驾驶员眼部状态识别方法的研究

驾驶员在正常驾驶、瞌睡驾驶及疲劳驾驶 3种状态下的眼睛张开程度有一定的区别。根据这一特点 ,设计了一种 3层BP网络 ,利用图像预处理获取到的眼部区域特征值作为网络输入向量 ,输出对应 3种不同状态。实验结果表明 ,该网络可快速有效地识别出驾驶员眼部精神状态。     

用圆谐-傅立叶矩描述图像

提出了一种描述图像特征的圆谐—傅立叶矩，对圆谐—傅立叶矩的特性进行了初步分析，用圆谐—傅立叶矩可以完整、无冗余地重建原图像，选取有限数量的低阶圆谐—傅立叶矩与同级次的圆谐—傅立叶函数的乘积叠加求和，可以近似地重建原图像，实验结果表明，圆谐—傅立叶矩有很好的图像描述能力，使用10阶以上的圆谐—傅立叶矩就能较清晰地重建原图像。     

内联网络安全的研究与探讨

本文论述了当前内联网络网络安全工作对于国家安全和经济建设的重要意义、它所面临的种种威胁、网络安全体系功能需求，并阐述网络安全技术最新发展，给出了一个较为完备的安全体系可以采用的各种加强手段，包括防火墙、加密认证、网络安全扫描、入侵检测等技术。     

基于层次分析模糊特征融合的目标识别

提出了基于层次分析法模糊特征融合的目标识别，给出了确定多因素属性特征参量相对重要性的量化关系和综合模糊推理识别的权重向量求解方法，利用综合模糊评判模型进行辐射源的属性判决识别。通过计算机仿真试验，证实了该方法的有效性。     

A new species of Gobiconodon （Triconodonta, Mammalia） and its implication for the age of Jehol Biota

A new species of Gobiconodon is found from the Yixian Formation of western Liaonlng, China. The new taxa,G zofiae sp. nov., has a confluent opening for branches Ⅱand Ⅲ of the trigeminal nerve on the anterior lamina of the petrosal. G zofiae sp. nov. is similar to Repenomamus in having an ossified Meckel‘s cartilage connecting the lower jaws and ear region. The new species, with enlarged I^1/I1, posteriorly located infraorbital foramen and four mental foramina,distinctly differs from the other species of Gobiconodon. The new material indicates that Gobiconodon has four, not five,upper molariforms. The presence of Gobiconodon in Jchol Biota makes it possible to correlate Jehol Biota with faunas in eastern Asia and North America, and suggests the age of the Yixian Formation to be Early Cretaceous.     

雄激素与鼠类的社会行为

雄激素引起的社会行为包括杀婴行为、攻击行为、交配行为和社会识别行为等 ,雄激素首先引起脑结构的性差 ,是雌雄个体社会行为发生差异的基础 .雄激素引起的杀婴行为目前还有争议 ,多数学者认为还与孕酮有关 ;雄激素引起的攻击行为还受年龄、生殖状态 (泌乳时期 )、婚配制度、父本扶养还是母本扶养等各种因素的影响 ;雄激素引起的交配行为、社会识别行为还与化学感觉系统有关 ,社会识别主要由抗利尿激素依赖雄激素而产生 .     

地质勘探图的矢量化方法研究

根据地质图中的图形元素的特点 ,给出了具有地质属性的工程图矢量化方法 ,从而将地质勘探图纸信息转化为具有地质信息的矢量数据。分块细化方法提高了大幅图纸的细化处理速度 ;数据优化处理从整体上考虑了勘探图素间的相关性 ,减少了矢量化过程中人为造成的误差 ;图形元素的部分非几何属性的自动识别提高了矢量化的自动化程度。这些方法在地质勘探图的矢量化系统中得到实现 ,并已在油田实际工作中应用。     

Microstructure and functional morphology of the Early Cambrian problematical fossil Rhombocorniculum

Rhombocorniculum cancellatum from the Lower Cambrian of southern Shaanxi Province (South China) is represented by the dextral and sinistral tooth-like sclerites (both in nearly equal numbers), indicating that the body plan of the organism with these sclerites probably was bilaterian. The main feature of the microstructure of the sclerites is the presence of longitudinally arranged, mutually contiguous hollow tubules, the shared walls consisting of microcrystalline apatite. In transverse cross sections, the sclerite wall mainly exhibits a spongy structure, with pore size decreasing adapically. Functional morphological analysis indicates that the sclerites serve as a defensive rather than a grasping function.     

Early Cambrian eodiscoid trilobites of the Yangtze Platform and their stratigraphic implications

Analysis of the taxonomy and stratigraphic distribution of the Early Cambrian eodiscoid trilobites of the Yangtze Platform indicates that species of Tsunyidiscus and Hupeidiscus can be used for biostratigraphic correlation. T. aclis occurs only in the lower Qiongzhusian, T. armatus occurs in the lower and middle Qiongzhusian, while T. niutitangensis and T. tingi occur mainly in the middle and upper Qiongzhusian, with only T. tingi extending upward into the lower Canglangpuian. H. orientalis first appears in the upper Qiongzhusian, reaching peak abundance in the lower Canglangpuian and becoming extinct above the Drepanuroides Zone. Biostratigraphic and lithostratigraphic correlations indicate that the limestone in the lower part of the Mingxinsi Formation, the Upper Member of Jiumenchong Formation, and the upper part of the Middle Member of the Huangbailing Formation, can be correlated with each other as Hupediscus, an index fossil of the lower Canglangpuian, is abundant in all these units. The lower part of the Niutitang and Jiumenchong formations in eastern Guizhou, which mainly represent Qiongzhusian strata, can be correlated with the Lower Member of the Huangbailing Formation. The basal part of the Niutitang Formation, which may be equivalent to the Upper Meishucunian Shiyantou Formation in eastern Yunnan, is very condensed. Well-preserved sponge faunas and non-mineralized fossils in the lower part of the Niutitang and Hetang formations are not older than Qiongzhusian in age.     

Initial organic geochemical investigation on Late Neoproterozoic-Early Cambrian sediments in the Yangtze region, China

Totally 19 samples of typical Upper Proterozoic-Lower Cambrian sedimentary rocks were collected and analyzed for an organic geochemical investigation. Almost all these rocks have high TOCs, super-maturities and similar biomarker distribution. As an exception, however, the Sinian Nantuo Tillite shows much lower TOCs and little phytane and pristane in comparison with those in other strata, which implies a very faint photosynthetic process, and a restricted euphotic zone and quite limited sunlight within the sedimentary water column during the Sinian glaciation age in the western Yangtze region providing an evidence for palaeo-oceanic environment of the Neoproterozoic Snowball Earth age.