全分集协作系统C-HARQ方案的设计及性能

为了进一步提高全分集协作(FDC)系统的可靠性和有效性,提出了两种协作混合自动请求重传(C-HARQ)方案.定长帧协作混合重传(FFC-HARQ)方案在不改变全分集协作系统原有帧结构的基础上,使用一定的检错重传策略提高系统吞吐量;变长帧协作混合重传(VFC-HARQ)方案则改变原有帧结构,进一步提高系统吞吐量.利用马尔...     

基于PLC和TD400C的建筑玻璃真空镀膜生产线电气系统控制

介绍了利用S7-200 CPU226和TD400C文本显示器友好人机界面构成真空镀膜生产线控制系统的组成、特点,程序编制及在应用中注意的问题.实现了建筑玻璃真空镀膜生产过程的自动化.     

油橄榄资源及育种研究现状

油橄榄是世界重要的经济作物,其果实既可以食用也可以榨取橄榄油.油橄榄原产地中海地区,现已在世界各地广泛种植.就其近年来国际上有关油橄榄传粉和坐果、品种鉴定的新途径,特别在育种技术方面的研究现状作一概述.     

基于真彩切片的MRI图片颜色迁移及三维重构分析

借助于可视人工程的真彩图片作为常用MRI、CT等灰度图片彩色化的颜色迁移的彩色特性源本,以MRI切片和真彩图片的亮度、纹理和几何作为映射间的配准参数而进行合理的颜色转换,以弥补医学灰度图片伪彩色方案中各组织非对应的彩色映射关系.通过真彩图片与灰色图片的亮度分布曲线的调整和纹理特征关系的调整和配准而到有效和符合真实人体器...     

安庆天柱山机场鸟类群落季节性变化与鸟击防范

在2008年2月至2009年2月间,对安庆天柱山机场及其周边地区的鸟类种类、种群数量进行了为期一年的调查.调查共记录到鸟类102种,隶属于12个目29个科,其中留鸟38种,占总数37.25%;夏候鸟28种,占总数27.45%;冬候鸟25种,占总数24.51%;旅鸟11种,占总数14.39%.在地理类型上,机场地区鸟类呈现古北界与东洋界过渡地带的特点,其中广布种37种,占总数36.27%;东洋界种类有34种,占总数33.33%;古北界种类31种,占总数30.39%.在机场及周边地区,春季观察到鸟类物种数要明显多于秋季及冬季,春季鸟类多样性也要高于秋季与冬季.在机场地区,每年5~6月份与10~11月份鸟类活动比较频繁.机场鸟击防范工作,应该根据鸟类活动特点,通过对重点区域栖息地的改造,降低生物多样性,从而减少鸟类在机场地区的活动,避免鸟击事件的发生.     

三维麦克斯韦方程的对称分裂时域有限差分方法能量守恒性分析

考虑三维电导率为零的麦克斯韦方程的对称分裂时域有限差分(SS-FDTD)方法的能量守恒性.通过新的能量方法与差分算子δx,δy,δz,笔者首次给出了数值逼近格式SS-FDTD在离散的H1模下的能量守恒式,并证明了格式在离散的H1模下的守恒性.数值算例验证了格式解的能量守恒性.     

信息熵的理解与验证

笔者在对信息熵原出处含义进行解读和对热力学熵原理进行理解的基础上,修正了信息量无限增加的理论解释.通过对计算机数据库中数据检索速度的测试,推导出速度公式,计算出每比特信息熵所需要的能量,发现实际数值与理论数值存在较大差异,得出布里渊的信息熵能量是信源与信道表面之间的熵变而非信源本身的熵变.     

Mitochondrial DNA variation analysis suggests extreme low genetic diversity in Guizhou snub-nosed monkeys （Rhinopithecus brelichi）

Guizhou snub-nosed monkey (Rhinopithecus brelichi) is a unique, endangered primate in China, mainly distributed in Fanjing Mountain National Natural Reserve, Guizhou Province, in an area of 275 km2. Recently, habitat loss and fragmentation have caused population isolation. To assess genetic diversity within this species and its population structure, we sequenced 400 bp of the hypervariable I segment from the mitochondrial DNA control region for 128 individuals. Only one haplotype was identified from these individuals. Compared with other primate species, R. brelichi can be regarded as a species with very low genetic diversity, which further adds to the conservation concern.     

Enhanced anti-sunward flow near local noon during a period of horizontal IMF and high solar wind velocity <Emphasis Type="Italic">V</Emphasis><Subscript><Emphasis Type="Italic">Y</Emphasis></Subscript>

It is believed that a southward interplanetary magnetic field (IMF) is mainly responsible for the energy input from solar wind into the magnetosphere. This paper presents an unusual case of strong anti-sunward plasma flow (up to 2 km/s) in the polar cap ionosphere and large cross-polar cap potential (CPCP) during a period of horizontal IMF (|B _Z | < 2 nT) observed by both ACE (at the L1 point) and Geotail (on the dusk flank of the magnetosheath). The CPCP is even higher than that under preceding B _Z ≈ −23 nT. Furthermore, GOES8 observed that the magnetosheath field turns northward as the anti-sunward plasma flow and CPCP start to increase, which implies that the magnetosheath field interacting with the Earth’s magnetopause has significantly rotated and differs from the IMF observed by ACE and Geotail. In accordance with previous theoretical work, we suggest that the magnetic field line draping produces a southward magnetosheath field and enhances anti-sunward plasma flow and the CPCP.     

Coral reef ecosystems in the South China Sea as a source of atmospheric CO<Subscript>2</Subscript> in summer

Field measurements of air-sea CO2 exchange in three coral reef areas of the South China Sea (i.e. the Yongshu Reef atoll of the Nansha Islands, southern South China Sea (SCS); Yongxing Island of Xisha Islands, north-central SCS; and Luhuitou Fringing Reef in Sanya of Hainan Island, northern SCS) during the summers of 2008 and 2009 revealed that both air and surface seawater partial pressures of CO2 (pCO2) showed regular diurnal cycles. Minimum values occurred in the evening and maximum values in the morning. Air pCO2 in each of the three study areas showed small diurnal variations, while large diurnal variations were ob-served in seawater pCO2. The diurnal variation amplitude of seawater pCO2 was ~70 μmol mol–1 at the Yongshu Reef lagoon, 420–619 μmol mol–1 on the Yongxing Island reef flat, and 264–579 μmol mol–1 on the reef flat of the Luhuitou Fringing Reef, and 324–492 μmol mol–1 in an adjacent area just outside of this fringing reef. With respect to spatial relations, there were large differences in air-sea CO2 flux across the South China Sea (e.g. ~0.4 mmol CO2 m–2 d–1 at Yongshu Reef, ~4.7 mmol CO2 m–2 d–1 at Yongxing Island, and ~9.8 mmol CO2 m–2 d–1 at Luhuitou Fringing Reef). However, these positive values suggest that coral reef ecosystems of the SCS may be a net source of CO2 to the atmosphere. Additional analyses indicated that diurnal variations of surface seawater pCO2 in the shallow water reef flat are controlled mainly by biological metabolic processes, while those of deeper water lagoons and outer reef areas are regulated by both biological metabolism and hydrodynamic factors. Unlike the open ocean, inorganic metabolism plays a significant role in influencing seawater pCO2 variations in coral reef ecosystems.