VAD技术反演平均风向风速的研究

采用实测的单普勒雷达速度资料，通过对比分析了，重点讨论了非均匀分布VAD计算方法和均匀分布VAD计算方法的异同，以了解非均匀分布VAD计算方法业务应用的可能性。结果表明，在多普勒速度场缺测值较少情况下，两者计算结果接近；在多普勒速度场缺测值较多时，两者计算的平均风向和风速有较大的差别，均匀分布VAD计算的风速偏小，而非均匀分布VAD计算结果比较合理。     

甘肃西部蝶类区系研究

1994－1998年7－8月间广泛收集到甘肃西部地区蝶类标本1200多号：经鉴定为127种及亚种，隶属于8科，73属：其中有44种及亚种为甘肃省新记录；经区系分析属于古北界种74种，占总数的58．8％，广布种为53种，占总数的41．2％，古北界占优势。     

带电沙粒的跃移云数值模型

给出吹过无限大平坦沙面的稳定风场中风、跃移沙粒及静电力相互耦合的方程 ,并用简化的沙粒——床面碰撞模型求解了方程 .计算结果表明静电力对沙粒跃移轨道及贴地风速有强烈影响 ,当跃移沙粒的带电量为 - 6 0 μC/ kg时 ,计算所得的跃移层中风速沿高程分布与实验结果相吻合     

加快西部旅游区城市化进程,促进旅游业的发展

旅游开发是当前西部大开发的重要内容。城市因是旅游开发的主要客源地、目的地和依托基地而成为区域旅游系统的核心。通过充分调研分析，认为加快西部旅游区城市化进程，对促进旅游业的发展和西部大开发均具有重要意义，而目前西部地区城市化的滞后严重制约了旅游开发。提出了必须从调整城市发展方针、适度加快大城市建设、有效保护自然生态环境、调整城市发展人口政策、加强城市形象建设以及加强东西部城市合作等方面着眼，加快西部地区、尤其是旅游区城市化进程，以此为先导，推进西部旅游开发和区域可持续发展。     

2.4m × 2.4m跨声速风洞多变量控制

针对2.4m风洞受风洞闭合回路的影响使得稳定段总压与试验段M数间存在着干扰耦合,构成了一个非线性,时滞,强干扰,强耦合的多变量控制系统.针对这一问题,设计了智能自适应解耦控制器,很好地解决了这一难题,并取得了良好的结果.     

Potash-rich volcanic rocks and lamprophyres in western Shandong Province: 40Ar39Ar dating and source tracing

Highly precise 40Ar39Ar dating results demonstrate that the ages of potash-rich volcanic rocks in western Shandong Province are 114.7-124.3 Ma, and that of the lamprophyres is 119.6 Ma. The potash-rich volcanic rocks have relatively high (87Sr/86Sr)i ratios ( 0.708715-0.711418)and distinctly negative εNd values ( -11.47 - -17.54), and are enriched in radiogenic lead (206Pb/204pb=17.341-17.622,207pb/204Pb=15.525-15.538, 208Pb/204pb = 37.563-37.684).Similarly, the lamprophyres also have quite low εNd values ( -11.57 - -19.64). Based on the fact that the Sr, Nd and Pb isotopic compositions of potash-rich volcanic rocks are very consistent with that of the clinopyroxene separates, and by integrating comprehensive analyses of their tectonic settings,and extensive comparisons of the Sr, Nd isotopic compositions with that of the related simultaneous rocks, it is concluded that the potash-rich volcanic rocks and lamprophyres in western Shandong Province were most possibly derived from the partial melting of enriched mantle which was caused by source contamination and metasomatism of subducted continental crustal materials.``     

Further support for a Cretaceous age for the feathered-dinosaur beds of Liaoning,China:New 40Ar/39Ar dating of the Yixian and Tuchengzi Formations

We report new 40Ar/39Ar dating results obtained from total fusion and incremental-heating analyses of sanidine and biotite from three tuffs found interbedded within the fossil-bearing deposits of Liaoning, northeast China. The first is a new sample of the Bed 6 Sihetun tuff from the Yixian Formation, previously dated by our team as middle Early Cretaceous, and recently considered by Lo et al., partially reset due to metamorphism from a nearby basaltic sill. The second is the Yixian Bed 9 tuff from Hengdaozi considered by Lo et al. to be unaffected by metamorphism and whose age, based on total fusion 40Ar/39Ar dating of biotite, argues for a Jurassic age for the Yixian Formation.The third tuff is a previously undated tuff from the upper part of the underlying Tuchengzi Formation. Single crystal total fusion 40Ar/39Ar analyses of the Sihetun sanidine showed homogeneous radiogenic Ar, Ca/K ratios, excellent reproducibility and gave a mean age of 125.0 ± 0.18 (1SD) ±0.04 (SE) Ma. Single sanidine crystal total fusion 40Ar/39Aranalyses of the Hengdaozi tuff gave a mean age of 125.0 +0.19 (1SD) ± 0.04 (SE) Ma, which is indistinguishable from the Sihetun tuff. The Tuchengzi Formation tuff gave a mean age of 139.4 ± 0.19 (1SD) ± 0.05 (SE) Ma. Detailed laser incremental-heating analyses of biotite from Sihetun, Hengdaozi, and Tuchengzi tuffs show disturbed Ar release patterns and evidence of trapped argon components. We conclude from these analyses that the total fusion dates on biotite by Lo et al. are erroneously old and isotopic dating of both biotite and sanidine from tuffs of the Yixian Formation point to a middle Early Cretaceous age. The upper part of the Tuchengzi Formation can be referred to the Early Cretaceous.``     

大跨度屋面风压分布拟合公式及风荷载取值

风流经大跨度屋面结构时会产生复杂的气流分离及再附着，因而大跨度屋盖表面的风压分布较为复杂，从迎风前缘区域到尾部的风压变化 梯度很大，这使得仅仅采用一个体型系数很难反映屋面的风荷载。为了既简洁而又准确地表达屋面风荷载，提出了风压分布的二维几何平面拟合方法及拟合公式，并进一步提出了二维几何平面及风向角的三维拟合方法及拟合公式。最后根据屋面风压分布规律，将屋面分成9个区域并给出各区域的风压系数。     

高速滑坡飞行气动特性的风洞试验研究

国内外已发生的许多大型高速滑坡在近程活动阶段均呈现飞行运动，高速滑体如同机翼一样，将产生机翼效应。这种空气动力学效应不仅使滑坡飞行得更远，而且使位能更多地转变成滑坡飞行的功能，使滑体获得更大的速度，将高速滑体制成相似的机翼模型，进行风洞试验，即可测定滑坡凌空飞行的空气动力学参数，从而计算大型高速滑坡凌空飞行的空气动力升力、飞行速度和飞行距离等。风洞试验结果表明：高速滑坡体的几何形与结构、飞行姿态对高速滑坡飞行气动特性有显著影响，而飞行速度对气动特性的影响甚小。     

鄂西-渝东区石炭系油气成藏影响因素及富集规律

针对鄂西－渝东区近年钻探效果不理想的问题，分析了该区油气成藏的影响因素和富集规律。结果表明，该区大型古隆起的继承性发育、区域性油气运移和圈闭形成时间早晚的匹配、石炭系储层的发育程度和上覆地层异常高压的存在、有效供气面积的大小，以及断裂的封堵性和渗入水的强度等，是影响油气聚集和保存的主要因素。认为该区石炭系的油气勘探，应以开江－梁平古隆起南缘和石柱古隆起为重点。