硝基芳烃对发光菌及其它水生生物毒性的相关性

测定了硝基芳烃对发光菌的毒性，并研究了它与硝基芳烃对其它水生生物毒性的相关性．结果表明，用发光细菌法能较好地预测鱼、藻等水生生物的毒性。     

周向平均形式的S_2流面计算

本文按照周向平均的方法,应用古川、井上给出的周向平均形式的平衡条件式,对翼形斜流叶轮考虑非轴对称时的S_2流面进行了计算,并将它与轴对称时的计算结果作了比较。     

平坦空间中的全脐点超曲面

本文给出了平坦空间V_(n+1)中全脐点超曲面V_n的两个特征:(1)H~2=K,其中H为V_n的平均曲率,K是V_n的黎曼曲率;(2)V_n是超球面或超平面,并且又给出了关于V_n的四个简单结果:(1)H=常数,K=常数;(2)测地线是长为2πR的闭曲线(3)无实的渐近方向(4)渐屈面不存在     

声光辐射对小麦育种的影响

试验料材选用粒大、色白、品质好的6811(1)-81小麦品系.色光辐射源采用高频超声设备,输出最大电功率300W,频效1.1MHz,换能器输出声能经声透镜聚焦后,焦区平均声强度50W/cm~2;光源采用氦氖激光器,光斑直径3mm.光束垂直于声波传播方向,直接照射于声场焦区内.     

灰铸铁中初生奥氏体树枝晶二维金相切面与三维空间结构之间的关系

本文应用晶体几何学原理,对灰铸铁中初生奥氏体树枝晶进行了解剖研究,发现金相试样中复杂纷乱的枝晶二维切面是不同位向的树枝晶沿一定晶面切开的结果。利用树枝晶二维和三维空间结构之间的几何对应关系,可以比较方便、准确地对树枝晶的生长方式及形貌特征进行分析和计算。     

悬浮液进样-火焰原子吸收光谱法快速测定强化乳粉中锌、铁、钙的研究

要用琼脂溶液对难溶粉固体物的分散作用，将悬浮液进样技术应用于原子吸收光谱分析中，以此建立了乳粉中微量元素锌，铁，钙的快速分析法，研究了悬浮液进样的最佳条件，并用硝酸镧消除基体干扰，本法具有快速，简便，准确且无需进行样品处理等优点，方法的相对标准偏差于1．2％－2．2％，回收率为96％－102％，测定值与湿法消解样品所测结果比较，结果令人满意。     

55CrSiA与JIS G3566—77油淬火弹簧钢丝的比较分析

在系统地对同规格的５５ＣｒＳｉＡ与ＪＩＳ Ｇ３５６６－７７油淬火钢丝的成分、组织、残留元素及力学性能进行了复查，并按相同工艺制成ＦＭ１４７发动机气阀弹簧做了比较试验后发现：该种弹簧钢丝与日本弹簧钢丝在质量上略有差距。     

石灰石类的石质保护

研制了一种可逆型的石质保护剂，涂刷在大理石、红砂石、和田玉、石灰石、青石等石质上形成保护层。经过一系列实验测试，表明该保护剂具有渗透力较强、憎水、抗酸雨等性能，可使石质耐风、雨、沙、冰冻、可溶盐、日光照射、温差变化和微生物等的侵蚀。     

Phosphorylation by aurora kinase A induces Mdm2-mediated destabilization and inhibition of p53

Aurora kinase A (also called STK15 and BTAK) is overexpressed in many human cancers. Ectopic overexpression of aurora kinase A in mammalian cells induces centrosome amplification, chromosome instability and oncogenic transformation, a phenotype characteristic of loss-of-function mutations of p53. Here we show that aurora kinase A phosphorylates p53 at Ser315, leading to its ubiquitination by Mdm2 and proteolysis. p53 is not degraded in the presence of inactive aurora kinase A or ubiquitination-defective Mdm2. Destabilization of p53 by aurora kinase A is abrogated in the presence of mutant Mdm2 that is unable to bind p53 and after repression of Mdm2 by RNA interference. Silencing of aurora kinase A results in less phosphorylation of p53 at Ser315, greater stability of p53 and cell-cycle arrest at G2-M. Cells depleted of aurora kinase A are more sensitive to cisplatin-induced apoptosis, and elevated expression of aurora kinase A abolishes this response. In a sample of bladder tumors with wild-type p53, elevated expression of aurora kinase A was correlated with low p53 concentration. We conclude that aurora kinase A is a key regulatory component of the p53 pathway and that overexpression of aurora kinase A leads to increased degradation of p53, causing downregulation of checkpoint-response pathways and facilitating oncogenic transformation of cells.     

Subduction and collision processes in the Central Andes constrained by converted seismic phases

The Central Andes are the Earth's highest mountain belt formed by ocean-continent collision. Most of this uplift is thought to have occurred in the past 20 Myr, owing mainly to thickening of the continental crust, dominated by tectonic shortening. Here we use P-to-S (compressional-to-shear) converted teleseismic waves observed on several temporary networks in the Central Andes to image the deep structure associated with these tectonic processes. We find that the Moho (the Mohorovici? discontinuity--generally thought to separate crust from mantle) ranges from a depth of 75 km under the Altiplano plateau to 50 km beneath the 4-km-high Puna plateau. This relatively thin crust below such a high-elevation region indicates that thinning of the lithospheric mantle may have contributed to the uplift of the Puna plateau. We have also imaged the subducted crust of the Nazca oceanic plate down to 120 km depth, where it becomes invisible to converted teleseismic waves, probably owing to completion of the gabbro-eclogite transformation; this is direct evidence for the presence of kinetically delayed metamorphic reactions in subducting plates. Most of the intermediate-depth seismicity in the subducting plate stops at 120 km depth as well, suggesting a relation with this transformation. We see an intracrustal low-velocity zone, 10-20 km thick, below the entire Altiplano and Puna plateaux, which we interpret as a zone of continuing metamorphism and partial melting that decouples upper-crustal imbrication from lower-crustal thickening.