324 resultados para Direct numerical simulation


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Tension leg platform (TLP) is an important kind of working station for deep water exploration and development in ocean, whose dynamic responses deserve a serious thought. It is shown that for severe sea state, the effects of nonlinearities induced by large displacements of TLP may be noteworthy, and then employment of small displacements model should be restrained. In such situation, large amplitude motion model may be an appropriate alternative. The numerical experiments are performed to study the differences of dynamic responses between the two models. It is shown that for most cases, differences between results of the two models are significant. The variances of the differences vs. the wave period are the most remarkable, and that of the differences vs. wave heading angle are also apparent.

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The microgravity research, as a branch of the advanced sciences and a spe- cialized field of high technology, has been made in China since the late 1980's. The research group investigating microgravity fluid physics consisted of our col- leagues and the authors in the Institute of Mechanics of the Chinese Academy of Sciences (CAS), and we pay special attention to the floating zone convection as our first research priority. Now, the research group has expanded and is a part of the National Microgravity Laboratory of the CAS, and the research fields have been extended to include more subjects related to microgravity science. Howev- er, the floating zone convection is still an important topic that greatly holds our research interests.

目录

1. models of floating zone convection
1.1 floating-zone crystal growth
1.2 physical model
1.3 hydrodynamic model
1.4 mathematical model
references
2. basic features of floating zone convection
2.1 equations and boundary conditions
2.2 simple solutions of fz convection
2.3 solution for two-layers flow
2.4 numerical simulation
2.5 onset of oscillation
references
3. experimental method of fz convection
3.1 ground-based simulation experiments for pr≥1
3.2 temperature and velocity oscillations
3.3 optical diagnostics of free surface oscillation
3.4 critical parameters
3.5 microgravity experiments
3.6 ground-based simulation experiment for pr《1
.references
4. mechanism on the onset of oscillatory convection
4.1 order of magnitude analysis
4.2 mechanism of hydrothermal instability
4.3 linear stability analysis
4.4 energy instability of thermocapillary convection
4.5 unsteady numerical simulation of 2d and 3d
4.6 two bifurcation transitions in the case of small pr number fluid
4.7 two bifurcation transitions in the case of large pr number fluid
4.8 transition to turbulence
references
5. liquid bridge volume as a critical geometrical parameter
5.1 critical geometrical parameters
5.2 ground-based and mierogravity experiments
5.3 instability analyses of a large prandtl number (pr≥1)fluid
5.4 instability analyses of a small prandtl number (pr《1)fluid
5.5 numerical simulation on two bifurcation process
references
6. theoretical model of crystal growth by the floating zone method
6.1 concentration distribution in a pure diffusion process
6.2 solutal capillary convection and diffusion
6.3 coupling with phase change convection
6.4 engineering model of floating zone technique
references
7. influence of applied magnetic field on the fz convection
7.1 striation due to the time-dependent convection
7.2 applied steady magnetic field and rotational magnetic field
7.3 magnetic field design for floating half zone
7.4 influence of magnetic field on segregation
references
8. influence of residual acceleration and g-jitter
8.1 residual acceleration in microgravity experiments
8.2 order of magnitude analyses (oma)
8.3 rayleigh instability due to residual acceleration
8.4 ground-based experiment affected by a vibration field
8.5 numerical simulation of a low frequency g-jitter
8.6 numerical simulation of a high frequency g-jitter
references

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目录

第一部分总论

环境流体力学――它的意义,内容与方法 李家春

用于大气环流模式的陆面物理过程参数化研究进展 戴永久,曾庆存,欧阳兵

植被-陆面过程耦合模式的动力框架 欧阳兵

第二部分均匀下垫面的陆面过程

干旱地区陆面过程的研究 李家春,姚德良,沈卫明

阿克苏地区陆面蒸发的数值研究 沈卫明,姚德良,李家春

塔里木盆地陆气水热交换数值模拟 姚德良,沈卫明,李家春

植物固沙区土壤水热运移耦合模型研究 姚德良,李家春,沈卫明

Numerical simulation of watercycling and heat balance in agricultural ecosystems D.L.Yao,W.M.Shen and J.C.Li

在植物耗水条件下土壤水分动态的数值模拟 姚德良,邱克俭,冀伟,孙菽芬

干旱地区陆面过程耦合模式及其应用 李家春,姚德良,沈卫明

Modelling of terrestrial ecosystem B.Ouyang

森林生态系统生物循环过程的耦合模型(BCM)及其数值模拟 欧阳兵

森林生态系统生物能流的瞬态分析 欧阳兵

第三部分非均匀下垫面的陆面过程

Turbulence in the atmosphere and ocean J.C.Li

非均匀下垫面上大气边界层的研究进展 徐大鹏

非均匀植被的群体蒸发 徐大鹏

第四部分 区域尺度以上的陆面过程与水文模型

Sensitivity of IAP two-level AGCM to surface albedo variations Z.H.Lin,Q.C.Zeng and B.Ouyang

估算区域蒸发的能量法研究 聂松媛,徐丰

用卫星数据估算区域水资源蒸发研究 聂松媛

负轮分析法在水环境规划与管理中的应用 聂松媛

第五部分 陆面过程观测的指标体系

Mathematical modelling and index system in ecology J.C.Li

陆面过程的观测指标体系研究 欧阳兵,李家春,姚德良

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在对喷流噪声研究进展广泛调研的基础上,本论文采用柱坐标下轴对称的线化欧拉方程(LEE)、空间四阶时间二阶精度的MacCormack差分格式,对水下气体喷流的混合噪声产生与辐射特性进行数值模拟研究。采用基于经验公式的积分计算方法来确定求解线化欧拉方程所需的平均流场,对边界条件给予特殊处理以避免声波通过时产生反射。本文计算声明,线化欧拉方程及其相应的高阶数值方法提供了一个可以预报水下气体喷流混合噪声传播的省时高效的途径。给出的结果指出:由于水介质的密度很大,水下气体喷流远场收集到的噪声强度比同样情况下空中气体喷流要小,这说明水下发射导弹更具隐蔽性。同时,由于水介质中的声速很大,水下的高速喷流噪声场呈现更加均匀的性态,而不是象空中混合噪声在下游沿一定的方向辐射。鉴于本文只考虑常温情况,气体喷流速度是影响喷流噪声产生与辐射的重要参数:马赫数增大,远场的噪声强度随之增大。另外,水下喷流噪声的特性还与扰动频率有关。

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非传播孤立波是近年来由中国学者发现的一种独特的孤立水波。本文通过数值求解非传播孤立波目前公认的控制方程-Miles导出的一个带共轭项的非线性立方Schrodinger方程,对非传播孤立波进行数值模拟。本文针对非传播孤立波的各种性质,作了大量的数值计算工作,并与实验观察的现象及人们对非传播孤立波的理论研究结果进行了比较和分析。为了得到稳定的非传播孤立波,本文讨论了Miles方程中的线性阻尼系数a的值,计算表明,线性阻尼a对能否形成稳定的非传播孤立波影响很大,在某些情况下,Laedke等人提出的Miles方程的非传播孤立波解的稳定性条件与我们对Miles方程的数值模拟的结果相当一致,a可在满足稳定性条件的区间内取值,但也发现在某些情况下Laedke等人的稳定性条件与我们的数值模拟不完全符合,证明Laedke等人关于非传播孤立波的稳定性条件只是一个必要条件,而不是充分条件。本文研究了两个非传播孤立波的相互作用,数值模拟表明,两个波的作用模式依赖于系统的参数,只有适当大小的外驱动频率和振幅及线性阻尼a可算出两个非传播孤立波周而复始的相互作用现象来,参数不合适时,两个波可能最终合并为一个非传播孤立波而不再分离,也可能彼此不发生作用,保持各自的独立。对不同的初始扰动及其演化的计算表明,要形成单个稳定的非传播孤立波,则初始扰动必须适当,否则扰动可能消失或发展成多个孤立波。关于形成非传播孤立波所需的外驱动条件,计算结果表明,只有适当大小的外驱动频率和振幅可形成稳定的非传播孤立波,数值结果可以描述驱动频率的上限和驱动振幅的上下限,但无法描述驱动频率的下限。我们的数值模拟工作说明Miles方程确实较好的描述了非传播孤立波的物理模型,该方程可以解释许多关于非传播孤立波的物理特性。但Miles方程无法对非传播孤立波的某些实验现象作出解释,因而有待于进一步研究改进。

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本文针对平面链网模型与空间链网模型,发展了模拟非均质材料的数值软件,旨在分析材料的损伤破坏特征,寻找材料细观结构同宏观力学行为之间的相互联系,探讨材料强韧化机理以及评估材料的力学性能。采用可视化技术设计的具有交互式功能的图象用户界面,能根据具体材料对象构造特定材料模型来分析其力学行为与服役能力。初步结果表明,无论是材料弹性阶段的性质还是损伤演化阶段材料中裂纹的萌生、扩展、汇集和材料的最终失效等现象都与已有的理论结果及试验结果符合得很好。另外,本文还对材料的强韧化机理作了探索。

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在本文的工作中,研制出了大气压层流等离子体发生器,并从试验和数值模拟两个方面对层流等离子体射流的特征和发生机理进行了分析和研究。试验观察表明,与湍流等离子体射流相比,层流等离子体射流有明显的特点,射流长而细,与周围环境气体掺混很少,能量的衰减很慢,而且几乎没有噪音。在层流等离子体发生器的研制过程中,研究了层流等离子体射流的产生机理,结果表明,工作气体流量、电源的输出特性、进气方式、电压的大小、发生器的结构和加工等对层流等离子体射流的产生有重要影响。本文还对层流和湍流等离子体射流进行了数值模拟,结果表明,工作气体的流量对层流等离子体的射流的长度有较大的影响;发生器出口的射流初始湍流度对射流的流动状态和长度也有很大的影响。数值模拟的结果和试验观察到的现象是一致的。

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A theoretical model has been developed to investigate the microfluidic transport of the signaling chemicals in the cell coculture chips. Using an epidermal growth factor (EGF)-like growth factor as the sample chemical, the effects of velocities and channel geometry were studied for the continuous-flow microchannel bioreactors. It is found that different perfusion velocities must be applied in the parallel channels to facilitate the communication, i.e., transport of the signaling component, between the coculture channels. Such communication occurs in a unidirectional way because the signaling chemicals can only flow from the high velocity area to the low velocity area. Moreover, the effect of the transport of the signaling component between the coculture channels on the growth of the monolayer cells and the multicellular tumor spheroid (MTS) in the continuous-flow coculture environment were simulated using 3D models. The numerical results demonstrated that the concentration gradients will induce the heterogeneous growth of the cells and the MTSs, which should be taken into account in designing the continuous-flow perfusion bioreactor for the cell coculture research.