平台用钢微观组织对其分层面上解理断裂应力的影响

利用专门设计的厚度方向缺口四点弯曲试样，结合相应的弹塑性有限元计算结果，在液氮温度下测取了一种海洋平台用钢的６种微观组织分层面上的解理断裂应力σ＊ｆ．结果显示，均匀细小的铁素体＋贝氏体组织具有比铁素体＋带状珠光体为高的σ＊ｆ值．对于同一终轧温度，轧后冷速愈高，其得到的微观组织之σ＊ｆ值愈高．而对于同一轧后冷却制度，则终轧于Ａｒ３与再结晶停止温度之间者其得到的微观组织具有最高的σ＊ｆ值．讨论了各微观组织组成相的作用     

含分层损伤复合材料层合板非线性热弹性分析

应用含分层损伤复合材料层合板的高阶理论精化有限元模型，对「０／９０」ｓ对称正交铺设层合板在热成型过程中的热变形及残余应力进行了非线性热弹性分析，考虑了材料弹性性能和热性质依赖于温度变化的影响，得到一些对工程应用有参考意义的结果。     

正丁醇/水混合溶剂中一步合成NO3-LDH的研究

以尿素为沉淀剂，正丁醇/水混合液为溶剂，采用水热法直接合成层状双金属氢氧化物ZnAl-NO₃-LDHs。通过X射线衍射（XRD）、傅里叶变换红外光谱（FT-IR）、扫描电镜（SEM）和元素分析（CHN）等对所得样品进行表征，证明在尿素存在条件下，NO₃^-进入LDHs层间；XRD、SEM结果和丁达尔现象显示所得NO₃-LDHs可在甲酰胺溶液中剥离。对尿素存在条件下形成NO₃-LDH而非CO₃-LDH的机理进行了探讨。以氯化盐和硫酸盐为原料，采用本文方法成功合成了Cl-LDH和SO₄-LDH，此研究结果可为制备不同阴离子插层的LDHs提供一种简单直接的方法。     

横向纤维搭桥下矩形脱层热屈曲数值模拟

基于板的小挠度理论以及热屈曲分析的ANSYS有限元法,考虑横向纤维搭桥的作用,对矩形薄板的脱层热屈曲进行数值模拟.有限元分析结果表明,随着纤维搭桥刚度的提高,热屈曲的临界屈曲温度随之增大,脱层屈曲区域逐渐减小.通过数值模拟的结果,能为工程结构中热屈曲问题提供参考.     

3D复合材料纤维搭桥对椭圆脱层屈曲的影响

用能量法求解了绑结层合板和编织层合板等3D复合材料中有纤维搭桥的椭圆搭桥的椭圆形表面脱层的屈曲问题，搭桥纤维被视为连续分布于脱层表面，可提供人与脱层屈曲挠度成正比的恢复力的线性弹簧，通过假定合理的屈曲模态，得到了满意的结果，算例表明，纤维搭桥对提高临界屈曲载荷的作用十分明显，随着纤维搭桥弹性系数的增大，临界屈曲载荷迅速提高，椭圆长轴的长度增大时，临界屈曲载荷减小并逐渐收敛。     

Thermodynamic evolution of lithosphere of the North China craton： Records from lower crust and upper mantle xenoliths from Hannuoba

Lithospheric thinning in East China attracts much attention of geologists. In many cases where a lithospheric thinning is inferred, the trigger for instability is a preced-ing episode of crustal thickening by the continental colli-sion[1]. Lithospheric processes (e.g. lithospheric thinning) could be recorded by the thermal history of the lower crustal and upper mantle xenoliths. Xu et al.[2] suggested that the cooling (from >1200 to 850℃) recorded by spinel harzburgite from Northeast China …     

Study on crustal, lithospheric and asthenospheric thickness beneath the Qinghai-Tibet Plateau and its adjacent areas

Based on the results of pure dispersions of Rayleigh wave tomography in the Qinghai-Tlbet Plateau and its adjacent areas, tsklng S wave velocities from previous linear inversion as the initial model, using the simulated annealing algorithm, a nonlinear simultaneous inversion has been carried out for S wave velocity and thickness of different layers, including the crust, the lithosphere and the asthenosphere. The results indicate： The crustal thickness shows strong correlation with geology structures sketched by the sutures and major faults. The crust is very thick in the Qinghal-Tibet Plateau, varying from 60 km to 80 kin. The Ilthospherlc thickness in the Qinghai-Tibet Plateau Is thinner （130-160 kin） than Its adjacent areas. And two blocks can be recognized, divided by an NNE strike boundary running between 90°E-92°E inside the plateau. Its asthenosphere is relatively thick, varies from 150 km to 230 kin, and the thickest area is located in the western Qiangtsng. India has a thinner crust （32-38 kin）, a thicker lithosphere of 190 km and a rather thin asthenosphere of only 60 kin. Sichuan and Tarlm basins have the crust thickness less than 50 kin. Their Iithospheres are thicker than the Qinghai-Tibet Plateau, and their asthenospheres are thinner. A discussion has been made on the character and formation mechanism of the typical crust-mantle transition zone in the western Qiangtsng block.     

复合材料层合厚板的冲击响应及分层损伤研究

复合材料层合结构是飞机的主要受力构件,研究其冲击响应及分层损伤非常重要。针对5 mm厚40层铺层的层合板分别进行15 J、30 J、45 J的落锤实验,研究低能量冲击的动力响应。然后进行超声C扫描检测获得各界面的分层损伤情况,以分析分层损伤在面内及厚度方向上的分布特性,并在此基础上研究损伤的形成机理,对分层的分布特性进行解释。据此,可对层合板界面分层损伤进行预测,使其得以在实际工程中评估剩余强度以保证构件安全,同时也将有助于层合板的结构优化设计。