前向神经网络粒子群优化学习算法研究

将粒子群优化算法用于前向神经网络权值的学习算法研究,以神经网络学习算法研究的典型问题之一的XOR问题作为研究实例,针对算法的收敛性、学习速度以及算法对初值的鲁棒性等性能指标,分别对标准的PSO算法、改进的PSO算法以及BP算法及其带动量项的BP算法进行了比较研究.研究表明,PSO算法在前向神经网络权值的学习算法中其所有的性能指标均优于传统的BP算法,PSO算法在神经网络的应用中具有广阔的前景.     

带随机收入风险模型的联合分布

考虑一类带随机收入的风险模型,运用吴的方法推导出了破产时、破产前瞬间余额和破产时赤字三者的联合分布．     

两种海洋微藻——强壮前沟藻与青岛大扁藻之间的相互作用研究

在实验生态条件下研究了两种海洋微藻:强壮前沟藻(Amphidinum carterae Hulburt)和青岛大扁藻(Platymonas helgolondica var.tsingtaoensis)之间的相互作用。结果发现:①在单培养体系中,强壮前沟藻和青岛大扁藻的生长曲线可用逻辑斯谛增长模型拟合:不同的起始密度对两种微藻的环境容量(K)有明显的影响,随着起始密度的增加K有逐渐减小的趋势;两种微藻的种群瞬时增长率(r)与起始接种密度之间也具有明显的相关性:强壮前沟藻的r随起始浓度的增加而增加,而青岛大扁藻的r则随起始密度的增加而减小。②在共培养体系中,两种微藻的r和K都受到了明显的抑制,与对照组(单培养体系)相比差异显著(P<0.05);其中强壮前沟藻受到的抑制作用明显强于青岛大扁藻;通过比较两种微藻的种间竞争系数可知,青岛大扁藻的种间竞争能力明显高于强壮前沟藻,这可能是青岛大扁藻在共培养体系中处于竞争优势的原因之一。     

含孔岩体破裂过程的无单元法数值模拟

根据岩体损伤程度对其渗透性和强度的影响,利用定义的损伤变量建立了应力-渗流-损伤的耦合分析模型.综合考虑应力、渗流、损伤之间的相互作用影响,模拟分析了含孔岩体在不同水压力作用下破裂的过程.分析表明,内水压力是促使裂纹扩展的一个重要因素,内水压力增加可以使原来停止扩展的裂纹重新扩展或者使原来闭合的裂纹重新张开,而且裂纹张开度的变化将导致裂纹内的渗流特性发生改变.     

秦岭晚古生代增生弧前盆地的热水成矿系统

目的 探讨中秦岭地区铅锌金多金属矿集区的成矿地质背景和成矿机制.方法 从板块构造角度进行分析.结果 位于商丹带与留坝-山阳断裂带之间的中秦岭地区,其主体是在华北南缘晚古生代活动陆缘环境下增生的一个介于秦岭古岛弧带和留坝-山阳古俯冲带(古海沟)之间,并建立在俯冲增生楔之上的弧前盆地,发育有大规模的热水成矿系统.结论 该区是横亘中国大陆中部的中秦岭岷礼-西成-凤太-山柞大型-超大型金、铅锌多金属矿集区.     

卡套式油管的制作

在汽车制动系统中对于Ф8以上较大管径油管的封接一直是个难题,这是因为制动油管通常采用的：喇叭口型和前锥115度型都不适用于大管径油管。而在一些卡车特别是重型卡车和大客车制动油管的管径,往往做到Ф10、Ф12甚至Ф15、中16,在这种大管径的制动系统中往往采用另一种连接方式——卡套式连接方式。另外由于车体空间的限制,一些油管连接端做得很短,例如Ф12管端仅30mm长,这在通常封接中是无法做到的。然而这些问题在卡套式油管中都被解决了。本文讲述了卡套式油管的制作方法,并且对卡套式油管的预先装配和装配过程中时常发生的漏油问题进行了探讨。     

构建我国小学教师职前培养体系的思考

在教师教育体系经历了一次大的调整和改革后,我国小学教师职前培养体系暴露出一些弊病,不能充分地满足基础教育对师资的需求。根据我国小学教师职前培养的历史特点,结合我国当前小学教师培养工作的现状,要加快小学教师培养体系的建设必须重点解决好培养机构的确定、办学层次的定位、培养模式的变更和培养工作的扶持性政策的完善这几个方面的问题。     

Cloning and characterization of 37 kD laminin receptor precursor in pearl oyster, Pinctada fucata

A 1063 bp cDNA clone encoding a putative 37 kDa laminin receptor precursor （37 kDa LRP） is isolated from the mantle tissue of pearl oyster, Pinctadafucata. The amino acid sequence predicted from the cDNA sequence is 301 residues long, with a calculated molecular mass of 33.5 kDa. RT-PCR analysis shows that 37 kDa LRP mRNA is especially highly expressed in the mantle while widely expressed in several tissues. In situ hybridization analysis reveals that 37 kDa LRP is expressed in the outer epithelial ceils of the mantle edge, suggesting its involvement in cell proliferation and secretion in P. fucata. The identification and characterization of 37 kDa LRP in the pearl oyster will help us to further understand the signal transduction in the processes of mantle epithelial cell proliferation and tissue formation.     

Evidence for metasomatic mantle carbonatitic magma extrusion in Mesoproterozoic ore-hosting dolomite rocks in the middle Kunyang rift, central Yunnan, China

The Kunyang rift lying on the western margin of the Yangtze platform is a rare Precambrian Fe-Cu mineralization zone. Wuding- Lufeng basin that is an important part of the zone is located on the west edge in the middle of the rift. The most important ore-hosting rocks are Mesoproterozoic dolomite rocks in the basin controlled by a ring fracture system, which is a fundamental structure of the basin. Plenty of silicate minerals and acicular apatite, feldspar phenocrysts and small vesicular, flown line and flown plane structures, melt inclusion and high temperature fluid inclusion found in most ore-hosting dolomites suggest that this kind of rocks could not be sedimentary dolomite, marble or hydrothermal carbonate rocks. The Zr/Hf and Nb/Ta values of the rocks are identical with those of associated mantle-derived rocks, and vary widely. For the monomineral dolomite, δ^18OSMOW‰=＋5.99 to ＋18.4 and δ^13CPDB‰ = -3.01 to ＋0.94, which fall within the range for all carbonatitic volcanic rocks of the world. As for the accessory minerals, the values of δ^18OSMOW‰ of magnetite （=＋3.47 to ＋5.99‰） are close to that of the mantle （〈5.7%）, and the δ^34S‰ values of sulfides （-5.09 to ＋5.78, averaging ＋1.50） are close to that of meteorite. For all the ore-bearing dolomite rocks, εNd = ＋0.19 to ＋2.27, and the calculated Isr=0.699143, while for the associated mantle-derived rocks, εnd = ＋3.18 to ＋3.72. All the data suggest that the mineral assemblage is not only igneous but also of metasomatic mantle origin. And the presence of acicular apatite indicates that the rocks were formed by magma rapidly cooling. And the phenocryst texture and vesicular, flown and ropy and pyroclastic structures suggest that the igneous rocks were extrusive. Therefore, the ore-bearing dolomite rocks are carbonatitic volcanic rocks. This conclusion implies that most iron and copper ore deposits hosted in the dolomite rocks should be of the carbonatite type.     

按比例分红策略下具有常利率的泊松风险模型——Gerber-Shiu折现罚金函数

根据按比例分红策略下具有常利率的古典风险过程,得到了关于Gerber-Shiu折现罚金函数的积分方程并给出了确切的解.