抑制共模电压的不对称NZPWM技术

为了抑制共模电压,消除死区效应导致的共模电压尖峰,提出一种可通过软件实现的不对称无零矢量脉宽调制技术。在对已有技术进行分析的基础上,调整了开关次序,并对有效矢量的作用时间作了限制。利用不对称的矢量合成算法,弥补最小作用时间限制导致的电压畸变。实验结果表明:该算法可以完全消除死区效应导致的异常脉冲尖峰,从而将共模电压幅值抑制到普通算法的1/3。因此,该方法具有较好的有效性和实用性。     

确定地下水污染强度的梯度正则化方法

将梯度正则化方法(Gradient-Regulation method)应用于地下水溶质运移数学模型(对流—弥散方程)的源项反演,研究了山东省淄博市张店区沣水南部区域地下水中硫酸盐年入渗强度的数值反演问题.算例结果表明了应用梯度正则化方法解决此类问题的有效性和可行性.     

浅谈水源热泵技术的国内外发展现状及趋势

详细地描述了水源热泵的特点并介绍了国内外关于地源应用的基本情况和中国目前水源热泵开发应用的前景和中国水源热泵推广应用中的一些问题.     

计算机监控的高压试验用大功率变频电源

针对当前电力系统中现场高压测试所面临的试验电源问题,提出了一种新型的高压试验用大功率变频电源的工作原理和设计方法,并在此基础上开发了其计算机监控系统,提高了该设备在使用过程中的安全性和自动化程度,现场试验和在实际中的应用证明该设备可靠性高、安全性好、实用性强。     

精密电压调节器TL431三种应用电路设计

介绍了三种精密电压调节器TL431的应用电路:不平衡直流电桥输出信号的稳定和线性化电路,恒流源电路,4~20mA/0~5V电流/电压转换电路。分析了电路工作原理,给出了电路设计方法。所设计的电路简单、新颖、实用。可广泛用于模拟电子电路,特别是传感器的信号调理电路中。由于采用了精密电压调节器TL431做基准电压源,因此电路精度高,稳定性能好。     

决定热传导方程源项的一个正则化策略

确定热传导方程中的线性源项是一类有重要应用背景的反问题,它在Hadamard意义是不适定的,讨论了获得其稳定数值解的计算方法,给出一种新的离散正则化策略.理论分析与数值试验结果表明给出的算法是稳定和有效的.     

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％.     

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。