基于计算流体力学的熔盐燃料电池电堆的仿真

基于计算流体力学技术，建立并仿真了10kW级顺流型熔融碳酸盐燃料电池（MCFC）电堆的三维模型，对电堆内部的物质、动量和能量守恒过程进行了理论分析，模型考虑了MCFC电堆的一个重要组成部分-波状板，并讨论了波状板尺寸对电堆性能的影响，结果表明，在采用较大尺寸波状板的电堆中，电化学反应进行得更加充分，所建模型对电堆内部流场的设计有一定意义。     

顺流型熔盐燃料电池电堆的电气特性模型

熔融碳酸盐燃料电池（MCFC）电堆的电气与温度特性决定其性能和可靠性，立足于控制MCFC电堆的输出电压，从单体电池推及电堆，比较全面地对MCFC电堆输出电压以及与之相关的电流密度，燃料气体利用率等特性加以分析，在系统级上建立了由一组变系数偏微分方程和积分方程描述的动态模型，并以外部负载扰动为例讨论了各状态量之间的相互关系，分析和建模的正确性为仿真结果所证实，所得结论有助于控制方案和流场的设计，以及电池材料的选择。     

Reservoir characteristics and genesis of high-porosity and high-permeability reservoirs in Tarim Basin

Based on detailed studies, this paper proposesthat in the Tarim Basin, hydrocarbon reservoirs widespreadeither in vertical sequences or in plane and high-porosity andhigh-permeability reservoirs are developed all over the basin.However, obvious difference and heterogeneity exist amongdifferent kinds of reservoirs. The lithologic characteristics,reservoir space types and reservoir properties in variousstrata have been probed. The result indicates that althoughthe Paleozoic carbonates have been deeply buried for a longperiod, high-quality reservoirs with the porosity of up to 5%—8% (12% as the maximum) and the permeability of10×10^-3—100×10^-3 μm² (1000×10^-3 μm² as the maximum)can be found in certain areas. These include the area withthe development of reefs and carbonate beaches, the weath-ered-crust buried-hill belts that have undergone thelong-term exposure, weathering and leaching, the area withthe development of dolomitization, and those areas that haveexperienced the resolution of carbonic acid and organic acidgenerated by the maturity of the organic matter. Finally, thegenesis of the high-porosity and high-permeability reservoirsin deep-buried conditions (with the depth more than 3500 m)have been investigated thoroughly.     

火焰原子吸收光谱法测定Mn3O4 产品中钙镁含量

用盐酸加热溶解四氧化三锰样品, 加入镧盐和锶盐混合释放剂, 消除70%左右基体锰的干扰, 直接测定其中钙、镁含量, 样品加标回收率为96.8%~ 98.2%,相对标准偏差为2.4%~3.2%.     

从碳酸轻稀土提取二氧化铈

本实验，首先根据铈易被氧化成四价铈的性质，使Ce(OH)3lfnywx o C(OH)4.须稀酸（PH≈2．5）中，Ce(OH)4不溶解，而E（OH）3能溶解，使铈与其他轻稀土元素得到初级分离，再根据四价铈容易被磷酸三丁酯（TBP）萃取的性质，使铈得到进一步纯化，后经草酸沉淀、过滤、灼烧得到纯的二氧化铈。     

鄂尔多斯盆地早奥陶世沉积特征及其演化

鄂尔多斯盆地的早奥陶世沉积可划分为西缘末端变陡的碳酸盐岩缓坡、东缘蒸发-局限台地和南缘镶边碳酸盐岩台地3个沉积区。岩相古地理的发展可划分为3个阶段,即冶理—亮甲山期为稳定的发展阶段,早、晚马家沟期为岩相分异阶段,峰峰期为中奥陶世陆源浊积盆地这一新的发展阶段的前奏。其演化具有东升西降的特点,东部沉积区的沉积相演化为一个向上变浅的沉积序列,而西部为一个向上变深的沉积序列。     

间氯偶氮安替比林双波长分光光度法同时测定钙和镁的研究

本文着重研究了用间氯偶氧安替比林作为显色剂,在 pH=10的硼砂缓冲溶液中,以三乙醇胺作为掩蔽剂,用双波长分光光度法同时测定钙和镁的新方法。测定钙选用655nm—587nm 作为波长对,测定镁选用600nm—674nm 作为波长对,有效地消除了钙镁之间的相互干扰。钙和镁的量均在5—30μg/25cm~3范围内符合比耳定律。提出的方法具有简便快速的特点,用于水样中钙和镁的同时测定,结果与原子吸收法测定值基本一致,回收率也令人满意。     

钙对人体运动能力的影响

本文依各学说论点为基础,进一步阐明了钙与肌肉收缩及舒张、运动性疲劳、肌肉延迟性酸痛、运动性肌肉损伤的新见解,对提高训练水平,增强运动能力都将有重要的现实意义.     

Characteristics of carbonate gas pool and multistage gas pool formation history of Hetianhe gas field, Tarim Basin, Northwest China

<正> Hetianhe is a big carbonate gas field which isfound and demonstrated in the period of "Chinese NationalNinth 5-Year Plan". The proved reserve of Hetianhe gas fieldis over 600 ×10⁸ m³. Its main producing layers are Carbon-iferous bioclastic limestone and Ordovician carbonate com-posed of buried hill. The former is stratified gas pool withwater around its side, and the latter is massive gas pool withwater in its bottom. The gases in the gas pools belong to drygases with normal temperature and pressure systems. Basedon the correlation of gas and source rock, the gases aremainly generated from Cambrian source rocks. According tothe researches on source rock and structure evolution, andthe observations on the thin section to reservoir bitumen andthe studies on homogenization temperature of fluid inclu-sions, the gas pool has been identified and divided into threeformation periods. The first is Late Caledonian when the oilgenerated from the Cambrian source rocks and migratedalong faults, as a form of liquid facies into Ordovician carbonate res-ervoir and accumulated there. After that, the crustuplifted, the oil reservoir had been destroyed. The second isLate Hercynian when condensate gases generated from theCambrian source rocks and migrated into Ordovician res-ervoir, as a form of liquid facies. Since the fractures hadreached P strata, so the trap might have a real poor preser-vation condition, and the large-scale gas pool formation hadnot happened. The third gas reservoir formation period oc-curred in Himalaya. The fractures on both sides of Hetianhegas field developed violently under the forces of compression,and thus the present fault horst formed. The dry gases gen-erated from Cambrian source rocks and migrated upwardsas the form of gas facies into Ordovician and Carboniferousreservoirs, and the large gas pool as discovered at presentwas formed finally.     

TCE的物理化学特性及其生物降解作用

以加拿大一厂址区碳酸盐岩水是中地下受到三氯惭烯（ＴＣＥ）化合物的污染作为实例,对ＴＣＥ的物理化学特性及其降解作用进行论述,指出ＴＣＥ污染物的生物降解作用的存在的,但是不完全,因此,当ＴＣＥ污染物深度明显超标时,仍应考虑采取去除污染措施。