组合逻辑电路的无反变量输入设计

本文阐述了组合逻辑电路无反变量输入的设计思想，并通过设计实例给出了具体的设计方法与步骤．     

清末政治制度的转型

鸦片战争以后，西方列强的侵略不仅使满清王朝颜面扫地，也动摇了中国传统政治制度的威信，打乱了它固有的发展轨迹。在外来政治制度的影响下，中国传统政治制度开始了向现代转型。这一转型大致经历了三个阶段：即洋务运动时期传统政治制度的动摇、戊戌变法时期西方政治制度的宣传、清末新政时期新式政治制度的起步三个阶段。尽管这一转型才刚刚开始，取得的成效也极为有限，但对其后中国政治制度的现代化却产生了极为重要的影响。     

The age of formation of the mirabilite and sand wedges in the Hexi Corridor and their paleoclimatic interpretation

The Hexi Corridor is located at the transition zone of the Asian summer monsoon and westerly airflow, and lies in an important position in terms of its ecological fragility and climatic sensitivity. During a recent field expedition to this region, we found a sedimentary mirabilite layer in a number of localities including Suwushan, Yanchi, Baitujing, Yanchi Gaotai, Huahai, Yumen, Halanuo扙r, and Dunhuang (Fig. 1), which have the potential to provide important information about environmenta…     

Temperature variations on the Tibetan Plateau over the last two millennia

The paleoclimate data recovered from ice cores,tree rings and lake sediments indicate regional features of cfimatic change on the Tibeta n Plateau (TP) during the last 2000 years. The composite temperature reconstructions in-dicate that several main climatic episodes, such as the “LittleIce Age“ between 1400 and 1900, the “Medieval Warm Pe-riod“ in 1150-1400, a less warm period in 800-1100, and an earlier cold period between the 3rd and 5th centuries,occurred in the TP. In addition, temperature varied from region to region. The period from AD 800 to 1100, which waswarm in northeastern TP, was contemporaneous with cool-ing in the western and southern TP. The southern TP ex-perienced warming between 1150 and 1400. For western TP,the δ^18O records of the Guliya ice core indicate that the pe-Hod 1250-1500 witnessed a clear warming. Large-scaletrends in the temperature history from northeastern TP aremore similar to those in eastern China than are the trendsfrom the Guliya ice cap far to the west and southern TP. The most prominent similarities between the temperature varia-tions of the TP and eastern China are such cold phases as 1100-1150, 1500-1550, 1650-1700 and 1800-1850, andthe latter three cold events match with three widespreadg lacial advances which occurred on the TP during the Little Ice A2e.     

"纲要信号"教学法在掷标枪最后用力技术教学中的应用研究

利用教学实验法将“纲要信号”教学法与传统教法进行了对比性教学实验,并对教学实验的结果利用录像解析、数理统计等方法进行了统计分析。结果表明,与传统教法相比教学效果明显。     

计算机图形学网络课程的开发与评价

对现代网络课程的定义、功能与分类进行了简要介绍.着重讨论了计算机图形学网络课程的开发与评价,并给出了一个具体的评价指标体系.最后提出了几点建议.     

末次间冰期全球变化区域响应的粒度旋回———萨拉乌苏河流域米浪沟湾剖面记录

位于毛乌素沙漠东南的萨拉乌苏河流域米浪沟湾剖面末次间冰期层系记录了8．5个古风成砂与河湖相和古土壤构成的显著的粗细韵律交替变化粒度旋回．通过对不同沉积相粒度的一般分布特征尤其是粒度参数-Mz、σ、Sk、Kg和SC／D值以及该地生物化石指示的古环境综合分析，认为所述粒度旋回主要是东亚冬夏古代季风交替影响下的气候旋回波动所致。     

r-首尾和循环线性方程组的求解

引入r-首尾和循环矩阵的新概念,利用多项式矩阵理论,给出求解r-首尾和循环线性方程组的快速算法.     

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.     

求周期序列线性复杂度的快速算法

基于有限域GF(q)上的分圆多项式理论,提出和证明了求周期为qnpm的GF(q)上序列的线性复杂度和极小多项式的一个快速算法,这里p与q均为素数,且q是模p2的本原根.该算法既推广了求周期为pm的GF(q)上周期序列的线性复杂度的一个快速算法,也推广了求周期为2npm的二元周期序列的线性复杂度的一个快速算法.