一类差分函数的不动点

研究了一类差分函数gn(z)=f(z+c1)+f(z+c2)+…+f(z+cn)-nf(z)以及差商函数G n(z)=g n(z)f(z)的不动点问题.在假设f的增长级小于1的条件下,分别就f为超越整函数和超越亚纯函数的情形,证明了函数g n(z)和Gn(z)都具有无穷多个不动点,进一步在λ(1/f)=σ(f)的假设下,得到了g n(z)的不动点收敛指数的估计.     

区间删失数据函数的均值估计

运用无偏转换思想构造了区间删失数据函数的均值估计,并在此基础上对所构造的估计量方差进行了研究.针对Ⅰ型区间删失情况和Ⅱ型区间删失情况,找到了估计量方差有限的条件.     

基于中期基准面旋回变化的沉积微相精细研究——以松辽盆地扶余油田泉四段为例

 从区域沉积背景出发,以岩心和测井资料分析为基础,对松辽盆地扶余油田泉四段的岩石类型、粒度分布、沉积构造、泥岩颜色及地球化学特征等各类沉积相标志进行分析,确定其为三角洲沉积,包含三角洲平原和前缘亚相。其中,平原亚相可识别出分支河道、决口扇、天然堤、废弃河道、湖泊沼泽微相;前缘亚相可细分为水下分支河道、河口坝、远沙坝、水下天然堤和支流间湾等微相。依据沉积微相与地层格架的成因关系,在中期基准面旋回的控制下应用取心关键井建立了沉积微相的定量识别图板,对非取心井进行沉积微相的定量识别与划分,并在此基础上绘制了沉积微相的平面及剖面图,总结了微相类型的平面和纵向展布规律及其与含油性的关系,指出分支河道砂体发育规模、连续性、储集性、含油性最好,其次为河口坝砂体,为研究区下一步的开发方案提供地质依据。     

一种包边模边界缩进控制方法

 将确定性优化方法用于板料包边设计.汽车板料包边仿真中变形区域小导致有限元模型在变形区域的网格很小,模型计算时间太长.本文针对影响板料包边后边界缩进较大的3个参数,建立目标函数的径向基函数近似模型,并用确定性优化方法对近似模型进行优化,近似模型计算效率高,提高了优化方法计算效率,使板料包边的优化设计成为可能,并为生产中的汽车板料控制包边后的边界缩进提供了一种新的思路.     

基于真彩切片的MRI图片颜色迁移及三维重构分析

借助于可视人工程的真彩图片作为常用MRI、CT等灰度图片彩色化的颜色迁移的彩色特性源本,以MRI切片和真彩图片的亮度、纹理和几何作为映射间的配准参数而进行合理的颜色转换,以弥补医学灰度图片伪彩色方案中各组织非对应的彩色映射关系.通过真彩图片与灰色图片的亮度分布曲线的调整和纹理特征关系的调整和配准而到有效和符合真实人体器...     

关于r次可加补数的一些复合函数的均值性质

运用初等方法,研究了关于正整数n的r次可加补数函数ar(n)与一些数论函数的复合函数的均值问题,给出了相应函数均值估计的渐近公式.     

Statistical models for intensity and phase fluctuation of laser light in a turbulent medium

The probability density function of irradiance fluctuations in a turbulent atmosphere remains an open topic of research.It is generally considered that the speckle field has an elliptical-Gaussian speckle distribution,but because of its complexity there is still no exact analytical solution.By introducing the concept of random fluctuation intensity and using an equiprobability density ellipse,exact models of the random fluctuation intensity and its phase are proposed.Through theoretical analysis and numerical simulation,it is concluded that the random fluctuation intensity and its corresponding phase are independent only under the circular-Gaussian approximation.     

Coral reef ecosystems in the South China Sea as a source of atmospheric CO<Subscript>2</Subscript> in summer

Field measurements of air-sea CO2 exchange in three coral reef areas of the South China Sea (i.e. the Yongshu Reef atoll of the Nansha Islands, southern South China Sea (SCS); Yongxing Island of Xisha Islands, north-central SCS; and Luhuitou Fringing Reef in Sanya of Hainan Island, northern SCS) during the summers of 2008 and 2009 revealed that both air and surface seawater partial pressures of CO2 (pCO2) showed regular diurnal cycles. Minimum values occurred in the evening and maximum values in the morning. Air pCO2 in each of the three study areas showed small diurnal variations, while large diurnal variations were ob-served in seawater pCO2. The diurnal variation amplitude of seawater pCO2 was ~70 μmol mol–1 at the Yongshu Reef lagoon, 420–619 μmol mol–1 on the Yongxing Island reef flat, and 264–579 μmol mol–1 on the reef flat of the Luhuitou Fringing Reef, and 324–492 μmol mol–1 in an adjacent area just outside of this fringing reef. With respect to spatial relations, there were large differences in air-sea CO2 flux across the South China Sea (e.g. ~0.4 mmol CO2 m–2 d–1 at Yongshu Reef, ~4.7 mmol CO2 m–2 d–1 at Yongxing Island, and ~9.8 mmol CO2 m–2 d–1 at Luhuitou Fringing Reef). However, these positive values suggest that coral reef ecosystems of the SCS may be a net source of CO2 to the atmosphere. Additional analyses indicated that diurnal variations of surface seawater pCO2 in the shallow water reef flat are controlled mainly by biological metabolic processes, while those of deeper water lagoons and outer reef areas are regulated by both biological metabolism and hydrodynamic factors. Unlike the open ocean, inorganic metabolism plays a significant role in influencing seawater pCO2 variations in coral reef ecosystems.     

Evolution of the East Asian monsoon and its response to uplift of the Tibetan Plateau since 1.8 Ma recorded by major elements in sediments of the South China Sea

Evolution of the East Asian monsoon and its response to uplift of the Tibetan Plateau has been investigated in the study of global change. Core sediment samples drilled in the South China Sea during ODP Leg184 are the best materials for studying long-term variability of the East Asian monsoon. R-mode factor analysis of major elements in the fine grain-sized carbonate-free sediments (<4 μm) of the upper 185 mcd splice of ODP Site 1146 drilled during Leg184 in the South China Sea shows that Ti, TFe2O3, MgO, K2O, P, CaO, and Al2O3 are representative of a terrestrial factor. The variation in the terrestrial factor score is subject to chemical erosion in the source region and thus indicates the evolution of the East Asian summer monsoon. The terrestrial factor score has three stepwise decreases at ~1.3 Ma, ~0.9 Ma, and ~0.6 Ma, indicating the phased weakening of the East Asian summer monsoon is related to wholly stepwise, quick uplifts of the Tibetan Plateau since 1.8 Ma. The periodic fluctuation of the terrestrial factor score since ~0.6 Ma indicates that the glacial-interglacial cycles have been the main force driving the evolution of the East Asian monsoon. As in the case of Chinese loess, the long-term evolution of the East Asian monsoon recorded in sediments of the South China Sea reflects a coupled effect of the glacial-interglacial cycle and uplift of the Tibetan Plateau.     

Cs相似度函数下正则谱聚类的收敛阶

用覆盖数逼近的方法给出Cs相似度函数下正则谱聚类的收敛阶.