密度均匀连续分层流体的内波格林函数

考虑自由表面的影响,从理论上建立了在密度均匀的连续分层流体中脉动点源生成内波的数理模型,应用Fourier变换和围道积分,推导出点源脉动频率的平方小于Brunt-Visl频率的平方条件下含自由面的连续分层流体中脉动点源的内波格林函数,并给出了详细的解析表达式,讨论了解的性质、内波的生成机理和自由面的干扰机理及波动特征.结果表明,所提出的连续分层流体中脉动点源的内波生成格林函数具有较好的准确性.     

严寒地区某示范工程土壤源热泵系统综合评估

通过实时监测严寒地区某教学楼示范工程土壤源热泵系统运行的各项参数,从技术性、节能性、环保性及经济性各自不同的角度全面进行综合评估。为严寒地区土壤源热泵系统的高效运行提供参考。     

Underdetermined DOA estimation and blind separation of non-disjoint sources in time-frequency domain based on sparse representation method

This paper deals with the blind separation of nonstation-ary sources and direction-of-arrival （DOA） estimation in the under-determined case, when there are more sources than sensors. We assume the sources to be time-frequency （TF） disjoint to a certain extent. In particular, the number of sources presented at any TF neighborhood is strictly less than that of sensors. We can identify the real number of active sources and achieve separation in any TF neighborhood by the sparse representation method. Compared with the subspace-based algorithm under the same sparseness assumption, which suffers from the extra noise effect since it can-not estimate the true number of active sources, the proposed algorithm can estimate the number of active sources and their cor-responding TF values in any TF neighborhood simultaneously. An-other contribution of this paper is a new estimation procedure for the DOA of sources in the underdetermined case, which combines the TF sparseness of sources and the clustering technique. Sim-ulation results demonstrate the validity and high performance of the proposed algorithm in both blind source separation （BSS） and DOA estimation.     

25Hz微电子交流计数站内电码化调试存在问题分析

分析了微电子交流计数站内电码化在车出清区段后不能自动复原的问题,探讨了解决问题的方案,并提出了在受端发码时受端发码电源的调试范围。     

百色地区下三叠统-泥盆系烃源岩有机地球化学特征及生烃潜力分析

百色盆地海相烃源岩主要为孤立台地和台间海槽碳酸盐岩.根据百色盆地周缘大量露头样品的残余有机碳含量、干酪根碳同位素、饱和烃色谱及色质等地球化学实验数据,分析了下三叠统-泥盆系海相烃源岩的有机质丰度、类型、热演化程度.针对地表烃源岩样品具有高热演化、低丰度的地化特征,在有机质丰度的热解损失和地表风化损失校正基础上,采用蒙特卡罗法模拟计算烃源岩生烃强度.在综合分析烃源岩地化特征和生烃强度的基础上,认为百色盆地下三叠统-泥盆系海相烃源岩具有低-中等级别的生烃能力.     

培养基中有机氮源对替考拉宁发酵的影响

替考拉宁是采用放线菌发酵生产的一种重要抗生素,发酵培养基中有机氮源的选择对替考拉宁的产量有较大影响,比较了培养基中分别添加豆饼粉、酵母粉及蛋白胨对替考拉宁发酵单位的影响,结果表明,2％酵母粉的效果最优,其效价比等量豆饼粉提高16％,比等量蛋白胨提高20％.     

变压及变压变频电源仿真模块的设计

基于Matlab/Simulink平台,研究了直流变压电源、交流变压电源和交流变压变频电源仿真模块的设计方法。该方法使用受控电压源与自定义非线性的变压及变压变频信号源相结合实现。对直流变压电源信号和交流变压电源信号使用Simulink中已有模块搭建,对交流变压变频电源信号提出了一种将参数存储于矩阵中的S-函数描述方法,并将变压及变压变频信号模型封装为仿真模块,嵌入到Matlab/Simlink平台中,对Simulink的仿真模块库进行了拓展,并通过仿真验证了设计方法的可行性。设计的变压及变压变频电源仿真模块库可为分析电力电子系统的动态行为和性能提供很大的便利,设计思想同样适用于Pspice和Saber等其他电路仿真软件的拓展。     

临南洼陷油气藏分布特征与油气富集主控因素分析

临南洼陷具有良好的油气资源潜力,但随着油气勘探的逐渐深入,临南洼陷的勘探难度越来越大.为了更好的指导今后的油气勘探工作,在研究临南洼陷油气藏基本特征的基础上,从烃源岩、储集层、构造特征等多方面入手,总结油气藏分布特征和规律,分析油气富集成藏的主控因素,剖析各要素对油气富集的影响.结果表明,临南洼陷油气藏类型丰富,主要为断块油气藏及与断层有关的复合油气藏,油气藏主要分布在馆陶组、沙二段和沙三段.临南洼陷油气藏平面上主要分布在临商断裂、夏口断裂及其伴生构造带上,呈环状分布;浊积扇、冲积扇及河流沉积是油气藏分布的主要沉积类型;其富集主要受烃源岩、沉积相、断层等因素控制.油气藏受烃源岩控制围绕生油洼陷展布;有利沉积相带在平面上连续展布,纵向上叠置连片,具有良好的储集条件;断层作为油气的运移通道控制油气的运移,并与地层产状、构造等相配合形成圈闭,控制油气的聚集.     

Characteristics of strontium isotopes and their implications in the Qixing Cave of Guizhou,China

The strontium isotopic compositions (87Sr/86Sr) of samples including soils, bedrock, soil waters, drip waters and their corresponding speleothems in the Qixing Cave (QXC), Guizhou Province, China, were systemically measured and analyzed. The results indicate that there are significant Sr isotopic differences among samples. The mean 87Sr/86Sr ratios in drip water for the samples 1#, 4# and 9# were 0.709568, 0.709139 and 0.708761, respectively, which possibly result from different flow paths, residence times, and other hydrogeological processes in the unsaturated zone overlying QXC. Meanwhile, levels of 40.8%, 57.6% and 72.4% of Sr in drip waters for 1#, 4# and 9#, respectively, were derived from bedrock dissolution, which was calculated by the mixture model of the two end-members (soil and bedrock). There is, however, no positive correlation between the relative proportion from bedrock dissolution (δ13C value is 1.8‰) and drip water δ13CDIC values. The mean drip water δ13CDIC value in 1# is the heaviest (–4.5‰) with the lowest contribution rate of bedrock dissolution, whereas the value in 9# is the lightest (–9.3‰) with the highest contribution rate of bedrock dissolution. The proportion from host rock dissolution in 4# is higher than that in 1# and lower than that in 9#, while its mean drip water δ13CDIC value (–8.6‰) is higher than that of 9# and lower than that for 1#. This suggests that the prior calcite precipitation (PCP) processes in the unsaturated zone overlying the cave are responsible for the δ13CDIC value differences between different drip waters, and not bedrock dissolution. Furthermore, this study also demonstrates that the 87Sr/86Sr ratios of speleothems in the 1# and 4# mainly reflect the variation in the relative proportions from the soil system (soil water) and bedrock dissolution overlying the cave. It is, therefore, feasible to use the strontium isotopic signals of speleothems as an indicator for soil chemical weathering intensity, and consequently as a monsoon proxy in the study area.     

下扬子五峰组上升流相烃源岩沉积特征

五峰组层状含放射虫硅质类地层是下扬子地区所发育的区域性优质烃源岩之一,为前陆挠折滞流盆地边缘斜坡上升流沉积产物。受上升流强度和阵发周期频率的控制,形成了多个厚度呈周期性变化、硅质生物组成略有不同的硅质岩和硅质页岩互层韵律沉积。五峰组沉积时期,水体缺氧程度高,有机质组成以无定形为优势,原始生烃潜力高,低等藻类和其它浮游生物是其主要生源。受上升流影响,硅质岩和硅质页岩沉积时期有机质的保护机制存在差异,有机质富集程度主要与粘土矿物对有机质较强的吸附和保护能力以及氧化硅矿物转化过程中有机质的损失相关。