高静态动作压力下粉尘爆炸泄放标准的可靠性

粉尘爆炸泄放设计标准的可靠性对能否实现爆炸防护尤为关键.以中径70μm石松子粉尘为介质,采用20 L球形粉尘爆炸装置进行了4种泄放口径、静态动作压力在0.12~0.6 MPa的爆炸泄放实验,对比了实验值与NFPA 68和EN 14491计算值.结果表明,NFPA 68在预测高静态动作压力下的泄放面积时,随着泄放口径的增大,预测结果由保守变为危险,但预测结果精度较好且数值稳定;EN 14491在预测高静态动作压力下的泄放面积时非常保守,预测精度较差,数据不可靠.依据两种标准推荐的经验函数关系,分析了NFPA 68和EN 14491在预测高静态动作压力时产生这种差异的原因.     

Influence of rarefaction wave on premixed flame structure and propagation behavior

To explore the influence of rarefaction wave on the structure and propagation behavior of the premixed propane/air flame in a rectangle combustion pipe, the techniques of high speed Schlieren photograph method, pressure measurement and so on are used to study the interaction processes between rarefaction wave and flame. Two cases of rarefaction wave-flame interaction were performed in the experiment. The experimental result shows that both the rarefaction waves can cause the flame transition from laminar to turbulent combustion quickly. The cowflow rarefaction wave decreases the flame speed, while the counterflow rarefaction wave leads the flame propagation speed to increasing on the whole, accompanied with sharp vibration.     

民用防爆汽化站设计探讨

对居民小区汽化站屋面防爆口做法进行改进，并对其他方面的建筑构造要求进行了探讨．     

层流中粉尘的火焰传播速度

建立了筛落式粉尘火焰试验装置和火焰信的号光电测量系统。提出确定火焰前沿位置的“最大斜率切线法”和判定火焰传播稳定性的“相对入射能量法”。测定了硅钙粉和煤粉的火焰传播速度和火焰厚度。结果表明数据合理,测量装置和方法可用于速度范围很宽的粉尘火焰传播研究,用修正的田中达夫模型计算的硅钙粉层流火焰传播速度与实验值接近。     

预应力混凝土箱梁爆炸损伤评估及公式拟合

对预应力混凝土箱梁进行爆炸损伤评估研究。首先,对矩形梁进行爆炸数值分析,结合现场试验结果验证了爆炸数值模型的准确性、可靠性。其次,基于箱梁剩余承载力,建立了箱梁爆后损伤评估准则。通过对预应力混凝土箱梁在不同爆炸工况下的爆后剩余承载力计算,建立箱梁各损伤程度下P?I（超压?冲量）曲线。研究发现,混凝土强度对箱梁超压和冲量临界值影响较大,钢筋屈服强度对超压和冲量临界值影响较小。随着结构损伤等级的增大,各参数对箱梁P?I曲线的影响幅度各不相同。最后,对不同混凝土强度箱梁中各损伤等级P?I曲线进行公式拟合,并对拟合参数β进行分析。     

液体燃料爆炸抛撒过程分析

该文建立了描述液体燃料空气炸药云雾运动规律的模型,给出了云雾膨胀过程３个阶段的速度—半径关系或速度—时间关系,以及云雾中燃料液滴的尺寸估计。     

锅炉炉膛防爆控制系统探析

介绍了炉膛爆炸的原因及防止措施，分析了传统炉膛压力控制系统的缺点，从高压保护回路、压力控制系统、运行程序、联锁系统等方面论述了新型炉膛防爆控制系统。     

湘西凤凰大马地区中、晚寒武世三叶虫

我国湘西大马-亥冲口-峨梨塘地区有大量三叶虫化石产出，它是我国南方已知含丰富化石产地之一．此地同样也是我国寒武系地层出露最完整的地区之一．特别是黔东和湘西交界处，寒武系岩石出露相当好，未变形，易辩认．部分产自亥冲口剖面的多节类三叶虫由现作者近年出版在别处，本文重点介绍几个近年新发现产自大马剖面的三叶虫．     

Microstructure and functional morphology of the Early Cambrian problematical fossil Rhombocorniculum

Rhombocorniculum cancellatum from the Lower Cambrian of southern Shaanxi Province (South China) is represented by the dextral and sinistral tooth-like sclerites (both in nearly equal numbers), indicating that the body plan of the organism with these sclerites probably was bilaterian. The main feature of the microstructure of the sclerites is the presence of longitudinally arranged, mutually contiguous hollow tubules, the shared walls consisting of microcrystalline apatite. In transverse cross sections, the sclerite wall mainly exhibits a spongy structure, with pore size decreasing adapically. Functional morphological analysis indicates that the sclerites serve as a defensive rather than a grasping function.     

Early Cambrian eodiscoid trilobites of the Yangtze Platform and their stratigraphic implications

Analysis of the taxonomy and stratigraphic distribution of the Early Cambrian eodiscoid trilobites of the Yangtze Platform indicates that species of Tsunyidiscus and Hupeidiscus can be used for biostratigraphic correlation. T. aclis occurs only in the lower Qiongzhusian, T. armatus occurs in the lower and middle Qiongzhusian, while T. niutitangensis and T. tingi occur mainly in the middle and upper Qiongzhusian, with only T. tingi extending upward into the lower Canglangpuian. H. orientalis first appears in the upper Qiongzhusian, reaching peak abundance in the lower Canglangpuian and becoming extinct above the Drepanuroides Zone. Biostratigraphic and lithostratigraphic correlations indicate that the limestone in the lower part of the Mingxinsi Formation, the Upper Member of Jiumenchong Formation, and the upper part of the Middle Member of the Huangbailing Formation, can be correlated with each other as Hupediscus, an index fossil of the lower Canglangpuian, is abundant in all these units. The lower part of the Niutitang and Jiumenchong formations in eastern Guizhou, which mainly represent Qiongzhusian strata, can be correlated with the Lower Member of the Huangbailing Formation. The basal part of the Niutitang Formation, which may be equivalent to the Upper Meishucunian Shiyantou Formation in eastern Yunnan, is very condensed. Well-preserved sponge faunas and non-mineralized fossils in the lower part of the Niutitang and Hetang formations are not older than Qiongzhusian in age.