一种基于正则化模型的Dai-Liao共轭梯度法

给出一种基于正则化模型的Dai-Liao共轭梯度法.首先,通过极小化3次正则化模型,得到新的Dai-Liao参数t,并在此基础上根据函数在迭代点附近的性质,产生一个自适应的Dai-Liao参数;其次,结合改进的Wolfe线搜索,提出一种基于正则化模型的Dai-Liao共轭梯度法;最后,证明该算法的搜索方向满足充分下降性,并在一般假设下建立该算法的全局收敛性.数值结果表明该算法有效.

Li过量的层状结构锂离子电池材料Li_(1+x)M_(1-x)O_2(x≥0)——I.LiAO_2-Li_2BO_3(A=Co,Ni,Cr·…;B=Mn,Ti…)固熔体材料

设计和研发锂过量层状Li1+xM1-xO2(M是一种或一种以上的过渡金属元素,x≥0)锂离子电池正极材料成为研究热点。此类材料展示不同寻常的电化学性能,如高比容量、优秀的循环能力以及新的电化学充放电机制。简单介绍此类材料的结构定义,结合我们的研究结果,着重综述了近几年LiAO2-Li2BO3(A=Co,Ni,Cr…;B=Mn,Ti…)固熔体锂过量层状材料的研究现状和发展趋势。

鼠尾伤害性刺激与颧Liao穴电针后弓状核—导水管周围灰质—延髓头端腹？…

成年ＳＤ大鼠分成对照，尾部电流所致伤害性刺激，面部颧Ｌｉａｏ穴电针三组，分别观察弓状核，中脑中央灰质和延髓头端腹内侧区原位杂交后在神经元中前脑啡肽原（ＰＰＥ）ｍＲＮＡ的表达与Ｆｏｓ免疫阳性神经元的分布，痛刺激后上述各部位的ＰＰＥｍＲＮＡ在神经元内均有不同程度表达，但当颧Ｌｉａｏ穴电针时表达更明显，细胞数也较多。尤其在延髓头端腹内侧区更显著，而在对照动物仅有面神经核等与运动有关核闭出现表面。

具有时滞的Liao混沌神经元系统的自适应同步

针对一类具有时滞的部分参数未知的Liao混沌神经元系统,研究不同结构时滞Liao混沌神经元系统的自适应同步问题.基于Lyapunov稳定理论,给出了自适应控制器的设计方法及参数自适应律的解析表达式.所设计的控制器实用有效,易于实现,能够使具有时滞的两个不同结构的Liao混沌神经元系统渐近同步.仿真示例验证了该方法的有效性.

基于Liao氏吸收边界条件的四阶FDTD算法

建立了在空间上用四阶差分的时域有限差分法的 L iao氏吸收边界 ,证明了四阶差分具有比二阶差分更小的数值色散 .空间上用四阶差分的时域差分法将有助于人们对尺寸较大的物体如光纤等光波导的数值分析 .

Identification and Genetic Diversity Analysis of Chinese Mitten Crab(Eriocheir sinensis) in the Liao River Area

Chinese mitten crab （Eriocheir sinensis） is an indigenous and ecologically and economically important species in the Liao River area, but its identification and genetic diversity remain poorly understood. To evaluate the germplasm resources of this species, samples were collected from these locations： four sub-populations from the Liao River area and one population from the Yangtze River area; one primer was used to distinguish between the Liao River and the Yangtze River crabs. Thirteen loci were used for crab genetic diversity analysis, and basic statistics showed that the collecting samples were purebred in the Liao River area. The average observed heterozygosity （H0） of the Liao River population was 0.5931, and the expected heterozygosity （He） was 0.8064. The polymorphism information content （PIC） was 0.7753, which showed that the Liao River population had high genetic diversity. The genetic differentiation index （FST） averaged 0.0342, meaning a low degree of differentiation; cluster analysis indicated that Hujia （HJ）, Xinli （XL） and Chenjia （CJ） sub-populations were allocated to the same cluster, while Baqiangzi （BQZ） sub-population was isolated. In summary, these data demonstrated that the crabs in the Liao River had high genetic diversity, but low genetic differentiation. Thus, the Liao River population had the potential for breeding selection. Furthermore, this study also provided valuable genetic information for the conservation of Chinese mitten crab.

Geological Features of Triassic Alkaline and Subalkaline Igneous Complexes in the Yan-Liao Area

A number of Triassic (245-195 Ma) alkaline or subalkaline igneous complexes were discovered in theYan-liao area in the northern part of the North China platform. These complexes are all poor in SiO_2; most ofthem are rich in Fe, Mg, K and P and such incompatible elements as Rb, Ba, U and Sr and REE; theinitial ^(87)Sr / ^(86)Sr ratios range from 0.7055 to 0.7057. They might have originated in the altered upper mantle.On that basis coupled with the distribution of the Triassic System and the tectonic deformation, it is suggestedthat there should have existed a tectono-magmatic belt in the area in Triassic time, which is an important mani-festation of the Indosinian movement in the area.

Geochemistry, Geochronology, and Hf isotopic Composition of the Late Paleoproterozoic Lujiapuzi Formation,NE Yan-Liao Rift, Northern Liaoning

The metasedimentary Lujiapuzi Formation crops out along the northeastern margin of the North China Craton, close to the Yan-Liao Rift. The age and tectonic setting of the formation, and its relationship with the Yan-Liao Rift are currently unclear. Here we present detrital zircon U-Pb ages, and Hf isotopic and geochemical data for the Lujiapuzi Formation to constrain the timing of deposition, the provenance of the formation, and the regional stratigraphy relationship. Zircon U-Pb dating constrains the timing of deposition of the Lujiapuzi Formation to younger than 1780 Ma, and indicates that most grains were sourced from the Longgang Block and the Paleoproterozoic Liao-Ji Belt. Detailed field investigations and a correlation of the regional stratigraphy reveal that much of the Lujiapuzi Formation is equivalent to the Tuanshanzi Formation in the Yan-Liao Rift; the lower section may represent the earliest sediments deposited within the Fanhe Basin. Based on these results and the findings of previous studies, we suggest that the base of the Changcheng System has an age of 1.80 Ga. Zircon Hf isotopic data indicate that the main period of crustal growth along the northeastern margin of the North China Craton occurred at 3.2–2.5 Ga, with a peak at 2.9–2.7 Ga.

Paleoproterozoic Granitoids on Liaodong Peninsula, North China Craton

Paleoproterozoic granitoids are an important constituent of the Jiao-Liao-Ji Belt(JLJB). The spatial-temporal distribution and types of Paleoproterozoic granitoids are closely related to the evolution of the JLJB. In this paper, we review the field occurrence, petrography, geochronology, and geochemistry of Paleoproterozoic granitoids on Liaodong Peninsula, northeast China. The Paleoproterozoic granitoids can be divided into pre-tectonic(~2.15 Ga;peak age=2.18 Ga) and post-tectonic(~1.85 Ga) granitoids. The pre-tectonic granitoids are magnetite and hornblende-biotite monzogranites and granodiorites. Pre-tectonic monzogranites are widespread in the JLJB and have A2-type affinities. In contrast, pretectonic granodiorites are only present in the Simenzi area and have adakitic affinities. The post-tectonic granitoids consist of porphyritic monzogranite, syenite, diorite, granodiorite, quartz monzonite, monzogranite, and granitic pegmatite, which are adakitic rocks and I-, S-, and A2-type granitoids. The assemblage of pre-tectonic A2-type granitoids and adakitic rocks indicates the initial tectonic setting of the JLJB was a continental back-arc basin. The assemblage of post-tectonic adakitic rocks and I-, S-, and A2-type granitoids indicates a post-collisional setting. The 2.20-2.15 Ga A2-type granitoids and adakitic rocks were associated with the initial stage of back-arc extension, and the peak of back-arc extension is inferred from the subsequent(2.15-2.10 Ga) mafic intrusive activity. The ~1.90 Ga adakitic rocks mark the beginning of the postcollisional stage, which was followed by the intrusion of low-temperature S-and I-type granitoids. High-to low-pressure granitoids(S-type) were generated during the peak of post-collisional lithospheric delamination and asthenospheric upwelling. The emplacement of later granitic pegmatites occurred during the waning of the orogeny.

Thermochronology of Mesozoic Sandstone from the Beipiao Basin and Its Implication to Meso-Cenozoic Tectonic Evolution of the Eastern Yan-Liao Orogenic Belt

Combining the single-grain low-temperature apatite fission track with high-temperature zircon U-Pb dating of sandstone can better reveal the temporal association between the source and depositional site, and identify both the age component of the source terrain and subsequent thermo-tectonic events after deposition. This paper introduces the single- grain zircon U-Pb dating and fission track (FT) dating of sediments from the Beipiao basin in Northeast China. The U-Pb ages of 18 single zircon grains collected from the early Jurassic Beipiao Formation range from 194.3±2.9 to 233.8±4.2 Ma and most of apatite FT ages are about 30-40 Ma, indicating that the eastern part of the Yan-Liao orogenic belt experienced an obvious tectonic seesawing during Meso-Cenozoic time. The eastern part of Liaoning Province (the Liaodong block) uplifted in the early Mesozoic (230-190 Ma) and formed a geological landscape of high mountains, while the western part of the province (the Liaoxi area) subsided relatively and thousand-meter-scale sediments were deposited. During the Cenozoic (30-40 Ma), the Liaoxi area uplifted as a whole, and the Xialiaohe Basin sank intensively. The topographic landscape had a great change: high mountains in the west and east of Liaoning Province and low plains in the central area.

Chaos control and reduced-order generalized synchronization for the Chen-Liao system

This paper deals with the problem of chaos control and synchronization of the Chen-Liao system. From rigorous mathematic justification, the chaotic trajectories of the Chen-Liao system are led to a type of points whose fourdimensional coordinates have a particular functional relation among them. Meanwhile, a new synchronization manner, reduced-order generalized synchronization （RGS）, is proposed which has the characteristic of having a functional relation between the slave and the partial master systems. It is shown that this new synchronization phenomenon can be realized by a novel technique. Numerical simulations have verified the effectiveness of the proposed scheme.

Application of Ordinal Set Pair Analysis in Annual Rainfall Prediction of Liao River Basin

[Objective] The research aimed to study the application of ordinal set pair analysis in the annual precipitation prediction of Liao River basin.[Method] The ordinal theory was introduced into the set pair analysis modeling,and the prediction model of set pair analysis was improved.A kind of rainfall prediction model based on the ordinal set pair analysis (OSPA) was put forward.The time sequence of annual rainfall in the hydrological rainfall station of Liao River basin during 1956-2006 was the research objective.The annual rainfall during 1998-2006 was predicted by the model,and the error analysis was given.[Result] In the relative errors of predicted results by ordinal set pair analysis,there were six relative errors within 5%,which occupied 66.7% of the total prediction number.One relative error was during 5%-10%,which occupied 11.1% of the total prediction number.Two relative errors were during 10%-15%,which occupied 22.2% of the total prediction number.All the relative errors were less than 20%,which met the precision requirement of annual rainfall prediction in Forecast Specification of Hydrological Information.[Conclusion] The rainfall prediction based on the ordinal set pair analysis model had high precision,and the prediction result was ideal.It was suitable for the annual rainfall prediction.

The early Proterozoic metamorphic geodynamics of the Jiao-Liao Massif, east China

Considering the mineral evolution and tectonic deformational history of the early Proterozoic metamorphic sequences in the Jiao Liao Massif, very similar CCW PTt D paths were established in east Liaoning and east Shandong district within this massif. Their style displays the process of developing and closing of some rifted depression belts within the rather stable continental crust of the Jiao Liao Massif during early Proterozoic, and they may be treated as a common kind of metamorphic geodynamic model.

The Contrast between‘already’‘liao’in Singlish and‘了’in Chinese

Singapore is a developed country in Southeast Asia.Its language environment is also very complex.As one of the most representative Creole languages,Singlish has also attracted much attention from linguists.This paper will analyze the relationship between‘liao’‘already’in Singlish and‘了’in Chinese by means of comparison,and explore the influence of history and culture on language structure.

DIWA TYPE OF GOLD MINERALIZATION IN THE YINSHAN-YANSHAN-LIAO-JI ORE BELT,CHINA

DIWA TYPE OF GOLD MINERALIZATIONIN THE YINSHAN-YANSHAN-LIAO-JIORE BELT, CHINAWang Fuquan(Changsha Institute of Geotectonics, Academia Sinica, Changsha, 410013, Hunan, China)Yinshan-Yanshan-Liao-Ji gold ore belt diwa type of gold mineralization, diwa regime, diwa type oftectono-magmatismThis studied gold ore belt is giant and very important in China. Its regional tectonics and evolutional process are complicated. There are a few of view points on its geotec-tonic attribute in the Mesozoic and Cenozoic eras and on the type of its some gold ore deposits, especially, on one hosted in the pre-diwa geological bodies. On the basis of the diwa theory, the author discussed the regionalization, and its evolutional process, and some features of diwa tectono-magmatism and diwa type of gold mineralization in this belt. The author proposed that(1)the main body zone is a part of the diwa regime in the Mesozoic and Cenozoic eras, and(2)the diwa tectono-magmatism had a series of features such as

A Functional-Equivalence Approach to Two English Versions of Hao’liao’ge

The understanding of Hao’liao’ge is very important for the understanding of Hong’lou’meng so Hao’liao’ge can be said to be the key point of the whole novel.Therefore,it is necessary to pay attention to the comparative study of English translation of Hao’liao’ge in the English translation studies of Hong’lou’meng.Nida's Functional Equivalence Theory will be used to com⁃pare and analyze the two translations of Hao’liao’ge and explore the different translation strategies of the two translators,hoping to have some inspiration for poetry translation and give Chinese and English readers a deeper understanding of Hao’liao’ge.