基于频繁模式树的约束最大频繁项目集挖掘算法研究

目前绝大多数频繁项目集(或最大频繁项目集)挖掘算法并没有考虑相关领域知识,其结果会产生许多无关的模式.因此,发现约束频繁(或约束最大频繁)项目集是多种数据挖掘应用中的关键问题,然而,这方面的研究工作却很少.为此该文提出了一种快速的基于频繁模式树(FP-tree:一种扩展前缀树结构)的约束最大频繁项目集挖掘及其更新算法.实验结果表明该算法是快速有效的.     

中学田径运动会改为健身运动会的讨论与实践

根据《决定》、《体育与健康教学大纲》、《体育课程改革基本理念》的精神，对田径运动会竞赛规程进行改革，实施3年都取得了良好效果，从而得出田径运动合改为健身运动合是可行的结论。     

基于启发式规则与和声搜索的配电网重构算法

提出一种基于启发式规则与和声搜索算法的配电网经济性重构方法.首先,根据配电网重构网络拓扑要求及和声搜索算法的特点,采用基于重构环解的和声向量编码方式,通过构建重构环特殊支路组、设定支路断开原则避免不可行解的产生;然后,以网损最小为目标分析初始网络,利用启发式规则将各重构环搜索范围压缩到最有可能的有效解范围之中;最后,利用和声搜索算法在有效解范围中全局寻优.该方法显著减少了候选解数目,能够快速搜索到全局最优解,且搜索性能不随网络规模的扩大而变差.IEEE典型算例的仿真结果验证了本文方法的正确性和有效性.     

Zircon U-Pb geochronology of basement metamorphic rocks in the Songliao Basin

Zircon LA-ICP MS U-Pb dating of six metamorphic rocks and a metagranite (breccia) from southern basement of the Songliao Basin are reported in order to constrain the formation ages of basement. The basement metamorphic rocks in the Songliao Basin mainly consist of metagabbro (L45-1), amphibolite (SN117), metarhyolitical tuff (G190), sericite (Ser) schist (N103), chlorite (Chl) schist (T5-1), biotite (Bi)-actinolite (Act)-quartz (Q) schist (Y205), and metagranite (L44-1). The cathodoluminesence (CL) images of the zircons from metagabbro (L45-1) and metagranite (L44-1) indicate that they have cores of magmatic origin and rims of metamorphic overgrowths. Their U-Pb isotopic ages are 1808±21 Ma and 1873±13 Ma, respectively. The zircons with oscillatory zoning from amphibolite (SN117) and Chl schist (T5-1), being similar to those of mafic igneous rocks, yield ages of 274 ± 3.4 Ma and 264 ± 3.2 Ma, re-spectively. The zircons from metarhyolitical tuff (G190) and Ser schist (N103) display typical magmatic growth zoning and yield ages of 424 ± 4.5 Ma and 287 ± 5.1Ma, respectively. Most of zircons from Bi-Act-Q schist (Y205) are round in shape and different in absorption degree in the CL images, implying their sedimentary detritals. U-Pb dating yield concordant ages of 427 ± 3.1Ma, 455 ± 12 Ma, 696 ± 13 Ma, 1384±62 Ma, 1649±36 Ma, 1778±18 Ma, 2450±9 Ma, 2579±10 Ma, 2793±4 Ma and 2953±14 Ma. The above-mentioned results indicate that the Precambrian crystalline basement (1808―1873 Ma) exists in the southern Songliao Basin and could be related to tectonic thrust, and that the Early Paleozoic (424―490 Ma) and Late Paleozoic magmatisms (264―292 Ma) also occur in the basin basement, which are consistent with the ages of the detrital zircons from Bi-Act-Q schist in the basement.     

葛泉岩溶陷落柱发育分布规律及预测研究

葛泉岩溶陷落柱非常发育且具有明显分布特征和规律：密集成群性、网络带状分布性、似等距分布性、构造控制性。多数陷落柱顶部发育到石盒子地层、发育下限为中奥陶统灰岩最下部含膏层。靠近向斜轴线的部位,特别是复向斜反“S”构造的转折部位并受到断层切割,是陷落柱发育的有利部位。     

基于数据挖掘诊断事件方法的网络入侵检测系统

简单论述了在入侵检测系统中数据挖掘技术的应用,并结合了数据挖掘挖等新概念,根据数据挖掘技术用于事件诊断的基本思想,利用粗糙集进行数据归纳,过滤大量事件数据中的冗余属性,得到精简事件数据集,并将得到的精简数据进行分类成所需的规则,并结合实例说明了该方法的工作步骤。由实例可知该方法用于事件诊断的可行性,最后指出实际应用过程中的一些技术难题。     

储层含油性识别中ANN和GA融合的模糊规则提取

提出一种基于ANN和GA融合的自学习自适应的模糊规则提取算法,用来对油层进行识别.其方法是:首先运用人工神经网络(ANN)对训练样本进行有导师学习,网络的输入是测井属性,输出表达为网络权值和输入的函数Ψk=f(xi(WG1)ij,(WG2)jk)(其中:Ψk代表含油性类别Ck的判别函数;C1为干层;C2为水层;C3为差油层;C4为油层).然后,以Ψk作为遗传算法(GA)中的适应度函数提取对应于类别Ck的模糊规则.最后,通过某油田oilsk81和oilsk83油井的实证研究表明,该方法能够有效地识别储层的含油性.     

一种基于逆动力学模糊规则的自适应控制方法

将模糊控制规则归结为控制对象的逆动力学过程模糊辨识问题,提出了一种基于逆动力学过程模糊规则模型的控制算法,通过控制对象逆动力学过程模糊规则模型离线辨识,直接产生形成与控制对象运动规律相适应的初始控制规则,并根据对象逆动力学过程模糊规则模型在线辨识结果,对控制规则进行在线调整.仿真结果表明,所设计的模糊控制器具有良好的控制效果与适应性.     

多车环境下智能货车的紧急转向决策及轨迹规划

决策与规划是实现自动驾驶的关键技术,针对自动驾驶货车在紧急转向避障时需要考虑换道时目标车道的安全性和规划出最优避障轨迹的问题,采用将换道时左右车道上的车辆与自车的相对距离和换道的最小安全距离的差值分别建立模糊关系的方法,通过比较模糊规则推理设计的安全值,选择更安全的车道进行转向避障,为了迅速规划出最优避障轨迹,采用三阶贝塞尔曲线,通过设计4个控制点坐标形成避障曲线,为了防止转向时横向加速度过大导致货车发生侧翻和速度过快与前车发生碰撞,设计车辆的稳定性边界和碰撞边界对控制点进行约束,使用MATLAB中的函数求解出不同车速下的最优换道轨迹,最后使用仿真软件进行仿真验证,结果表明设计出的避障决策和轨迹规划可以安全、有效地避开障碍。     

Zircon SHRIMP U-Pb ages of the “Xinghuadukou Group” in Hanjiayuanzi and Xinlin areas and the “Zhalantun Group” in Inner Mongolia, Da Hinggan Mountains

A report is presented of SHRIMP zircon U-Pb dating data of meta-igneous and meta-sedimentary rocks of the Xinghuadukou Group(Xinlin-Hanjiayuanzi area,Heilongjiang Province)and meta-volcanic rocks of the Zhalantun Group(Zhalantun district,Inner Mongolia).The SHRIMP analyses show that the meta-igneous rocks from the Xinghuadukou Group formed at 506±10―547±46 Ma,belonging to Early-Middle Precambrian,whereas the meta-sedimentary rocks yielded detrital zircons,with ages of 1.0―1.2,1.6―1.8 and 2.5―2.6 Ga,indicative of deposition age at least<1.0 Ga. Meta-basic volcanic rocks from the Zhalantun Group have a formation age of 506±3 Ma.These data suggest that both the Xinghuadukou and Zhalantun Groups formed during Cambrian and/or Neoproterozoic time,rather than Paleoproterozoic time as previously thought.Early Precambrian inherited zircons in the meta-igneous rocks and numerous Precambrian detrital zircons in the meta-sedimentary rocks imply that these rocks were formed proximal to older crust.It is inferred that the Xinghuadukou and Zhalantun Groups represent Cambrian and/or Neoproterozoic vol- cano-sedimentary sequences formed in an active continental margin setting.