PIV测速中实时可调同步脉冲光照系统的设计与应用设

根据PIV测速系统的需要，设计了与CCD摄像机和半导体激光器同步的实时可调脉冲发生器，结合一体化微光摄像技术，成功地实现了对流场的单帧多次曝光，有效地解决了流动图像获取技术中的光源问题，通过对实际流场的摄取，说明了本文方法的实际意义。     

采金船圆形跳汰机脉冲式液压系统分析

分析了采金船圆形跳汰机脉冲式液压系统的工作原理．介绍了交流液压技术及跳汰工艺．并对脉冲式液压系统中蓄能器响应性能进行了研究．     

超声多普勒方向性血流信息的提取

本文以窄带随机信号理论为基础，对方向性血流信息提取的原理作了有别于文献报导的分析，并指出了时城后处理方法在提取方向信息中存在的问题。此外，本文还就在前置放大器中使用丙类放大器对谱分析结果所造成的失真作了分析。在上述理论分析的基础上介绍了新试制的方向性多普勒血流计原理框图。     

轴对称管道中的应力孤波

本文用奇异摄动方法研究了轴对称管道中的非线性应力波.去掉了在推导基本方程时ε_r为小量的近似假定.在长波极限下,管道中的非线性应力波满足Korteweg and de Vries方程。     

槽边抽风的流场理论分析

工业用槽边抽风的流场分布,目前尚缺乏完整的理论分析和理论与实验相结合的分析计算式。本文利用较简单的数学分析法,可以解决这方面的问题,所得的计算式便于理解和分析计算。     

氧化铝物料在立筒预热器内的气固相逆流运动规律

研究了氧化铝物料在立筒预热器内的运动特征和规律。探讨了影响氧化铝物料在立筒内沉降率的因素、停留时间,提供了立筒预热器的结构和操作参数。     

镀液流速对复合电沉积的影响

通过对Ag-MoS_2复合镀层在氰化物镀液中电沉积的研究,定量测定了镀液流速、微粒在镀液巾的悬浮量以及阴极电流密度对MoS_2微粒与Ag共沉积的影响。发现复合镀层中MoS_2含量是镀液流速、微粒悬浮量及电流密度的函数,并由此提出了能比较满意地反映在该复合共沉积体系中微粒共沉积量与镀液流速、微粒悬浮量和电流密度间关系的数学模型。     

大血管中的血液流动 (一)刚性管情况

本文讨论了血液在大血管中的非定常振荡流动问题,导出了一组血液流动的速度分布、压力分布公式。分析表明,本文公式既适用于入口区域的流动,也适用于远离入口区域的流动;既可描述定常流动,也可描述非定常的振荡流动。数值算例还表明,本文结果不但和已有的理论结果相一致,而且较之简单,并和实验结果相当吻合。     

Particle methods for multiscale simulation of complex flows

The multi-scale structures of complex flows have been great challenges to both theoretical and engineering researches, and multi-scale modeling is the natural way in response. Particle methods (PMs) are ideal constitutors and powerful probes of multi-scale models, owing to their physical insight and computational simplicity. In this paper, the role of different PMs for multi-scale modeling of complex flows is critically reviewed and possible development of PMs in this background is prospected, with the emphasis on pseudo-particle modeling (PPM). The performances of some different PMs are compared in simulations and new development in the fundamentals and applications of PPM is also reported, demonstrating PPM as a unique PM for multi-scale modeling.     

Breakdown of lawsonite subsequent to peak UHP metamorphism in the Dabie terrane and its implication for fluid activity

Abundant occurrences of quartz vein within eclogites in the Dabie-Sulu orogen provide us an opportunity to study metamorphic fluid flow during subduction and exhumation of continental crust. It is, however, usually short of petrological constraints on pressure and temperature of vein formation. This study focuses on kyanite-quartz veins within Iow-T/high-P eclogite in the Dabie terrane that contain unique polycrystalline aggregates, interpreted as pseudomorphs after porphyroblasts of lawsonite. Coesite pseudomorphs were found for the first time in garnet from eclogite, resulting in a revised estimate of peak P-T conditions at 670℃ and 3.3 GPa for the eclogite. This indicates a stability field at graphite/diamond transition, thus upgrading the HP unit to a UHP unit. Neither foliation texture, undulose extinction of quartz nor coesite were observed in quartz veins,although the peak P-T conditions were estimated the same as that in host eclogite in light of thermodynamic calculation based on mineral assemblage in kyanite-quartz veins.Therefore, the formation of the kyanite-quartz veins as wellas the breakdown of lawsonlte into the kyanite-quartz-zoisite assemblage took place during exhumation subsequent to the peak UHP conditions. In this regard, the continental subduction not only brought the water of water-bearing mineral such as lawsonite into the deep mantle, but also released the water from the mineral during exhumation.