极尖区电离层离子与地磁活动及太阳风的相关分析

对2001~2003年间Cluster星簇穿越极尖区期间观测到的电离层起源的离子(O⁺离子, He⁺离子和H⁺离子)特性进行了统计分析, 主要研究了这些离子的数密度与地磁活动以及太阳风动压之间的关系. 结果表明: O⁺离子数密度和地磁活动指数Kp之间存在着正相关关系, He⁺离子数密度和地磁活动指数Kp不相关, O⁺离子和He⁺离子数密度都和太阳风动压之间存在着显著的正相关关系; H+离子数密度与太阳风动压之间存在着正相关关系, 而和地磁活动指数Kp不相关. 最后, 对这些离子的特性与太阳风动压及地磁活动之间的关系进行了讨论.     

美国东北部早熟和晚熟玉米杂交种年际间产量稳定性

玉米是美国东北部奶牛业的主要能量来源，杂交种的选择是提高玉米产量、降低生产成本的关键和前提。连续5年在美国麻省大学农学实验站的典型砂壤土耕地上进行试验，结合当地气象部门提供的生育期间玉米的生长期生长度日数和降雨量，对3个早熟杂交种和3个晚熟杂交种的产量进行了年际间稳定性比较。结果表明：产量与年际间气候条件无关，无论是青贮饲料产量还是穗棒产量，晚熟品种的产量均高于早熟品种（2001年杂交种E409L）。5年平均晚熟品种的青贮饲料产量和穗棒产量分别比早熟品种高出10．9％和8．0％。相同年份品种间产量存在差异，同一品种年际间产量差异显著。低温年份，相对冷凉的生育前期和温热的生育后期不利于美国东北部玉米生产。生育期间较高的降雨量有利于青贮产量的形成。选择种植晚熟品种是该区农民提高玉米产量、降低生产成本的有效途径。只有热量多且雨量充沛的年份才有利于玉米产量潜力的挖掘。有关某种玉米基因型对当地气候适应性方面的知识，将有利于育种者选择有价值的种质资源。表6，参17。     

INFORMATION CHARACTERIZATION OF COMMUNICATION CHANNELS FOR SYSTEM IDENTIFICATION

This paper studies identification of systems in which the system output is quantized, transmitted through a digital communication channel, and observed afterwards. The concept of the CR Ratio is introduced to characterize impact of communication channels on identification. The relationship between the CR Ratio and Shannon channel capacity is discussed. Identification algorithms are further developed when the channel error probability is unknown.     

The Classification of States for Markov Chain in Random Environments and m-irreducible

First of all,we introduces the concept of m-irreducible of Markov chain in random environment. Then under the condition of m-irreducible,the relationship of recurrent and positive recurrent between two states is studied. We also give several conditions that can imply a state is recurrent and positive recurrent. And then the period of a state is discussed and we obtained that under the condition of m-irreducible,for any two states in X ,they have the same period.     

Watching cartoons activates the medial prefrontal cortex in children

The medial prefrontal cortex (MPFC) of human adults is involved in attributing mental states to real human agents but not to virtual artificial characters. This study examined whether such differential MPFC activity can be observed in children who are more fascinated by cartoons than adults. We measured brain activity using functional magnetic resonance imaging (fMRI) while 10-year-old children watched movie and cartoon clips, simulating real and virtual visual worlds, respectively. We showed neuroimaging evidence that, in contrast to adults, the MPFC of children was activated when perceiving both human agents and artificial characters in coherent visual events. Our findings suggest that, around the age of 10 years, the MPFC activity in children is different from that in adults in that it can be spontaneously activated by non-human agents in a virtual visual world.     

农村流通体系建设:现状、问题与政策建议

改革开放30年来,我国农村市场体系建设取得重要进展,主要表现在农村市场规模不断扩大、交易方式和流通业态逐步提升、农村市场主体呈多元化格局。目前,我国农村市场流通仍存在比较突出的问题。建议强化农村流通基础设施建设,发展现代流通方式和新型流通业态,培育多元化、多层次的市场流通主体,构建开放统一、竞争有序的农村市场体系。     

Electronic Properties of Organic Semiconductors Based on Nonconjugated Polymers

1 Results The paper presented review of experimental results on the charge transport study in the polymer materials,possessed charge instability.The base of these materials is noncojugated polyaromatic compounds.Characteristic feature these materials is a wide of band gap up to 4.3 eV and the value of first ionization potential about 6 eV.Electronic energetic parameters like these are typical for insulator materials.However it was established that there are not only hopping mechanism of charge transport possible but coherent too in such organic systems.Wide band gap organic material capable to transport charge carrier effectively under certain conditions and the same time conductivity can reach 105 (Ohm·cm)-1 value and current density up to 106 A/cm2 and more.Transformation to conducting phase may occur with different fields and influences,such as electric field,magnet field,pressure,temperature and others.These transformations are reversible as a rule.There is three main of the phenomena fields may be emphasize: electro-optical,switching,and electronic phenomena,including nanophenomena.Electro-optical phenomena are electroluminescence first of all[1].Switching phenomena unites as following switching induced by electric field[2],pressure[3],magnet field[4],boundary condition changing[5],traps thermoionization[6],particle irradiation[7].Electronic phenomena which can observe in thin polyarylide films are as follow electron cold emission[8],superconductivity[9],charged induced nanomemory[10],quantum dot generation[11].     

Field trial of an HTS filter system on a CDMA base station

This paper presents the field trial results of a high temperature superconductor filter system (HTSFS) in a code division multiple access (CDMA) mobile communication base station (BTS) in Tangshan, China. The center frequency of the HTSFS is 830 MHz with 1.4% fractional bandwidth. The noise figure (NF) of the HTSFS, including connectors and cables, is 0.8 dB. The field trial results show that after the HTSFS was installed in the receiver front-end of a CDMA base station, the transmitting power of handset was decreased by 3.1 dB on average. Up to now, the HTSFS has been running steadily in the base station for more than 22 months, demonstrating the reliability and stability of the system.     

When and how did plate tectonics begin？ Theoretical and empirical considerations

Plate tectonics is the horizontal motion of Earth’s thermal boundary layer (lithosphere) over the convecting mantle (asthenosphere) and is mostly driven by lithosphere sinking in subduction zones. Plate tectonics is an outstanding example of a self organizing, far from equilibrium complex system (SOFFECS), driven by the negative buoyancy of the thermal boundary layer and controlled by dissipation in the bending lithosphere and viscous mantle. Plate tectonics is an unusual way for a silicate planet to lose heat, as it exists on only one of the large five silicate bodies in the inner solar system. It is not known when this mode of tectonic activity and heat loss began on Earth. All silicate planets probably experienced a short-lived magma ocean stage. After this solidified, stagnant lid behavior is the common mode of planetary heat loss, with interior heat being lost by delamination and “hot spot” volcanism and shallow intrusions. Decompression melting in the hotter early Earth generated a different lithosphere than today, with thicker oceanic crust and thinner mantle lithosphere; such lithosphere would take much longer than at present to become negatively buoyant, suggesting that plate tectonics on the early Earth occurred sporadically if at all. Plate tectonics became sustainable (the modern style) when Earth cooled sufficiently that decompression melting beneath spreading ridges made thin oceanic crust, allowing oceanic lithosphere to become negatively buoyant after a few tens of millions of years. Ultimately the question of when plate tectonics began must be answered by informa- tion retrieved from the geologic record. Criteria for the operation of plate tectonics includes ophiolites, blueschist and ultra-high pressure metamorphic belts, eclogites, passive margins, transform faults, paleomagnetic demonstration of different motions of different cratons, and the presence of diagnostic geochemical and isotopic indicators in igneous rocks. This record must be interpreted individually; I interpret the record to indicate a progression of tectonic styles from active Archean tectonics and magmatism to something similar to plate tectonics at ~1.9 Ga to sustained, modern style plate tectonics with deep subduction——and powerful slab pull——beginning in Neoproterozoic time.     

Recent temperature increase recorded in an ice core in the source region of Yangtze River

Interests on climate change in the source region of Yangtze River have been raised since it is a region with the greatest warming over the Tibetan Plateau (TP). A 70-year history of precipitation δ~(18)O has been recovered using an ice core record retrieved in a plat portion of the firn area in the Guoqu Glacier (33°34′37.8″N, 91°10′35.3″E, 5720 m a.s.l.), Mt. Geladaindong (the source region of Yangtze River), in November, 2005. By using a significant positive relationship between ice core δ~(18)O record and summer air temperature (July to September) from the nearby meteorological stations, a history of summer air temperature has been reconstructed for the last 70 years. Summer temperature was relatively low in 1940s and high in 1950s to the middle of 1960s. The lowest temperature occurred in the middle of 1970s. Temperature was low in 1980s and dramatically increased since 1990s, keeping the trend to the begin-ning of the 21st century. The warming rate recorded in the ice core with 0.5℃/10 a since 1970s is much higher that that in the central TP and the Northern Hemisphere (NH), and it becomes 1.1℃/10 a since 1990s which is also higher than these from the central TP and the NH, reflecting an accelerated warm-ing and a more sensitive response to global warming in the high elevation region.