计算聚合物驱相对渗透率的新方法

根据聚合物溶液在多孔介质中的流变性，提出了计算聚合物溶液驱相对渗透率的新方法，通过实例说明了该方法的正确性，同时证实了聚合物驱提高采收享的机理在于提高了非均质油藏的波及体积，而并非减小了最终残余油饱和度。     

多站径流随机模型与梯级水电站死水位的计算

本文应用单站多阶月自回归模型与空间分解模型相结合的方法,建立了红水河梯级电站的多站月径流模型.在此基础上,本文还应用动态规划法,以梯级电站的总保证出力为目标函数,计算了各梯级电站的最优死水位,並以实测系列对?这个随机模型所确定的水利参数进行了统计检验;並计算了这些参数的抽样误差.     

用模糊聚类法划分旋风除尘器类型

本文运用模糊聚类分析法，综合考虑旋风除尘器的除尘效率、压降和钢耗等因素，将现有的旋风除尘器分为四类。本文详细叙述了它的分类方法和步骤。此分类法直观、实用。     

Thermal effect of the cable-stayed bridge tower

0　IntroductionXiantaoHanjiangRiverHighwayBridgelocatesonnorth westsuburbofXiantaocity ,crossesovertheHanjiangRiv er.Thecable stayedbridgeisasingle towersystemwiththespansof (5 0 + 82 + 180 )m .Thenon symmetricalstructureisusedheresothatthemainpiercankeepoffthemainchannel.Thesectionofthegirderisnotconstantinorderthatthedeadloadcanbeinbalancealthoughthespansaredifferent.Thedeckwidthis 2 3m (notincludingthewidthofthecablelane) ,laterallayoutisthatofdouble directionfour lanewithoutsidewalk ,b…     

基于自适应遗传算法的拟态蜜罐演化策略

借鉴生物遗传进化现象,将遗传算法引入拟态蜜罐系统中,提出了基于自适应遗传算法的拟态蜜罐演化策略,详细讨论了拟态蜜罐系统演化中特征形式化编码、遗传算子设计、适应度函数、演化触发控制与终止条件等关键问题,设计实现了具有自适应遗传演化功能的拟态蜜罐原型系统并进行了原型测试,实验数据表明了基于自适应遗传算法的拟态蜜罐演化策略具有良好的自适应性和有效性.     

自由基对水稻叶片衰老的影响

以附体水稻叶片为材料,研究了叶片自然衰老时的生理生化变化,并从自由基诱发剂和清除除剂ＡＣＣ转化为乙烯的影响,探讨了自由基对附体水稻叶片衰老的影响。     

锅炉加热系统的FUZZY—PID控制

根据锅炉系统的炉温实验数据及其工作原理,建立了加热系统的数学模型,并针对该系统的大延迟和模型不确定性,将FUZZY—PID控制引入到锅炉系统的炉温控制中。理论分析和仿真结果表明,应用这种方法设计出的锅炉加热系统,在响应速度和稳态精度方面均优于单一的FUZZY及PID控制。该研究具有一定的使用价值,为FUZZY—PID控制锅炉加热系统中的应用打下了理论基础。     

接地电阻测量回路中辅助电极位置的变化规律

针对测量接地电阻时通常采用的三电极法所存在的不足,提出增加辅助电流极的个数,用多电极法测量接地电阻.从三电极法出发,导出了四电极、五电极、六电极、八电极法及任意电极法测量接地电阻时电位过零点、误差补偿点的表达式,并通过计算得出了随着电流极数目的增加电位过零点和误差补偿点的位置的变化规律.以四电极、六电极法为例,用电解槽模拟试验证明了理论分析和计算的正确性.     

新型屏蔽暂堵钻井完井液技术研究

针对胜利油田不同区块水敏性强、渗透率差异大的特点，将不同类型的油层保护剂加入有机正电胶钻井液，研制出一种新型屏蔽暂堵保护油气层钻井完井液体系。该体系突破传统屏蔽暂堵技术观念，封堵效果好，抑制作用强，返排渗透率恢复率高，是一种理想的保护油气层钻井液。     

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.