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.     

基于邻域粗糙集的不完整决策系统特征选择算法

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宽带认知无线电网络分布式协作压缩频谱感知算法

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深基坑出碴方案比选

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一类离散时滞系统的极小极大鲁棒控制

针对一类离散时滞系统设计有记忆的状态反馈控制器,使得在最坏的干扰和不确定性下,闭环系统渐近稳定且性能指标存在一个最小上界.给出离散时滞系统的极小极大控制定义,利用李亚普诺夫方法和线性矩阵不等式(LMI)方法给出了极小极大鲁棒控制器的存在条件和设计方法.通过建立、求解凸优化问题得到最优极小极大控制器参数和性能指标的最小上界.最后给出数值算例,说明所设计的极小极大控制器只需付出较小的代价成本就能很好地抑制干扰.     

4WS车辆μ综合鲁棒主动侧倾操纵性能控制

为提高车辆的抗侧倾性能及降低高速下的侧翻危险性,应用μ综合鲁棒控制理论,针对四轮转向车辆,以横摆角速度跟踪和侧倾角速度反馈为控制逻辑,合理选择加权函数,设计鲁棒控制器和最优控制器抑制车辆侧倾.经仿真比较,设计的μ综合鲁棒控制器更具有良好操纵性能鲁棒性和稳定鲁棒性,对于轮胎侧偏刚度等引起的侧向干扰具有很好的抑制性能,实现传统四轮转向难以实现的主动侧倾操纵控制和跟踪性能.     

基于 Rough Set理论的商务决策支持系统知识发现的研究

以商务决策作为研究背景,基于Rough Set理论解决商务决策支持系统中信息不确定,数据量大的困难.从Rough Set理论的基本概念出发,给出决策表的知识表达系统,提出计算最小决策规则的算法,最后通过运用Rough Set理论和方法对商务决策支持系统的实例进行属性及属性值的约简,挖掘其中隐含的知识,从而得出最小决策规则.     

沧州高盐环境嗜盐放线菌多样性研究

利用NaCl的质量分数为10%和20%的不同培养基从35份采自河北沧州高盐环境样品中分离得到33株中度嗜盐放线菌和13株耐盐放线菌.多相分类研究表明,嗜盐菌株具有形态、生理、生化和分子分类特征的多样性,在系统发育上试验菌株分别属于拟诺卡氏菌属、链霉菌属和纤维单胞菌科一新属.分析结果表明,沧州地区高盐环境中嗜盐放线菌主要类群是拟诺卡氏菌属和链霉菌属,另有少量纤维单胞菌科放线细菌;也说明高盐环境是分离新物种的重要来源.     

地黄属资源植物中梓醇的分布及积累动态

采用液质联用（HPLC-UV-MS）法对同地栽培的地黄属各物种中梓醇的分布及积累规律进行了检测.研究发现地黄属6种植物都含有丰富的梓醇成分,茄叶地黄、高地黄和裂叶地黄梓醇含量较高,接近于地黄中梓醇的含量.并发现地黄属植物块根中梓醇含量高峰在入冬前的成年期,而地上部分梓醇含量高峰在越冬后的开花结实期.在各物种内,地上部分梓醇含量通常高于地下部分,粗壮和木质化程度低的块根中高于纤细和木质化程度高的块根中.探讨了地黄属资源植物的应用前景和梓醇分布和积累规律的形成原因.     

基于PCA和相位差校正法的风切变预警算法

为了提高相干激光雷达风切变预警算法的预警率,提出一种基于主成分分析（principal component analysis,PCA）和相位差校正法的风切变预警算法。首先,利用PCA对雷达回波信号进行低阶主成分向量提取以实现信号重构,提高信噪比。其次,采用基于快速傅里叶变换的相位差校正法对回波信号峰值频率进行校正,降低回波信号能量泄露。然后,分别利用旋转电机实验数据和小型飞机实验数据对所提算法进行性能评估。结果表明,采用所提算法估计相干激光雷达回波信号峰值频率的平均绝对误差为0.26 MHz,对实际低空风切变的预警率为92.31%。所提算法可以有效降低相干激光雷达回波信号频率估计误差,实现低空风切变预警。