基于贝叶斯分类的分布式网络故障诊断模型

该文提出了一个基于Agent的分布式网络故障诊断系统模型框架，该模型对贝叶斯分类理论进行了推广。模型将先验知识和观察数据结合起来，从而大大改进了系统的诊断性能。模型采用一定的状态检查和验证策略，保证了Agent的自身安全和通信安全。Agent之间各自独立，相互协作，合作完成诊断任务。该模型与特定的系统应用环境无关。因此，该文提供了一个通用的网络故障诊断系统框架。     

利用空间大地测量技术研究地球动力学最新进展

空间大地测量以高精度，高时空分辨率测定地球整体（地球自转）和各圈层（特别是大气，海洋与地壳）的运动，使地球动态变化的监测，研究及应用呈现了崭新的面貌，本文介绍了近年来国际地球动力学最新发展概况，内容包括地壳运动，地球自转，重力场时间变化等。     

甘肃灯心草科植物种皮亚显微结构研究及其分类学意义

对甘肃灯心草科(Juncaceae)、地杨梅属(Luzula)、灯心草届(Juncus)20个种及变种植物的种子形态和种皮表面结构进行了光学显微镜和扫描电镜的研究．结果表明：在扫描电镜下，本科植物种子表面纹饰有3种不同的类型，即网纹型、条状突起型和纵条纹型．电镜下的种皮表面纹饰为本科植物的分类提供了新的依据．     

江南丘陵区土地利用/覆被分类

江南丘陵区土地利用/履被类型相对比较复杂，传统的基于光谱特征的计算机自动分类的精度难以达到实际应用的需求．为了提高分类精度，需要模仿目视解译过程，从遥感信息机理与地学规律的综合分析人手，综合其它辅助信息进行分类．在对绍兴试验区地学背景知识和遥感数据光谱特性充分分析的基础上，获取了试验区各类典型地物分类的知识，并以规则的形式表示这些知识，集成TM影像亮度值、亮度值关系和DEM、坡度和坡向地理辅助数据对试验区土地利用/履被进行分类．结果表明，该方法可以方便有效地综合多种辅助数据进行分类，得到令人满意的分类结果，本次试验的分类精度为86．66％。     

利用GMS—5红外资料进行云的分类识别

利用GMS－5 3个红外通道（2个分裂窗区通道和1个水汽通道）的亮温资料，依据各种云不同的辐射特征对其进行分类，由此识别出积雨云（Cb）、浓积云（Cg）、卷云（Ci）、积云（Cu）、中云（Cm）、密云（Dense）等6种主要云类以及雾（Fog）和晴空区域。结合安徽寿县地面观测基准站1998年6、7月份的地面观测资料，对分类结果进行了检验，得到了较为令人满意的结果，准确率接近70％。     

Classification of Medical Brain Images

Since brain tumors endanger people‘s living quality and even their lives, the accuracy of classification becomes more important. Conventional classifying techniques are used to deal with thosedatasets with characters and numbers. It is difficult, however, to apply them to datasets that include brain images and medical history (alphanumeric data), especially to guarantee the accuracy.For these datasets, this paper combines the knowledge of medical field and improves the traditional decision tree. The new classification algorithm with the direction of the medical knowledge not only adds the interaction with the doctors, but also enhances the quality of classification. The algorithm has been used on real brain CT images and a precious rule has been gained from the experiments. This oaoer shows that the ahzorithm works well for real CT data.     

论FDI对西部制度变迁的影响及对策

本文首先对我国西部地区利用FDI的现状进行了描述 ,然后运用回归分析的方法分析了FDI和制度变迁的关系 ,指出FDI是影响区域制度变迁的重要因素 ,FDI在区域分布上的不均衡严重制约着西部地区制度变迁的进程。西部地区应该加快体制改革的步伐 ,改善投资环境 ,吸引FDI ,进而通过FDI带动西部地区制度变迁的进程 ,最终形成FDI和制度变迁相互推动、相互促进的良性循环。     

Holocene lake deposits of Bosten Lake, southern Xinjiang, China

A 9.25-m-long sediment core from Bosten Lake,Xinjiang, provides detailed information about changes in the water budget and biological acticity over the last 8400 cal-endar years. The chronology is constructed from six AMS radiocarbon dates on the terrestrial plant remains. Based onanalyses of TOC, CO3, detrital compounds and biogenic SiO2,lake level fluctuations and periods of remarkably-negative water budget appeared at 8.4-8.2 cal ka, 7.38-7.25 cal ka,5.7-5.5 cal ka, 3.7-3.4 cal ka and 3.3-2.9 cal ka, respec-tively. As they are in-phase with low lake levels at Sumxl Co and Bangong Co in western Tibet Plateau and with paleo-lakes in Inner Mongolia, a climate-induced change to some-what drier and warmer conditions is inferred. A further drop in lake level after 1320 AD of about 200 yr duration may heattributed to a negative water balance prior to the main phase of the Little Ice Age. Deep and stable lake phases of 1500 yr and 1800 yr duration at 7.2-5.7 cal ka and 5.5-3.7cal ka coincide with maximum moisture during the Holocene Megathermai in China. The long term trend towards aridity since about 4.3 cal ka can dearly be recognised. The reduced water budget of Bosten Lake from 640-1200 AD may be attributed to local effects.     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

改变水分子簇的结构及诱发的生物效应研究

概述了水分子簇理论研究的基本状况,以及改变水分子团簇结构的4种方法,包括外加磁场、外加电场、激光辐射以及直接加热法;最后简要介绍了改变水分子团簇结构所诱发的生物效应.