Finesse 全瓷冠适合性的体外实验研究

目的 :测量Finesse全瓷冠的边缘浮出量及粘固剂的厚度 ,并与金属全冠及金瓷全冠相比较 ,为Finesse全瓷冠的临床应用提供适合性方面的理论依据。方法 :用片切法测量 3组全冠粘固前、后边缘浮出量及粘固剂的厚度。结果 :Finesse全瓷冠粘固前、后的边缘浮出量分别为 (37 6 1± 9 13) μm、(6 5 85± 15 11) μm ,粘固剂厚度为 (40 84± 9 73) μm ,与金属全冠及金瓷全冠相比较 ,均无显著性差异 ;3组全冠粘固前和粘固后的边缘浮出量有显著性差异。结论 :Finesse全瓷冠适合性良好 ,完全可为临床应用 ;粘接对全冠修复体的边缘浮出量有影响。     

放射性废树脂水泥固化中水化热的降低

降低放射性废树脂水泥固化中水化热可以降低温度应力、减少裂纹。比较了添加沸石、轻烧高岭石粉、矿渣和粉煤灰对ASC特种水泥树脂固化体抗压强度的影响。根据强度测试结果,选择了使固化体强度可以满足要求的配方。通过比较相同散热条件下所选配方的最高中心温度,选择得到了添加20%沸石的最佳配方。实测了用最佳配方进行200L固化的温度曲线。结果表明:该配方的最高温度为75.4℃,且固化体表面不出现裂纹,树脂包容量体积分数达到55%～60%,实现了放射性废树脂的高效固化。     

碳钢粉末渗铝试验研究

对 2 0碳钢进行了粉末包埋渗铝试验 ,优化了渗剂配方及渗铝工艺。采用X射线衍射仪分析了渗铝层的相成分 ,并对渗铝层的微观组织和渗铝钢的力学性能进行了测试。结果表明 ,使用 3号渗剂的 2 0碳钢的表面渗铝效果最好。 2 0碳钢渗铝层内未出现高铝脆性相 (FeAl3 、Fe2 Al5等 ) ,这有利于改善渗铝钢的力学性能和焊接性能。 2 0碳钢经渗铝处理后 ,其机械性能略有降低 ,高温持久性能明显降低 ,而抗高温氧化性能大大提高。     

Ordinary Toxicity of Chlorine Dioxide and By-products Chlorite and Chlorate in Water

Acute toxicity and accumulated toxicity of chlorine dioxide (ClO2) and by-products chlorite (ClO2-) and chlorate (ClO3-) in water acted on mice are studied by the method of Horn and accumulation coefficient. Subchronic toxicity of the mixture of ClO2 and ClO2-and ClO3- in water acted on rat is studied though feeding test for 90 days, including statistical analysis of variance on weight gaining, food utilization efficiency,index of blood and serum,liver (or kidney) to body weight ratio, and histopathological examination on liver and kidney. The results show that aqueous solution of ClO2, NaClO2 and NaClO3 ( with the concentration of 276.5 mg/L, 200 mg/L and 200 mg/L respectively) and the mixed aqueous solution of ClO2 with the concentration of 553 mg/L are actually non-poisonous , and non-cumulative aqueous solution as well.     

小波变换在检测粘接件信号特征中的应用

在对金属与非金属粘接件性能检测的分析处理中，应用小波变换的方法对这种非平稳过程的信号进行分析，有效提取了性能检测所需要的特征参数，为提高金属与非金属粘接件性能检测的准确率和效率奠定了基础。     

端磨渗碳钢时磨削烧伤的预测和控制

通过实验，分析了端磨渗碳钢时影响磨削烧伤的因素，提出了对磨削烧伤进行预测和控制的途径。结论对生产实际有一定的参考价值。     

环渤海地区云量的动力过程相似预报方法

利用环渤海35个台站1954-2002年近50年逐日平均总云量和低云量的观测资料,统计关注区域内少云、中等云量、多云的发生情况;再用同期NCEP再分析资料,计算出预报关注区域内与不同云量形成相关性较好的各种不同要素的平均场,依据动力过程相似原理,利用T213数值预报产品相邻24h预报场,以域块距离为依据,建立云量预报模型,制作日平均总云量和低云量4～9天的预报.经过2003-2007年的预报结果与实况资料的对比检验表明:依据动力过程相似方法建立的云量预报模型对日平均总云量和日平均低云量的预报准确率较高;日平均低云量预报准确率要高于日平均总云量;冬半年预报准确率高于夏半年;天空出现少云的预报准确率高于中等云量和多云的情况.     

Evans图法研究SbO_Zn置换体系的反应速度

本文采用旋转电极上的动电位扫描法以及旋转杯盘电极技术研究了硫酸钠溶液中(pH=4.0)的SbO~+/Zn置换反应,并根据Evans图法,计算了SbO~+/Zn置换反应的速度常数(k).900rpm时;k=(1.7±0.2)×10~(-5)m·s~(-1).Evans图表明,SbO~+离子可被金属锌还原至SbH_3,其反应过程受SbO~+离子向电极表面的扩散过程控制.     

Solidification of Spent Ion Exchange Resin Using ASC Cement

IntroductionSpent ion exchange resins(IERs) comprise themajor fraction of low and intermediate levelradioactive wastes in nuclear facilities,such asnuclear fuel reprocessing plants and nuclear powerstations.This kind of radwaste is difficult to treatand there is no practicable treatment technologycurrently available in China. Solidification of spentIER by cement has been used in several countriesdue to simple operation,low expense andendurance in the disposal environment[1] .However,some de…     

Authigenic sulfide minerals and their sulfur isotopes in sediments of the northern continental slope of the South China Sea and their implications for methane flux and gas hydrate formation

This is a report of the study of the authigenic sulfide minerals and their sulfur isotopes in a sediment core (NH-1) collected on the northern continental slope of the South China Sea, where other geo-physical and geochemical evidence seems to suggest gas hydrate formation in the sediments. The study has led to the findings: (1) the pyrite content in sediments was relatively high and its grain size relatively large compared with that in normal pelagic or hemipelagic sediments; (2) the shallowest depth of the acid volatile sulfide (AVS) content maximum was at 437.5 cm (>2 μmol/g), which was deeper than that of the authigenic pyrite content maximum (at 141.5-380.5 cm); (3) δ 34S of authigenic pyrite was positive (maximum: 15‰) at depth interval of 250-380 cm; (4) the positive δ 34S coincided with pyrite enrichment. Compared with the results obtained from the Black Sea sediments by Jorgen-sen and coworkers, these observations indicated that at the NH-1 site, the depth of the sulfate-methane interface (SMI) would be or once was at about 437.5-547.5 cm and the relatively shallow SMI depth suggested high upward methane fluxes. This was in good agreement with the results obtained from pore water sulfate gradients and core head-space methane concentrations in sediment cores collected in the area. All available evidence suggested that methane gas hydrate formation may exist or may have existed in the underlying sediments.