公共图书馆如何吸引读者参与读者活动

近年来,政府加大了对公共图书馆事业的投入力度,公共图书馆不再仅限于传统的图书借还功能,组织举办读者活动已成为图书馆的重点工作. 分析了公共图书馆举办的读者活动引不起读者兴趣的原因,提出了解决这一问题的对策和建议.     

激光快速成型TC4合金显微组织及力学性能

采用金相显微镜、扫描电镜、电子拉伸机等，研究了激光快速成型TC4合金沉积态在平行沉积方向和垂直沉积方向的组织和力学性能.结果表明:激光快速成型TC4合金沉积态宏观组织沿沉积方向生长的粗大β柱状晶呈明暗相间的条带状结构，具备典型的魏氏组织特征;垂直沉积方向的强度比平行沉积方向的强度高，但塑性低;合金断口为韧窝状断口，垂直沉积方向的断口韧窝尺寸比平行沉积方向的小.     

高温作用后砂岩物理力学性质阈值温度的确定——基于机器学习算法

通过采用机器学习算法，提出了高温作用后砂岩物理力学性质变化的阈值温度的确定方法。基于Python语言，利用K-Means、SVM算法，实现了对样本数据的分类和聚类，确定了阈值温度区间，验证了二分类法的合理性和准确性.结果表明，砂岩样本的阈值温度区间为400~600 ℃，阈值温度上下砂岩的物理力学性质存在显著差异，体现为阈值温度区间以下的岩样物理力学性质较为分散，而阈值温度区间以上的岩样物理力学性质较为集中.     

温度和机械载荷联合作用下油田超深井中硬质涂层膨胀锥与套管的屈服挤毁压强及试验验证

在充分考虑温度载荷、机械载荷、硬质涂层膨胀锥硬度、套管硬度对膨胀锥与套管之间屈服挤毁压强影响的基础上,根据分形理论和接触力学推导出膨胀锥与套管之间屈服挤毁压强的计算公式.数值分析表明:膨胀锥与套管之间的屈服挤毁压强随最终温度、分形粗糙度、线膨胀系数、硬质涂层膨胀锥布氏硬度、中间主应力系数、套管壁厚的增大而增大;当分形维数从1增大时,膨胀锥与套管之间的屈服挤毁压强随分形维数的增大而减小;当分形维数增大到接近于2时,膨胀锥与套管之间的屈服挤毁压强随分形维数的增大而增大;随拉压强度比的增大,膨胀锥与套管之间的屈服挤毁压强减小.屈服挤毁压强的计算值与试验测试值之间的相对误差为-8.9253%～-0.9901%.     

喷射共沉积6066Al/SiCp复合材料热处理塑性变化机理分析

研究了T6热处理对6066Al/SiCp复合材料材料力学性能的影响,结果表明,复合材料经530℃固溶1 h后,170℃时效8 h达到峰时效,其抗拉强度达418.6 MPa;复合材料延伸率随时效时间的增加不断降低.     

电磁场中带电粒子束运动的力学模拟

研究以不同初速度进入互相垂直的匀强磁场和均强电场中的带电粒子束的运动情形，并同相似的力学运动相比拟，建立了直观的力学模型。     

O－芳基－苯基硫代膦酰氯和O－芳基－苯基硫代膦酸异硫氰基酯的研究

合成一些新的有机磷化物，组成为（ＡｒＯ）ＰｈＰ（ｓ）Ｙ（Ｙ＝Ｃｌ、ＮＣＳ）．测定了ｍＰ、ＩＲ、ＨＮＭＲ并进行了元素分析．Ｉａ的除草活性尚好．     

医用降温仪的设计与试验研究

介绍应用机械制冷方法设计医用降温仪的过程，并对所研制的降温仪进行试验和分析研究。     

Developmental modes of the Neoproterozoic-Lower Paleozoic marine hydrocarbon source rocks in China

Based on the researches on rock type, the mode of occurrence, diagnostic minerals and creatures, the sedimentary geochemistry and organic facies of Chinese marine source rocks from wells and outcrops, and on the research findings of developmental modes of foreign marine source rock, the authors consider that it is impossible to objectively make clear the formation mechanism of hydrocarbon source rock with high organic matter abundance by either single mode of preservation or high organic matter productivity. According to the Chinese geological features, the formation mechanism of the Neoproterozoic-Lower Paleozoic marine source rock is generalized into four modes, namely, thermal water activity-upwelling flow-anoxic; carbonate gentle slope-upwelling flow; xerothermic climate-brine euxinic milieu; and humid climate-retained euxinic milieu; as the Lower Cambrian undercompensation basin organic facies （the Tarim Basin, South China and southwestern margin of North China）, carbonate gentle lime mud bound organic facies （the Upper Ordovician in Tazhong region of the Tarim Basin and the Lower Silurian in the Upper Yangtze Platform）, the Middle Cambrian evaporation laggon organic facies （the Tarim Basin and the Upper Yangtze Platform）, enclosed undercompensation terrigenous bay organic facies （the Middle-Upper Ordovician in the west of the Tarim Basin, the Lower Silurian Long- maxi Formation in the Upper Yangtze platform）. Chinese marine sedimentations with lower organic matter abundance are generalized into two modes of consumption-dilution mode of open epicontinental sea and depletion-dilution mode of supercompensation basin.     

A NEW DESCRIPA NEW DESCRIPTOR OF AMINO ACIDS BASED ON THE THREEDIMENSIONAL VECTOR OF ATOMIC INTERACTION FIELD

QUANTITATIVE STRUCTURE ACTIVITY RELATIONSHIP (QSAR) IS A VERY IMPORTANT TOPIC FOR MANY SCIENTIFIC FIELDS AND CAN BE TERMED AS QUANTITATIVE SEQUENCE ACTIVITY MODELS(QSAM)[1] WHEN REFERRED TO THE RESEARCH ON RELATION- SHIPS BETWEEN STRUCTURES AND ACTIVITIES OF BIOLOGICAL MOLECULES, SUCH AS PROTEINS, AND NUCLEIC ACIDS. HOW- EVER, IT IS VERY DIFFICULT TO ESTABLISH A QSAM MODEL,…