T800/5228E复合材料层合板动态冲击力学响应

研究了宽冲击能量范围(12.8、25.5、34.2、42.3与51 J)内T800/5228E复合材料层合板动态冲击力学响应历程.结果表明,复合材料层合板损伤历程依次为裂纹引发→分层扩展→最大损伤→二次损伤等,冲击能量基本不会对其发展演化历程产生影响;力学损伤参数研究发现,赫兹失效载荷Fh与冲击能量成线性关系,而最大作用载荷Fmax与冲击能量为特定指数函数关系.不可逆能量Lw与能量吸收率η研究表明,两者均与冲击能量保持单调递增关系,反映复合材料板的损伤程度在加重,但损伤面积基本趋于稳定,纤维断裂等二次损伤可能成为新型能量吸收方式.     

工艺因素对RFI复合材料渗透成型影响的试验研究

采用模拟试验的方法研究了复合材料树脂膜渗透成型(Resin Film Infusion RFI)过程中树脂粘度及压力对渗透高度及浸渍质量的影响。实验结果表明,总体上树脂的粘度提高,复合材料的渗透浸渍高度下降。成型压力则对不同粘度体系及增强材料预处理情况有不同的结果,一方面提高树脂渗透驱动力,另一方面压实纤维床从而降低渗透率。但压力的提高总是有利于提高渗透浸渍质量,减少孔隙率。分析认为压力影响渗透高度的实质是渗透压力变化及纤维床的压实两种因素的共同作用结果。     

先进复合材料的CAE虚拟技术

国际先进复合材料技术目前的发展更倾向于利用虚拟的设计-制造-验证一体化环境,将真实的设计、制造、材料、验证、应用乃至维修和全寿命管理等诸多环节统一起来,从而最大限度地缩短新品研制周期,降低研制成本,提高产品的市场竞争力,在这个过程中,CAE技术已成为国防工业创新设计以及数字化设计、制造技术的核心之一。     

Discrimination of aqueous and aeolian paleoenvironments by atomic force microscopy-- a database for the characterization of martian sediments

In the search for aqueous habitats on Mars direct proof of (ancient) flowing water is still lacking, although remote sensing has provided indications of young fluvial systems. To demonstrate that such proof can be given, we examined surface marks on recent terrestrial sand grains by atomic force microscopy (AFM) and applied a quantitative three-dimensional analysis that can numerically distinguish between aeolian and aquatic transport mechanisms in sedimentary deposits on Earth. The surfaces of natural quartz grains as well as olivine, feldspar pyroxene, and monazite sands of known origin were imaged, each image yielding a three-dimensional map of the mineral surface. A fully automated analysis of distribution patterns of the structural elements that constitute the grain surfaces shows that wind-transported quartz grains have short linear elements irregularly distributed on the surface. Linear elements on water-transported grains, however, are longer with orientations that reflect the mineral symmetry. Because the surface patterns found on aqueous grains are due to preferential etching, they can be used as diagnostic fingerprints for the existence of past or present aqueous transport systems. We used a cluster analysis of the cross-correlation distance of distribution patterns in the structures of aeolian and aquatic sand grains to build a phenogram that provides a map for the relationship of the various sediments found on earth. The analysis shows that the method is highly significant and that water and wind transport can clearly be differentiated. In particular, feldspar and olivine sands contributed even more to the discrimination than quartz grains, which indicated that the method is promising for its application on future missions to Mars. Assuming that martian aqueous sand grains exhibit similar erosional patterns to mineral grains on Earth, simple AFM experiments on a Mars lander would be capable of proving the activity of flowing water in modern runoff systems and of analyzing the paleoenvironments of Mars.