三角矩阵余代数上的倾斜余模

基于经典的同调代数方法,通过研究三角矩阵余代数上的倾斜内射余模,得到三角矩阵余代数的右倾斜整体维数的上、下界。     

“盗窃符号”类别、特点及理论性分析初探

随着我国盗窃犯罪日渐专业化,"盗窃符号"开始在社会中广泛显现,并日益威胁着社会治安与居民安全感。对"盗窃符号"的概念进行了类别划分,总结出"盗窃符号"具有总体数量多、增长趋势明显、城市间差异大、区域性明显、隐蔽性高这五个特点。结合犯罪社会学相关理论进行分析,发现其反映出理性选择理论与日常活动理论的丰富内涵,并显现出犯罪专业化的趋势,提出了相关的防控对策。     

用小波变换和奇异指数表征蔡氏混沌信号键带

计算了蔡氏电路混沌信号的离散二进小波变换及奇异指数，结果发现，当尺度2∧5上的小波变换结果的模大于某一阈值时，其所对应的信号段就是键带，在混沌信号的键带处，奇异指数限大的正值，而在非键带处，奇异指数取负值或小的正值。     

Research on catalysis of sodium-metallochlorophylls in Ni/MH battery

The effects of sodium-metallochlorophylls including sodium-iron chlorophyllin, sodium-copper chlorophyllin and sodium-magnesium chlorophyllin on performance of Ni/MH battery were investigated. The results show that sodium-iron chlorophyllin can effectively activate the gases produced during charge in Ni/MH battery, therefore reducing the reduction potential of oxygen and the oxidation potential of hydrogen, and the increased speed of inner pressure of battery is decreased significantly. With the aid of DMol3 software, the activation process of oxygen and hydrogen by sodiummetallochlorophylls was simulated and analyzed. It was found that the catalysis behavior is in agreement with the experimental results, and the activation process also gets a reasonable explanation from the calculated results.     

有机磷农药与牛血清白蛋白的相互作用及分析应用

应用荧光光谱、同步荧光光谱和紫外吸收光谱研究了3种有机磷农药(敌百虫、乐果和甲基对硫磷)与牛血清白蛋白(BSA)的相互作用.实验表明敌百虫和甲基对硫磷与BSA的相互结合作用是单一静态猝灭过程,而乐果与BSA的相互结合作用是静态为主、动态为辅的猝灭过程.首次发现有机磷药物与BSA结合作用同药物疏水性直接相关:随着有机磷药物疏水性增大,猝灭常数KSV增大、BSA构象改变增大、药物与BSA的结合距离减小.有机磷药物与BSA的结合作用随着有机磷疏水性增强而增加.基于蛋白质与有机磷的结合作用研究,初步探讨了水产品中有机磷药物残留的提取方法,并利用气相色谱法检测了水产品中乐果和甲基对硫磷的含量,方法的回收率为85.71％～107.21％.该方法准确度高、简单、快速.     

钢铁企业轨梁万能生产线仿真建模

针对钢铁企业的轨梁万能生产线在生产中存在的新产品调试生产周期过长、生产瓶颈不易诊断、设备利用率低等问题,分析了钢铁企业轨梁万能生产线不同于传统离散制造以及流程制造过程的特点,在此基础上建立了半连续半离散的轨梁万能生产线的Petri网模型和各设备的仿真组件模型,开发了轨梁万能生产线的仿真系统,并用一个实际的工程应用案例,验证了该仿真模型及其系统的可操作性以及有效性,达到了提高生产现场轨梁万能生产线的生产效率和产能的目的.     

Response of the northwestern Pacific upper water δ~(13)C to the last deglacial ventilation of the deep Southern Ocean

The deglacial δ~13C minimum events that originated from the ventilation of the deep Southern Ocean around Antarctica, have been recorded in a range of marine sediments from the southern to tropical oceans in late Pleistocene. However, the broad δ~13C minimum event was also reported as far as to the northern middle latitudes, in northwestern Pacific marginal sea areas, during the last deglaciation. In the northwestern Pacific, forcing from the northern high latitudes is strongly expressed, while the records of in- fluence from the southern high latitudes are few. The Kuroshio Source Region (KSR) forms a boundary between the northwestern Pacific and the southern, tropical Pacific. So, high-resolution planktonic foraminiferal records in core MD06-3054 from the KSR are well positioned to identify signals from the southern hemisphere in the northwestern Pacific. Planktonic foraminiferal tests from the upper 1030 cm of the core were subject to AMS14C, carbon and oxygen isotopic measurements. A negative excursion was found to occur from about 20.0-6.0 ka BP in δ~13C records of both surface (Globigerinoides ruber) and subsurface (Pulleni- atina obliquiloculata) dwellers, but the overall trends of the two curves have reversed since 26.5 ka BP. Moreover, the δ~13C rec- ord of G. ruber (the surface dweller) shows a robust link to the record of atmospheric CO2, and its changes precede the records of P. obliquiloculata (the subsurface dweller). According to the hydrologic conditions, the broad δ~13C minimum event recorded in the KSR is also a response to the increasing ventilation of the deep Southern Ocean around Antarctica during the last deglaciation. The inconsistency between the records of the surface and subsurface dwellers was possibly caused by the ways that the low δ~13C signal was transmitted. Subsurface water primarily received the low δ~13C signal from the Antarctic Intermediate Water (AAIW), whereas the surface water was probably mainly impacted by atmospheric CO2 in the KSR. The records from the KSR confirm the deduction that the broad δ~13C minimum event in the Okinawa Trough was due to the impact of tropical Pacific surface water dur- ing the last deglaciation, and suggest that signals from the southern high latitudes also can be delivered to the northern middle latitudes.     

海洋粘土矿物的古环境含意辨析

粘土矿物组合反映了源区气候冷、暖周期性变化,记录了沉积区域古环境演化的重要信息,为古环境重塑提供了有力证据.但沉积岩中粘土矿物组合及含量变化用于古气候的解释目前尚存在一定的局限性和复杂性,例外情况时有发生.各种非气候因素,如源区、沉积环境、成岩作用、差异输送、自生作用,影响粘土矿物的分布和含量,使粘土矿物的古气候含意变得错综复杂.可能只有当沉积盆地很小或者是陆盆,沉积物中的粘土矿物对古气候才可能是有用的指示器.比较大的沉积盆地,尤其是海盆,是从遥远的源区接受岩屑载荷的,代表了一种多样化的环境条件.重组的距离越长,扩散过程越复杂,沉积的粘土矿物组合古气候信息越不清晰.粘土微粒要经过一个长距离才能从土壤到达海洋,因此沉积学家和古气候学家应该多注意土壤和沉积粘土矿物之间关系的复杂性.目前海洋粘土组合的古气候解释,可能代表一种相当宽泛的古气候信息或提供了所有气候影响的整合记录.