鄂尔多斯盆地城华地区长3油组高分辨率层序地层学分析

运用高分辨率层序地层学的基准面旋回原理,以钻井、测井资料的综合研究为基础,对鄂尔多斯盆地城华地区长3油层组进行高分辨率层序地层学分析,将其划分为超短期、短期和中期3个级次的基准面旋回层序.各级基准面旋回可进一步分为向上"变深"和向上"变浅"非对称型与对称型两大类3种基本层序类型和更多的亚类型.重点论述了超短期基准面旋回层序沉积背景、叠加式样和沉积动力学过程.在研究超短期和短期旋回叠加和分布规律的基础上,总结出短期基准面旋回的分布模式.研究表明自水下分流河道向河口坝中期基准面旋回层序结构稳定的变化规律,与处于三角洲强烈进积期的长3油层组沉积演化特征是一致的.     

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。     

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.     

试论地下水更新能力与再生能力

从循环、更新和再生的基本定义出发,论述了地下水运动在全球水循环过程中的重要作用及地下水更新能力和再生能力的含义,指出"地下水循环"这一说法存在一定不足;提出地下水更新能力和再生能力是含水层系统的自然属性,地下水在含水层系统中更新和再生同时发生.地下水从含水层系统的界面补给与排泄,通过界面与其他系统发生水量交换,地下水在含水层中更替的多寡不影响含水层系统的更新能力;地下水在含水层中更新的过程中,同时发生自然作用(物理、化学和生物作用等)和人为作用(地下水污染控制与修复),其结果反映出含水层系统的再生能力,该过程受水文地球化学条件影响较大,水位变动带内尤甚,含水层系统的地下水再生能力比更新能力的影响因素要复杂得多.     

脂肪细胞分化: 一个故事、两个章节

细胞分化是多细胞个体发育和干细胞实现功能活动的基本过程. 作为诱导白色脂肪细胞分化的体外模型, 小鼠3T3-L1前脂肪细胞系的定向分化过程由依赖于细胞周期特定时相(接触抑制期)的许可阶段和独立于细胞周期的执行阶段所组成. 在接触抑制期, 通过细胞代谢方式、细胞周期调控因子和细胞信号转导通路之间的相互作用, 决定了各种染色质表观遗传修饰因子的活动, 从而导致具备脂肪细胞分化潜能的染色质表观遗传修饰模式的形成. 在随后的执行阶段, 这种分化潜能被激素诱发, 通过复杂的基因调控网络的动态活动, 使各种控制脂肪细胞分化基因表达的转录因子按既定的分化时间表打开或者关闭, 并决定相关的靶基因的表达, 最终导致了脂肪细胞的形成.     

图的局部连通性与上可嵌入性

研究局部连通图中支撑树的变换. 给出L.Nebesk定理的一个新证明, 并将其推广得到一类新的上可嵌入图.     

系统全寿命经济分析的一个模型

研究系统的全寿命经济分析问题.该系统既有可修故障,也有不可修故障,在综合考虑系统全寿命中的收益、建造费用、检测费用、修理费用和善后费用等各项费用的条件下,利用概率分析、补充变量、定积分和Laplace变换等方法,求出了基于系统全寿命的总利润函数和利润率函数.作为利润率函数的一个应用,讨论了系统的最优检测策略问题.     

高师数学教学实习的模式探索与研究

教育实习是师范教育实践教学的最重要部分,课堂教学实习是教育实习的首要内容。关于数学教学实习的模式,国内外也在积极地探索与研究,不断有一些新的模式出现,但是这些模式宏观性,共同性较多,而针对性、专业性的较少。为了适应教育发展与改革的需要,在多年数学教学实习经验的基础上,构建了高师院校数学教育专业"双循环"教学实习模式,以提高数学教学实习的效率和质量。     

农历置闰月方法的解析

指出农历的历法要素与公历的历法要素的不同点.从数学角度对农历“19年7闰”的置闰方法进行详细的推演,即首先将农历平年与回归年的差值同朔望月时长的比值通过辗转相除表为连分数,逐次截取连分式,得一渐近分数序列.在渐近分数序列中选取适当的分数作为所求比值的近似值,由此就得到了农历的置闰方法.探讨农历复合置闰的可能性.指出由于传统农历的一些特殊约定,使得采用复合置闰变得价值不大