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141.
谱元法(SEM)是基于有限元(FEM)的一种算法,在地震正演模拟中应用广泛,但是大部分研究都是基于四边形网格下的谱元法.本文给出了2阶谱元法在三角网格中(TSEM)的基本原理,包括Lagrange形函数的构建,数值积分公式的选取.在此基础上,分析了2阶TSEM方法的数值频散特性以及稳定性条件,并引入三角网格下3阶有限元方法进行分析对比,数值算例的结果证明2阶TSEM相比于3阶FEM具有更高的计算精度,以及更宽松的稳定条件.最后,本文将TSEM方法应用于中国西部地区的两个含溶洞介质的地质模型中,数值模拟结果表明TSEM方法能够有效地模拟复杂结构的介质,有助于对地震波场传播特性的认识. 相似文献
142.
Gervásio Annes Degrazia Umberto Rizza Franciano Scremin Puhales Antônio Gledson Goulart Jonas Carvalho Guilherme Sausen Welter Edson Pereira Marques Filho 《Boundary-Layer Meteorology》2009,131(2):277-292
A variable vertical mesh spacing for large-eddy simulation (LES) models in a convective boundary layer (CBL) is proposed.
The argument is based on the fact that in the vertical direction the turbulence near the surface in a CBL is inhomogeneous
and therefore the subfilter-scale effects depend on the relative location between the spectral peak of the vertical velocity
and the filter cut-off wavelength. From the physical point of view, this lack of homogeneity makes the vertical mesh spacing
the principal length scale and, as a consequence, the LES filter cut-off wavenumber is expressed in terms of this characteristic
length scale. Assuming that the inertial subrange initial frequency is equal to the LES filter cut-off frequency and employing
fitting expressions that describe the observed convective turbulent energy one-dimensional spectra, it is feasible to derive
a relation to calculate the variable vertical mesh spacing. The incorporation of this variable vertical grid within a LES
model shows that both the mean quantities (and their gradients) and the turbulent statistics quantities are well described
near to the ground level, where the LES predictions are known to be a challenging task. 相似文献
143.
各类抛弃式探头下沉运动的数值计算研究都需要对探头表面和整个计算域进行网格划分的前处理过程,选择不同的网格划分方法和划分精度,会影响数值计算速度和计算精度,最终生成的网格质量决定了计算结果的收敛性和准确性。针对抛弃式探头的复杂结构,对比了两种网格划分方法、三种网格划分精度,完成探头计算区域的网格划分,采用k-ε湍流模型,进行抛弃式探头下沉运动的数值计算,并将计算结果与水箱和水库实验结果进行对比,验证了混合网格划分方法和普通精度网格对抛弃式探头下沉运动数值计算的适用性,研究结果对类似较为复杂结构的水下运动体的数值计算前处理过程具有一定的参考和借鉴意义。 相似文献
144.
Steel bar in concrete structures under harsh environmental conditions, such as chlorine corrosion, seriously affects its service life. Bidirectional electromigration rehabilitation (BIEM) is a new method of repair technology for reinforced concrete structures in such chloride corrosion environments. By applying the BIEM, chloride ions can be removed from the concrete and the migrating corrosion inhibit can be moved to the steel surface. In conventional engineering, the concrete structure is often configured with a multi-layer steel mesh. However, the effect of the BIEM in such structures has not yet been investigated. In this paper, the relevant simulation test is carried out to study the migration law of chloride ions and the migrating corrosion inhibitor in a concrete specimen with complex steel mesh under different energizing modes. The results show that the efficiency of the BIEM increases 50% in both the monolayer steel mesh and the double-layer steel mesh. By using the single-sided BIEM, 87% of the chloride ions are removed from the steel surface. The different step modes can affect the chloride ion removal. The chloride ions within the range of the reinforcement protective cover are easier to be removed than those in the concrete between the two layers of steel mesh. However, the amount of migrating corrosion inhibitor is larger in the latter circumstances. 相似文献
145.
为研究浅埋隧道掌子面稳定性及获取精细化的破坏模式,提出了一种上限有限元非结构化网格自适应加密策略。以单元耗散能权重指标作为网格自适应加密评判准则,该策略同时兼顾了单元尺度与塑性应变。应用高阶的6节点三角形单元并建立上限有限元线性规划模型,以多次反复计算和网格加密的方式实现了二维自适应上限有限元分析并编制了计算程序。利用条形基础地基极限承载力课题,从上限解精度和网格加密形态方面验证了该程序的有效性。针对浅埋隧道掌子面稳定性问题,展开多参数条件下的自适应上限有限元计算,分析了网格加密过程中单元总数与上限解精度的关系,列出不同隧道埋深和内摩擦角对应的隧道掌子面稳定性临界值的上限解,揭示出掌子面稳定性变化规律及精细化的破坏模式。 相似文献
146.
A. E. Gilmour 《新西兰海洋与淡水研究杂志》2013,47(1):75-95
Hydrological data, including current observations, from a line of five stations across seasonal ice in McMurdo Sound, Antarctica, are presented. The observations, which were made during the 1972–73 summer, gave evidence for a net flux of approximately 0.4 × 106m3.s‐1 flowing towards the south to pass under the Ross Ice Shelf. There was a small northward flux (0.04 × 106m3.s‐1) on the western side of the sound, but over most of the width the flow was to the south. Diurnal tidal currents, which were analysed in terms of K1, P1, and O1 components, were superposed on the drift currents. Temperature and salinity measurements revealed signs of surface water dilution and warming down to 200 m in the region of southerly drift. Temperatures associated with the northerly drift on the western side of the section were close to freezing at all depths. This water can be identified as coming from under the Ross Ice Shelf. 相似文献
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数据组织模型是对科学数据进行有效管理、共享与应用的基础。日地空间物理学科通常采用基于语义标注的传统数据组织模型,但是该模型忽略了数据间的时空关系,难以支持大规模数据处理与关联分析,应建立一种支持时空计算的数据组织模型,从而有效支持当前日地空间物理领域对数据快速发现、精细结构识别、耦合关系研究与时空演化分析等方面的应用需求。鉴于此,本文提出了HTM-ST离散化时空数据组织模型,该模型在层次三角网格的基础上,在时间维度通过等长剖分进行扩展,从而形成离散化的时空剖分,采用时-空耦合编码将高维的剖分单元组织到一维空间中,并基于上述剖分结构与编码算法在HBase环境下设计了模型的存储方案。本文利用多颗极轨卫星的能量粒子探测数据实现了该数据组织模型的原型示范系统,并设计了基于该模型的时空查询算法和地方时全球数据插值算法,用于对该模型进行实验验证。实验分析表明,HTM-ST模型具有高效性和鲁棒性,可以作为面向时空关系的日地空间物理数据组织与存储基础。 相似文献