Premixed jet flame characteristics of syngas using OH planar laser induced fluorescence

Lean premixed flame characteristics of several typical low calorific value (LCV) syngases (basis CO/H2/CH4/CO2/N2),including bituminous coal,wood residue,corn core,and wheat straw gasification syngas,were investigated using OH planar laser induced fluorescence (PLIF) technology.OH radical distributions within the turbulent flame were measured for different turbulence intensities.Flame structures of syngases were analyzed and characterized with respect to burnt and unburnt regions,flame curvature (sharp cusp),local extinction (holes and penetration),OH reaction layer thickness,wrinkling,and other features,with OH-PLIF instantaneous images and statistical analysis.Results show that H2 content,LCV,and turbulence intensity are the most effective factors influencing the OH radical intensity and thickness of OH radical layers.The bituminous coal gasification syngas with relatively higher LCV and H2 content tends to burn out easily.Through changes in thickness of the OH radical layers and signal intensities,the reaction layer can be compressed by intensifying turbulence and thereby the combustion processes of syngas.     

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.     

A high-resolution environmental change record since 19 cal ka BP in Pumoyum Co,southern Tibet

A 380-cm-long sediment core was acquired from the deep water area of Pumoyum Co, southern Tibet. Twenty-five plant residue samples were selected, and organic carbon stable isotopes were obtained using the AMS ¹⁴C chronological method. The ¹⁴C age and carbon reservoir effect were calibrated with surface sedimentation rate measurements using ²¹⁰Pb dating. Results showed that the core sediment deposited over 19 cal ka BP. Based on a multi-proxy analysis of TOC and IC contents, grain size and pollen assemblage data, the palaeoclimatic evolution of Pumoyum Co was reconstructed since the last glacial. Pumoyum Co was a shallow lake prior to 16.2 cal ka BP; although the glacier around the lake began to melt due to increasing temperatures, climate was still cold and dry. In the interval of 16.2–11.8 cal ka BP, the sedimentary environment fluctuated drastically and frequently. Two cold-events occurred at 14.2 and 11.8 cal ka BP, and these may correspond to the Older Dryas and the Younger Dryas events, respectively. After 11.8 cal ka BP, Pumoyun Co developed into the deep lake as it is now. The lake water temperature was relatively lower at that time because of influx of cold water from glacial meltwater entering the lake. As a result, the multi-proxy indicators showed no sign of warm conditions. Comparisons between the sedimentary record of Pumoyum Co with that of other lakes of the same age in southern Tibet indicate a warmer climate following the last deglaciation influenced the southeastern Tibetan Plateau. These results imply that the southwest Asian monsoon gradually became stronger since the deglaciation during its expansion to the inner plateau. The glacial-supplied water of the lake responded sensitively to cold-events. The entire southern Tibet region was dominantly influenced climatically by the southwest Asian monsoon during the Holocene.     

非双倍测度下多线性Calderón-Zygmund算子及其交换子在Herz型空间上的有界性

本文引入非齐型空间上的Herz空间,并证明了多线性Calderon-Zygmund算子及其交换子在这些空间上的有界性.     

基体分子量对PP/POE共混体系脆——韧转变的影响

通过临界基体层厚度理论研究了基体分子量对PP/POE共混体系脆韧转变的影响.结果表明,在相同的基体分子量下,脆韧转变温度随基体层厚度增大而增大.PP/POE共混体系的临界基体层厚度（IDc）随基体分子量地增加而减小.PP/POE共混体的脆韧转变既可以在较小的基体层厚度,较低的温度下获得;也可以在较大的基体层厚度,较高的温度下获得.     

PMSM矢量控制下逆变器母线电流频谱分析

逆变器直流母线电流频谱的准确解析是对电磁干扰进行分析及母线电容选取的重要理论基础。针对永磁同步(PMSM)作为负载时逆变器直流母线电流频谱的数学表达和理论求解方法分析了相电压基波和高次谐波对应的等效阻抗。分析得出:非凸极PMSM各次谐波对应的视在电感相等并且恒定;凸极式PMSM的基波电流可以在直轴和交轴上进行相量分解,其对应电感为直轴和交轴电感,高次谐波对应的电感随着转子的位置变化。理论计算时可以通过忽略高次谐波或取平均电感的方法来进行近似。给出了母线电流频谱计算的方法与过程。仿真和实验都证明了本文给出的计算方法及公式的正确性和有效性。     

基于托达罗模型的辽宁沿海经济带农村人力资源转移模式

运用托达罗基本分析模型分别从宏观和微观两个层面研究辽宁沿海经济带农村人力资源转移问题,分析农村人力资源状况、城乡收入差距、总体就业形势等因素以及教育水平、文化差异、心里舒适度等个人心理成本因素的影响.在托达罗分析模型的基础上,结合辽宁沿海经济带整体开发背景,提出坚持政府推动和市场主导相结合、增强城市吸纳能力和扩大在农业(农村)内部就业相结合的人力资源转移方向,构建辽宁沿海经济带农村人力资源转移的基本模式.     

上海市进一步推进海洋经济发展的若干战略思考

纵观人类社会发展的历史,一个明显的轨迹就是沿着流水的边线,从大江大河的中上游地区走向下游及河口地区,从河口走向海岸带,从海洋走向全球.随着经济的高速增长,陆域资源、能源、空间的压力日益加剧,人类已将经济发展的重心逐渐移向海洋世界.     

德江高堆山滑坡稳定性评价及防治对策

文章通过对高堆山滑坡结构及变形特性的研究,结合水文地质环境因素,采用传递系数法对滑坡的稳定性进行评价分析,得出相关结论,并提出了设置纵横排水沟工程、支护工程等治理措施.     

基于Bayes估计的一般原则及在平方损失下的简单应用

讨论了求Bayes估计一般方法的理论依据,给出一种新的证明途径.并进一步给出了平方损失下,二项分布参数以Beta分布为先验分布时的Bayes估计以及正态均值在正态先验分布下的Bayes估计.