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.     

Geothermal field and its relation with coalbed methane distribution of the Qinshui Basin

The average geothermal gradient in the Qin-shui Basin, Shanxi Province, North China, estimated from temperature logging data of 20 boreholes is 28.2±1.03℃/km. The thermal conductivities of 39 rock samples are measured and 20 heat flow values are obtained. The estimated heat flow ranges from 44.75 mW7m2 to 101.81 mW/m2, with a mean of 62.69±15.20 mW/m2. The thermal history reconstruction from the inversion of vitrinite data, using Ther-model for Windows 2004, reveals that the average paleo-heat flow at the time of maximum burial in late Jurassic to early Cretaceous is 158.41 mW/m2 for the north part, 119.57 mW/m2 for the central part and 169.43 mW/m2for the south part of the basin respectively. The reconstruction of the buried history of the strata indicates that the age for the end of sedimentation and the beginning of erosion for the basin is 108-156 Ma, and that the eroded thickness of the strata is 2603 m in the north, 2291 m in the central, and 2528.9 m in the south of the basin respectively. The "higher in the north and the south, lower in the central" distribution pattern of the paleo-heat flow coincides with the distribution of the coal-bed methane spatially and temporally, which shows that the coal-bed methane is controlled by the paleo-geotem-perature field in the basin.     

LM_2钢恒温超塑性及其显微组织的变化

LM_2钢经1050℃快速加热淬火后,基体晶粒尺寸可细化至4.2μm 以下,碳化物平均截线长小于0.32μm。处理后的钢在830～850℃,■=(1.0～2.3)×10~(-2)min~(-1)变形时均可获得较好的超塑性,其最大延伸率为183%,而流变应力仅55.2MPa。在超塑变形中,碳化物长大倾向比单纯温度作用下要大,但不明显。由于该铜原始组织中存在一定数量的一次碳化物,直接影响其超塑性的较好发挥。     

基于MSFG的机载BITE故障定位算法研究

故障定位是机载BITE的重要功能,定位结果的准确性对维修测试有着重要影响。基于多信号流图模型,在构造故障-测试关联矩阵和故障-故障关联矩阵的基础上,引入故障信息矢量和故障定位矩阵,并给出适用于机载BITE故障定位的矢量描述和矩阵定义,进而提出一种简单、有效的故障定位算法。实例验证表明,该算法能够对系统中的故障源进行准确定位。     

甘肃燕儿沟泥石流形成条件及特征参数分析

"5.12"大地震后,甘肃陇南山区地质环境急剧恶化,崩塌、落石、滑坡和地裂缝频发,导致燕儿沟流域内山体更加破碎,为泥石流发育提供了充足的物源条件。在强降雨条件下,极易形成泥石流,严重威胁灾区的生产生活。根据现场调研,对燕儿沟泥石流形成条件进行了分析;并对泥石流的运动学和动力学参数进行了分析计算。结合燕儿沟泥石流形成发育特点,提出了以稳定沟床和排导为主;主、支沟治理相结合;工程治理及生物水保措施相结合的综合治理建议,也为同类工程提供了参考依据。