涡旋诱发重联模型(Ⅰ)——动力学特性

本文首先从理论上系统地研究了涡旋诱发重联的基本动力学特性.包括:涡旋诱发重联的物理机制;Kelvin—Helmholtz(K-H)不稳定性和撕裂模不稳定性耦合过程;磁流体涡管的基本特性;不同尺度涡旋间的相互作用,动能和磁能间的转化及准稳态时流线、磁力线、等涡度线和等电流密度线的相似性等.用二维MHD数值模拟方法研究了上述一些特性,并与理论分析结论进行了比较.结果表明,模拟结果证实了理论推论.涡旋诱发重联是产生局部磁场重联的重要机制之一,该模型在磁顶区的应用将另文发表.     

Toroidal oscillations of a transradially isotropic elastic sphere

In order to consider the effect of anisotropy on the periods of the oscillations of the Earth, the problem of toroidal oscillations of a transradially isotropic elastic sphere is considered. At each point, the medium is assumed to be transversely isotropic about the radius through the point. The roots of the frequency equation are obtained for different values of the anisotropy parameter α. It is found that, for large order oscillations, the percentage change in the frequency of the toroidal oscillations on account of the anisotropy is nearly equal to |α-1| × 100.     

Br—BTAQ分光光度法测定硅质试样中铁

本文研究了5-(6-溴-2-苯并在噻唑偶氮)-8-羟基喹啉(Br-BTAQ)与Fe(Ⅲ)的显色反应。结果表明,在pH 3.6的邻苯二甲酸氢钾-HCl缓冲介质中,Fe(Ⅲ)与Br-BTAQ能形成蓝色配合物,其最大吸收位于635nm处,表观摩尔吸光系数为3.26×10~4 L·mol~(-1)·cm~(-1),铁量在0—20μg/25ml范围内符合比尔定律。采用NaF和H_2O_2掩蔽Al和Ti后,直接用于硅砂、粘土和硅砖中氧化铁的测定,取得了满意的结果。     

汞型活性碳纸富集—XRF法测定地质试样中痕量碘

本文用特制的汞型活性碳纸富集地质样品中痕量碘并用X-射线荧光光谱进行测定。方法操作简便,样品测定限为0.25ppm,测定含I~-量25μg薄试样片(n=10),其相对标准偏差为3％。经地质标准样品验证,结果与推荐值符合。     

滤纸薄样片—X射线荧光光谱法测定钨和锡

本文用蜡环成形滤纸定量吸附由微量进样器分取的50μl试液,制成薄样进行X射线荧光光谱分析,实现了对样品中高含量WO_3、SnO_2的定量测定。被测组份的荧光强度与浓度在0—500μg/50μl范围内有良好线性关系。方法操作简单、制样速度快、成本低、稳定性好。     

云南省楚雄盆地二氧化碳气成藏模式分析

二氧化碳是自然界整个碳循环中比较稳定的组分,广泛存在于岩石圈、水圈、生物圈和大气圈中,是一种无色、无味的气体,化学式CO2,密度1.977 g/cm3。云南省楚雄盆地是中新生代沉积的构造残留盆地,面积3.66万km2。本文通过对楚雄盆地所发现主要二氧化碳气苗的解剖,总结该区CO2成藏模式。     

牡蛎中氨基酸的傅里叶变换近红外光谱法快速定量测定

本文通过乘法散射校正(multiplicative scattering correction MSC)、一阶求导(1st Derivative,Db1)和Norris平滑等傅里叶变换近红外光谱定量分析数学模型,用交叉验证法确定了最优化建模参数,构建了牡蛎中氨基酸的快速定量测定方法。结果表明,牡蛎近红外光谱与氨基酸含量化学计量学拟合,线性相关系数为0.9860,交叉验证后线性相关系数为0.9794,对牡蛎样品进行检测,结果与传统的氨基酸分析仪的测试结果相比,相对误差小于2.5%,方法的精密度(RSD)小于1.0%,本文建立的傅里叶变换近红外光谱法定量分析牡蛎中氨基酸具有快速、准确、操作简便等特点,测定重复性优于氨基酸分析仪法。     

BDS/GPS/GLONASS组合单历元姿态测量性能对比分析

相比于单一卫星导航系统,多卫星导航系统组合具有显著增加可用卫星数目、改善卫星空间几何结构等优点,因而多卫星导航系统组合应用成为近年来关注的热点。在复杂观测条件下,利用BDS/GPS/GLONASS组合进行载体姿态测量具有单系统无法比拟的优势。首先阐述了BDS/GPS/GLONASS组合超短基线解算的双差模型以及姿态测量基本原理;然后分析了BDS/GPS/GLONASS组合多频单历元姿态测量性能。通过实测静态数据设置不同高度截止角进行分析表明:相比于单系统及双系统组合的姿态测量,BDS/GPS/GLONASS组合能够有效地提高姿态测量的精度、稳定性和可用性。当运动载体处于高楼、峡谷等受遮挡严重的复杂环境时,BDS/GPS/GLONASS组合单历元姿态测量更具有应用价值。     

The Southwest Indian Ocean thermocline dome in CMIP5 models: Historical simulation and future projection

Using 20 models of the Coupled Model Intercomparison Project Phase 5 (CMIP5), the simulation of the Southwest Indian Ocean (SWIO) thermocline dome is evaluated and its role in shaping the Indian Ocean Basin (IOB) mode following El Niño investigated. In most of the CMIP5 models, due to an easterly wind bias along the equator, the simulated SWIO thermocline is too deep, which could further influence the amplitude of the interannual IOB mode. A model with a shallow (deep) thermocline dome tends to simulate a strong (weak) IOB mode, including key attributes such as the SWIO SST warming, antisymmetric pattern during boreal spring, and second North Indian Ocean warming during boreal summer. Under global warming, the thermocline dome deepens with the easterly wind trend along the equator in most of the models. However, the IOB amplitude does not follow such a change of the SWIO thermocline among the models; rather, it follows future changes in both ENSO forcing and local convection feedback, suggesting a decreasing effect of the deepening SWIO thermocline dome on the change in the IOB mode in the future.     

基于Dirichlet-to-Neumann映射计算半无限二维光子晶体的表面模式

介绍了一种基于Dirichlet-to-Neumann（DtN）映射的计算半无限二维光子晶体表面模式的有效数值方法.首先利用三种不同单元晶格的DtN算子构造出超级晶胞的DtN映射,然后在超级晶胞的两条边界上建立特征值问题来计算光子晶体表面模式,建立的特征值问题是线性的,而且其中的矩阵比较小.最后用两个数值算例验证了数值方法的有效性.