倾斜微孔端面气体密封的动压特性研究

为提高多孔端面气体密封的动压特性, 提出 １种双列倾斜椭圆微孔端面密封结构． 基于气体润滑理论模 型, 采用数值方法分析了操作参数和微孔几何参数对密封泄漏率和开启力的影响规律, 探讨了倾斜微孔的上、 下游 泵送作用对气体密封动压特性的作用机理． 结果表明： 与单列倾斜微孔端面气体密封相比, 双列倾斜微孔端面气体 密封可使动压开启力显著增加, 低压侧微孔环带可将下游流体沿微孔倾斜方向向上游泵送, 使得泄漏率显著降低, 气体密封动压效应明显增强; 密封动压性能受反向开孔比、 微孔倾角、 面积比和孔深等几何参数的影响, 本文给出了 这些参数的优化取值范围．     

汉诺坝玄武岩及其超镁铁质岩包体的成因岩石学研究

本文提出的超镁铁质岩包体的全岩成分,矿物化学和微量元素地球化学的全部资料表明,大部分二辉橄榄岩包体代表饱满的地幔样品,而黑色二辉岩包体代表来自下部地壳的麻粒岩样品。二辉橄榄岩包体在980—1120℃有限的温度范围内平衡,但是平衡压力在计算的温度下变化相当大(12.5—24千巴)。黑色二辉岩包体有相对低的平衡条件(850—950℃,8千巴)。和大洋、地盾地温相比,在深度小于100公里时,由二辉橄榄岩体包体所确定的古地温有陡得多的斜率。可以推断最少亏损的地幔可能直接位于被研究的地区之下。     

干涉型光纤传感器相位生成载波解调方法改进与研究

提出了基于干涉型光纤传感器的相位生成载波解调方法（PGC）的改进方法,通过算法上的改进和增加抗混叠滤波器,有效地改善了解调结果,并大大降低了系统的采样频率,结论对设计干涉型光纤传感器解调系统有重要的参考意义     

稀土催化剂本体聚合异戊二烯的生胶性能

本体聚合与溶液聚合相比,具有能耗低,反应平稳,转化率高等特点。杨彩云等用稀土催化剂对异戊二烯(Ip)进行本体聚合,聚合转化率达80%以上,聚合物中无疑胶,且分子量分布较窄(M_w/M?<2)。本文报道和讨论本体聚合放大试验胶样的生胶特性。 异戊二烯胶样(BLn-IR)本所自制。溶液钛催化聚异戊二烯IR-1Q为日本JSR生产。天然橡胶(NR)系海南岛3~#烟片。门尼粘度按GB1232测定。应力-应变性能(23℃),用DL-1000B型电子拉力机测定,拉速500mm/min。玻璃化温度(T_g)用PE DSC-2C型仪测定,升温速率     

PETROLOGY OF BLUESCHIST IN WESTERN YUNNAN PROVINCE,CHINA,AND ITS TECTONIC SIGNIFICANCE

The blueschists in western Yunnan Province are distributed in Lancangjiang and Ailaoshan metamorphic belts and occur as interlayer in green schist and mica schist. Their protolith is basaltic and pelitic rocks with a mineral assemblage of Cr (or Win)+Ab+Qz+Chl+Ph+Ep+Sph+Act and Gl+Ph+Tc+Ep+Alm+Qz+Do, respectively. The P-T conditions of blueschist metamorphism range from 170—443℃ at c. 4—6. 7 kbar. The origin of blue schist of the Lancangjiang belt is related to the subduction and the close of the paleo-Tethys oceanic basin. The Ailaoshan blueschist, however, may be related to the continent continent collision and the dynamic metamorphism.     

THE BOUNDEDNESS OF MULTILINEAR COMMUTATORS ON WEIGHTED SPACES AND HERZ-TYPE SPACES

The boundedness of maximal multilinear commutator on certain weighted spaces is obtained. The boundedness of mulitilinear commutators of singular integrals with Calderon-Zygmund kernel on Herz-type spaces is also considered.     

CENOZOIC VOLCANIC ROCK SERIES IN SOUTHEASTERN CHINA——PETROCHEMISTRY

In this paper, the age, spatial distribution and petrochemistry of Cenozoic volcanic rocks of southeastern China are discussed. They are subalkalic and alkalic. Except for the Pleistocene calc-alkalic volcanic rocks of northern Taiwan and the Late Tertiary tholeiitic rocks of Eastern Coastal Range of Taiwan, the alkalic basaltic rocks form the majority. Only alkalic and strongly alkalic basaltic and ultrabasic volcanic rocks occur in the inland to the west of the Haifeng-Zhenghe-Shangyu fracture zone. It follows that the petrochemical nature of the Cenozoic volcanics studied exhibits a marked trend of variation with time and space, implying that their formation was obviously controlled by the geotectonic setting.     

Bi系高温超导体的119Sn的穆斯堡尔谱研究

本文采用¹¹⁹Sn作为探针原子,对Bi_1.68Pb_0.32Sr_1.75Ca_1.75Cu_2.65-xSn_xO_y(0.2≤x≤0.8)样品进行室温下穆斯堡尔谱测量,结合X射线衍射与电性能测量结果,分析Sn在样品中的占位情况与电性能之间的关系,并得出四配位Cu位对高T_c相的超导电性起着较关键作用的结论。 关键词：     

CENOZOIC VOLCANIC ROCK SERIES IN SOUTHEASTERN CHINA (Ⅱ)——TRACE ELEMENT GEOCHEMISTRY

On the premise of the sister paper, the trace element geochemistry of Cenozoic volcanic rocks of southeastern China is discussed in detail in this paper. The data presented in this paper indicate that the upper mantle beneath the area studied is enriched in the strongly HYG elements as compared with the chondritic mantle, and that the depth of Cenozoic basaltic magma sources progressively increases from the coast to the inland. The Cenozoic basaltic volcanism has occurred in a geotectonic setting of rifting continental margin; on the contrary, the Mesozoic volcanic rocks are predominated by the felsic volcanics erupting in a geotectonic setting of active continental margin. It can be inferred from the studies of ultramafic inclusion-derived geotherm that the Cenozoic rifting of eastern China continent has been mainly controlled by the thermal mantle diapirism.