混流式转轮中流场的大涡模拟

建立了基于微可压缩流体理论的相对运动的大涡模拟方法,并对混流式转轮流场进行了三维非恒定粘性数值模拟,计算方法采用了有限体积法和预测-校正方法,对固体边壁的处理使用了“壁函数”法。得到了混流式转轮的三维速度场和压力分布,与k-ε模型计算结果进行比较表明,所建立的相对运动的大涡模拟方法对转轮性能预测更加精确、合理,对转轮改型设计具有十分重要的参考价值。     

测雹板标定试验研究

对聚苯乙烯测雹板性能的检定试验以及1988－1998年野外观测取样结果表明：（1）聚苯乙烯测雹板性能稳定，吸湿性差，能经受风吹、雨打、日晒，不变形、不变质，适合在野外雹暴天气中使用。（2）聚苯乙烯材料弹性小，测量误差小，模拟风、雨等天气条件时，平均误差为4.3%－12.2%。因此，可以较准确地测出野外实际冰雹大小及数密度。     

昭苏县防雹雷达站防雹业务技术规程

在总结昭苏县25年雷达探测冰雹云和指挥防雹作业技术的基础上，研究并编写了昭苏县防雹雷达站防雹业务技术规程，本文扼要介绍雷达观测、雹云识别、作业指挥，效果分析等部分主要技术规程。     

黑龙江省冰雹天气气候特征及防雹预警指标

以统计的近40年冰雹资料为基础，分析了黑龙江省冰雹天气分布规律及近年冰雹气候特征的变化。利用天气系统背景、卫星云图、不稳定因子以及雷达回波等指标，为人工防雹天气时机选择和作业方案设计提供了综合预警指标，为省级防雹预警系统提供了新的更接近实况的科学预警依据。     

大腔体人造金刚石合成工艺的研究

分析了我国现阶段金刚石的合成工艺－φ23mm腔体工艺的基础上，利用变功率合成技术和瓶颈效应后改变组装方式，使腔体内的物量比合理化，以达到腔体内合成温度和压力均匀，控制金刚石的生长速度，在较低的合成压力和合成功率下，在φ28.5mm腔体和φ31mm腔体上，合成优质高产金刚石。     

The world''s large lake basins as denudation-accumulation systems and implications for their lifetimes

The mechanical denudation rates of 81 large lake basins (lake area > 500 km²) were determined from long-term river loads and erosion maps. Using the drainage area/lake area ratios the mean sedimentation rates of the lakes were calculated for a porosity of 0.3. The mean sedimentation rates of different lake types vary between 0.1 mm/a (glacial lakes, lowland) and 5.4 mm/a (mostly sag basin lakes). The calculated lifetimes of the lakes are based on the lake volumes and mean sedimentation rates, assuming steady-state conditions and solely clastic material. On average, glacial lakes in highlands and fault-related lakes show the shortest lifetimes (c. 70 ka), glacial lakes in lowlands and rift lakes have the longest lifetimes (c. 1 Ma). Some lakes remain unfilled for very long time spans due to rapid subsidence of their basin floors. The calculated lifetimes are compared with those derived from sediment core studies. Most core studies indicate lower mechanical sedimentation rates than the calculated ones because a major part of the incoming sediment is trapped in deltas. However, a number of lakes (e.g., the Great Lakes of North America) show the opposite tendency which is largely caused by extensive shoreline erosion and resuspension. The lifetimes of large glacial lakes often exceed the duration of interglacials. Hence, their lifetimes are restricted by glaciation and not by sediment infill. Rift lakes persist for long time periods which exceed the calculated lifetimes in some cases. Time-dependent subsidence, basin extension, as well as the impact of climate change are briefly described.     

孵漂石地层大口径钻头与钻进工艺的选择

根据工程实例，通过钻头和钻进工艺的对比试验，得出了利用大直径滚刀钻头，在致密卵漂石地层施工中大口径桩孔，能大幅度提高钻进效率。     

Bestimmung der Phytoplanktonvolumina — Methodik und Ergebnisse am Beispiel Niederrhein

For data treatment of phytoplankton countings in the Lower Rhine the specific biovolume was calculated. The used computer-aided method is described, and the correlation between phytoplankton biomass, cell number and chlorophyll a is presented.     

Distorted Froude‐scaled flume analysis of large woody debris

This paper presents the results of a movable‐boundary, distorted, Froude‐scaled hydraulic model based on Abiaca Creek, a sand‐bedded channel in northern Mississippi. The model was used to examine the geomorphic and hydraulic impact of simplified large woody debris (LWD) elements. The theory of physical scale models is discussed and the method used to construct the LWD test channel is developed. The channel model had bed and banks moulded from 0·8 mm sand, and flow conditions were just below the threshold of motion so that any sediment transport and channel adjustment were the result of the debris element. Dimensions and positions of LWD elements were determined using a debris jam classification model. Elements were attached to a dynamometer to measure element drag forces, and channel adjustment was determined through detailed topographic surveys. The fluid drag force on the elements decreased asymptotically over time as the channel boundary eroded around the elements due to locally increased boundary shear stress. Total time for geomorphic adjustment computed for the prototype channel at the Q₂ discharge (discharge occurring once every two years on average) was as short as 45 hours. The size, depth and position of scour holes, bank erosion and bars created by flow acceleration past the elements were found to be related to element length and position within the channel cross‐section. Morphologies created by each debris element in the model channel were comparable with similar jams observed in the prototype channel. Published in 2001 John Wiley & Sons, Ltd.     

西昌—滇中地区大、中型内生矿床分布规律及预测

用王亚光研究大型矿床空间分布规律理论来研究西昌—滇中地区大、中型内生矿床的分布规律及预测,用“矿结”一词来表明经纬线方向深大断裂交汇处是大矿的分布空间。1990年所预测的一些成矿区为1991年地质找矿工作所证实,如大红山式铁铜矿的新发现和会东发嵩铝锌矿的新进展。