珠江口盆地番禺4洼珠江组层序地层及其约束下砂体发育模式

根据钻测井资料及地震资料,对番禺4洼珠江组层序地层进行研究,明确砂体发育特征与层序地层的关系,进一步分析二级层序不同演化阶段海平面变化、物源供给、构造沉降要素对砂体发育的影响,并建立二级层序控制要素作用下砂体发育模式。结果表明研究区珠江组可划分为1个二级层序,5个三级层序,各三级层序均只发育海侵体系域和高位体系域;不同三级层序的结构特征存在差异,其中三级层序SQ1和SQ2海侵体系域和高位体系域均较为发育,而三级层序SQ3~SQ5以高位体系域为主;砂体发育特征与二级层序基准面演化及三级层序结构密切相关,二级层序基准面上升半旋回,砂岩含量整体有降低趋势,单层砂岩厚度减小;二级层序基准面下降半旋回,砂岩含量整体有增大趋势,晚期单层砂岩厚度明显增大;三级层序SQ3~SQ5砂体主要发育在高位域;全球三级海平面升降旋回控制研究区三级层序的发育及结构类型,进一步控制不同结构三级层序的砂体发育规律;物源与二级相对海平面共同控制二级层序内砂体的垂向叠置样式和平面演化。     

深海浊积砂岩油田高效注水策略及实践

以尼日尔三角洲盆地典型的深海浊积砂岩油田AKPO为研究目标,剖析了浊积水道和朵叶的储层特征,以注采井组间砂体连通方式为基础,结合生产动态特征评价了注采井组间的连通性,确定油田在无水采油期的注水策略。基于时移地震揭示了不同储层类型的水驱波及特征,形成了油田注水突破后的注水以及控堵水策略,建立了适宜油田不同开发阶段的高效注水策略。在无水采油期阶段,基于注采井组间砂体的连通方式应用以“控制压力”为重点的注水强度优化策略,实现不同井组的分级配产配注;在中低含水阶段,基于储层沉积类型应用以“提高波及”为重点的注水强度优化方法,即依靠水动力学方法来改善水驱波及系数,水道储层注采井组采用周期注水提高“纵向”波及系数;朵叶储层注采井组采用改变液流方向提高“平面”波及系数;在高含水阶段,应用适宜深海油田的“低成本”分段控堵水方法,实现深海油田经济有效的控堵水。上述深海浊积砂岩油田高效注水策略经AKPO油田实践,实现AKPO油田高峰采油速度达到5.5%,连续7 a实现稳产,预测油田采收率达到53%。系统形成深海浊积砂岩油田在不同开发阶段的高效注水策略,该策略简单易行、经济有效,可以指导同类深海油田的注水优化。     

声表面行波器件及其在微纳领域的应用

 声表面行波因其非接触性及生物相容性，在生物医学、诊断学领域得到了广泛关注。概述了声表面行波（TSAW）发生器件的基本结构，叉指换能器（IDT）的结构、参数、种类及引起声表面行波的内在机理，讨论了对微流体状态及微流体中粒子的声控制机理；综合当前该技术国内外研究现状，分析了在微纳领域中声表面行波相对于其他物理场的优势；针对声表面行波在微纳领域应用的技术难点及研究过程中存在的问题，提出了该技术的研究方向，并展望了其未来发展趋势。     

时变海面舰船目标动态雷达特征信号模型

提出了一种时变海面舰船目标动态雷达特征信号的仿真方法。建立了海面舰船目标雷达回波多径效应模型、二维动态粗糙海面的时变复反射系数模型和动态海面舰船运动的水动力模型,并同目标电磁散射计算的高频方法相结合,形成了时变海面舰船目标动态雷达特征信号仿真模型。利用海面浮球的测量数据对模型进行了验证,并对典型舰船目标的动态雷达特征信号进行了仿真和分析。     

Radar Sea Clutter Suppression and Target Indication with a Spatial Tracking Filter

It is an important issue to study sea clutter suppression because it could interfere with the detection of targets above the sea surface severely. Spatial spectrum analyses show that the majority of sea clutter has low-frequency characteristics, compared to the high-frequency characteristics of the targets. This paper proposes a frequency-based spatial tracking filter to suppress sea clutter to facilitate targets identification. Experimental results show that the signal-to-clutter ratio can increase by more...     

细胞内圆柱形空间钙波的Fire-Diffuse-Fire模型

考察Fire-Diffuse-Fire模型在圆柱区域内钙波的传播情况.通过求解扩散方程,得到了圆柱区域内Ca2+浓度的解析表达式.分析证明了钙波的存在性、稳定性依赖于半径和Ca2+泵率,产生钙释放的阈值在有限区间内随半径增大而增大.此结果有助于了解细胞内的内质网以及Ca2+泵在细胞Ca2+动力学上的作用.     

P波作用下地下输流管道的动力响应分析

采用复变函数法研究了地下输流管道在平面P波作用下的动应力集中问题.建立了地下输流管道的流固耦联波函数,求解了地下输流管道在地震波作用下的波函数动力学方程.研究表明:流体作用对管道内的径向动应力集中分布的影响较大;无量纲的空间频率显示,在低频P波作用下,管内流体所产生的径向动应力集中沿管周呈均匀分布,当空间频率加大时,管道内流体震荡增强,影响了管道的应力分布形态;低频域下管道的环向动应力集中峰值点较多,随着入射波空间频率的增加,应力集中程度呈衰减趋势.     

A high-resolution clay mineralogical record in the northern South China Sea since the Last Glacial Maximum,and its time series provenance analysis

High-resolution clay mineralogical analysis of Core MD05-2904 in the northern South China Sea (SCS) covering the period since the Last Glacial Maximum shows that illite (29%–48%), smectite (14%–45%), chlorite (17%–28%), and minor kaolinite (6%–14%) comprise the clay mineral assemblage, and that time series variation does not present glacial-interglacial cyclicity. Provenance analysis indicates three end-member sources: almost all smectite derives from Luzon, all kaolinite is sourced from the Pearl River, and illite and chlorite originate from both the Pearl River and Taiwan. By comparing clay mineral compositions in surface sediments from the three major source areas and of the SCS, we reconstructed a time series of clay mineral contribution from the major provenances to the northern slope of the SCS using the linear separation method for illite crystallinity. There were three stages of provenance change. (1) During 24.1–17.5 ka BP, contributions from Taiwan and Luzon were similar (30%–40%), while that from the Pearl River was only 25%. (2) During 17.5–14.0 ka BP, the contribution from Luzon decreased rapidly to 20%–25%, while that from Taiwan increased to 35% from an average of 25% at 18 ka BP, and that from the Pearl River increased largely to 40%. (3) During the Holocene, differences in contributions from the three major provenances increased: the contribution from Luzon increased slightly and then remained at 27%–35%, that from Taiwan increased rapidly and then remained at 55%–60%, and that from the Pearl River decreased to 15%. The change in clay mineral contributions from different provenances is influenced mainly by clay mineral production, monsoon rainfall denudation, oceanic current transport, and sea-level change.     

角度截断双尺度模型模拟粗糙海面后向散射特性

针对传统双尺度法中尺度截断波数的选取尚无统一标准可依的情况,提出了一种基于局部入射角划分来选择相应的海面电磁散射计算方法的角度截断双尺度模型：局部入射角小于限定角（约为20°）时,使用基尔霍夫近似计算占主导的镜反射分量;当局部入射角大于限定角时,用微扰法处理小尺度粗糙度所支配的漫射分量。该模型充分利用了基尔霍夫近似和微扰法各自的优点,同时避免了选取截断波数的棘手问题。应用该模型计算并讨论了风速、极化状态以及风向对后向散射系数的影响,并与实验数据进行了比较,取得了较好的吻合,证明了该模型的有效性。     

冲击射流的间断有限元仿真研究

采用间断有限元方法对轴对称可压缩Euler方程组进行数值离散,并对非稳态垂直冲击射流进行了仿真模拟。计算结果表明,采用该方法能够较好地捕捉到起始冲击波在平板上反射后形成的曲面激波、马赫反射以及三波交点等复杂流场波系结构;随着时间的发展,冲击平板中心区域有明显的回流现象;平板表面的压力系数分布曲线与实验测量结果吻合较好;表明该方法是有效的,为冲击射流的数值仿真提供一种新的手段。

Abstract：

Unsteady impinging jet was simulated numerically using discontinuous finite element method which discretized axisymmetric compressible Euler equations.The computed results show that the complicated shock wave structures of interest including bowed shock waves,Mach reflected wave and the triple point are well captured using this method.Recirculating flow near the center impinging zone of surface can be observed obviously with the lapse of time.Comparisons of Surface pressure coefficient distribution showed better agreements between the computed results and experimental measurements,which indicate that this method is efficient and provide a new means for simulating the impingement jet.