealed (Ga,Mn)As samples is obtained. A larger effective g-factor at lower temperature and an increase of the spin relaxation with increasing in-plane magnetic field are observed and attributed to the stronger p-d exchange interaction between holes and the localized magnetic ion spins, leading to a larger Zeeman splitting and heavy-hole-light-hole mixing. An abnormal dip structure of the g-factor in the vicinity of the Curie temperature suggests that the mean-field model is insufficient to describe the interactions and dynamics of spins in DMS because it neglects the short-range spin correlation effect. (c) 2008 American Institute of Physics.

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采用野外样线取样与室内萌发相结合的方法研究了黄土高原丘陵沟壑区退耕地种子库的组成、密度、分布特征、季节动态、种子库类型。结果表明,土壤种子库中共发现50种植物的种子,隶属15个科,39个属,主要物种组成与密度季节间差异不显著;在演替过程中土壤种子库的物种数量与密度随退耕年限的增加表现出:增加-减少-增加的趋势,同时阳坡种子库密度波动较阴坡剧烈;土壤种子库密度年内变化范围为1 067~14 717粒/m2,土壤种子库平均密度是夏季>秋季>春季;研究区域退耕地土壤种子库类型属于以猪毛蒿为优势种,并具有其他一年生、多年生草本植物与灌丛种子的没有显著的季节动态的持久种子库,是物种适应黄土丘陵沟壑区特有生态环境条件的繁殖更新策略;从土壤种子库的物种组成、密度、类型来看,黄土丘陵沟壑区退耕地具有一定的自然恢复潜力。

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土壤氨基糖因其异源性和稳定性可用以指示微生物对土壤碳(C)氮循环的相对贡献。但由于氨基糖是微生物在土壤中长期残留的平衡结果,其数量变化无法准确反映在微生物作用下无机态氮(N)向氨基糖转化的动态过程和机制,从而使氨基糖对土壤氮内循环的指示作用受到限制。如果能够利用新的技术手段研究土壤氨基糖的微生物转化过程,将使土壤氮素内循环研究产生突破。同位素技术是研究土壤C,N转化过程的有效手段。但是研究特定化合物如氨基糖的微生物转化过程还需要新的技术支持,本研究首先建立了稳定同位素培养-气质联机技术测定土壤氨基糖同位素富集比例新方法。对于15N培养样品,由于氨基糖分子中只有一个N原子,15N富集比例可通过m/z(F+1)与F相对丰度的比值计算;对于13C培养样品,由于葡萄糖c整体掺入形成氨基糖c骨架,所以利用m/z(F+n)与F相对丰度的比值计算13c在土壤氨基糖中的富集(n为质谱碎片中骨架C原子数)。同位素富集用原子百分超(APE)表示。EI和cI两种方式测得的APE有很好的同一性,且不受土壤基质的影响,表明方法的可靠性和广泛适用性。利用以上方法,进行了土壤样品的同位素培养与测定,以跟踪土壤氨基糖微生物合成动态,进行氨基糖的微生物转化与更新研究。主要结论如下:1.当以葡萄糖为碳源且每周施入底物时,NH4+和NO3-均可被微生物迅速同化并进行氨基糖的合成。但NO3-必须被还原成NH4+才能被微生物利用,因而NO3.存在短暂的滞后期,之后被微生物快速利用。氨基葡萄糖(GluN)和胞壁酸(MurN)不同的同位素富集特征表明,N源形态对细菌增殖无显著影响,但真菌更倾向于利用NH4+。在NO3-培养中氨基糖的增量及微生物对C的截获均小于NH4+。2.分别利用u一13c一glucose一NH4十和glLlcose一ISNH4+进行样品培养时,同位素富集趋势相同,但APE(13C)大于APE(15N),这种差别反映了了土壤微生物利用C,N的时间特征及土壤有机质含量对C,N循环的影响。3.以gtucose-15NH4+为底物时,施入N素频率的改变也会影响微生物的活性。尤其是细菌的快速生长受到N素不足的限制,转而代之以细菌和真菌的持续的低速生长。微生物活性的降低减少了对有机c的截获。DCD的加入有效抑制了NH4+向NO3一的转化,但对氨基糖的合成无显著影响。4.土壤氨基糖反映的主要是土壤中已经死亡了的微生物的一种长期过程而产生的残留,同土壤微生物量无明显的相关性。但经外加底物培养后,氨基糖同位素富集比例的变化则来源于微生物的转化,因而与微生物量碳有直接的相关性。5.从原理上说,在氨基糖的微生物合成过程中,葡萄糖没有发生C骨架的断裂,而是直接转化成为氨基葡萄糖的骨架。但在复杂的土壤基质中,氨基葡萄糖的合成必然受到葡萄糖其他生物化学过程的影响。使少量葡萄糖经酵解后再次参与己糖胺的合成。以全取代葡萄糖为底物时,葡萄糖碳骨架的断裂与重排不影响13c同位素的富集。但对于单取代葡萄糖培养来说,必须要考虑因葡萄糖碳骨架断裂而产生的同位素的重新分配,Mass(F+1)和Mass(F+2)的丰度变化的总和真正代表了氨基葡萄糖的同位素富集。6.添加有机物料和N素进行土壤样品培养时,对外加氮素的同化远低于相应的葡萄糖培养。碳源尤其是能源不足限制了N的转化。微生物分解高C加的有机物料需吸收外加N源以满足自身生长需要。N素的加入频率影落响微生物对外加N素的利用。当加入的N不能满足微生物分解有机物料的需要,就会降低微生物对有机物料的分解速度,使无机N向氨基糖态N转化速度降低。应用稳定同位素技术,发现施到土壤中的无机氮素可被微生物快速转化成某种形态有机氮,这种有机态氮处于不断转化循环之中,构成土壤有效氮的暂存"过渡库",其中氨基糖是重要成分之一。过渡库现象的发现为氮肥的有效利用提供了新的思路。根据土壤有效氮"过渡库"的模型,氮月巴高效利用调控实际上就是土壤氮素微生物转化过程的调控。提高土壤无机氮素向土壤有机氮的转化速率和转化强度可以有效减少无机氮在土壤中的积累,从而降低肥料和土壤氮素的硝化和反硝化损失,提高氮肥利用率。研究还发现,土壤有效氮"过渡库"容量与循环速率不仅取决于N源自身性质,碳源的可利用性显著影响施入土壤的N素微生物转化特征。只有适当提高可利用碳源即活性碳源的数量,才能提高氮素的微生物同化,土壤有效氮"过渡库"容量,从而减少氮素损失。