华南一次飑线过程线状对流模态变异机理研究

利用高时空分辨率的地面观测资料、探空资料、NCEP再分析资料和多普勒天气雷达资料,并结合中尺度数值模式WRF分析2013年5月15日发生在广西广东地区的一次强飑线过程,着重分析了中尺度对流系统(Mesoscale Convective System,MCS)由平行型(PS)模态到拖尾型(TS)模态的转变过程及机理。结果表明,此次飑线过程发生于高层弱辐散区,500 hPa有明显短波槽东移发展,850 hPa有切变线和低空暖湿急流,地面有冷锋和低压倒槽。西侧初始对流发展为PS型MCS模态,成熟期无雷暴高压。东侧减弱的初始对流再次加强发展后与西侧PS型MCS合并发展成为TS型MCS模态。数值模拟结果显示,PS型模态具有平行于对流线的气压梯度力和加速度分量,该分量产生了平行于对流线的风分量。TS型模态中,平行于对流线的气压梯度力和加速度很小,而垂直于对流线的气压梯度力和加速度很大,正是由于平行于对流线的加速度分量的消失和垂直于对流线的加速度分量的增强促使对流线内部相对系统流场由平行向转变为垂直向,导致MCS模态由PS型转为TS型。     

地震活动中地壳深部流体的作用研究进展

综述了地震深部流体研究的进展并提出了在地震领域应该深入研究的方面。已有大量资料表明岩石圈是一含流体的系统，也是地震发育的主要场所。深部流体赋存相态，运移方式及其与岩石的反应，对震源介质和构造活动有重要影响。     

中华绒螯蟹精子形成过程酸性磷酸酶的分布特征

将金属盐法与光镜、电镜技术相结合，研究中华绒螯蟹精子形成过程中酸性磷酸酶分布的变化．研究表明，在精子形成的早期，酸性磷酸酶由细胞质中的内质网小泡上产生，随后出现在细胞核内、顶体囊膜上及顶体管内，并且反应产物逐渐由分布均匀的细密颗粒聚集成分布均匀的较大的颗粒；当精子成熟后酸性磷酸酶均匀分布在顶体管中，反应产物颗粒比较大，穿孔器部分发现有少量酸性磷酸酶分布。     

海洋平台结构动力响应优化设计与灵敏度分析

研究了海洋平台结构动力响应优化设计以结构动力响应的灵敏度计算方法。给出了结构稳态频率响应和瞬态时程响应的灵敏度分析算法，并通过数值试验讨论了瞬态响应灵敏度分析算法的精度和差分法中变量摄动量的影响。在JIFEX软件中实现了结构动力响应灵敏度计算，建立海洋平台结构优化模型和求解方法。数值算例表明了本文方法和程序的有效性。     

TAGGING EXPERIMENTS OF THE PENAEID SHRIMP IN THE BOHAI SEA AND HUANGHAI SEA IN AUTUMN SEASON

There exists obvious difference in recapture rate of tagged shrimp in various sea areas and years in autumn season, but the majority of them (98%) are recaptured in the releasing year. Although the main portion of each shrimp group in the Bohai Sea has separate distribution area, they intermingle in autumn season to search for food, thus forming a principal fishing ground located in the central Bohai Sea.Those shrimps wintering in south-central portion of the Huanghai Sea are generally divided into two populations. One is called the Korean population, inhabiting along the western coast of Koera, which is less in abundance and smaller in shrimp size; and the other is called the Chinese population, inhibiting along the Bohai Sea coast and the Huanghai Sea coast of China, which is richer in abundance and larger in shrimp size. The spawning grounds of the latter extend throughout the Bohai Sea and off the Huanghai Sea coast of China, from the Yalujiang Estuary area in the north to the coastal waters of Haiz     

船载微波波高计的船体颠簸校正技术

提出了一种可用于船(舰)载的Ku波段微波波高计,它是一种非接触式的波高测量设备,可架设于船头,动态测量海浪波高参数.为了修正船体颠簸对测量结果的影响,在微波探测单元上设置了加速度传感器,提出了两种不同的数学模型——加速度匀变模型和简谐振动模型,分别计算船体的实时颠簸位移,并对理论上可能出现的最大误差进行了分析.测量结果表明,两种模型均能有效地校正船体颠簸的影响,实测海浪波高的平均误差小于8%.     

用图像质量评价量实现的真实图像和计算机生成图像的鉴别方法

真实图像和计算机生成图像的鉴别是数字图像盲取证中的一个重要问题.提出了一种真实图像和计算机生成图像的鉴别方法.借用模式识别中的二分类概念,采用图像质量评价量来建立模型,以捕获真实图像和计算机生成图像的统计差异,选用支持向量机作为分类器进行训练和测试.实验结果表明,该方法计算方便、实用性强、可靠性高.     

Effect of Different Microphysical Parameterizations on the Simulations of a South China Heavy Rainfall

A heavy rainfall event in south China was simulated by the Weather Research and Forecasting (WRF) model with three microphysics schemes, including the Morrison scheme, Thompson scheme, and Milbrandt and Yau scheme (MY), which aim to evaluate the capability to reproduce the precipitation and radar echo reflectivity features, and to evaluate evaluate their differences in microphysics and the associated thermodynamical and dynamical feedback. Results show that all simulations reproduce the main features crucial for rainfall formation. Compared with the observation, the MY scheme performed better than the other two schemes in terms of intensity and spatial distribution of rainfall. Due to abundant water vapor, the accretion of cloud droplets by raindrops was the dominant process in the growth of raindrops while the contribution of melting was a secondary effect. Riming processes, in which frozen hydrometeors collect cloud droplets mainly, contributed more to the growth of frozen hydrometeors than the Bergeron process. Extremely abundant snow and ice were produced in the Thompson and MY schemes respectively by a deposition process. The MY scheme has the highest condensation and evaporation, but the lowest deposition. As a result, in the MY scheme, the enhanced vertical gradient of condensation heating and evaporation cooling at low levels produces strong positive and weak negative potential vorticity in Guangdong, and may favor the formation of the enhanced rainfall center over there.     

老挝班康姆铜金矿床地质特征及找矿方向

老挝班康姆铜金矿位于老挝西北部,受琅勃拉邦断裂带影响,在本区发育一系列次级断裂,矿体受NE―NNE向韧脆性剪切带控制,本文通过综合分析班康姆铜金矿床成矿地质背景、矿区地质特征、围岩蚀变特征及矿床成因等,认为班康姆铜金矿为构造热液叠加改造型矿床,具有较大的找矿潜力,并提出了对本区该类型金矿的找矿方向。     

内蒙古红花尔基钨钼矿云英岩化白云母Ar-Ar定年及其地质意义

红花尔基钨多金属矿是近年在大兴安岭中北部地区发现的一处大型钨多金属矿床,主要矿化蚀变为云英岩化、绢英岩化,主要有用金属矿物为白钨矿和辉钼矿,岩体内辉钼矿与白钨矿有上钼下钨的带状分布特点,地质特征显示该矿床为一高温热液型钨(钼)矿床。为准确限定成矿热液活动时间,本文对矿区典型蚀变矿物——云英岩化蚀变带白云母进行Ar-Ar同位素定年,获得Ar-Ar坪年龄为174.4±1.2 Ma,等时线年龄为173.2±4.3 Ma。根据矿区云英岩化带与钨钼矿化带空间上重合和密切共生的关系,可知白云母的形成是与白钨矿、辉钼矿形成同源、同时,且辉钼矿Re-Os年龄(176.8±2.2 Ma)与Ar-Ar年龄在误差范围内具有一致性,该年龄代表了钨钼矿热液成矿时代。结合野外地质特征及锆石U-Pb、辉钼矿Re-Os年龄,进一步限定该矿床成矿时代为早中侏罗世,属燕山期构造岩浆活动的产物。