前寒武纪微体古植物化石的采集和处理

前寒武纪微古植物已经成为前寒武纪地质学研究的重要内容 ,并且在解决区域地层划分对比问题时能够很好地佐证其它方面的信息 ,如地质年代学、地层学等 ,因而引起国内外地质学者的广泛重视和关注。由于微古植物赋存状态的特殊性 ,必须采取一些特殊的方法 ,才可获取可靠的微古植物信息。借在全国开展新一轮国土资源大调查之际 ,作者愿将多年工作经验 ,简文奉献给同行。本文从野外采样到室内分析等逐一进行总结 ,以推动前寒武纪研究领域的进展 ,为国土资源大调查做点滴贡献。     

巨野煤田赵楼井田构造发育规律

在野外地质和勘查资料分析的基础上,结合区域构造背景,论述了赵楼井田构造发育、组合及分布规律。研究表明：石炭-二叠纪成煤期后,多期性质、强度不同的构造作用相互叠加、改造,致使赵楼井田构造以断裂为主．褶皱发育次之。断裂构造主要有近NS、NW、NE及NNE向四组,其中以NE、NNE向为主,NW向断层组多为落差、延展长度都较小的断层。断裂以正断层为主,在剖面上主要表现为堑-垒构造组合,这种组合特征不仅使矿井构造更加复杂,而且使煤层的连续性受到破坏。井田东南部断层发育,断层叠加于早期的褶皱之上,破坏了褶皱的完整性．构成井田的构造复杂区。赵楼井田构造发育规律及成因机制的研究为今后矿井建设与生产提供了地质依据。     

Diagenesis impact on a deeply buried sandstone reservoir (Es1 Member) of the Shahejie Formation,Nanpu Sag,Bohai Bay Basin,East China

Diagenesis has a significant impact on reservoir quality in deeply buried formations. Sandstone units of the Shahejie Formation (Es₁ Member) of Nanpu Sag, Bohai Bay Basin, East China is a typical deeply buried sandstone with large hydrocarbon accumulations. The methodology includes core observations and thin section studies, using fluorescence, scanning electron microscope (SEM), cathodoluminescence (CL), fluid inclusion and isotope and electron probing analysis as well as the numerical determination of reservoir characteristics. The sandstones consist of medium to coarse-grained, slight to moderate sorted lithic arkose and feldspathic litharenite. Porosity and permeability values range from 0.5 to 30% and 0.006 to 7000 mD, respectively. The diagenetic history reveals mixed episodes of diagenesis and deep burial followed by uplift. The main diagenetic events include compaction, cementation alteration, dissolution of unstable minerals and grain fracturing. Compaction resulted in densification and significantly reduced the primary porosity. Quartz, calcite and clay are the dominant pore-occluding cement and occur as euhedral to subhedral crystals. Alteration and dissolution of volcanic lithic fragments and pressure solution of feldspar grains were the key sources of quartz cement whereas carbonate cement is derived from an external source. Clay minerals resulted from the alteration of feldspar and volcanic lithic fragments. Porosity and permeability data predict a good inverse relationship with cementation whereas leaching of metastable grains, dissolution of cement and in some places formation of pore-lining chlorite enhanced the reservoir quality. The best reservoir is thicker sandstone bodies that are medium to coarse-grained, well-sorted sandstone with low primary ductile grains with a minor amount of calcite cement. The present study shows several diagenetic stages in the Es₁ Member, but the overall reservoir quality is preserved.     

Reductions of PM<Subscript>2.5</Subscript> in Beijing-Tianjin-Hebei urban agglomerations during the 2008 Olympic Games

The Atmospheric Environmental Monitoring Network successfully undertook the task of monitoring the atmospheric quality of Beijing and its surrounding area during the 2008 Olympics.The results of this monitoring show that high concentrations of PM2.5 pollution exhibited a regional pattern during the monitoring period(1 June-30 October 2008).The PM2.5 mass concentrations were 53 μg m 3,66 μg m 3,and 82 μg m 3 at the background site,in Beijing,and in the Beijing-Tianjin-Hebei urban agglomerations,respectively.The PM2.5 levels were lowest during the 2008 Olympic Games(8-24 August):35 μg m 3 at the background site,42 μg m 3 in Beijing and 57 μg m 3 in the region.These levels represent decreases of 49%,48%,and 56%,respectively,compared to the prophase mean concentration before the Olympic Games.Emission control measures contributed 62%-82% of the declines observed in Beijing,and meteorological conditions represented 18%-38%.The concentration of fine particles met the goals set for a "Green Olympics."     

低层风场在暴雨发生中的动力作用

通过对两次中尺度暴雨过程的计算,分析研究了风的散度与涡度的变化以及与暴雨的关系。指出散度场比涡度场的变化快、尺度小。辐合增加的地区与暴雨区配合最好。对于中尺度系统、完全的散度方程中风速平流的散度项是一个重要的项,它的正值分布区与暴雨区的位置比其他各项有较好的对应。低层流场中大风速中心或低空急流的出现直接导致了散度方程中A项及带有风速垂直切变项的增大,构成了暴雨发生的不可忽视的动力因素。     

青藏高原西部改则地区大气边界层特征

利用第二次青藏高原大气科学考察试验（TIPEX）改则站大气边界层物理观测资料,着重揭示了该地区边界层结构的观测事实,尤其是近地层风、温、湿特征和土壤温、湿特征。主要结果如下:（1）边界层内风速随高度呈多极值分布,即使在白天混合层内,空气上下混合也较差;（2）边界层内白天温度递减率较大,可达到1.6 ℃/100 m;（3）白天,边界层常出现逆湿现象。     

暴雨模拟中多普勒雷达径向速度变分同化的应用

针对2008年6月广东地区的一次强降雨过程,利用WRF中尺度数值模式及其三维变分同化系统(WRF-3DVAR),进行了多普勒雷达径向速度变分同化对暴雨过程模拟效果影响研究。结果表明:WRF-3DVAR能够有效地同化多普勒雷达径向速度,同化后的主要影响在于改进了初始动力场,使得初始场包含有更详尽的中尺度特征信息,进而显著提高模式对广东局地暴雨过程的模拟效果。在高分辨率中尺度数值模式中有效地利用多普勒天气雷达资料,是提高中尺度降雨预报的关键。     

西太平洋副热带高压对热带 海温异常响应的研究

利用多年的观测资料,研究了西太平洋副热带高压对热带海温异常的响应及其相互作用过程。着重研究冬、夏季西太平洋副高对同期及前期不同海域（特别是赤道东、西太平洋以及印度洋海域）海温异常的响应;用SVD方法分析了夏季副热带高压与前冬、前春及同期各月全球海温的最佳耦合模态。在对比研究西太平洋副热带高压异常时其垂直环流变化的基础上,进而研究海气相互作用对副热带高压影响的物理过程。     

基于51单片机的气象数据无线传输系统的设计开发

针对自动气象站探测数据短距离无线传输的需要,设计了一套气象数据无线传输系统。系统由发送器、接收器组成,基于51单片机和NRF905无线射频控制芯片开发。该系统对不同型号自动气象站具有良好的自适应能力。实现了气象数据的无线传输、显示和存储。经测试系统在环境适应性和传输能力方面均达到了设计要求,系统运行稳定、可靠。本文从工作原理,系统构成,硬件设计、单片机程序设计及系统测试几个方面对传输器开发方法进行了详细介绍。