楔叶茶蔗（Ribes diacanthum Pall．）果实营养成分及其食用价值评价

对楔叶茶藤果实的营养成分进行测定。结果表明，其阴干果实富含糖、粗蛋白、粗脂肪、粗纤维、维生素C、维生素B1、维生素B2、维生素PP、维生素A、维生素E、胡萝卜素、10种矿质元素和18种氨基酸等丰富的营养物质,具有很高的食用价值，可以将其开发为内蒙古兼有经济和生态双重功能的乡土资源植物．     

内蒙古外来入侵植物的初步研究

运用野外调查和文献研究方法，对内蒙古自治区境内分布的外来人侵植物进行了初步研究．结果表明．内蒙古外来入侵植物共有22种，全部从国内其他地区扩散而来．从外来入侵植物在内蒙古的分布变化看．牛膝菊和光梗蒺藜草已表现出蔓延趋势．最后，对内蒙古外来入侵植物的深入研究提出建议．     

改进的粒子群优化算法结合人工神经网络用于有机物毒性的QSAR研究

介绍了粒子群优化算法和Alopex-B算法的基本原理,提出了一种用Alopex-B算法改进的粒子群优化算法,并将其应用于函数优化和有机物毒性的QSAR研究。结果表明:改进型粒子群算法对复杂的测试函数搜索效率明显提高,应用于有机物毒性的QSAR研究能提高计算的精确度,降低预测误差。     

射频PECVD方法生长含氢非晶碳膜的结构及摩擦学性能

利用射频等离子体增强化学气相沉积技术在不锈钢表面制备了含氢非晶碳膜.采用Raman光谱、红外光谱、X射线光电子能谱和原子力显微镜等研究了薄膜的微观结构和表面形貌,在栓盘摩擦磨损试验机上考察了薄膜在不同载荷与滑动速度下的摩擦学性能.结果表明:所制备的含氢非晶碳膜具有典型的类金刚石结构特征,薄膜均匀、致密,表面粗糙度小;薄膜与不锈钢球对磨时显示出良好的抗磨减摩性能;薄膜的抗磨减摩性能同对磨件表面上形成的转移膜以及摩擦过程中薄膜结构的石墨化相关.     

基于FPGA的信号滤波系统设计与实现

探讨了信号滤波的FPGA实现过程,在芯片内部设计DDS信号发生器和FIR滤波器两大电路功能模块,并利用EDA工具软件中所附带的嵌入式逻辑分析()出了滤波前后信号实时监测结果.相比于一般实现方法更高效和快捷.     

天然气成藏动力学机制发展趋势分析

目的研究天然气成藏机理与分布规律。方法国内外相关文献综合分析。结果对天然气成藏动力学机制的研究主要围绕背斜圈闭气藏(含上倾型构造及地层圈闭)、向斜圈闭气藏(深盆气圈闭)及煤层气藏(源内气藏)3类气藏进行,但是,研究的侧重点差别很大。其中,对背斜气藏的研究主要侧重天然气初次运移、二次运移、聚集及保存机制的研究,对向斜圈闭气藏的研究主要侧重于气水倒置形成、气藏异常压力形成机制的研究,而对煤层气藏的研究则主要侧重煤孔隙的形成、煤层气富集及保存机制研究。存在问题:其一,把背斜气藏和向斜气藏当成两种成藏动力学机制完全不同的气藏类型,其动力学依据不充分;其二,没有解决气源岩内天然气初次运移机制和聚集机制的矛盾。结论建议应加强两方面的研究:其一,以盆地升降运动为动力学基础,研究天然气成藏的动力学机制;其二,以烃源岩—断裂—储气层为基本输导格架,研究不同输导介质中天然气成藏的动力学机制。上述研究有望解决不同类型天然气藏形成动力学存在的问题。     

体育教育专业大学生的专业承诺研究

运用科学的心理研究方法对当前体育教育专业大学生四年学习历程和心理历程进行实证研究,实现了对现象从归纳总结到定性定量研究的转变.本研究主要以专业承诺为核心,以大学生的理想信念、前途和规范准则三方面为主线展开,并对研究结果进行科学合理的解释,为学校管理、大学生心理健康和就业指导,甚至于为高校以人为本的教育教学改革提供参考数据.     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.     

聚噻吩衍生物的结构和在金属表面取向的NEXAFS研究

采用电化学方法将噻吩衍生物[3-(2-甲氧基苯)噻吩和3-溴代噻吩]聚合沉积到Pt片上,利用同步辐射光源采集聚噻吩衍生物中C的近边X射线吸收精细结构(NEXAFS)谱,以特征吸收峰强度对光的入射角度的依赖性为判据,实验证明了聚噻吩衍生物分子在金属表面的分子取向.由于噻吩环上取代基团电负性的差异,分子在衬底表面的取向有所不同:聚3-(2-甲氧基苯)噻吩无序的堆积在Pt表面,聚3-溴代噻吩倾斜于金属Pt表面.     

Test of magnetic susceptibility and grain-size age models of loess

Ages of the stratigraphic boundary MIS1/2 and MIS3/4 of the Yuanbu loess section in Linxia are used as the basis of the nodal control age. The age of MIS1/2 and MIS3/4 are obtained from the latest international research result—the climatic events recorded in the stalagmite in the Hulu Cave in Nanjing, that MIS1/2 is 11.5 kaB.P. and MIS3/4 is 59.8 kaB.P.. The ages of the two climatic events contain three nodal age control models (Model 1: 0 kaB.P.—59.8 kaB.P.; Model 2: 0 kaB.P.—11.5 kaB.P. and 11.5 kaB.P.—59.8 kaB.P.; Model 3: 11.5 kaB.P.—59.8 kaB.P.), which are used as the nodal control age separately. The deposition times of various stratigraphic horizons are calculated by using the magnetic susceptibility age model and grain-size age model, and then compared with each other. In addition, the AMS14C age, OSL age and the ages of YD and H events are compared with the ages of the corresponding horizons calculated by the three models of nodal control ages. From the analyses of lithologic characters and climatic stages it has been found that both the magnetic susceptibility age model and the grain-size age model have some defects. Because the accurate control ages are selected as the nodal points of the glacial period or interglacial period, the stratigraphic deposition times determined by the high resolution of magnetic susceptibility age model and grain-size age model approximate to the actual ages. As for the relative accuracy of the two age models, the magnetic susceptibility age model is more accurate than the grain-size age model.